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VEGETATION RESPONSE TO CLIMATE CHANGE IN THE SOUTHERN PART OF QINGHAI-TIBET PLATEAU AT BASINAL SCALE
NDVI Vegetation Climate Change the Qinghai-Tibet Plateau
2018/5/15
Global climate change has significantly affected vegetation variation in the third-polar region of the world – the Qinghai-Tibet Plateau. As one of the most important indicators of vegetation variatio...
The interaction of northern wind flow with the complex topography of Crete Island – Part 2: Numerical study
The interaction northern wind flow the complex topography Crete Island
2010/10/20
During the summer months, when northerly winds are blowing over the Aegean Sea the island of Crete modifies significantly the regional airflow as well as the pressure and temperature fields due to its...
Some Features of the Microclimate of a Luxuriant Turnip Rape Field on a Clear Day.Part II
Features Microclimate Luxuriant Turnip Rape Field
2009/6/18
Some Features of the Microclimate of a Luxuriant Turnip Rape Field on a Clear Day.Part II.
Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 2: feedbacks with emphasis on the location of the ITCZ and mid- and high latitudes heat budget
PMIP2 Mid-Holocene Last Glacial Maximum ITCZ mid- and high latitude
2008/11/6
A set of coupled ocean-atmosphere(-vegetation) simulations using state of the art climate models is now available for the Last Glacial Maximum (LGM) and the Mid-Holocene (MH) through the second phase ...
Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 1: experiments and large-scale features
PMIP2 Mid-Holocene Last Glacial Maximum large-scale features
2008/11/6
A set of coupled ocean-atmosphere simulations using state of the art climate models is now available for the Last Glacial Maximum and the Mid-Holocene through the second phase of the Paleoclimate Mod...
University of Kansas’s Center for Remote Sensing of Ice Sheets takes part in global research effort(图)
Remote Sensing International Polar Year
2007/3/6