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Our study indicates that the model can be applied to study the interaction between land surface processes and atmospheric boundary layers over various underlying surfaces and their regional climate effects.
      
This paper will establish a solid foundation to investigations on the coupling of climate models and the biosphere.
      
This area has a harsh climate due to low temperatures and low air pressure at high elevations.
      
With a temperate continental monsoon climate, the mountain area belongs to the warm temperate deciduous broad-leaved forest region.
      
It is important to be able to monitor and estimate forest biomass and production, regional carbon storage, and global climate change impacts on these important vegetation types.
      
The endemism was formed when some dispersal routes such as the North Atlantic Land Bridge, and the Bering Bridge became discontinuous during the Tertiary, as well as the climate change and glaciations in the late Tertiary and the Quaternary.
      
Correlation analysis of Normalized Different Vegetation Index (NDVI) difference series and climate variables in the Xilingole st
      
There is a crucial need in the study of global change to understand how terrestrial ecosystems respond to the climate system.
      
This data replacement is helpful to eliminate the cumulative effect that exist in original NDVI time series, and thus is more appropriate to understand how climate system affects vegetation growth in a short time scale.
      
soongorica populations under the same climate conditions are compared, δ13C values increase obviously from east to west and from north to south.
      
Holocene climate reconstructions of Ulungur Lake (Xinjiang, China) inferred from ostracod species assemblages and stable isotope
      
The climate changed from moderate-dry to cool-wet, and then to warm-wet in turn, and the lake level rose accordingly, showing the characteristic of a high lake level.
      
The climate turned from the early warm-dry to the late warm-wet and the lake level fell and rose again.
      
The temperature was low and then increased after the 1920s and the climate was dry.
      
It responded to regional environmental changes and global abrupt climate events, following the westerly climate change mode on 100-year-scale, primarily with cold-wet and warmdry characteristics.
      
The annual change of eco-environment water demand is in according with the climate change and hydrological characters.
      
These strains provide a basis for developing biodegrader preparations applicable to the bioremediation of oil-polluted sites under the conditions of a cold climate.
      
The Role of Antarctica in the Formation of the Cenozoic Climate and Contemporary Open Sea Abyssal Fauna
      
Morphophysiological monitoring of winter wheat in spring in the context of global climate warming
      
living in Central Yakutia, a region with a harsh continental climate and long and very cold winters, are presented in comparison with other insects of Yakutia.
      
 

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