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Artykuły w czasopismach na temat „Climatic change”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 lipca 2025

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1

Hare, Robert M. "Climactic climatic change." Medical Journal of Australia 184, no. 11 (2005): 581. http://dx.doi.org/10.5694/j.1326-5377.2006.tb00368.x.

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2

Tabor, Lisa, and John Harrington. "Teaching about Local Climates, Global Climate, and Climatic Change." Journal of Geography 122, no. 6 (2023): 155–62. http://dx.doi.org/10.1080/00221341.2023.2284390.

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3

Oriangi, George, Yazidhi Bamutaze, Paul Isolo Mukwaya, and Edekebon Elaijah. "Medium Term Climate Change Effects on Millet Yields in Gulu District, Northern Uganda." African Journal of Climate Change and Resource Sustainability 3, no. 1 (2024): 150–64. http://dx.doi.org/10.37284/ajccrs.3.1.1919.

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Climate change is expected to adversely affect crop yields and livelihoods of agro-dependent societies, especially in Sub-Saharan Africa. However, there remain gaps on the effects of expected regional climatic changes on key food security crops. This study assessed the projected climatic conditions and expected changes in millet yields for Paicho Sub County (S/C) in Gulu District up to the year 2033 using a cross sectional study design. To determine future climatic conditions, PRECIS (Providing Regional Climates for Impact Studies) model was used based on projected conditions at a 50 km spatia

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4

Davies, T. D. "Climatic change." Science and Public Policy 14, no. 3 (1987): 171–74. http://dx.doi.org/10.1093/spp/14.3.171.

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5

Parry, Martin, Timothy Carter, and Nicolaas Konijn. "Climatic Change." Environment: Science and Policy for Sustainable Development 27, no. 1 (1985): 4–43. http://dx.doi.org/10.1080/00139157.1985.9930810.

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6

Elsen, Paul R., William B. Monahan, Eric R. Dougherty, and Adina M. Merenlender. "Keeping pace with climate change in global terrestrial protected areas." Science Advances 6, no. 25 (2020): eaay0814. http://dx.doi.org/10.1126/sciadv.aay0814.

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Protected areas (PAs) are essential to biodiversity conservation, but their static boundaries may undermine their potential for protecting species under climate change. We assessed how the climatic conditions within global terrestrial PAs may change over time. By 2070, protection is expected to decline in cold and warm climates and increase in cool and hot climates over a wide range of precipitation. Most countries are expected to fail to protect >90% of their available climate at current levels. The evenness of climatic representation under protection—not the amount of area protected—posit

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7

Cang, F. Alice, Ashley A. Wilson, and John J. Wiens. "Climate change is projected to outpace rates of niche change in grasses." Biology Letters 12, no. 9 (2016): 20160368. http://dx.doi.org/10.1098/rsbl.2016.0368.

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Climate change may soon threaten much of global biodiversity, especially if species cannot adapt to changing climatic conditions quickly enough. A critical question is how quickly climatic niches change, and if this speed is sufficient to prevent extinction as climates warm. Here, we address this question in the grass family (Poaceae). Grasses are fundamental to one of Earth's most widespread biomes (grasslands), and provide roughly half of all calories consumed by humans (including wheat, rice, corn and sorghum). We estimate rates of climatic niche change in 236 species and compare these with

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8

Barcellos, Afonso Lopes, Renata Da Silva Pereira Saccol, Nathalia Leal Carvalho, and Luana Filippin Rosa. "A simple reflection on climate change." Revista Eletrônica em Gestão, Educação e Tecnologia Ambiental 23 (June 1, 2019): 18. http://dx.doi.org/10.5902/2236117034387.

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In order to discuss climate change and our role, this literature review was developed. The term climate change, climate change or climate change refers to global-scale climate change or Earth's regional climates over time. These variations refer to changes in temperature, precipitation, cloudiness and other climatic phenomena in relation to historical averages. Such variations can alter climatic characteristics in a way to change their didactic classification. These changes can be caused by processes internal to the Earth-atmosphere system, by external forces, or by the result of human activit

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9

Kovács-Láng, E., Gy Kröel-Dulay, M. Kertész, et al. "Changes in the composition of sand grasslands along a climatic gradient in Hungary and implications for climate change." Phytocoenologia 30, no. 3-4 (2000): 385–407. http://dx.doi.org/10.1127/phyto/30/2000/385.

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10

Perry, John S. "Climatic Change:Getting Serious About Climatic Change." Environment: Science and Policy for Sustainable Development 27, no. 10 (1985): 2–3. http://dx.doi.org/10.1080/00139157.1985.9931314.

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11

Bryson, Reid A. "Civilization and Rapid Climatic Change." Environmental Conservation 15, no. 1 (1988): 7–15. http://dx.doi.org/10.1017/s037689290002840x.

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Research over the past century has shown that the rates and magnitudes of climatic change constitute a continuum. Changes have now been identified in the climatic record that range in duration from interannual through decades and centuries to the multi-millennial time-scale. Examples range from the drought years of the 1930 and 1970 decades to the ponderous comings and goings of the ice-ages. More recently it has become clear that some changes can be quite rapid. In recent decades great progress has been made in identifying the causes of climatic variation.The present understanding of the caus

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12

Griesbauer, Hardy P., and D. Scott Green. "Regional and ecological patterns in interior Douglas-fir climate–growth relationships in British Columbia, Canada." Canadian Journal of Forest Research 40, no. 2 (2010): 308–21. http://dx.doi.org/10.1139/x09-197.

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How climate change will affect tree growth across species’ geographic and climatic ranges remains a critical knowledge gap. Tree-ring data were analyzed from 33 interior Douglas-fir ( Pseudotsuga menziesii var. glauca (Beissn.) Franco) stands spanning wide geographic and climatic conditions in the interior of British Columbia to gain insights into how within-species growth responses to climate can vary based on local environmental conditions over a broad climatic and geographic range, including populations growing at the species’ range and climatic margins. Populations growing in relatively wa

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13

Jäger, Jill. "Anticipating Climatic Change." Environment: Science and Policy for Sustainable Development 30, no. 7 (1988): 12–33. http://dx.doi.org/10.1080/00139157.1988.9930899.

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14

Green, David. "Adverse climatic change." International Journal of Environmental Studies 77, no. 2 (2020): 190. http://dx.doi.org/10.1080/00207233.2020.1745551.

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15

Houghton, Richard A., and George M. Woodwell. "Global Climatic Change." Scientific American 260, no. 4 (1989): 36–44. http://dx.doi.org/10.1038/scientificamerican0489-36.

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16

Tabai, Ieremia. "Global climatic change." Marine Policy 18, no. 2 (1994): 183–85. http://dx.doi.org/10.1016/0308-597x(94)90025-6.

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17

Hardy, Steve, and Werner Gaiser. "Forming Climatic Change." Architectural Design 77, no. 6 (2007): 154–57. http://dx.doi.org/10.1002/ad.593.

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18

Ruget, F., J. C. Moreau, M. Ferrand, et al. "Describing the possible climate changes in France and some examples of their effects on main crops used in livestock systems." Advances in Science and Research 4, no. 1 (2010): 99–104. http://dx.doi.org/10.5194/asr-4-99-2010.

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Abstract. The effects of climate change on forage and crop production are an important question for the farmers and more largely for the food security in the world. Estimating the effect of climate change on agricultural production needs the use of two types of tools: a model to estimate changes in national or local climates and an other model using climatic data to estimate the effects on vegetation. In this paper, we will mainly present the effects of climate change on climatic features, the variability of criteria influencing crop production in various regions of France and some possible ef

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19

Singh, Sanjay, Dr Sushma Kumari, and Dr Ravinder Singh. "UN CONVENTION ON CLIMATE CHANGE AND OUR NATIONAL PLAN FOR CLIMATIC CHANGES." International Journal of Engineering Applied Sciences and Technology 8, no. 1 (2023): 37–42. http://dx.doi.org/10.33564/ijeast.2023.v08i01.006.

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Paper highlights the contemporary issues of climatic change and its serious global environmental concern. It is primarily caused by the building up of Green House Gases (GHG) in the atmosphere. The global increases in carbon dioxide concentration (CO2) are primarily due to fossil fuel use and due to agriculture land use change yielding the methane and nitrous oxide. Global Warming is a specific example of the broader term “Climate Change”. It also discuss the scientific studies about UN framework convention on climate change (UNFCCC), conferences of parties (CoP) on climate change, our nationa

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20

Riebsame, William E. "Climate hazards, climatic change and development planning." Land Use Policy 8, no. 4 (1991): 288–96. http://dx.doi.org/10.1016/0264-8377(91)90019-f.

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21

Toprak, Z. Fuat, Nizamettin Hamidi, Şahin Toprak, and Zekâi Şen. "Climatic identity assessment of the climate change." International Journal of Global Warming 5, no. 1 (2013): 30. http://dx.doi.org/10.1504/ijgw.2013.051480.

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22

Dąbski, Maciej. "Global climate change, CO2 and climatic catastrophes." Przegląd Geologiczny 73, no. 5 (2025): 486–94. https://doi.org/10.7306/2025.56.

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23

Wigley, T. M. L., and S. C. B. Raper. "Climatic change due to solar irradiance changes." Geophysical Research Letters 17, no. 12 (1990): 2169–72. http://dx.doi.org/10.1029/gl017i012p02169.

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24

Brizuela-Torres, Diego, Raymundo Villavicencio-García, José Ariel Ruiz-Corral, and Angela P. Cuervo-Robayo. "Effects of climate change on the potential distribution of a dominant, widely distributed oak species, Quercus candicans, in Mexico." Atmósfera 37 (May 12, 2023): 455–80. http://dx.doi.org/10.20937/atm.53182.

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Mexican temperate forests are among the most biodiverse in the world. At present, they face anthropogenic pressures and climatic changes. Quercus candicans is a canopy-dominant, widely distributed species common in the moist habitats of these ecosystems. Its ecological importance, habitat vulnerability, and wide distribution make it a useful model of the vulnerability of Mexican tree forest species to climate change. We used ecological niche modeling to estimate future climatic suitability for this species and its potential range shifts under two emissions scenarios and three-time frames. We a

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25

Hunt, B. G., and T. I. Elliott. "Interaction of climatic variability with climatic change." Atmosphere-Ocean 42, no. 3 (2004): 145–72. http://dx.doi.org/10.3137/ao.420301.

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26

Khourchid, Ammar M., Salah Basem Ajjur, and Sami G. Al-Ghamdi. "Building Cooling Requirements under Climate Change Scenarios: Impact, Mitigation Strategies, and Future Directions." Buildings 12, no. 10 (2022): 1519. http://dx.doi.org/10.3390/buildings12101519.

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Climate change affects building cooling demand; however, little has been done to explore this effect and show its variability in different climatic zones. This review organizes and summarizes studies which have simulated the impact of climate change on building cooling requirements, and critically analyzes the effectiveness of the mitigation strategies proposed by these studies to alleviate this impact. The review methodology selected studies that reported cooling demand and discussed mitigation strategies in future climates. The studies were then grouped based on their climate zone and impact

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27

Khaliq, Imran, Christian Hof, Roland Prinzinger, Katrin Böhning-Gaese, and Markus Pfenninger. "Global variation in thermal tolerances and vulnerability of endotherms to climate change." Proceedings of the Royal Society B: Biological Sciences 281, no. 1789 (2014): 20141097. http://dx.doi.org/10.1098/rspb.2014.1097.

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The relationships among species' physiological capacities and the geographical variation of ambient climate are of key importance to understanding the distribution of life on the Earth. Furthermore, predictions of how species will respond to climate change will profit from the explicit consideration of their physiological tolerances. The climatic variability hypothesis, which predicts that climatic tolerances are broader in more variable climates, provides an analytical framework for studying these relationships between physiology and biogeography. However, direct empirical support for the hyp

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28

Сhirаnjeeb, Kumаr. "Effect of Climatic Change on Soil Microbial Community." Emerging Trends in Climate Change 1, no. 2 (2022): 1–8. http://dx.doi.org/10.18782/2583-4770.106.

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Climate change is the most severe problem that adversely affects crop productivity and negatively impacts soil microbial biodiversity, which is considered the key component of soil fertility indicators. Microbial biodiversity regulates all necessary functions to strengthen and maintain the stability of the ecosystem. Climate change primarily affects the crop microclimate, which in turn destroys the ecological balance and disrupts the ideal growth conditions for the crops and hampers the proliferation of microorganisms in the environment, thus decreasing crop production over a particular region

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29

Mohammad Reza, Khaleghi. "Application of dendroclimatology in evaluation of climatic changes." Journal of Forest Science 64, No. 3 (2018): 139–47. http://dx.doi.org/10.17221/79/2017-jfs.

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The present study tends to describe the survey of climatic changes in the case of the Bojnourd region of North Khorasan, Iran. Climate change due to a fragile ecosystem in semi-arid and arid regions such as Iran is one of the most challenging climatological and hydrological problems. Dendrochronology, which uses tree rings to their exact year of formation to analyse temporal and spatial patterns of processes in the physical and cultural sciences, can be used to evaluate the effects of climate change. In this study, the effects of climate change were simulated using dendrochronology (tree rings

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30

SARKER, RP, and V. THAPLIYAL. "CLIMATIC CHANGE AND VARIABILITY." MAUSAM 39, no. 2 (1988): 127–38. http://dx.doi.org/10.54302/mausam.v39i2.3512.

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Idso, Sherwood B. "CO2 and Climatic Change." BioScience 38, no. 7 (1988): 442. http://dx.doi.org/10.2307/1310944.

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32

TAKAHASHI, Koichiro. "Climatic change and society." Journal of Geography (Chigaku Zasshi) 99, no. 3 (1990): 209–16. http://dx.doi.org/10.5026/jgeography.99.3_209.

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33

Smith, R. "Doctors and climatic change." BMJ 309, no. 6966 (1994): 1384–85. http://dx.doi.org/10.1136/bmj.309.6966.1384.

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34

Schneider, Stephen H. "Climatic change has stabilized." Climatic Change 23, no. 1 (1993): vii—viii. http://dx.doi.org/10.1007/bf01092677.

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35

Engström, Gustav. "Structural and climatic change." Structural Change and Economic Dynamics 37 (June 2016): 62–74. http://dx.doi.org/10.1016/j.strueco.2015.11.007.

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36

Muñoz-López, F. "Climatic change and asthma." Allergologia et Immunopathologia 35, no. 2 (2007): 41–43. http://dx.doi.org/10.1157/13101336.

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37

Skaggs, Richard H. "Persistence and Climatic Change." Geographical Analysis 12, no. 2 (2010): 189–95. http://dx.doi.org/10.1111/j.1538-4632.1980.tb00028.x.

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38

Wilkinson, Michael James. "Pollen and climatic change." Aerobiologia 5, no. 1 (1989): 3–8. http://dx.doi.org/10.1007/bf02446482.

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Heintzenberg, J. "Aerosols and climatic change." Journal of Aerosol Science 26 (September 1995): S1—S2. http://dx.doi.org/10.1016/0021-8502(95)96908-p.

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40

Huntley, Brian. "Climatic change and reconstruction." Journal of Quaternary Science 14, no. 6 (1999): 513–20. http://dx.doi.org/10.1002/(sici)1099-1417(199910)14:6<513::aid-jqs486>3.0.co;2-e.

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41

Frank, Hartmut. "Climatic change: Professional indifference?" Journal of High Resolution Chromatography 15, no. 12 (1992): 781. http://dx.doi.org/10.1002/jhrc.1240151202.

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42

Wheeler, D. A. "CLIMATIC CHANGE IN SUNDERLAND?" Weather 45, no. 6 (1990): 229–31. http://dx.doi.org/10.1002/j.1477-8696.1990.tb05624.x.

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Palmer, Georgina, Philip J. Platts, Tom Brereton, et al. "Climate change, climatic variation and extreme biological responses." Philosophical Transactions of the Royal Society B: Biological Sciences 372, no. 1723 (2017): 20160144. http://dx.doi.org/10.1098/rstb.2016.0144.

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Extreme climatic events could be major drivers of biodiversity change, but it is unclear whether extreme biological changes are (i) individualistic (species- or group-specific), (ii) commonly associated with unusual climatic events and/or (iii) important determinants of long-term population trends. Using population time series for 238 widespread species (207 Lepidoptera and 31 birds) in England since 1968, we found that population ‘crashes’ (outliers in terms of species' year-to-year population changes) were 46% more frequent than population ‘explosions’. (i) Every year, at least three species

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44

Shim, Kyo-Moon, Gun-Yeob Kim, Kee-An Roh, Hyun-Cheol Jeong, and Deog-Bae Lee. "Evaluation of Agro-Climatic Indices under Climate Change." Korean Journal of Agricultural and Forest Meteorology 10, no. 4 (2008): 113–20. http://dx.doi.org/10.5532/kjafm.2008.10.4.113.

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45

Croce, Pietro, Paolo Formichi, and Filippo Landi. "Climate Change: Impacts on Climatic Actions and Structural Reliability." Applied Sciences 9, no. 24 (2019): 5416. http://dx.doi.org/10.3390/app9245416.

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Climatic loads on structures are commonly defined under the assumption of stationary climate conditions; but, as confirmed by recent studies, they can significantly vary because of climate change effects, with relevant impacts not only for the design of new structures but also for the assessment of the existing ones. In this paper, a general methodology to evaluate the influence of climate change on climatic actions is presented, based on the analysis of observed data series and climate projections. Illustrative results in terms of changes in characteristic values of temperature, precipitation

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46

Grove, Matt. "Climatic change and climatic variability: An objective decomposition." Quaternary Science Reviews 271 (November 2021): 107196. http://dx.doi.org/10.1016/j.quascirev.2021.107196.

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47

Lewis, Trevor, and Walter Skinner. "Inferring Climate Change from Underground Temperatures: Apparent Climatic Stability and Apparent Climatic Warming." Earth Interactions 7, no. 9 (2003): 1–9. http://dx.doi.org/10.1175/1087-3562(2003)007<0001:iccfut>2.0.co;2.

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48

Mishra, Ashok K., and Valerian O. Pede. "Perception of climate change and adaptation strategies in Vietnam." International Journal of Climate Change Strategies and Management 9, no. 4 (2017): 501–16. http://dx.doi.org/10.1108/ijccsm-01-2017-0014.

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Purpose The purpose of this study is to first examine the factors affecting the intra-household perception of climate change. Second, the study investigates the impact of the perception of climatic stress on the operators’ and spouses’ intra-household adaptation strategies (farm and household financial strategies). Design/methodology/approach The study uses household survey data from Vietnam’s Mekong Delta. The study uses probit and negative binomial count data approaches to evaluate the empirical model. Findings Results confirm the existence of intra-household gender differences in the adapta

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Mortey, Eric Mensah, Thompson Annor, Joël Arnault, et al. "Interactions between Climate and Land Cover Change over West Africa." Land 12, no. 2 (2023): 355. http://dx.doi.org/10.3390/land12020355.

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Climate–land interaction over West Africa has often been assessed using climate simulations, although the model-based approach suffers from the limitations of climate models for the region. In this paper, an alternative method based on the analysis of historical land cover data and standardized climatic indices is used to investigate climate–land interactions, in order to establish climatic conditions and their corresponding land cover area changes. The annual variation in land cover area changes and climatic changes are first estimated separately and then linked using various spatiotemporal s

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50

Gyllenhaal, Eric D. "Reconciling the lithologic and paleobotanic records of climatic change during the Pennsylvanian." Paleontological Society Special Publications 6 (1992): 116. http://dx.doi.org/10.1017/s2475262200006766.

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Both lithologic and paleobotanic data have been used to construct climatic curves for the Pennsylvanian of the Appalachian Basin (Figure 1). The strengths and weaknesses of each type of evidence must be considered when reconciling these data into a composite curve. (1) The calibrated lithologic curve is based ultimately on the geographic ranges of sediments and soils relative to modern precipitation. Although it provides quantitative estimates of precipitation, the calibrated curve cannot detect minor fluctuations in climate, and time-averaging of range data can lead to an over-estimate of the

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