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Liang Zhang, Sha Sha, Qiang Zhang, Funian Zhao, Jianhua Zhao, Hongyu Li, Sheng Wang, Jianshun Wang, Yanbin Hu and Hui Han
The interaction between soil moisture (SM) and evaporative fraction (EF), which reflects the degree of exchange of water and energy between the land and the atmosphere, is an important component of the theory of land?atmosphere coupling. Exploring the re...
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Hailiang Zhang, Junjian Liu, Huoqing Li, Xianyong Meng and Ablimitijan Ablikim
Soil moisture is a critical parameter in numerical weather prediction (NWP) models because it plays a fundamental role in the exchange of water and energy cycles between the atmosphere and the land surface through evaporation. To improve the forecast ski...
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Alan K. Betts and Raymond L. Desjardins
Analysis of the hourly Canadian Prairie data for the past 60 years has transformed our quantitative understanding of land–atmosphere–cloud coupling. The key reason is that trained observers made hourly estimates of the opaque cloud fraction t...
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Souleymane Sy, Nathalie de Noblet-Ducoudré, Benjamin Quesada, Ibrahima Sy, Amadou Moctar Dieye, Amadou Thierno Gaye and Benjamin Sultan
Land Use Land-Cover Change (LULCC), such as deforestation, affects the climate system and land-atmosphere interactions. Using simulations carried out within the LUCID (Land Use and Climate, IDentification of robust Impacts) project framework, we first qu...
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ANANDU D. VERNEKAR,JIAYU ZHOU,BENJAMÍN KIRTMAN
FForecast errors exhibit the characteristics of approximations in simulating dynamical and physical processes in models. The models are very complex and hence it is not always possible to identify the approximations responsible for any particular erro...
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