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In essence, their reconstruction appears to tell us about past changes in climate with a resolution of about 400 years.
We demonstrate how such variations depend on changes in hydrological conditions driven by land use, meteorological variations and potential changes in climate with important implications on mitigation strategies, water ecology and utilization of water resources.
This date coincides with the attainment of present day elevations across the whole Qinghai-Tibet Plateau [ 98] and global changes in climate, with the Himalaya obstructing global air circulation and the predominance of a monsoon climate in the region [ 99].
Changes in climate with warmer temperature and more incidents of extreme weather that interfere with soil surface may cause more frequent exposure of ruminants to old anthrax spores and thus new outbreaks in areas currently regarded as "free".
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This causes seasonal change in climate, with summer in the northern hemisphere occurring when the North Pole is pointing toward the Sun, and winter taking place when the pole is pointed away.
In a previous study with this species, we demonstrated a strong evolutionary response in flowering phenology to a change in climate, with a natural drought leading to an evolutionary shift to earlier flowering time after just a few generations (Franks et al. 2007).
Here we develop and apply an approach for downscaling RCM output using local topographic lapse rates (empirically-estimated spatially and seasonally variable changes in climate variables with elevation).
The researchers then compared the timing of the extinctions with changes in climate and precipitation, and with human migration.
Climate scenarios can range from relatively qualitative narratives about changes in climate (e.g., "warmer with increased precipitation" vs. "warmer with decreased precipitation") to more quantitative and spatially explicit simulations based on global or regional climate models.
The present study investigates long-term changes in climate aridity in association with urbanization, industrial development and the use of land in Thriasio plain, Greece.
Resulting estimates of actual evapotranspiration [AET] based on changes in soil moisture with changes in climate from projections can be used to calculate climatic water deficit [CWD].
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com