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| Role of Black Carbon-Induced Changes in Snow Albedo in Predictions of Temperature and Precipitation during a Snowstorm |
| ZHANG Ying,LIAO Hong,ZHU Ke-Feng,YIN Yan |
| Key Laboratory for Atmospheric Physics and Environment (LAPE), Nanjing University of Information Science and Technology, Nanjing; State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing,State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing,Laboratory of Cloud-Precipitation Physics and Severe Storms (LACS), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing,Key Laboratory for Atmospheric Physics and Environment (LAPE), Nanjing University of Information Science and Technology, Nanjing |
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Abstract In this study the authors apply the chemistry version of the Weather Research and Forecasting model (WRF-Chem) to examine the impacts of black carbon (BC)-induced changes in snow albedo on simulated temperature and precipitation during the severe snowstorm that occurred in southern China during 0800 26 January to 0800 29 January 2008 (Note that all times are local time except when otherwise stated). Black carbon aerosol was simulated online within the WRF-Chem. The model results showed that surface-albedo, averaged over 27-28 January, can be reduced by up to 10% by the deposition of BC. As a result, relative to a simulation that does not consider deposition of BC on snow/ice, the predicted surface air temperatures during 27-28 January can differ by -1.95 to 2.70 K, and the predicted accumulated precipitation over 27-28 January can differ by -2.91 to 3.10 mm over Areas A and B with large BC deposition. Different signs of changes are determined by the feedback of clouds and by the availability of water vapor in the atmosphere.
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Received: 30 April 2009
Revised: 09 July 2009
Accepted: 09 July 2009
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