Dissertations / Theses on the topic 'IPCDC'
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Högberg, Sverker. "Utveckling av rättvisebegreppet i IPCC-rapporterna 1990 - 2014." Thesis, Stockholms universitet, Statsvetenskapliga institutionen, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-139012.
Full textChong, Yuk-lan, and 莊玉蘭. "Review and analyze the IPCC future climate change projections." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B4673434X.
Full textOnça, Daniela de Souza. "\"Quando o sol brilha, eles fogem para a sombra...\": a ideologia do aquecimento global." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/8/8135/tde-01062011-104754/.
Full textThis research aims to gather scientific proofs and evidences against anthropogenic global warming hypothesis and to elucidate its meaning in the present. We argue that climate is in a permanent transformation, not resuming itself to a product of atmospheric carbon dioxide concentration variations and that worries about climatic changes are not new but, despite this, our ignorance on the functioning of the climate system is still challenging. We conclude that anthropogenic global warming hypothesis is not consensual and exerts nowadays the function of late capitalism legitimating ideology, perpetuating social exclusion transvestiting itself as a commitment to future generations.
Erkkilä, Patrik. "Modellering av metangasproduktionen på Koviks återvinningsanläggning." Thesis, Högskolan i Gävle, Avdelningen för bygg- energi- och miljöteknik, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:hig:diva-20040.
Full textBy using a modeling tool developed by IPCC, this report examines the production of methane in the landfill at Koviks recycling facility. Models for calculating methane production has existed since the 1980s and the results can serve as a basis for decisions on investments in equipment for gas extraction and energy production. Landfilling has occurred at Kovik since 1964 and the gas extraction started in the mid-1980s. Methane gas production and methane emissions at the facility have for several years been calculated with the EPER France model. However, studies show that this model tends to underestimate the methane emissions and thereby probably also the methane production. A review of the calculations at Kovik also shows that wrong data for the amount of landfilled waste has been used. For these reasons, it is interesting to use correct data in another model to get a more accurate result. The model used in this report is a First-order Multi-phase model. It takes into account a number of factors, including quantities of landfilled waste, its age, its half-life time and its content of degradable organic carbon. The waste is divided into such categories as Household Waste, Industrial Waste and Sludge. Household waste is also divided into Food, Garden, Paper, Wood, Textile and Inert waste. The different types of waste affect the production of methane gas in different degrees. Due to the lack of information regarding the composition of the landfilled household waste the result is presented in three scenarios with different composition. The composition in scenario 1 is assumed to be the most realistic. Although the results differ slightly among the scenarios, all those scenarios suggest that methane gas production peaked around 2005. The amount of waste, and thereby the methane production, then decreases quickly because of the ban on landfilling of organic matter. The results of scenario 1 shows that methane potential from 2015 to 2030 is about 15 % of the total produced methane gas from the landfill starting year 1964 to 2030, the final year in the modeling tool. This corresponds to a remaining methane potential of about 30 kilotons by 2030. The extraction of methane gas can continue at the current level for about five years. It should be mentioned that the uncertainty of the parameters that have been used and the lack of data on landfilled waste could result in a limited reliability of the calculated gas production.
Neto, Petronio de Tilio. "Ecopolítica das mudanças climáticas: o IPCC e o ecologismo dos pobres." Universidade de São Paulo, 2008. http://www.teses.usp.br/teses/disponiveis/8/8131/tde-09102008-175152/.
Full textThis is a study about the international ecopolitics of climate change. It analyses the conflicts of interests among States concerning environmental questions more specifically, concerning changes in the planets climate. Over the last decades and centuries the human being has shifted the composition of the atmosphere, and the whole climatic system is being pushed to warming. For that reason human being is supposed to understand the problem, assess its consequences and develop answer measures. In the international arena the IPCC, Intergovernmental Panel on Climate Change, was created to help in such efforts. The Panels function is to provide the political decisions concerning the climate with the necessary scientific basis. In that sense IPCC is meant to take into account policy relevant questions, but with a policy neutral perspective. This study inquires into IPCCs neutrality when it presents the climate change impacts and when it points out eventual answer measures. The analytical approach selected to investigate this question is the Environmentalism of the Poor. This approach argues that human societies distribute unequally the environmental benefits and costs. From this point of view, analyzing the IPCC reports brings evidence that the Panel may be not so policy neutral as it announces. Maybe it is not immune to political disputes among States. As a result IPCC may be not the most efficient alternative to respond to climate change.
Lindelöf, Åsa. "Metangasutsläpp från deponier och osäkerheter i beräkningsmodeller kring detta." Thesis, KTH, Industriell ekologi, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-96418.
Full textThere are a large number of landfill sites in Sweden. The total number is estimated to be somewhere between 4000 to 8000 landfills. In 2007 there were 142 landfill sites still operating, three years later the number of operating landfills decreased to 76. The municipalities are at present carrying out an inventory of old landfill sites in Sweden. The focus is on the location and risk classification of the landfill sites. There is a substantial uncertainty of the content and the progress of the degradation process unless the landfill is dug out. Methane containing landfill gas is produced when the organic matter in the waste is degraded. Since methane is a potent green house gas the emissions of landfill gas will contribute to the green house effect. The extent of the emissions is usually quantified using the IPCC model or similar. The models require certain estimations to be made such as the amount of gas that is extracted, the half-life of the organic matter and the composition of the waste. The aim of the report was therefore to look into these estimations and how these can effect the landfill gas production. The aim was also to evaluate whether the methane emissions from landfills is a major contributor to the green house gas emissions in comparison to other sources. The master thesis has been carried out through a literature study and interviews with landfill owners that resulted in a sensitivity analysis. The plausibility of the IPCC model was studied by carrying out a sensitivity analysis of the efficiency of the gas extraction system and how this will influence the total emissions of landfill gas. An overview of the connection between the land fill gas production and the decomposition of the organic matter could be realized by analyzing the material in the landfill through tests on different depths in the landfill when drilling new gas wells. The extracted amounts of landfill gas are also contradictive to the estimation of the half-life of 7,5 years that is assumption regularly made within the IPCC- model. This theory is supported by the inadequate decomposition of organic material in old landfill sites. The reduced amounts of waste that is landfilled and the prohibition of landfilling of organic and combustible waste in 2005 are also supporting this theory. The main methane sources in Sweden are ruminants from the agricultural sector and landfills. In 1990 the forecast of the methane emissions of the two sectors were equal. The forecast of today shows that the agricultural emissions are more or less the same but the emissions from landfill are halved. Another conclusion was that the efficiency of the gas extraction is varying in a short- term and in a long-term perspective. Depending on when a measurement is carried out there will be a variation of the efficiency of the gas extraction system. Anyhow annual values of the extracted amounts are calculated based on a few occasional measurements over very short time periods. Moreover, the yearly efficiency is determined based on real extracted values of methane and calculated total values of methane production that are non-comparable. The potential of gas extraction is probably larger than what has been predicted and the period of gas extraction is probably longer than expected. Supported by the low operation costs for the gas extraction the extraction should be carried out as long as it is technically possible and economically reasonable. Analyzing the material in the landfill site will increase the understanding of the gas production and the degradation of the waste in the landfill.
De, Pryck Kari. "Expertise under controversy : the case of the Intergovernmental Panel on climate change (IPCC)." Thesis, Paris, Institut d'études politiques, 2018. http://www.theses.fr/2018IEPP0037/document.
Full textIn the last decades, international expertise has been essential to put global environmental problems on the international agenda. These assessments are often contested, especially on issues where facts and values are profoundly entangled. This thesis investigates the case of the Intergovernmental Panel on Climate Change (IPCC), one of the most authoritative, albeit contested expert organisation. It is more generally interested in how these organisations construct and maintain their authority, drawing on insights from Science and Technology Studies and sociological approaches to international organisations. A central argument is that, partly as a result of the controversial universe in which it has evolved, the IPCC has grown into an international bureaucracy. The thesis identifies four institutional arrangements on which the organisation has relied to maintain its authority. First, it has strived for a balanced representation of all nations, and in particular between developed and developing countries. Second, it has put in place governing mechanisms that allow governments to play a central role in the assessment process, encouraging the ‘ownership’ of its conclusions. Third, it has increasingly proceduralised the assessment, to formalise the role of its different parts and protect the organisation against criticism. Four, it has been more attentive to the management of the information displayed about its work. These arrangements are regularly renegotiated in the context of new challenges and controversies. Beyond the IPCC, they provide relevant lenses to observe the intertwining of political and epistemic authority at the international level
Hughes, Hannah R. "Practices of power and knowledge in the Intergovernmental Panel on Climate Change (IPCC)." Thesis, Aberystwyth University, 2013. http://hdl.handle.net/2160/ed950eee-0676-419b-9d2f-864b3e49f3dd.
Full textFerrero, Bruno. "Estudo comparativo da estrutura e variabilidade das massas de água a partir das simulações numéricas do 4RA/IPCC." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/21/21132/tde-29042010-162547/.
Full textThe development and sophistication of numerical models in recent years has allowed to perform many climate system\'s simulations. Such simulations aim to reproduce the dynamics and variability of the climate and consequently predict future climate and possible climate changes. Oceanic processes such as formation and distribution of water masses have an important role in understanding the oceans as a reservoir of salt, dissolved gases and heat. Considering that changes in such processes may have great impact in global and regional climate this work aims to describe spatial and temporal variability of water masses in the South Atlantic Ocean and Southern Ocean. Data from the numerical simulations used for the preparation of the Intergovernmental Panel on Climate Change Fourth Assessment Report (4AR/IPCC) were used. Four climate models were chosen: ECHAM5/MPI-OM, IPSL-CM4-V1, MIROC3.2, NOAA / GFDL CM2.1. Results from the Climate of the 20th Century (20c3m) and the 1% per year CO2 increase (to doubling) experiment (1pctto2x) were analyzed. The four models show a positive trend of temperature and a freshening trend of the Antartic Intemediate Water (AAIW), Circumpolar Deep Water (CDW) and the Antartic Deep Water (AADW). The densities of these water masses become significantly lighter in the 20c3m scenario. In the 1pctto2x scenario in the AAIW and CDW moved to upper layers. Also in this scenario there is a cooling of the AADW, moving this water mass to deeper layers.
Beck, Silke. "Das Klimaexperiment und der IPCC Schnittstellen zwischen Wissenschaft und Politik in der internationalen Politik." Marburg Metropolis-Verl, 2000. http://d-nb.info/995863210/04.
Full textPereira, Augusto Andrade. "Projeções futuras do oceano Atlântico Sudoeste em dois cenários de aquecimento global." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/21/21132/tde-20042012-160438/.
Full textSouthwestern Atlantic comprises one of the most energetic region of the world: Brazil-Malvinas Confluence (BMC). This region lies within the Southern Atlantic Subtropical Gyre and holds fundamental importance for this oceanic dynamics as well as for the regional climate. Through numerical modeling output coupled to IPCC\'s 4th Report, it is sunk to describe this region behavior for two distinct future scenarios: high greenhouse gases emission (A1b) and a milder one in terms of anthropic impacts (B2). Both scenarios have shown strong temperature increasing tendencies, especially on the surface (reaching up to 0.065°C/year in A1b and 0.055°C/year in B2). Surface salinity have also shown strong positive tendency from the Equator to the BMC region, and negative in higher latitudes. BMC medium position is shifted around 1.1°S in A1b scenario (between 2066 and 2010) and 0.9° in B2. Spectral pattern on this position (dominated for XX century annual cycle) is controlled by low-frequency variabilities in A1b scenario. These modifications in average and spectral patterns of BMC position are linked to the intensification and changing of Brazil current.
Sjökvist, Malin, and Rasmus Axelsson. "”Man får inte vatten i stövlarna på en gång” : En undersökning om miljöbevakningen i Rapport och Dagens Nyheter i samband med IPCC:s klimatrapporter." Thesis, Södertörns högskola, Institutionen för samhällsvetenskaper, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:sh:diva-21542.
Full textMorgan, Maurice Richard. "Climate change in the North Atlantic relevant to the global warming hypothesis." Thesis, University of Exeter, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.312070.
Full textVolsky, Uladzimir. "Prepare Russia to meet IPCC 2050, based on dynamic MFA approach for greenhouse gas emissions." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for vann- og miljøteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-19217.
Full textRoeder, Geoffrey Gilbert. "Climate models in modal adverbials : representational practice and deep uncertainty in the IPCC summary documents." Thesis, University of British Columbia, 2011. http://hdl.handle.net/2429/39937.
Full textMahony, M. "Epistemic geographies of climate change : the IPCC and the spaces, boundaries and politics of knowing." Thesis, University of East Anglia, 2013. https://ueaeprints.uea.ac.uk/48699/.
Full textTavares, Mônica Weber. "Temperatura e precipitação na América do Sul: situação atual e perspectivas futuras do IPCC/AR5." Universidade Federal de Viçosa, 2013. http://locus.ufv.br/handle/123456789/5274.
Full textCoordenação de Aperfeiçoamento de Pessoal de Nível Superior
Sea Surface Temperature (SST) is able to influence the atmospheric circulation and consequently changes weather patterns in both local and global scale. This study aimed to understand how temperature and precipitation in South America respond to modes of climate variability such as the El Niño-Southern Oscillation (ENSO) and the Atlantic Dipole (AD), for current and future conditions, considering an extreme emission scenario of GreenHouse effect (GHG). We used four models as part of coupled model of Inter-governmental Panel on Climate Change/Fifth Assessment Report (IPCC/AR5), intercomparison project, Phase 5 (CMIP5): MRI (Meteorology Research Institute, Japan), INM (Institute for Numerical Mathematics, Russia), NCC (Norwegian Climate Center, Norway) and ECHAM / MPI (Max Planck Institute for Meteorology, Germany). The results have shown that the dominant patterns in the Pacific and Atlantic Oceans, are respectively the ENSO and Dipole Atlantic which were better simulated by the models MPI and NCC (INM and MRI) and proved satisfactory (unsatisfactory) and able (unable) to reproduce the response of precipitation and temperature in relation to observed climate over the South America. For future conditions it has been found more intense episodes of ENSO, while for AD the inter-hemispheric gradients is more intense. Furthermore, it is projected that this pattern, known as the negative phase of AD, may significantly influence the atmospheric circulation and alter the patterns of temperature and precipitation in South America.
A Temperatura da Superfície do Mar (TSM) é capaz de influenciar na circulação atmosférica e consequentemente alterar os padrões climáticos tanto em escala local quanto global. Este trabalho buscou entender como a temperatura e precipitação na América do Sul respondem em função dos modos de variabilidade climática El Niño Oscilação-Sul (ENSO) e Dipolo do Atlântico (DA), para as condições atuais e futuras, considerando um cenário extremo de emissão de Gases de Efeito Estuda (GEE). Foram utilizados quatro modelos climáticos acoplados do Inter-governmental Panel on Climate Change/Fifth Assessment Report (IPCC/AR5), pertencentes ao Projeto de Intercomparação de Modelos Acoplados, Fase 5 (CMIP5): MRI (Meteorology Research Institute, Japão), INM (Institute for Numerical Mathematics, Rússia), NCC (Norwegian Climate Center, Noruega) e ECHAM/MPI (Max Planck Institute for Meteorology, Alemanha). Os resultados mostraram que os padrões dominantes nos Oceanos Pacífico e Atlântico, são respectivamente o ENSO e Dipolo do Atlântico e foram melhor reproduzidos pelos modelos MPI e NCC (INM e MRI) e se mostraram satisfatórios (insatisfatórios) e capazes (incapazes) de reproduzir a resposta da precipitação e temperatura, em relação ao clima observado sobre a AS. Para condições futuras têm-se episódios de ENSO mais intensos, enquanto que para configurações do tipo DA notam-se gradientes inter-hemisféricos mais intensos, onde se observou TSM's mais baixas no Atlântico Norte. Além disso, projeta-se que este padrão, conhecido como fase negativa do DA, poderá influenciar significativamente na circulação atmosférica e alterar os padrões de temperatura e precipitação na AS.
Hirst, David. "Negotiating climates : the politics of climate change and the formation of the Intergovernmental Panel on Climate Change (IPCC), 1979-1992." Thesis, University of Manchester, 2014. https://www.research.manchester.ac.uk/portal/en/theses/negotiating-climates-the-politics-of-climate-change-and-the-formation-of-the-intergovernmental-panel-on-climate-change-ipcc-19791992(ee23545e-3448-4a74-aa8a-36b5d622a81a).html.
Full textVeltrone, Allan Rogério. "Interdisciplinaridade na questão climática : a participação das ciências sociais no Painel Intergovernamental de Mudanças Climáticas (IPCC)." Universidade Federal de São Carlos, 2017. https://repositorio.ufscar.br/handle/ufscar/8776.
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
Our goal in this study is to analyze the production, formation and acting of the authorscoordinators of the two most relevant chapters of the fifth report of the IPCC Working Group II (Intergovernmental Panel on Climate Change) that deal with human dimensions of climate change, and so discuss the contribution of social sciences around this debate. The discussion of the thesis is placed within a framework of interdisciplinary, in which demand for scientific cooperation between different areas appears as a necessity imposed by environmental issues. Our hypothesis is that the fact the interdisciplinary is happening, but when it occurs, that occurs in a hierarchical fashion, where the strands of the social sciences participating in the debate, only do so when they use the same parameters used by the ruling science in discussions climate change. The research shows that the hypothesis is partially confirmed, but there is a progressive tendency to incorporate the classic areas of social sciences, such as anthropology, political science and sociology by the IPCC.
Nosso objetivo neste trabalho é analisar a produção, formação e atuação dos autorescoordenadores dos dois capítulos mais relevantes do quinto relatório do grupo de trabalho II do IPCC (Intergovernmental Panel on Climate Change) que versam sobre dimensões humanas das mudanças climáticas, e assim discutir a contribuição das Ciências Sociais em torno deste debate. A discussão da tese é colocada dentro de um quadro de interdisciplinaridade, no qual a demanda por cooperação cientifica entre diferentes áreas aparece como uma necessidade imposta pelas questões ambientais. Nossa hipótese é a de que a interdisciplinaridade de fato vem ocorrendo, mas quando ocorre, ocorre de maneira hierárquica, onde as vertentes das ciências sociais que participam do debate, somente o fazem quando se valem dos mesmos parâmetros utilizados pelas ciências dominantes nas discussões sobre mudanças climáticas. A pesquisa mostra que a hipótese parcialmente se confirma, mas observa-se uma tendência progressiva de incorporação das áreas clássicas das ciências sociais, como antropologia, ciência politica e sociologia por parte do IPCC.
Davis, Michael A. "Cloud-Radiative Feedback and Ocean-Atmosphere Feedback In the Southeast Pacific Ocean Simulated by IPCC AR4 GCMs." The Ohio State University, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=osu1313350254.
Full textSurendrababu, Jayashree. "Modeling the Impact of Projected Land Cover on Lyme Disease Emergence." Thesis, Virginia Tech, 2014. http://hdl.handle.net/10919/64242.
Full textMaster of Science
Girod, Bastien. "Why six baseline scenarios? a research on the reasons for the growing baseline uncertainty of the IPCC scenarios /." Zürich : ETH, Eidgenössische Technische Hochschule Zürich, HES, Institute for Human-Environment Systmes, 2006. http://e-collection.ethbib.ethz.ch/show?type=dipl&nr=277.
Full textTrulsson, Sara. "Active Learning : a Supportive Teaching Method to Address Climate Change in Higher Education." Thesis, KTH, Industriell ekologi, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-191308.
Full textUniversitet världen över gör ansträngningar för att integrera undervisning av klimatförändringarna i sina utbildningsprogram, men klimatförändringarna är ett utmanande ämne: klimatsystemet är komplext, framtidsprognoser innefattar svårtolkade sannolikhetstermer och ämnet som sådant väcker många känslor. Simulationer och spel att en lärandemetod för att beröra ämnet, och samtidigt som det finns ett allt större utbud av undervisningsmaterial om klimatförändringarna på internet, sker en snabb förändring i hur online-material används för att förse studenter med information i den högre utbildningen. I vissa kurser flyttas en del av det informativa kursmaterialet till online-plattformar för att frigöra mer tid för aktivt lärande – lärande, i vilket studenten är mer aktiv än att enbart lyssna. I den här masteruppsatsen utreds huruvida aktivt lärande kan stödja studenter i lärandet om klimatförändringarna i högre teknisk utbildning. Data till studien samlades från tre studentgrupper som deltog i interaktiva klimatseminarier på Kungliga Tekniska Högskolan, KTH, och på Universitetet i Graz. För att uppnå aktivt lärande användes ett klimatbrädspel, med övningar i begrepp, vokabulär och diskussioner samt bearbetning av vetenskapliga förklaringar kring klimatförändringarna. En studentgrupp lyssnade till en föreläsningsserie före deltagandet i spelseminariet, de andra två grupperna deltog däremot enbart i ett seminarium med flipped classroom metoden: studenterna följde en instuderingsinstruktion med online-material och vetenskapliga skrifter innan de kom till spelseminariet. Analys av enkätsvar (n=102), mind-map-reflektioner (n=14) och intervjuer (n=5) ledde till tre huvudsakliga slutsatser: (1) studenternas attityder kring lärandet av klimatförändringarna påverkas av känslor, (2) studiens spelseminarier ökade studenternas förståelse av klimatförändringarna och (3) efter den aktiva lärandemetoden var studenterna mer bekväma med att förklara klimatförändringarna samt fick större förtroende till sin kunskap i ämnet. Vidare kan resultaten i den här studien tolkas som att klimatundervisning i högre utbildning kan utgöra en viktig roll för mottagandet av klimatkommunikation; om ett universitet förser studenter med en introduktion till vetenskap om klimatförändringarna kan studenterna ”tvingas över en tröskel”, så att framtida deltagande i diskussioner i ämnet kan bli mindre avlägsna. Studenterna i studien upplevde nämligen en brist på trovärdig information om klimatförändringarna i det dagliga nyhetsflödet, därför uppskattade de att ta del av vetenskaplig information och komplexa diskussioner under spelseminariet. Att använda utbildande brädspel som en aktivt-lärande-metod kan öka studenters självsäkerhet och förståelse av klimatförändringarna – på ett stödjande och glädjefyllt sätt.
Grönfors, Sara. "Klimatförändringar på ön Fongafale, Tuvalu : En analys av miljöpåverkan och attityder." Thesis, Linnéuniversitetet, Institutionen för biologi och miljö (BOM), 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-26370.
Full textSerra, Yolande L., and Kerrie Geil. "Historical and Projected Eastern Pacific and Intra-Americas Sea TD-Wave Activity in a Selection of IPCC AR5 Models." AMER METEOROLOGICAL SOC, 2017. http://hdl.handle.net/10150/624034.
Full textOliveira, Flavio Natal Mendes de. "Climatologia de bloqueios atmosféricos no hemisfério Sul: observações, simulações do clima do século XX e cenários futuros de mudanças climáticas." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/14/14133/tde-02102011-115448/.
Full textThis study discusses 59-yr climatology (1949-2007) of Southern Hemisphere (SH) blockings using daily 500-hPa geopotential height data from National Center for Environmental Prediction / National Center for Atmospheric Research (NCEP-NCAR reanalysis. The spatiotemporal variability of blocking events and associations with El Nino/Southern Oscillation (ENSO) are examined. Additionally, blockings were examined in two Intergovernmental Panel for Climate Change (IPCC) Coupled General Circulation Models (CGCM), ECHAM5/MPI-OM and MIROC 3.2. Two sets of simulations were examined: the climate of the 20th century and the A1B emission scenario. ENSO episodes were identified using two methods. The first method was the Monthly Oceanic Niño Index (ONI) from the Climate Prediction Center (CPC-NCEP). The second method was based on Empirical Orthogonal Function (EOF) and was applied to identify ENSO episodes in the CGCMs. Similarly, the combined influence of ENSO and the Antarctic Oscillation (AAO) on the occurrence and characteristics of blockings was also examined. The daily AAO index was obtained from CPC/NCEP. Most conventional blocking indices detect longitudinal variations of blockings. In this study we propose a new blocking index that detects longitudinal and latitudinal variations of blockings. The following relevant sectors of blocking occurrence were identified and examined in detail: Southeast Indian (SB1), Southwest Pacific (SB2), Central Pacific (SB3), Southeast Pacific (SB4) and Southwest Atlantic (SB5) oceans. In addition, we investigated two large regions of South Pacific: West Pacific and East Pacific. We found that the typical timescale of a blocking event is about ~1.5 2.5 days. Nonetheless, the duration of events depends on the latitude, with larger durations observed at higher latitudes. Statistically significant differences in the longitude of blockings are observed between Warm (ENSO+) and Neutral ENSO phases from the Austral fall to spring. Moderate to strong Warm ENSO episodes modulate the preferred locations of blockings but do not play a significant role for variations in their frequency. On the other hand, weak ENOS+ episodes were associated with relatively high frequency of blockings. Blocking events during ENSO+ last on average one more day compared to events that occur during Neutral episodes. In contrast, Cold (ENOS-) ENSO episodes are characterized by a decrease of blockings over the Central Pacific sector, except during the Austral summer months. However, no statistically significant differences are detected in the duration. Composites of 200-hPa zonal wind anomalies indicate that the weakening (strengthening) of the polar jet around 60oS during negative (positive) AAO phases in both ENSO phases plays a major role for the relative increase (decrease) of blocking events. A statistically significant increase of events over Southeast Pacific is observed during negative AAO phases in both ENSO phases. Moreover, an increase (decrease) of events is observed over West Pacific region when negative (positive) AAO phases occur during ENSO-. In contrast, during ENSO+ there is no statistically significant difference in the longitudinal distribution of events separated according to opposite AAO phases, although there is an increase (decrease) in the events from West Pacific region to East Pacific during negative (positive) AAO phase. The CGCMs investigated in this study correctly simulated the amplitude of observed annual cycle of geopotential height in the extratropics. Also, both CGCMs show a better performance in simulating the duration and preferred locations of blockings than their frequency. None of these CGCMs simulated well the frequency during Neutral ENSO phase. The ECHAM5/MPI-OM (run2) shows systematic biases in some regions. For instance, this model overestimates the frequency of blockings over East Pacific region during Cold and Neutral ENSO phases. The differences between the two versions of MIROC 3.2 indicate that the increase in resolution improves the performance of the model in simulating the frequency of blockings.
Rajagopal, Seshadri. "Assessing Water Management Impacts of Climate Change for a Semi-arid Watershed in the Southwestern US." Diss., The University of Arizona, 2012. http://hdl.handle.net/10150/228475.
Full textKarpíšková, Dana. "Analýza platebních systémů v České a Irské republice." Master's thesis, Vysoká škola ekonomická v Praze, 2009. http://www.nusl.cz/ntk/nusl-18827.
Full textAparício, Sara Filipa Marques Nunes. "Impacts of climate change scenarios on terrestrial productivity and biomass for energy in the Iberian Peninsula: assessment through the JSBACH model." Master's thesis, Faculdade de Ciências e Tecnologia, 2012. http://hdl.handle.net/10362/9093.
Full textGreenhouse gas abatement policies (as a measure of preventing further contribution to global warming) are expected to increase the demand for renewable sources of energy driving a growing attention on Biomass as a valuable option as a renewable source of energy able to reduce CO2 emissions, by displacing fossil fuel use. The vulnerability of the Iberian Peninsula (IP) to climate changes, along with the fact that it is a water-limited region, drive a great concern and interest in understand the potentials of biomass for energy production under projected climate changes, since water shortage is a projected consequence of it. Henceforth the goals stated for this work include the understanding of the impact magnitude that climate changes and the solely effect of rising CO2 (in accordance to the prescribed in A1B scenario from IPPC) have on biomass and productivity over the IP; the modeling of the interannual variability in terrestrial productivity and biomass across de region (having the period 1960-1990 as reference) and the energy potentials derived by biomass in future scenarios (2060-2090 and 2070-2100 periods). The carbon fluxes were modeled by JSBACH model and its results were handled using GIS and statistical analysis. A better understanding of the applicability (and reliability) of this model on achieving the latter stated goals was another goal purposed in this work. IP has shown a broadly positive response to climate change, i.e. increased productivity under scenarios admitting elevation of atmospheric CO2 concentration (increases in GPP by ~41%; in forest NPP by ~54% and herbaceous NPP by ~36%, for 2060-2090 period), and smaller and negative response under scenarios disregarding rising CO2 levels (i.e. CO2 constant at 296ppm). The productivity and biomass correlation with changing climate variables also differed between different CO2 scenarios. The increase of water-use efficiency by 58% was as a result of CO2 fertilization effect, could explain the increase of productivity, although many limitations of the model (such as disregard of nitrogen cycle and land-use dynamics) poses many considerations to the acceptability of results and the overestimating productivity comparatively to many projections for the IP. Notwithstanding the comparison of changes in climate variables, showed a great correlation of results with other authors. A comprehensive analysis of biomass supply and its availability during scenarios with elevated CO2, shown that by 2060-2090, residues from thinning and logging activities over forest biomass have a potential of 0,165 and 0,495 EJ, and residues from agricultural activities (herbaceous biomass) have a potential of 0,346 EJ under a HIGH-YIELD scenario (assuming 40% of residues removal rate), corresponding to a share of current energy consumption of 13, 42 and 30%, respectively. The reasonability of these results was assessed by comparing with similar studies during the reference period.
Lamarca, Daniel Sá Freire [UNESP]. "Impacto de ondas de calor na produção de ovos de poedeiras: sistema de previsão de mortalidade aplicado à cenários do IPCC." Universidade Estadual Paulista (UNESP), 2018. http://hdl.handle.net/11449/152722.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
A temperatura da superfície do planeta vem aumentando no decorrer dos anos. O Painel Intergovernamental de Mudanças Climáticas (Intergovernmental Panel on Climate Change - IPCC) reúne pesquisadores de diversos países e áreas de atuação, tendo como objetivo gerar e organizar as informações formulando cenários futuros de variação de temperatura e precipitação, para que seja possível projetar os possíveis impactos socioeconômicos e ambientais. A agropecuária é um dos setores mais influenciado pelas variações do clima (temperatura e precipitação), visto que os processos de produção agrícola e de produção animal, para cada espécie, possuem faixas ideais de condições ambientais para obter níveis de produção adequados. Na produção de ovos de poedeiras, verifica-se que as mudanças climáticas atingirão o sistema de produção, sendo destaque a mortalidade das aves por ondas de calor. Diante do contexto apresentado, o objetivo geral dessa pesquisa foi desenvolver um sistema fuzzy para previsão de mortalidade de poedeiras e simular cenários futuros baseados na previsão de mudanças climáticas para a região de Bastos-SP, de acordo com o relatório AR5 do IPCC. O modelo de previsão de mortalidade foi baseado em sistema fuzzy e possui como variáveis de entrada: duração da onda de calor (em dias), a temperatura máxima (ºC) e a idade da ave (em semanas) e como única variável de saída a mortalidade (nível de mortalidade). O sistema fuzzy de previsão de mortalidade foi construído a partir de dados e informações presentes na literatura e apresentou um bom nível de predição em termos de acurácia. O sistema obteve uma média 75,48% de taxa de acurácia entre os 25 aviários de duas granjas analisados durante seu processo de validação. A capacidade de predição do sistema apontou uma taxa de acurácia do sistema que variou entre 50% e 100%. Os resultados da pesquisa para projeções climáticas apontam que mesmo nos cenários otimistas do IPCC, segundo as previsões do sistema fuzzy construído, que haverá aumento preocupante de taxa de mortalidade de poedeiras para a região de Bastos-SP.
The surface temperature of the planet has been increasing over the years. The Intergovernmental Panel on Climate Change (IPCC) brings together researchers from different countries and areas of action, with the objective of generating and organizing information by formulating future scenarios of temperature variation and precipitation, so that it is possible to design possible socioeconomic and environmental impacts. Agriculture is one of the sectors most influenced by climatic variations (temperature and precipitation), since the agricultural production and animal production processes, for each species, have ideal ranges of environmental conditions to obtain adequate levels of production. In the production of eggs of laying hens, it is verified that the climatic changes will reach the system of production, being emphasized the mortality of birds by heat waves. In view of the presented context, the general objective of this research was to develop a fuzzy system to predict mortality of laying hens and to simulate future scenarios based on the prediction of climatic changes for the Bastos-SP region, according to the IPCC report AR5. The model of mortality prediction was based on fuzzy system and has as entry variables: heat wave duration (in days), maximum temperature (ºC) and bird age (in weeks) and as the only output variable a mortality (level of mortality). The fuzzy system of mortality prediction was constructed from data and information present in the literature and presented a good level of prediction in terms of accuracy. The system obtained an average 75.48% accuracy rate among the 25 aviaries from two farms analyzed during its validation process. The system prediction capability showed a system accuracy rate ranging from 50% to 100%. The results of the research for climatic projections show that even in the optimistic scenarios of the IPCC, according to the fuzzy system constructed, there will be a worrying increase in the mortality rate of laying hens for the region of Bastos-SP.
CAPES - DEMANDA SOCIAL: 367/16
FAPESP: 2016/25464-8
LÃzaro, Yvonne Magdalena Campos. ""MudanÃa ClimÃtica no Nordeste do Brasil, AmazÃnia e Bacia do Prata: AvaliaÃÃo dos Modelos do IPCC e CenÃrios para o SÃculo XXI"." Universidade Federal do CearÃ, 2011. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=6685.
Full textOs modelos globais do CMPI3 para o quarto relatÃrio do Intergovernmental Panel on Climate Change (IPCC-AR4) sÃo avaliados para a regiÃo do Nordeste, AmazÃnia e bacia da Prata quanto à representaÃÃo da sazonalidade e da variabilidade plurianual da precipitaÃÃo para o perÃodo de 1901 a 1999. Essa avaliaÃÃo à realizada utilizando-se os dados do Climatic Research Unit (CRU) e a reanÃlise 20th Century Reanalysis V2 do National Oceanic and Atmospheric Administration (NOAA). Quanto à sazonalidade propÃe-se a criaÃÃo de um Ãndice de desempenho, baseado em medidas de correlaÃÃo e erro quadrÃtico mÃdio, para a avaliaÃÃo e classificaÃÃo dos modelos. Quanto à variabilidade plurianual, à aplicada a transformada de ondeletas aos dados observados, e em seguida as rodadas dos modelos sÃo avaliadas e classificadas baseadas em medidas de correlaÃÃo espectral e distÃncia euclidiana entre a variÃncia nas bandas existentes na sÃrie observada. Logo, os modelos sÃo classificados seguindo a avaliaÃÃo geral, sendo para o Nordeste o modelo CSIRO.MK3.0.RUN2, para a regiÃo da bacia da Prata o CCCMA.CGCM3.1.RUN2 e para a regiÃo AmazÃnica o GISS.MODEL.E.R.RUN6 os que melhor representaram a precipitaÃÃo no sÃculo XX. Para o cenÃrio A1B à feito um anÃlise de projeÃÃes sazonais e tendÃncias plurianuais dos modelos melhor colocados na avaliaÃÃo sazonal e geral de cada regiÃo. Quanto à projeÃÃo sazonal a anÃlise consiste no cÃlculo das anomalias de precipitaÃÃo em todos os modelos para os perÃodos 2010-2039, 2040-2069 e 2070-2099 em relaÃÃo ao cenÃrio de simulaÃÃes 20C3M durante o perÃodo 1901-1999. Quanto à tendÃncia plurianual para o perÃodo de 2010 a 2099, as precipitaÃÃes anuais sÃo padronizadas, com base nos parÃmetros do cenÃrio 20C3M. Logo à feita uma anÃlise de tendÃncias usando a mÃdia e mediana mÃvel de 10 anos, regressÃo linear, Mann Kendall Sen e Ondeletas. Na tendÃncia por ondeletas o modelo MRI.CGCM2.3.2A.RUN3, nÃo indica tendÃncia o GISS.MODEL.E.R.RUN2 indica uma tendÃncia de aumento a partir de 2030, o UKMO.HADCM3.RUN1 mostra uma tendÃncia de reduÃÃo atà 2050 na regiÃo do Nordeste. Na bacia da Prata o CCCMA.CGCM3.1.RUN2 indica tendÃncia de aumento ao longo do sÃculo XXI, o CCCMA.CGCM3.1.RUN1mostra aumento a partir de 2030 e o modelo NCAR.PCM1.RUN1 nÃo mostra nenhuma tendÃncia. Na AmazÃnia os modelos CSIRO.MK3.0.RUN1, CCCMA.CGCM3.1.RUN1, INGV.ECHAM4.RUN1 nÃo indicam nenhuma tendÃncia ao longo do sÃculo XXI.
The global models of CMPI3 to the fourth report of Intergovernmental Panel on Climate Change (IPCC-AR4) are evaluated for the Northeast Brazilian region, Amazon region and La Plata basin for the representation of seasonality and multiannual variability of precipitation for the period 1901 to 1999. This evaluation is performed using data from the Climatic Research Unit (CRU) and the 20th Century Reanalysis V2 do National Oceanic and Atmospheric Administration (NOAA). For the seasonality study is proposed to create a performance index based on measures of correlation and mean square error to the evaluation and model classification. For the multiannual variability, is applied the wavelet transform to the observed data, and then models are evaluated and ranked based on measures of spectral correlation and Euclidean distance between the observed variance and models variance in each band. Then, models are classified following the general classification, for the Northeast the CSIRO.MK3.0.RUN2 model; for La Plata basin the CCCMA.CGCM3.1.RUN2 model; for the Amazon region the GISS.MODEL.E.R.RUN6 model those which best represented the rainfall in the twentieth century. At A1B scenario, is made an analysis of seasonal forecast and multiannual trends of better placed models in the seasonal and general classification. For the seasonal projection, analysis consist in the anomalies precipitation calculations on all models for the periods 2010-2039, 2040-2069 and 2070-2099 during the period 1901- 1999. For the multiannual trends for the period 2010 to 2099, annual observed data are standardized, based on the parameters of the scenario 20C3M. Then is done an analysis with average moving, median moving of 10 years, regression linear, Mann Kendall Sen and Wavelet transform. In wavelets trends the MRI.CGCM2.3.2A.RUN3 model does not indicate trend, the GISS.MODEL.E.R.RUN2 model indicates an increasing trend from 2030, the UKMO.HADCM3.RUN1 model shows a declining trend by 2050 in the Northeast. In La Plata basin, the CCCMA.CGCM3.1.RUN2 indicates increasing trend throughout the twenty first century, the CCCMA.CGCM3.1.RUN1 shows an increase trend from 2030 and the NCAR.PCM1.RUN1 model shows no trend. In the Amazon region, the CSIRO.MK3.0.RUN1, CCCMA.CGCM3.1.RUN1, INGV.ECHAM4.RUN1 models do not indicate any trend over the twenty-first century.
Lázaro, Yvonne Magdalena Campos. "Mudança climática no nordeste do Brasil, Amazônia e Bacia do Prata: avaliação dos modelos do IPCC e cenários para o século XXI." reponame:Repositório Institucional da UFC, 2011. http://www.repositorio.ufc.br/handle/riufc/17230.
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The global models of CMPI3 to the fourth report of Intergovernmental Panel on Climate Change (IPCC-AR4) are evaluated for the Northeast Brazilian region, Amazon region and La Plata basin for the representation of seasonality and multiannual variability of precipitation for the period 1901 to 1999. This evaluation is performed using data from the Climatic Research Unit (CRU) and the 20th Century Reanalysis V2 do National Oceanic and Atmospheric Administration (NOAA). For the seasonality study is proposed to create a performance index based on measures of correlation and mean square error to the evaluation and model classification. For the multiannual variability, is applied the wavelet transform to the observed data, and then models are evaluated and ranked based on measures of spectral correlation and Euclidean distance between the observed variance and models variance in each band. Then, models are classified following the general classification, for the Northeast the CSIRO.MK3.0.RUN2 model; for La Plata basin the CCCMA.CGCM3.1.RUN2 model; for the Amazon region the GISS.MODEL.E.R.RUN6 model those which best represented the rainfall in the twentieth century. At A1B scenario, is made an analysis of seasonal forecast and multiannual trends of better placed models in the seasonal and general classification. For the seasonal projection, analysis consist in the anomalies precipitation calculations on all models for the periods 2010-2039, 2040-2069 and 2070-2099 during the period 1901- 1999. For the multiannual trends for the period 2010 to 2099, annual observed data are standardized, based on the parameters of the scenario 20C3M. Then is done an analysis with average moving, median moving of 10 years, regression linear, Mann Kendall Sen and Wavelet transform. In wavelets trends the MRI.CGCM2.3.2A.RUN3 model does not indicate trend, the GISS.MODEL.E.R.RUN2 model indicates an increasing trend from 2030, the UKMO.HADCM3.RUN1 model shows a declining trend by 2050 in the Northeast. In La Plata basin, the CCCMA.CGCM3.1.RUN2 indicates increasing trend throughout the twenty first century, the CCCMA.CGCM3.1.RUN1 shows an increase trend from 2030 and the NCAR.PCM1.RUN1 model shows no trend. In the Amazon region, the CSIRO.MK3.0.RUN1, CCCMA.CGCM3.1.RUN1, INGV.ECHAM4.RUN1 models do not indicate any trend over the twenty-first century.
Os modelos globais do CMPI3 para o quarto relatório do Intergovernmental Panel on Climate Change (IPCC-AR4) são avaliados para a região do Nordeste, Amazônia e bacia da Prata quanto à representação da sazonalidade e da variabilidade plurianual da precipitação para o período de 1901 a 1999. Essa avaliação é realizada utilizando-se os dados do Climatic Research Unit (CRU) e a reanálise 20th Century Reanalysis V2 do National Oceanic and Atmospheric Administration (NOAA). Quanto à sazonalidade propõe-se a criação de um índice de desempenho, baseado em medidas de correlação e erro quadrático médio, para a avaliação e classificação dos modelos. Quanto à variabilidade plurianual, é aplicada a transformada de ondeletas aos dados observados, e em seguida as rodadas dos modelos são avaliadas e classificadas baseadas em medidas de correlação espectral e distância euclidiana entre a variância nas bandas existentes na série observada. Logo, os modelos são classificados seguindo a avaliação geral, sendo para o Nordeste o modelo CSIRO.MK3.0.RUN2, para a região da bacia da Prata o CCCMA.CGCM3.1.RUN2 e para a região Amazônica o GISS.MODEL.E.R.RUN6 os que melhor representaram a precipitação no século XX. Para o cenário A1B é feito um análise de projeções sazonais e tendências plurianuais dos modelos melhor colocados na avaliação sazonal e geral de cada região. Quanto à projeção sazonal a análise consiste no cálculo das anomalias de precipitação em todos os modelos para os períodos 2010-2039, 2040-2069 e 2070-2099 em relação ao cenário de simulações 20C3M durante o período 1901-1999. Quanto à tendência plurianual para o período de 2010 a 2099, as precipitações anuais são padronizadas, com base nos parâmetros do cenário 20C3M. Logo é feita uma análise de tendências usando a média e mediana móvel de 10 anos, regressão linear, Mann Kendall Sen e Ondeletas. Na tendência por ondeletas o modelo MRI.CGCM2.3.2A.RUN3, não indica tendência o GISS.MODEL.E.R.RUN2 indica uma tendência de aumento a partir de 2030, o UKMO.HADCM3.RUN1 mostra uma tendência de redução até 2050 na região do Nordeste. Na bacia da Prata o CCCMA.CGCM3.1.RUN2 indica tendência de aumento ao longo do século XXI, o CCCMA.CGCM3.1.RUN1mostra aumento a partir de 2030 e o modelo NCAR.PCM1.RUN1 não mostra nenhuma tendência. Na Amazônia os modelos CSIRO.MK3.0.RUN1, CCCMA.CGCM3.1.RUN1, INGV.ECHAM4.RUN1 não indicam nenhuma tendência ao longo do século XXI.
Miranda, Nicole. "Meta-analysis of GHG mitigation potentials of the application of anaerobic digestion in dairy farms." Thesis, University of Oxford, 2016. https://ora.ox.ac.uk/objects/uuid:d613759f-8f42-494e-8e95-e977a5fc41b4.
Full textAzevedo, Juliana Bruning. "Análise do ciclo biológico do Aedes aegypti(Diptera: Culicidae) exposto a cenários de mudanças climáticas previstas pelo IPCC (Intergovernmental Panel on Climate Change)." Instituto Nacional de Pesquisas da Amazônia, 2015. http://bdtd.inpa.gov.br/handle/tede/2201.
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES
The Aedes aegypti is considered the main vector of dengue virus, urban yellow fever and Chikungunya fever. Insects are susceptible to changes in environmental factors such as rainfall and temperature. Responsible for regulating population size and aspects of mosquito biology, such as larval growth, development time, body size, longevity, fertility and blood supply. The Intergovernmental Panel on Climate Change (IPCC) predicts an increase of 2° to 4° C in average global temperature over the next century. These climatic changes may result in significant changes in landscapes and ecological patterns of infectious diseases, and interfere directly in the development and behavior of A. aegypti. This study evaluated different aspects of vector biology as amount amount of ingested blood, fertility, egg laying and hatching of eggs and longevity, climate change scenarios, planned for the year 2100, intermediate and extreme scenarios. Among the predicted variables to undergo changes due to climate change, the temperature is primarily responsible for changing the biology and vector behavior. Concentrations of CO2, even three times the current concentration does not significantly affect the results obtained in this study. The amount of blood ingested by females raised in higher temperature was higher compared to females who lived at lower temperatures, longevity is low at temperatures above 32° C, living approximately 40 days and no longevity difference between sex. The fertility is greatly affected by temperature, being reduced by half in higher temperatures. The oviposition is impaired in temperatures above 32° C, but this effect was not observed in the outbreak. Mathematical models project an increase in the number of dengue cases and geographic expansion in vector distribution. However, our data indicate that, in future scenarios of climate change, some aspects of the biology of A. aegypti will be affected. With the above information, it was possible to better understand the biology of the vector and taking also into account climate change, serving as a basis for other studies.
O Aedes aegyptié considerado o principal vetor do vírus da Dengue, Febre amarela urbana e da Febre Chikungunya. São insetos suscetíveis à variação de fatores ambientaiscomo, quantidade de chuva e temperatura. Responsáveis porregular o tamanho populacional e aspectos da biologia do mosquito, como o crescimento larval, tempo de desenvolvimento, tamanho corporal,longevidade, fecundidade e alimentação sanguínea. O Painel Intergovernamental sobre Mudança do Clima (IPCC) prevê um aumento de 2° a 4° C na temperatura média global, durante o próximo século. Essas alterações climaticas poderão resultar em mudanças significativas nas paisagens e nos padrões ecológicos das doenças infecciosas, e interferir diretamente no desenvolvimento e comportamento do A. aegypti. Neste trabalho foram avaliados diferentes aspectos da biologia do vetor como, ingestão de sague, fecundidade, oviposição e eclosão de ovos e longevidade, sobre cenários de mudanças climáticas, previstas para o ano de 2100, cenários intermediários e extremos.Dentre as variáveis preditas para sofrem alterações devido a mudanças do clima, a temperatura é principal responsável por alterar a biologia e o comportamento do vetor. As concentrações de CO2, mesmo três vezes maior que a concentração atual, não influenciou significativamente os resultados obtidos neste estudo.A quantidade de sangue ingerida por fêmeas criadas em temperatura mais elevada foi maior quando comparadas com as fêmeas que viviam em temperaturas menores, a longevidade é menor em temperaturas superiores a 32°C, vivendo aproximadamente 40 dias e não houve diferença de longevidade entre os sexos. A fecundidade é extremamente afetada pela temperatura, sendo reduzida pela metade em temperaturas maiores. A oviposição é prejudicada em temperaturas superiores a 32°C, porém esse efeito não foi observado na eclosão.Modelos matemáticos projetam um aumento no número de casos de dengue, além de uma expansão geográfica na distribuição do vetor. No entanto, nossos dados indicam que, em cenários futuros de mudanças climáticas, alguns aspectos da biologia do A. aegypti serão afetados. Com as informações acima mencionadas, foi possível conhecer melhor a biologia do vetor e levando também em consideração as mudanças climáticas, servindo como base para outros estudos.
Dubois, Alejandra. "Analyse des processus intersectoriels en tant que stratégie pouvant influencer les déterminants de la santé : étude de cas régionaux au Québec." Thèse, Université d'Ottawa / University of Ottawa, 2013. http://hdl.handle.net/10393/30250.
Full textFigueredo, Everthon Fernandes. "Nocaute do gene ipdC no Bacillus sp. (RZ2MS9) com a técnica de CRISPRCas9 e influência sobre a biossíntese do AIA dependente do L-triptofano." Universidade de São Paulo, 2018. http://www.teses.usp.br/teses/disponiveis/11/11138/tde-22012019-175701/.
Full textAmong the mechanisms related to the bacterium-plant interaction, the bacterial biosynthesis of indole acetic acid (AIA) plays a fundamental role in the promotion of plant growth, since it is capable of influencing innumerable physiological processes in plants. Different metabolic pathways are used by bacteria for the biosynthesis of IAA, with the indole-3-pyruvic acid (IPyA) pathway being the most commonly described. In this pathway, the indole-3-pyruvate decarboxylase (ipdC) gene has a vital role in the production of IAA using the amino acid L-tryptophan as a precursor. In this context, molecular studies about the metabolic pathways and the genes involved in this process are preponderant for the understanding of the interrelationship of the regulatory pathways with the phytormonium synthesis. The rhizobacterium Bacillus sp. (RZ2MS9) has been showing satisfactory activity in promoting plant growth. The sequencing of its genome pointed to the presence of a wide range of genes related to growth promotion, especially genes encoding auxins. Thus, the objective of the present study was to verify the function of the ipdC gene in the IAA biosynthesis L-tryptophan dependent through the knockout of the ipdC in the plant growth-promoting rhizobateria (PGPR) Bacillus sp. (RZ2MS9). Therefore, the knockout was realized using the CRISPR-Cas9. The knockout of the ipdC gene was efficient, generating disruptive mutants for the said gene. IAA biosynthesis by the ΔipdC strain showed reductions in phytormonium concentrations, according to the growth time, being 87.96% in 24 hours, 88.25% in 48 hours and 58.27% in 72 hours of growth compared to the Wild Type (WT). In addition, the biosynthesis of IAA in the absence of the amino acid L-tryptophan was also evaluated, with no phytormonium synthesis being observed at any growth time, both in the wild type and ΔipdC strain. The present study pioneered the knockout of the ipdC gene in a Bacillus strain using the CRISPR-Cas9. The results obtained contribute to a better understanding of the influence of the ipdC gene and the IPyA pathway in the IAA biosynthesis through the RZ2MS9 strain, and its role in plant growth promoting will be demonstrated in the future.
Larsson, Emma. "Science and Policy in the International Framing och the Climate Change Issue." Thesis, Linköping University, Department of Thematic Studies, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-2527.
Full textThe IPCCand the FCCC are both central institutions in the international handling of the climate change issue. How these institutions frame and define the climate change issue is decisive for the action taken in response. The aim of this thesis was to analyze and describe how the climate change problem is framed and defined within the FCCC and the IPCC. Furthermore, the aim was also to examine if there are any differences between the IPCC’s and the FCCC’s framings and definitions of the climate change problem, and if so, what those differences consist of. The analysis was based on a line of documents from the IPCC and the FCCC, which were analyzed through a qualitative textual analysis.
The results of the analysis indicate that there are both similarities and dissimilarities between the institutions. The definitions of the term climate change differ in the sense that the FCCC only regards human-induced changes in climate, as climate change. The IPCC, on the other hand, includes both natural variability and human-induced changes in its definition of climate change. In the practical usage the definitions are similar, and the results indicate that the IPCC in practice has adopted the FCCC’s definition and only focuses on anthropogenic climate change. The climate change issue is by both of the institutions perceived as a greenhouse gas question, and the consequences are described as very extensive and serious. The FCCC gives advantages to mitigative responses in relation to adaptive, and also the IPCC describes mitigative responses as advantageous. Finally, the study indicates that there is a linking between the scientific and political spheres, which is extended by the fact that the FCCC’s definition of climate change creates a demand for scientific input in the decision-making process. The science and policy relationship builds upon mutual expectations of what the respective spheres can contribute with in terms of useful knowledge and policy-relevant questions.
Dübeck, Helena. "What does one drop of oil really cost? : A study of climate change, social movements and global politics with a didactic perspective." Thesis, Karlstad University, Faculty of Social and Life Sciences, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:kau:diva-5116.
Full textThis essay aims to research the climate change issue and the relationship social movements, scientist and policymakers have to climate change. Furthermore, this essay has a didactic perspective and aim to illuminate how the climate change issue can be used within the school subject social studies. The policy decided upon by the world leaders during the climate summit in Copenhagen, Cop15, will stand further from the scientific view of climate change in relation to sustainable development than what the social movements’ demands are. To find the relationship a case study have been made, where an observation at the alternative forum Klimaforum09 was made to establish what relationship social movements have with policymakers and scientists. A close reading of the IPCC Synthesis Report (AR4) was made to see the scientific view on climate change and the relationship to policymakers and social movements. The relationship policymakers have with science and social movements have not been researched, since the Cop15 did not result in a global deal. Despite that there was no deal the thesis have been investigated, and the result is that social movements have a close, but critical relationship towards both world leaders and politicians, and to the scientific view of climate change. It is also suggested that science have a relationship to social movements. The thesis cannot be refuted or confirmed.
Santos, Thalyta Soares dos. "C?lculo das incertezas clim?ticas sobre Am?rica do Sul utilizando modelos do CMIP5: aferi??o atrav?s das redes neurais artificiais." Universidade Federal do Rio Grande do Norte, 2015. http://repositorio.ufrn.br/handle/123456789/20763.
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Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior (CAPES)
Neste trabalho objetivamos analisar as incertezas envolvidas nas proje??es de mudan?as clim?ticas na Am?rica do Sul (AS) simuladas por in?meros modelos num?ricos de circula??o geral acoplado oceano-atmosfera (MCGOA) da Quinta Fase do Projeto do Modelo Intercompara??o Acoplado (CMIP5) para a Am?rica do Sul. As incertezas nas proje??es das mudan?as clim?ticas futuras surgem a partir de fontes diferentes e s?o introduzidos na sequ?ncia de passos no processo de modela??o, produzindo assim uma cascata de incertezas (Knutti et al. de 2010;. Giorgi 2005). Essas incertezas projetadas pelos modelos clim?ticos ser?o calculadas atrav?s do m?todo Reliability Ensemble Averaging (REA) desenvolvido por Giogi e Mearns (2002) que ? utilizado para calcular o intervalo de incerteza e uma medida de confiabilidade das mudan?as clim?ticas simuladas por um conjunto de diferentes modelos de circula??o geral da atmosfera. O m?todo leva em conta dois crit?rios de confiabilidade; i) o desempenho do modelo em reproduzir o clima atual e, ii) converg?ncia das mudan?as simuladas entre os modelos. O REA ser? aplicado para os s?culos XX e XXI em diferentes cen?rios do IPCC (Intergovernmental Panel on Climate Change ou Painel Intergovernamental sobre Mudan?as Clim?ticas). Em uma segunda fase, ser? aplicado tamb?m Redes Neurais Artificias (RNA) juntamente com o c?lculo das incertezas, para avaliarmos se uso das RNA ser?o uma boa ferramenta para diminuir as incertezas geradas pelos modelos, melhorando assim a precis?o dos mesmos. Assim sendo, com o estudo proposto espera-se avaliar e quantificar detalhadamente os intervalos de incerteza nas mudan?as clim?ticas apresentadas no CMIP5 para a AS, com e sem a utiliza??o de RNA, relacionadas ao uso de diferentes modelos num?ricos e futuras emiss?es de gases de efeito estufa. Avaliando os n?veis de incerteza, disponibilizaremos uma ferramenta muito ?til para os estudos de impacto, adapta??o e vulnerabilidade. Os resultados preliminares deste estudo mostraram que a varia??o REA para a precipita??o ? um pouco menor sobre a Am?rica Sul em compara??o com a m?dia simples conjunto de modelos. A confiabilidade do conjunto de modelos foi satisfat?ria para toda a Am?rica do Sul, indicando boa simula??o dos modelos nessa regi?o.
Gonçalves, Daniel Ruiz Potma. "Soil carbon balance in long-term no-till in a sub-tropical environment." Universidade Estadual de Ponta Grossa, 2018. http://tede2.uepg.br/jspui/handle/prefix/2525.
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior
Solos podem ser uma fonte ou um dreno de CO2 atmosférico, dependendo do seu sistema de manejo. Atualmente, o uso do solo e mudança de uso do solo emitem 1,3 ± 0,5 Pg C ano-1, equivalente a 8% das emissões globais. Técnicas como a agricultura de baixa emissão de C têm sido desenvolvidas para sequestrar C nos solos e reduzir a emissão de gases do efeito estufa. Porém, além dos desafios políticos e sociais envolvendo a doção destes sistemas, ainda há muita incerteza sobre o seu real potencial de mitigação. Assim, os objetivos desse estudo foram: i) Quantificar as fontes históricas e atuais de emissão de gases do efeito estufa na região dos Campos Gerais do Paraná, Brasil; ii) quantificar o potencial das melhores práticas de manejo agrícola baseadas nos três pilares da agricultura de conservação: Solo permanentemente coberto, plantio direto e rotação de culturas, em longo prazo (30 anos) para sequestrar carbono no solo, utilizando a fazenda Paiquerê (localizada na região dos Campos Gerais) como um modelo de sucesso; iii) estimar o impacto da adoção das melhores práticas de manejo nas áreas agrícolas da região e globalmente onde adequadas pelos próximos 100 anos utilizando os modelos Century e Roth-C. As fontes de gases do efeito estufa foram apresentadas como um inventário e mostraram que as emissões históricas (1930 – 2017) foram 412,18 Tg C, no qual as mudanças de uso do solo contribuíram com 91% (376,2±130 Tg C). As florestas sequestraram 51.7 ± 23.9 Tg C em 0.6 Mha em 47 anos (1.8 Tg C Mha-1 ano-1) e o plantio direto sequestrou 30.4 ± 23.9 Tg C em 1.9 Mha em 32 anos (0.5 Tg C Mha-1 ano-1). Ambos os modelos tiveram uma boa performance e o modelo Century foi mais eficiente em simular os estoques de carbono do solo, o resíduo médio da simulação foi 10 Mg C ha−1 (13%) para n = 91. O resíduo do modelo aumentou com a quantidade de óxidos no solo, sugerindo que a inclusão do controle mineralógico pode reduzir o viés de simulação. As predições do Century mostraram que o sistema tem potencial para mitigar 13 anos de emissões regionais (330 Tg C em 100 anos) ou 105 anos de emissões do setor agricultura, floresta e pecuária (40 Tg em 100 anos) na região. Da mesma forma, globalmente o sistema apresenta um potencial para sequestrar 2,5 ± 0.02 Pg C na profundidade 0–20 cm e 11,7 ± 3 Pg C na profundidade 0-100 cm em 86 milhões de ha distribuídos por todo o mundo. Este valor é equivalente à 11% das emissões globais dos setores agricultura, floresta e pecuária e mudanças de uso do solo. Assim, a nossa metodologia possa ser utilizada como um modelo para divulgar o potencial da agricultura conservacionista em sequestrar C nos solos e suportar políticas públicas que visem à mitigação das emissões de gases do efeito estufa.
Soils can be a source or sink of atmospheric CO2, according to land use and management. Currently the land use and land use change (LULUC) emits 1.3 ± 0.5 Pg carbon (C) year-1, equivalent to 8% of the global annual emission. Techniques such as low carbon agriculture, has been developed to sequester C in soils and reduce greenhouse gas (GHG) emissions. However, besides political and social challenges for the system adoption, there’s still great uncertainty related to its real mitigation potential. This study aimed: i) Quantify the historical and current main sources of GHG emissions for Campos Gerais region in Paraná state, Brazil; ii) quantify the potential of long term (30 years) agricultural best management practices, based on the three pillars of conservative agriculture: permanent soil cover, crop rotation and no-till, to sequester C in soils, using Paiquerê farm (located in Campos Gerais region) as a successful model; iii) estimate the impact of best management practices adoption in the region croplands and globally for the next 100 years where is suitable using Century and Roth-C models. The GHG emission sources were presented as an inventory and showed that historical (1930 – 2017) GHG emissions in the region was 412.18 Tg C, in which LULUC contributes 91% (376.2±130 Tg C). Forestry sequestered 51.7 ± 23.9 Tg C in 0.6 Mha in 47 years (1.8 Tg C Mha-1 year-1) and no-till sequestered 30.4 ± 23.9 Tg C in 1.9 Mha in 32 years (0.5 Tg C Mha-1 year-1). Both models performed well, and Century was more efficient for simulate the SOC stocks, the mean residue was 10 Mg C ha−1 (13%) for n = 91. The model residue increased along with the oxides content in the soil clay fraction, suggesting that mineralogical control inclusion can reduce the model simulation bias. Century predictions showed that the system currently practiced at Paiquerê farm have the potential to mitigate 13 years of regional total emissions (330 Tg C in 100 years) or 105 years of agriculture, forestry and other land use (AFOLU) sector emissions (40 Tg in 100 years) in the region. In the same way, it has the potential to sequester 2.5±0.02 Pg C at 0-20 cm and 11.7±3 Pg C at 0-100 cm soil depth in 86 million ha globally. This is equivalent to 11% of global annual emissions from LULUC sector. In this way, our methodology can be used as a model to access the potential of conservation agriculture to sequester C and support public policies aiming to mitigate GHG emissions.
Bylund, Martin. "Syndaren: Människan : En kritisk diskursanalys av klimatfrågans gestaltning i svensk dagspress." Thesis, Linnéuniversitetet, Institutionen för medier och journalistik (MJ), 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-45933.
Full textVice, President Research Office of the. "Cover and Contents." Office of the Vice President Research, The University of British Columbia, 2009. http://hdl.handle.net/2429/9511.
Full textWesterberg, Anna, and Emma Mörlin. "Analysis of trends in policies and pathways for climate neutrality within the steel industry : A case study of powder metal company Höganäs AB." Thesis, KTH, Hållbar utveckling, miljövetenskap och teknik, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-299519.
Full textFilho, Carlos Eduardo Gomes Cassaú. "Potencial de geração de metano em aterros sanitários através dos modelos IPCC, USEPA e Scholl Canyon estudo de caso do aterro sanitário de Moskogen, Kalmar, Suécia." Universidade do Estado do Rio de Janeiro, 2012. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=8169.
Full textThe use of methane (CH4) present in the biogas generated by the anaerobic degradation of organic wastes in landfills as an energy source is an expanding technology, especially in developing countries. To ensure a proper utilization of CH4 and the economic feasibility of the energy recovery project it is necessary that these landfills evaluate their capability to produce this gas over the years, even after the end of waste disposal. The generation potential is commonly estimated from first-order kinetic models proposed by reputable institutions, however, recent studies indicate a high level of uncertainty and significant differences between the results obtained with each method. This study aims to analyze the variation of the results of methane generation estimatives, from the models recommended by the USEPA, the World Bank (Scholl Canyon Model) and the IPCC using field data and information provided by Moskogen landfill, located in Kalmar, Sweden, which was operated from 1977 to 2008. In addition to estimating the CH4 generation potential, the objective is to identity which model whose results are closer to the data of the amount of biogas effectively measured and to discover how much gas still can be extracted from the landfill. The study also evaluated how different values to the model main parameters affect the final generation estimative. The IPCC model proved to be the most reliable among the others analyzed, estimating that Moskogen will produce over 102 million m of CH4 between 1977 and 2100, which 39.384 can be extracted from 2012 to 2100. The other models presented inadequate assumptions in comparison to the reality of the studied landfill. Nevertheless, despite the fact that the model proposed by the IPCC has been judged as the most faithful, larger studies are needed on the area, in order to identify more field data, such as the occurrence of passive gas flow through the top covering layers of the landfill and a better estimative of the amount of degradable organic compounds in each fraction of waste disposed in Moskogen.
Rothballer, Michael. "In situ Lokalisierung, PGPR-Effekt und Regulation des ipdC-Gens der Azospirillum brasilense Stämme Sp7 und Sp245 bei verschiedenen Weizensorten, sowie endophytische Kolonisierung durch Herbaspirillum sp. N3." Diss., lmu, 2004. http://nbn-resolving.de/urn:nbn:de:bvb:19-17956.
Full textGuimarães, Amanda. "Global Warming, Health and the Animal Industry. A Critical Discourse Analysis of Advertisements from the Animal Industry in EU after the Reports by WHO, FAO and IPCC." Thesis, Malmö högskola, Fakulteten för kultur och samhälle (KS), 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:mau:diva-23153.
Full textKuchler, Magdalena. "Fields of Gold : The Bioenergy Debate in International Organizations." Doctoral thesis, Linköpings universitet, Tema vatten i natur och samhälle, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-80858.
Full textUnder de senaste två decennierna har idén om att producera energi av biomassa rönt stor uppmärksamhet bland forskare, företagare, beslutsfattare och i samhället i övrigt. De förhållandevis många kontroverser och alternativ som är förbundna med produktion av biobränslen, deras koppling till de tre problemområdena energi, klimat och jordbruk, samt deras etablering inom samtida geopolitiska, socioekonomiska och miljömässiga sammanhang, gör dem till en aktuell fråga att analysera. Avhandlingen belyser den internationella debatten genom att fokusera överväganden och ståndpunkter inom tre globala institutioner: FN:s mat- och jordbruksorgan (FAO), Internationella Energiorganet (IEA) och FN:s klimatpanel (IPCC). Huvudsyftet är spåra och analysera hur begreppet bioenergi formas och kontextualiseras i bedömningsrapporter och policydokument producerade av FAO, IEA och IPCC under perioden 1990-2010. Ett ytterligare syfte är att problematisera och reflektera över de socioekonomiska förhållanden som bioenergibegreppet ingår i. Forskningsfrågorna är formulerade utifrån fyra kontroversiella områden i debatten: biobränsleproduktion i utvecklingsländer, dilemmat mat kontra biobränsle, bioenergi som en ”win-win-win-lösning” och den framtida roll som tillskrivs andra generationens bioteknologi. Forskningsfrågorna operationaliseras genom att var och en knyts till ett av fyra teoretiska perspektiv: världssystemteori, Michel Foucaults genealogi, Ernesto Laclaus och Chantal Mouffes diskursteori respektive Fredric Jamesons kritiska ansats. I debatten framställs ofta bioenergi som ett enkelt och rimligt alternativ med kapacitet att tillfälligt lösa samhälleliga utmaningar som energi-osäkerhet, klimatförändringar och jordbrukskrisen, dock utan att den socioekonomiska strukturen ändras nämnvärt. Analysen visar emellertid att begreppsliggörandet istället påvisar interna diskrepanser i det hegemoniska, kapitalistiska systemet. Huruvida bioenergi verkligen kan fungera som en sådan ”win-win-win”- lösning framstår som sekundärt i dessa texter. Det är kostnadseffektiviteten som har störst betydelse, men samtidigt skapar man här allvarliga begreppsliga diskrepanser inom organisationerna. Utfallet av analysen pekar på två huvudslutsatser. Å ena sidan är bioenergin oundvikligen låst av det hegemoniska systemets struktur och de motsägelser som det rymmer. Å andra sidan tycks debatten inom organisationerna söka efter en stabilisering av det instabila begreppsliggörandet av bioenergin så att den framstår som konsistent och möjlig. Vidare visar analysen också att de tre organisationerna har liknande argumentationsmönster, och det likartade sätt på vilket de diskuterar energi från biomassa illustrerar en stabilisering av mening inom diskursen där bioenergibegreppet anpassas till det hegemoniska systemet.
Dawson, Thomas. "Red Lines & Hockey Sticks : A discourse analysis of the IPCC’s visual cultureand climate science (mis)communication." Thesis, Uppsala universitet, Institutionen för ABM, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-445887.
Full textFernandes, Wescley de Sousa. "AvaliaÃÃo do Impacto das MudanÃas ClimÃticas na Oferta HÃdrica da Bacia HidrogrÃfica do ReservatÃrio Ãros usando os Modelos de MudanÃas ClimÃticas do IPCC-AR4, levando em ConsideraÃÃo as Diversas Incertezas Associadas." Universidade Federal do CearÃ, 2012. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=8377.
Full textNo presente trabalho as projeÃÃes de vazÃes para a bacia do Ãros (CearÃ) foram obtidas usando as precipitaÃÃes dos modelos globais do quarto relatÃrio do Intergovernmental Panel on Climate Change (IPCC-AR4) para o perÃodo de 2010 a 2099 do cenÃrio A1B. As vazÃes foram geradas pelo modelo hidrolÃgico Soil Moisture Account Procedure (SMAP). Para a obtenÃÃo destas, as precipitaÃÃes foram corrigidas estatisticamente a partir dos dados observados, considerando as sÃries distribuiÃÃes do tipo gama. Quanto à evaporaÃÃo de entrada do modelo chuva-vazÃo foram feitas duas consideraÃÃes, a primeira consideraÃÃo utiliza vazÃes obtidas pelo modelo hidrolÃgico SMAP inicializado com evaporaÃÃo fornecidas pelo INMET e a segunda considera que a inicializaÃÃo foi feita por evaporaÃÃes estimadas pelo mÃtodo de Penann Mothieth. Para a anÃlise das variaÃÃes interanuais foram observadas as caracterÃsticas de tendÃncias das sÃries (usando mÃtodo clÃssico de Mann-Kendall-Sen) nos padrÃes de variaÃÃo (anÃlise da mÃdia e do coeficiente de variaÃÃo da sÃrie) e a anÃlise de extremos (comparaÃÃo das curvas de distribuiÃÃo acumulada do sÃculo XX e XXI). Para anÃlise sazonal considerou-se a anomalia na climatologia mÃdia dos modelos do sÃculo XXI em relaÃÃo ao sÃculo XX. Para a anÃlise interanual foi observado que a inicializaÃÃo do modelo hidrolÃgico SMAP com evaporaÃÃes estimadas pelo mÃtodo de Penann Motheith modificado pode surgir como implementaÃÃo para o teste de hipÃtese de Mann Kendall Sen. O calculo do coeficiente de variaÃÃo demonstrou que apesar da pouca divergÃncia quanto a ocorrÃncia de variabilidade, tratando-se de sÃries de vazÃes obtidas pelo SMAP inicializado com evaporaÃÃes estimadas, as rodadas dos modelos MIROC3_2_MEDRES relatou aumentos de variabilidade para o sÃculo XXI em relaÃÃo ao sÃculo XX. Quando a inicializaÃÃo no SMAP ocorre por meio de evaporaÃÃes fornecidas pelo INMET ocorre uma grande diversificaÃÃo nos valores de variabilidade. Ainda na anÃlise interanual, a curva de funÃÃo de distribuiÃÃo acumulada (CDF) demonstrou que dos 8 modelos analisados (modelos inicializados com evaporaÃÃes estimadas pelo mÃtodo de Penann-Motheith modificado) 3 apresentam maior freqÃÃncia de eventos secos, 3 apresentam uma freqÃÃncia de eventos mais Ãmidos e 2 modelos nÃo apresentando anÃlises significativas aproximando-se da curva gerada pela sÃrie de vazÃo observada. Quanto à anÃlise sazonal das vazÃes à observado que quando se utiliza o mÃtodo de Penann Motheith modificado para evaporaÃÃo (na inicializaÃÃo do SMAP) os valores de vazÃes tornam-se menores do que os valores obtidos por sÃries geradas pelo modelo hidrolÃgico inicializado com evaporaÃÃes fornecidas pelo INMET, relacionando o sÃculo XXI com o sÃculo XX.
In the present work flow projections for the basin Ãros (CearÃ) were obtained using the precipitation of global models of the fourth report of the Intergovernmental Panel on Climate Change (IPCC-AR4) for the period 2010 to 2099 the A1B scenario. The flows were generated by the hydrologic model Soil Moisture Account Procedure (SMAP). To obtain these, the precipitations were statistically corrected from the observed data, considering the distributions of the type series range. The evaporation model input rainfall-runoff were two considerations, the first consideration obtained by using flow hydrologic model initialized with SMAP evaporation provided by INMET and considers that the second boot occur by evaporation estimated by the method of Penann Mothieth. For the analysis of interannual variations were observed the characteristics of trends of the series (using the classical method of Mann-Kendall-Sen), the changing patterns of variation (analysis of the mean and coefficient of variation of the series) and the analysis of extremes (compared cumulative distribution curves of the twentieth century and XXI). For seasonal analysis considered the climate anomaly in the middle of the XXI century models over the twentieth century. For analysis it was observed that interannual hydrologic model initialization SMAP with evaporation estimated by the modified Penann Motheith can arise as an implementation for the hypothesis test of Mann Kendall Sen. The calculation of the coefficient of variation showed that despite the short confrontation over the occurrence of variability, in the case of streamflow series obtained by SMAP initialized with estimated evaporation, the rounds of the models MIROC3_2_MEDRES reported increases in variability for the XXI century in relation to the twentieth century. When booting into SMAP occurs through evaporation provided by INMET is a great diversification in the values of variability. Although the interannual analysis, the curve of cumulative distribution function (CDF) showed that eight of the analyzed models (models initialized with evaporation estimated by the method of Penann Motheith-modified) 3 have a higher frequency of dry events, have a third event frequency wet and two models showing no meaningful analyzes approaching the curve generated by the series of observed flows. As for seasonal analysis of the flow is observed that when using the method of Penann Motheith modified to evaporation (initialization SMAP) values of flow rates become smaller than the values obtained by series generated by the hydrologic model initialized with evaporation provided by INMET , relating the new century, the twentieth century.
Fernandes, Wescley de Sousa. "Avaliação do impacto das mudanças climáticas na oferta hídrica da bacia hidrográfica do reservatório Óros usando os modelos de mudanças climáticas do IPCC-AR4, levando em consideração as diversas incertezas associadas." reponame:Repositório Institucional da UFC, 2012. http://www.repositorio.ufc.br/handle/riufc/3962.
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In the present work flow projections for the basin Óros (Ceará) were obtained using the precipitation of global models of the fourth report of the Intergovernmental Panel on Climate Change (IPCC-AR4) for the period 2010 to 2099 the A1B scenario. The flows were generated by the hydrologic model Soil Moisture Account Procedure (SMAP). To obtain these, the precipitations were statistically corrected from the observed data, considering the distributions of the type series range. The evaporation model input rainfall-runoff were two considerations, the first consideration obtained by using flow hydrologic model initialized with SMAP evaporation provided by INMET and considers that the second boot occur by evaporation estimated by the method of Penann Mothieth. For the analysis of interannual variations were observed the characteristics of trends of the series (using the classical method of Mann-Kendall-Sen), the changing patterns of variation (analysis of the mean and coefficient of variation of the series) and the analysis of extremes (compared cumulative distribution curves of the twentieth century and XXI). For seasonal analysis considered the climate anomaly in the middle of the XXI century models over the twentieth century. For analysis it was observed that interannual hydrologic model initialization SMAP with evaporation estimated by the modified Penann Motheith can arise as an implementation for the hypothesis test of Mann Kendall Sen. The calculation of the coefficient of variation showed that despite the short confrontation over the occurrence of variability, in the case of streamflow series obtained by SMAP initialized with estimated evaporation, the rounds of the models MIROC3_2_MEDRES reported increases in variability for the XXI century in relation to the twentieth century. When booting into SMAP occurs through evaporation provided by INMET is a great diversification in the values of variability. Although the interannual analysis, the curve of cumulative distribution function (CDF) showed that eight of the analyzed models (models initialized with evaporation estimated by the method of Penann Motheith-modified) 3 have a higher frequency of dry events, have a third event frequency wet and two models showing no meaningful analyzes approaching the curve generated by the series of observed flows. As for seasonal analysis of the flow is observed that when using the method of Penann Motheith modified to evaporation (initialization SMAP) values of flow rates become smaller than the values obtained by series generated by the hydrologic model initialized with evaporation provided by INMET , relating the new century, the twentieth century.
No presente trabalho as projeções de vazões para a bacia do Óros (Ceará) foram obtidas usando as precipitações dos modelos globais do quarto relatório do Intergovernmental Panel on Climate Change (IPCC-AR4) para o período de 2010 a 2099 do cenário A1B. As vazões foram geradas pelo modelo hidrológico Soil Moisture Account Procedure (SMAP). Para a obtenção destas, as precipitações foram corrigidas estatisticamente a partir dos dados observados, considerando as séries distribuições do tipo gama. Quanto à evaporação de entrada do modelo chuva-vazão foram feitas duas considerações, a primeira consideração utiliza vazões obtidas pelo modelo hidrológico SMAP inicializado com evaporação fornecidas pelo INMET e a segunda considera que a inicialização foi feita por evaporações estimadas pelo método de Penann Mothieth. Para a análise das variações interanuais foram observadas as características de tendências das séries (usando método clássico de Mann-Kendall-Sen) nos padrões de variação (análise da média e do coeficiente de variação da série) e a análise de extremos (comparação das curvas de distribuição acumulada do século XX e XXI). Para análise sazonal considerou-se a anomalia na climatologia média dos modelos do século XXI em relação ao século XX. Para a análise interanual foi observado que a inicialização do modelo hidrológico SMAP com evaporações estimadas pelo método de Penann Motheith modificado pode surgir como implementação para o teste de hipótese de Mann Kendall Sen. O calculo do coeficiente de variação demonstrou que apesar da pouca divergência quanto a ocorrência de variabilidade, tratando-se de séries de vazões obtidas pelo SMAP inicializado com evaporações estimadas, as rodadas dos modelos MIROC3_2_MEDRES relatou aumentos de variabilidade para o século XXI em relação ao século XX. Quando a inicialização no SMAP ocorre por meio de evaporações fornecidas pelo INMET ocorre uma grande diversificação nos valores de variabilidade. Ainda na análise interanual, a curva de função de distribuição acumulada (CDF) demonstrou que dos 8 modelos analisados (modelos inicializados com evaporações estimadas pelo método de Penann-Motheith modificado) 3 apresentam maior freqüência de eventos secos, 3 apresentam uma freqüência de eventos mais úmidos e 2 modelos não apresentando análises significativas aproximando-se da curva gerada pela série de vazão observada. Quanto à análise sazonal das vazões é observado que quando se utiliza o método de Penann Motheith modificado para evaporação (na inicialização do SMAP) os valores de vazões tornam-se menores do que os valores obtidos por séries geradas pelo modelo hidrológico inicializado com evaporações fornecidas pelo INMET, relacionando o século XXI com o século XX.