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Satellite Monitoring of the Surface Water and Energy Budget in the Central Tibetan Plateau 被引量:1

Satellite Monitoring of the Surface Water and Energy Budget in the Central Tibetan Plateau
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摘要 The water and energy cycle in the Tibetan Plateau is an important component of Monsoon Asia and the global energy and water cycle. Using data at a CEOP (Coordinated Enhanced Observing Period)-Tibet site, this study presents a first-order evaluation on the skill of weather forecasting from GCMs and satellites in producing precipitation and radiation estimates. The satellite data, together with the satellite leaf area index, are then integrated into a land data assimilation system (LDAS-UT) to estimate the soil moisture and surface energy budget on the Plateau. The system directly assimilates the satellite microwave brightness temperature, which is strongly affected by soil moisture but not by cloud layers, into a simple biosphere model. A major feature of this system is a dual-pass assimilation technique, which can auto-calibrate model parameters in one pass and estimate the soil moisture and energy budget in the other pass. The system outputs, including soil moisture, surface temperature, surface energy partition, and the Bowen ratio, are compared with observations, land surface models, the Global Land Data Assimilation System, and four general circulation models. The results show that this satellite data-based system has a high potential for a reliable estimation of the regional surface energy budget on the Plateau. The water and energy cycle in the Tibetan Plateau is an important component of Monsoon Asia and the global energy and water cycle. Using data at a CEOP (Coordinated Enhanced Observing Period)-Tibet site, this study presents a first-order evaluation on the skill of weather forecasting from GCMs and satellites in producing precipitation and radiation estimates. The satellite data, together with the satellite leaf area index, are then integrated into a land data assimilation system (LDAS-UT) to estimate the soil moisture and surface energy budget on the Plateau. The system directly assimilates the satellite microwave brightness temperature, which is strongly affected by soil moisture but not by cloud layers, into a simple biosphere model. A major feature of this system is a dual-pass assimilation technique, which can auto-calibrate model parameters in one pass and estimate the soil moisture and energy budget in the other pass. The system outputs, including soil moisture, surface temperature, surface energy partition, and the Bowen ratio, are compared with observations, land surface models, the Global Land Data Assimilation System, and four general circulation models. The results show that this satellite data-based system has a high potential for a reliable estimation of the regional surface energy budget on the Plateau.
出处 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2008年第6期974-985,共12页 大气科学进展(英文版)
基金 the "100-Talent" Project of Chinese Academy of Sciences
关键词 Tibetan Plateau CEOP microwave land data assimilation surface energy budget satellite products Tibetan Plateau, CEOP, microwave land data assimilation, surface energy budget, satellite products
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  • 1Young,G. S.Turbulence structure of the convective boundary layer.Parts I & II, J[].Atmospheric Science.1988
  • 2Hahn,D. G.The role of mountains in the South Asia Monsoon circulation, J[].Journal of the Atmospheric Sciences.1975
  • 3Nitta,T.Observational study of heat source over the eastern Tibetan Plateau during the summer monsoon, J[].Journal of the Meteorological Society of Japan.1983
  • 4Young,G. S.Convection in the atmospheric boundary layer[].Earth Science Reviews.1988
  • 5Yasunari,T.A quasi-stationary appearance of 30-40 day period in the cloudiness during the summer monsoon over India, J[].Meteorological Soc Japan.1980

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