Gotowe bibliografie tematyczne / Anthropogenic forcing

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Gotowa bibliografia na temat „Anthropogenic forcing”

Autor: Grafiati

Data publikacji: 12 października 2024

Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Anthropogenic forcing"

Sexton, David M. H., Howard Grubb, Keith P. Shine, and Chris K. Folland. "Design and Analysis of Climate Model Experiments for the Efficient Estimation of Anthropogenic Signals." Journal of Climate 16, no. 9 (2003): 1320–36. http://dx.doi.org/10.1175/1520-0442-16.9.1320.

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Abstract Presented herein is an experimental design that allows the effects of several radiative forcing factors on climate to be estimated as precisely as possible from a limited suite of atmosphere-only general circulation model (GCM) integrations. The forcings include the combined effect of observed changes in sea surface temperatures, sea ice extent, stratospheric (volcanic) aerosols, and solar output, plus the individual effects of several anthropogenic forcings. A single linear statistical model is used to estimate the forcing effects, each of which is represented by its global mean radi

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Polson, Debbie, Gabriele C. Hegerl, Xuebin Zhang, and Timothy J. Osborn. "Causes of Robust Seasonal Land Precipitation Changes*." Journal of Climate 26, no. 17 (2013): 6679–97. http://dx.doi.org/10.1175/jcli-d-12-00474.1.

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Abstract Historical simulations from phase 5 of the Coupled Model Intercomparison Project (CMIP5) archive are used to calculate the zonal-mean change in seasonal land precipitation for the second half of the twentieth century in response to a range of external forcings, including anthropogenic and natural forcings combined (ALL), greenhouse gas forcing, anthropogenic aerosol forcing, anthropogenic forcings combined, and natural forcing. These simulated patterns of change are used as fingerprints in a detection and attribution study applied to four different gridded observational datasets of gl

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Beenstock, M., Y. Reingewertz, and N. Paldor. "Polynomial cointegration tests of anthropogenic impact on global warming." Earth System Dynamics Discussions 3, no. 2 (2012): 561–96. http://dx.doi.org/10.5194/esdd-3-561-2012.

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Abstract. We use statistical methods for nonstationary time series to test the anthropogenic interpretation of global warming (AGW), according to which an increase in atmospheric greenhouse gas concentrations raised global temperature in the 20th century. Specifically, the methodology of polynomial cointegration is used to test AGW since during the observation period (1880–2007) global temperature and solar irradiance are stationary in 1st differences whereas greenhouse gases and aerosol forcings are stationary in 2nd differences. We show that although these anthropogenic forcings share a comm

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Knutson, T. R., T. L. Delworth, K. W. Dixon, et al. "Assessment of Twentieth-Century Regional Surface Temperature Trends Using the GFDL CM2 Coupled Models." Journal of Climate 19, no. 9 (2006): 1624–51. http://dx.doi.org/10.1175/jcli3709.1.

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Abstract Historical climate simulations of the period 1861–2000 using two new Geophysical Fluid Dynamics Laboratory (GFDL) global climate models (CM2.0 and CM2.1) are compared with observed surface temperatures. All-forcing runs include the effects of changes in well-mixed greenhouse gases, ozone, sulfates, black and organic carbon, volcanic aerosols, solar flux, and land cover. Indirect effects of tropospheric aerosols on clouds and precipitation processes are not included. Ensembles of size 3 (CM2.0) and 5 (CM2.1) with all forcings are analyzed, along with smaller ensembles of natural-only a

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Penner, J. E., Y. Chen, M. Wang, and X. Liu. "Possible influence of anthropogenic aerosols on cirrus clouds and anthropogenic forcing." Atmospheric Chemistry and Physics Discussions 8, no. 4 (2008): 13903–42. http://dx.doi.org/10.5194/acpd-8-13903-2008.

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Abstract. Cirrus clouds have a net warming effect on the atmosphere and cover about 30% of the Earth's area. Aerosol particles initiate ice formation in the upper troposphere through modes of action that include homogeneous freezing of solution droplets, heterogeneous nucleation on solid particles immersed in a solution, and deposition nucleation of vapor onto solid particles. Here, we examine the possible change in ice number concentration from anthropogenic soot originating from surface sources of fossil fuel and biomass burning, from anthropogenic sulfate aerosols, and from aircraft that de

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Hao, Xin, Shengping He, Huijun Wang, and Tingting Han. "Quantifying the contribution of anthropogenic influence to the East Asian winter monsoon in 1960–2012." Atmospheric Chemistry and Physics 19, no. 15 (2019): 9903–11. http://dx.doi.org/10.5194/acp-19-9903-2019.

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Abstract. The East Asian winter monsoon (EAWM) is greatly influenced by many factors that can be classified as anthropogenic forcing and natural forcing. Here we explore the contribution of anthropogenic influence to the change in the EAWM over the past decades. Under all forcings observed during 1960–2013 (All-Hist run), the atmospheric general circulation model is able to reproduce the climatology and variability of the EAWM-related surface air temperature and 500 hPa geopotential height and shows a statistically significant decreasing EAWM intensity with a trend coefficient of ∼-0.04 yr−1,

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Hansen, J., M. Sato, A. Lacis, and R. Ruedy. "The missing climate forcing." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 352, no. 1350 (1997): 231–40. http://dx.doi.org/10.1098/rstb.1997.0018.

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Observed climate change is consistent with radiative forcings on several time–scales for which the dominant forcings are known, ranging from the few years after a large volcanic eruption to glacial–to–interglacial changes. In the period with most detailed data, 1979 to the present, climate observations contain clear signatures of both natural and anthropogenic forcings. But in the full period since the industrial revolution began, global warming is only about half of that expected due to the principal forcing, increasing greenhouse gases. The direct radiative effect of anthropogenic aerosols c

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Baker, Hugh S., Tim Woollings, and Cheikh Mbengue. "Eddy-Driven Jet Sensitivity to Diabatic Heating in an Idealized GCM." Journal of Climate 30, no. 16 (2017): 6413–31. http://dx.doi.org/10.1175/jcli-d-16-0864.1.

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The eddy-driven jet is studied using a dry idealized model to determine its sensitivity to thermal forcings. The jet latitude, speed, and variability are investigated under a series of Gaussian patch thermal forcing simulations applied systematically on a latitude–sigma grid in the troposphere. This work builds on previous studies by isolating the responses of the jet speed and latitude as opposed to combining them into a single annular mode index. It also explores the sensitivity of the jet to much smaller spatial heatings rather than applying forcing patterns to simulate anthropogenic climat

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Penner, J. E., Y. Chen, M. Wang, and X. Liu. "Possible influence of anthropogenic aerosols on cirrus clouds and anthropogenic forcing." Atmospheric Chemistry and Physics 9, no. 3 (2009): 879–96. http://dx.doi.org/10.5194/acp-9-879-2009.

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CHARLSON, R. J., S. E. SCHWARTZ, J. M. HALES, et al. "Climate Forcing by Anthropogenic Aerosols." Science 255, no. 5043 (1992): 423–30. http://dx.doi.org/10.1126/science.255.5043.423.

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Rozprawy doktorskie na temat "Anthropogenic forcing"

Acosta, Navarro Juan Camilo. "Historical anthropogenic radiative forcing of changes in biogenic secondary organic aerosol." Licentiate thesis, Stockholms universitet, Institutionen för miljövetenskap och analytisk kemi, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-123188.

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Human activities have lead to changes in the energy balance of the Earth and the global climate. Changes in atmospheric aerosols are the second largest contributor to climate change after greenhouse gases since 1750 A.D. Land-use practices and other environmental drivers have caused changes in the emission of biogenic volatile organic compounds (BVOCs) and secondary organic aerosol (SOA) well before 1750 A.D, possibly causing climate effects through aerosol-radiation and aerosol-cloud interactions. Two numerical emission models LPJ-GUESS and MEGAN were used to quantify the changes in aerosol f

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Speranza, Alessandra Olga Maria. "Solar and anthropogenic forcing of late-Holocene vegetation changes in the Czech Giant Mountains." [S.l. : Amsterdam : s.n.] ; Universiteit van Amsterdam [Host], 2000. http://dare.uva.nl/document/84035.

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Kemena, Tronje Peer [Verfasser]. "Assessment of Feedbacks in the Earth System under Anthropogenic Forcing: Two Case Studies / Tronje Peer Kemena." Kiel : Universitätsbibliothek Kiel, 2018. http://d-nb.info/1153401169/34.

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Haywood, James Matthew. "Model investigations into the radiative forcing of climate by anthropogenic emissions of sulphate and soot aerosol." Thesis, University of Reading, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.283234.

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Bistinas, Ioannis. "Global interactions between fire and vegetation, human activities and climate." Doctoral thesis, ISA-UL, 2016. http://hdl.handle.net/10400.5/12022.

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Doutoramento em Engenharia Florestal - Instituto Superior de Agronomia - UL<br>Vegetation fires are an important component of the earth’s system land processes and have a significant impact on the vegetation and CO2 dynamics. The global fire patterns are not thoroughly explored and the drivers of fire regimes in global scale are interconnected. However, several modelling assumptions are contradicted by exploring those relationships partially. At global scale, fire extent is fuel limited, with climatic variables showing both positive and negative influence on fuel moisture conditions, and human

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Leupold, Maike [Verfasser], Miriam Akademischer Betreuer] Pfeiffer, Peter [Akademischer Betreuer] [Kukla, and Jens [Akademischer Betreuer] Zinke. "Coral-based climate reconstructions in the central and western Indian Ocean from the Holocene to the present-day : orbital forcing, internal variability and anthropogenic disturbances / Maike Leupold ; Miriam Pfeiffer, Peter Kukla, Jens Zinke." Aachen : Universitätsbibliothek der RWTH Aachen, 2019. http://d-nb.info/1221697366/34.

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Forest, Chris Eliot, Peter H. Stone, and Andrei P. Sokolov. "Estimated PDFs of Climate System Properties Including Natural and Anthropogenic Forcings." MIT Joint Program on the Science and Policy of Global Change, 2005. http://hdl.handle.net/1721.1/29791.

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We present revised probability density functions (PDF) for climate system properties (climate sensitivity, rate of deep-ocean heat uptake, and the net aerosol forcing strength) that include the effect on 20th century temperature changes of natural as well as anthropogenic forcings. The additional natural forcings, primarily the cooling by volcanic eruptions, affect the PDF by requiring a higher climate sensitivity and a lower rate of deep-ocean heat uptake to reproduce the observed temperature changes. The estimated 90% range of climate sensitivity is 2.4 to 9.2 K. The net aerosol forcing stre

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Caillet, Justine. "Contribution de la calotte Antarctique au niveau des mers du 19ème au 21ème siècle et liens avec le forçage anthropique." Electronic Thesis or Diss., Université Grenoble Alpes, 2024. http://www.theses.fr/2024GRALU024.

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Bien qu’historiquement inattendu, la calotte Antarctique contribue à l’élévation du niveau des mers depuis plusieurs décennies. Les satellites révèlent que la calotte perd de la masse via la fonte massive induite par l’océan au droit des terminaisons flottantes de ses glaciers, notamment dans les secteurs d’Amundsen et d’Aurora. Le rôle du forçage anthropique dans cette fonte reste néanmoins largement méconnu en raison de la variabilité naturelle, très présente dans la région, et de la durée d’observations relativement restreinte.L’intrusion des eaux profondes circumpolaires relativement chaud

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Simonneau, Anaëlle. "Empreintes climatiques et anthropiques sur le détritisme holocène : étude multiparamètres et intégrée de systèmes lacustres d'Europe Occidentale." Phd thesis, Université d'Orléans, 2012. http://tel.archives-ouvertes.fr/tel-00805471.

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L'érosion mécanique des surfaces continentales, ou "détritisme", résulte du forçage climatique mais peut être amplifiée par le forçage anthropique. Cette érosion des sols, et sa compréhension, représentent aujourd'hui un questionnement sociétal majeur. Le présent travail s'est donc intéresse aux relations étroites liant climat, Homme et détritisme, dans les environnements continentaux holocènes. Associée à une démarche analytique multiparamètres, couplant quantification et modélisation de l'érosion des sols, l'étude intégrée et la comparaison de différents systèmes lacustres d'Europe occidenta

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Kelley, Colin Patrick. "Recent and future drying of the Mediterranean region: anthropogenic forcing, natural variability and social impacts." Thesis, 2014. https://doi.org/10.7916/D8CR5RFV.

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The Mediterranean region has experienced persistent drying since the middle of the 20th Century and global climate models project further drying in the future as a consequence of increasing greenhouse gases. The Mediterranean region is also known to oscillate between decades of relatively wet and dry conditions due to the strong influence of multidecadal North Atlantic Oscillation (NAO). It is therefore of great importance to understand the relationship between forced long-term drying resulting from human influences and those due to natural variability. To this end, we used observations, reana

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Książki na temat "Anthropogenic forcing"

George C. Marshall Space Flight Center, ed. Solar cycle and anthropogenic forcing of surface-air temperature at Armagh Observatory, Northern Ireland. National Aeronautics and Space Administration, Marshall Space Flight Center, 2010.

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Kelley, Colin Patrick. Recent and future drying of the Mediterranean region: Anthropogenic forcing, natural variability and social impacts. [publisher not identified], 2014.

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Final report on anthropogenic sulfate, clouds, and climate forcing: NASA contract NAGW-3735. National Aeronautics and Space Administration, 1997.

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Solar Cycle and Anthropogenic Forcing of Surface-Air Temperature at Armagh Observatory, Northern Ireland. Independently Published, 2020.

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Brook, Barry W., Erle C. Ellis, and Jessie C. Buettel. What is the evidence for planetary tipping points? Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198808978.003.0008.

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This chapter critically evaluates the likelihood that planet Earth will cross one or more global environmental tipping points, resulting in a degraded state that would be difficult to reverse. Ecological tipping points occur when components of a system change rapidly due an initial forcing that is amplified by positive feedbacks, resulting in a regime shift. The chapter examines the evidence in support of biological and geophysical boundaries that clearly delimit a “safe operating space” for people and biodiversity. For individual ecosystems, abrupt state transitions have been documented. Howe

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Board on Atmospheric Sciences and Climate, Climate Research Committee, Committee on Radiative Forcing Effects on Climate, Division on Earth and Life Studies, and National Research Council. Radiative Forcing of Climate Change: Expanding the Concept and Addressing Uncertainties. National Academies Press, 2005.

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Cook, Kerry H. Climate Change Scenarios and African Climate Change. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.545.

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Accurate projections of climate change under increasing atmospheric greenhouse gas levels are needed to evaluate the environmental cost of anthropogenic emissions, and to guide mitigation efforts. These projections are nowhere more important than Africa, with its high dependence on rain-fed agriculture and, in many regions, limited resources for adaptation. Climate models provide our best method for climate prediction but there are uncertainties in projections, especially on regional space scale. In Africa, limitations of observational networks add to this uncertainty since a crucial step in i

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Goswami, B. N., and Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.

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Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the sta

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Omstedt, Anders. The Development of Climate Science of the Baltic Sea Region. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.654.

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Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water l

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Części książek na temat "Anthropogenic forcing"

Beniston, Martin. "Anthropogenic Forcing of the Climate System." In Advances in Global Change Research. Springer Netherlands, 2004. http://dx.doi.org/10.1007/1-4020-2346-4_4.

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Schwartz, S. E., and A. Slingo. "Enhanced Shortwave Cloud Radiative Forcing Due To Anthropogenic Aerosols." In Clouds, Chemistry and Climate. Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-61051-6_9.

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Kong, Xianghui, Xiaoxin Wang, Huopo Chen, et al. "Mapping Precipitation Changes." In Atlas of Global Change Risk of Population and Economic Systems. Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-6691-9_3.

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AbstractCompared to the observed changes in temperature, the changes in precipitation show more uncertainty (Hartmann et al. 2013). The IPCC AR5 indicated that anthropogenic forcing has contributed to a global-scale intensification of heavy precipitation since the second half of the twentieth century (IPCC 2013) and the intensity of daily precipitation increases more under the higher warming scenarios (Weber et al. 2018).

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Marcos, Marta, Ben Marzeion, Sönke Dangendorf, Aimée B. A. Slangen, Hindumathi Palanisamy, and Luciana Fenoglio-Marc. "Internal Variability Versus Anthropogenic Forcing on Sea Level and Its Components." In Space Sciences Series of ISSI. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-56490-6_15.

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Bethoux, J. P., M. S. El Boukhary, D. Ruiz-Pino, P. Morin, and C. Copin-Montégut. "Nutrient, Oxygen and Carbon Ratios, CO2 Sequestrationand Anthropogenic Forcing in the Mediterranean Sea." In The Mediterranean Sea. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/b107144.

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Fousiya, A. A., Javed N. Malik, and Supriyo Chakraborty. "Climatic Variability and Anthropogenic Forcing on Marine Ecosystems: Evidence from the Lakshadweep Archipelago." In Coasts, Estuaries and Lakes. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-21644-2_6.

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Borsari, Bruno. "Climate Change Education Through Agroecology Curricula in Sierra Leone." In Practices, Perceptions and Prospects for Climate Change Education in Africa. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-84081-4_13.

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Abstract Global climate change is the keystone anthropogenic factor that for decades has been debated and analyzed from various levels of governance in an effort of achieving a sustainable future. Yet, increasing greenhouse gas emissions (GHGs) continue impacting the livelihoods of millions of people, forcing human displacement and mass migrations. Often these events trigger crop failures leading to food shortages. Their causes are multifaceted and prompted by drastic changes to the environment like floods, uncontrollable fires and/or soil erosion, which expand desertification, and biodiversit

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Dameris, M., R. Deckert, M. Dameris, and R. Deckert. "Simulation of Long-term Evolution of Stratospheric Dynamics and Chemistry: Role of Natural and Anthropogenic Forcings." In Advances in Global Change Research. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6766-2_19.

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"Anthropogenic forcing." In History and Climate Change. Routledge, 2005. http://dx.doi.org/10.4324/9780203995686-17.

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Wang, Hai. "South Asian summer monsoon response to anthropogenic aerosol forcing." In Indian Summer Monsoon Variability. Elsevier, 2021. http://dx.doi.org/10.1016/b978-0-12-822402-1.00006-5.

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Streszczenia konferencji na temat "Anthropogenic forcing"

Yu, Fangqun, Gan Luo, and Xiaoyan Ma. "Ion mediated nucleation and anthropogenic aerosol indirect radiative forcing." In NUCLEATION AND ATMOSPHERIC AEROSOLS: 19th International Conference. AIP, 2013. http://dx.doi.org/10.1063/1.4803360.

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Ostrander, Chadlin, Olaf Dellwig, Vera Hübner, et al. "Anthropogenic forcing of the Baltic Sea thallium cycle since ~1956." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.24344.

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V. Efimov, V., and A. E. Anisimov. "Assesing the climate change in Ukraine in XXI century and the role of anthropogenic forcing." In 9th EAGE International Conference on Geoinformatics - Theoretical and Applied Aspects. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609.201402804.

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Kalisoras, Alkiviadis, Aristeidis K. Georgoulias, Dimitris Akritidis, Robert J. Allen, Vaishali Naik, and Prodromos Zanis. "Estimating the Effective Radiative Forcing of Anthropogenic Aerosols with the Use of CMIP6 Earth System Models." In COMECAP 2023. MDPI, 2023. http://dx.doi.org/10.3390/environsciproc2023026040.

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Chapanov, Yavor. "LATITUDINAL VARIATIONS OF VOLCANIC SULFATE AND ITS INFLUENCE ON AIR TEMPERATURE." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/4.1/s19.43.

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The climate change is strongly affected by the increase of anthropogenic greenhouse gas emissions, such as carbon dioxide, methane, nitrous oxide, and fluorinated gases. Other important atmospheric factors of climate change are stratospheric sulfur aerosols, whose ability to reflect solar radiation back to the space cause cooling effect. Sulfur aerosols have common natural and anthropogenic origin. The volcanos are a major source of particles in the stratosphere, whose lifetime depends on various atmospheric processes � water condensation, rains and winds. Chapanov determines long-term influen

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Demetrashvili, Demuri, Vepkhia Kukhalashvili, Diana Kvaratskhelia, and Aleksandre Surmava. "MARINE FORECAST FOR THE EASTERNMOST PART OF THE BLACK SEA." In GEOLINKS Conference Proceedings. Saima Consult Ltd, 2021. http://dx.doi.org/10.32008/geolinks2021/b1/v3/50.

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Modelling and forecasting of dynamic processes and distribution of various substances of anthropogenic and natural origin in coastal and shelf zones of the seas and oceans are of great interest due to the high anthropogenic load of these zones. The aim of this paper is to present some examples of modelling and short-term forecasting of dynamic fields – the current, temperature and salinity in the easternmost Black Sea covering Georgian sector of the Black Sea and adjacent water area using a high-resolution regional model of the Black Sea dynamics. The z-level regional model is based on a full

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Seleznev, Aleksei, Andrey Gavrilov, Dmitry Mukhin, and Alexander Feigin. "Reconstruction of the North Atlantic Oscillation variability and its response to anthropogenic forcing using data-driven stochastic models based on artificial neural networks." In 27th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, edited by Oleg A. Romanovskii and Gennadii G. Matvienko. SPIE, 2021. http://dx.doi.org/10.1117/12.2601900.

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Bitner-Gregersen, Elzbieta M., and Odin Gramstad. "Potential Changes in the Joint Probabilistic Description of the North Atlantic Wave Climate." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-77592.

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Climate changes include natural climate variability and anthropogenic climate change. The latter is leading to global warming and causes changes in metocean conditions. For most marine structures waves represent the dominant environmental load. Therefore, projections of changes of wave characteristics in the 21st century are crucial with respect to design and marine operations. The study investigates potential changes in simultaneous occurrence of significant wave height and spectral wave period in twelve North Atlantic locations by comparing the past and future wave climate. Two IPCC emission

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Beltsidis, Ioannis Marios, Chara Georgopoulou, George Dimopoulos, and Lefteris Koukoulopoulos. "Concept assessment of a marine carbon capture system for vessel regulatory lifetime extension." In SNAME 8th International Symposium on Ship Operations, Management and Economics. SNAME, 2023. http://dx.doi.org/10.5957/some-2023-043.

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Anthropogenic Greenhouse gas emissions increase rapidly throughout years, forcing International Maritime Organization (IMO) to set strict targets on reducing emission in shipping. Carbon Capture (CC) could be one of the solutions within the decarbonization spectrum, given its potential for significant emission reduction. The shipping community is already exploring CC solutions through concept studies, joint development projects and pilot demonstrations. However, no clear window for CC inclusion in CII calculations has been provided by IMO, at the time this paper is written. The objective of th

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Oroud, Ibrahim M. "The Impacts of Anthropogenic and Climate Change Forcings on Water Resources Demands and Availability in Jordan in the Near Future." In Qatar Foundation Annual Research Conference Proceedings. Hamad bin Khalifa University Press (HBKU Press), 2016. http://dx.doi.org/10.5339/qfarc.2016.eepp3380.

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Raporty organizacyjne na temat "Anthropogenic forcing"

Anderson, Dylan, and Nicholas Cohn. Future coastal tundra loss due to compounding environmental changes in Alaska. Engineer Research and Development Center (U.S.), 2025. https://doi.org/10.21079/11681/49782.

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Anthropogenic climate change is amplified in the Arctic, where less sea ice enables energetic wave climates while higher air and soil temperatures increase tundra erodibility. These changes are likely to exacerbate retreat of coastal tundra yet remain poorly constrained on timescales relevant to storm wave impacts. A stochastic weather generator is used to create 1,000 synthetic hourly time series of waves, water levels, offshore sea ice concentration, and air temperatures used as forcing for an efficient coastal tundra model. The ensemble set of morphological change simulations provides a pro

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