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Biome Models - Potsdam Institute for Climate Impact Research
Biome Models - Potsdam Institute for Climate Impact Research

... maps based on weather stations, both geographers and climatologists have often considered biomes as indicators for climate in areas with insufficient weather stations (Köppen, 1884; Cramer and Leemans, 1993). Climatic factors may be used to identify environmental correlates or even causes for the d ...
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5 th 6 Weeks - Weather Vocabulary
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... d. temperature increases with altitude due to  solar radiation  5. Exosphere  a. outermost layer where satellites can be found  b. temperature in this layer decreases with lower air pressure  ...
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Climate Change -- Projections and Implications
Climate Change -- Projections and Implications

... The key area of interest for Alberta pertains to our water. Warmer average temperatures are forecast to translate into several changes to our hydrological systems. Increased precipitation is expected for Edmonton of 5% by the 2050s, and 9% by the 2080s, with some models forecasting an increase of up ...
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... in Texas. Enrollment preference will be given to environmental geoscience and environmental studies majors. GEOS 210 Climate Change Credits 3. 3 Lecture Hours. Examination of the science of climate change; how greenhouse gases warm the planet; scientific evidence that the earth is warming; scientifi ...
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Climate



Climate is the long-term pattern of weather in a particular area. It is measured by assessing the patterns of variation in temperature, humidity, atmospheric pressure, wind, precipitation, atmospheric particle count and other meteorological variables in a given region over long periods of time. Climate is different from weather, in that weather only describes the short-term conditions of these variables in a given region.A region's climate is generated by the climate system, which has five components: atmosphere, hydrosphere, cryosphere, lithosphere, and biosphere.The climate of a location is affected by its latitude, terrain, and altitude, as well as nearby water bodies and their currents. Climates can be classified according to the average and the typical ranges of different variables, most commonly temperature and precipitation. The most commonly used classification scheme was originally developed by Wladimir Köppen. The Thornthwaite system, in use since 1948, incorporates evapotranspiration along with temperature and precipitation information and is used in studying animal species diversity and potential effects of climate changes. The Bergeron and Spatial Synoptic Classification systems focus on the origin of air masses that define the climate of a region.Paleoclimatology is the study of ancient climates. Since direct observations of climate are not available before the 19th century, paleoclimates are inferred from proxy variables that include non-biotic evidence such as sediments found in lake beds and ice cores, and biotic evidence such as tree rings and coral. Climate models are mathematical models of past, present and future climates. Climate change may occur over long and short timescales from a variety of factors; recent warming is discussed in global warming.
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