Journal
ENVIRONMENTAL RESEARCH LETTERS
Volume 6, Issue 4, Pages -Publisher
IOP Publishing Ltd
DOI: 10.1088/1748-9326/6/4/045401
Keywords
climate change; regional climate model; snow cover
Funding
- National Basic Research Program of China [2007CB411505, 2010CB950903]
- National Natural Science Foundation of China [40975041]
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On the basis of the climate change simulations conducted using a high resolution regional climate model, the Abdus Salam International Centre for Theoretical Physics (ICTP) Regional Climate Model, RegCM3, at 25 km grid spacing, future changes in snow cover over China are analyzed. The simulations are carried out for the period of 1951-2100 following the IPCC SRES A1B emission scenario. The results suggest good performances of the model in simulating the number of snow cover days and the snow cover depth, as well as the starting and ending dates of snow cover to the present day (1981-2000). Their spatial distributions and amounts show fair consistency between the simulation and observation, although with some discrepancies. In general, decreases in the number of snow cover days and the snow cover depth, together with postponed snow starting dates and advanced snow ending dates, are simulated for the future, except in some places where the opposite appears. The most dramatic changes are found over the Tibetan Plateau among the three major snow cover areas of Northeast, Northwest and the Tibetan Plateau in China.
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