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Actual daily evapotranspiration estimated from MERIS and AATSR data over the Chinese Loess Plateau
Actual daily evapotranspiration MERIS AATSR data Chinese Loess Plateau
2010/2/1
The Chinese Loess Plateau is located in the north of China and has a significant impact on the climate and ecosystem evolvement over the East Asian continent. Estimates of evapotranspiration (ET) at a...
Monitoring Soil Condition in the Northern Tibetan Plateau Using SSM/I Data
Monitoring Soil Condition Northern Tibetan Plateau SSM/I Data
2009/10/23
A combination of a low 37 GHa brightness temperature and a negative 19 and
37 GH7 spectral gradient can be an effective discriminant for frozen and thawed
soil. SSMII data for 1988 are used to study...
Recent advances on the study of atmosphere-land interaction observations on the Tibetan Plateau
Tibetan Observation and Research Platform Atmospheric Boundary Layer
2009/7/22
As a unique geological and geographical unit, the Tibetan Plateau dramatically impacts the world's environment and especially controls climatic and environmental changes in China, Asia and even in th...
An overview of the LOess Plateau mesa region land surface process field EXperiment series (LOPEXs)
LOess Plateau field EXperiment series land surface
2009/7/22
A series of land surface process field experiments were carried out in a mesa region of the Chinese Loess Plateau in each of the years from 2004 to 2008 (acronymized as LOPEX04, LOPEX08, etc.). The g...
Influence of thermodynamic soil and vegetation parameterizations on the simulation of soil temperature states and surface fluxes by the Noah LSM over a Tibetan plateau site
thermodynamic soil soil temperature states vegetation parameterizations
2009/7/22
In this paper, we investigate the ability of the Noah Land Surface Model (LSM) to simulate temperature states in the soil profile and surface fluxes measured during a 7-day dry period at a micrometeor...
Some practical notes on the land surface modeling in the Tibetan Plateau
land surface models land-atmosphere interactions Tibetan Plateau
2009/7/22
The Tibetan Plateau is a key region of land-atmosphere interactions, as it provides an elevated heat source to the middle-troposphere. The Plateau surfaces are typically characterized by alpine meadow...
Soil water storage and groundwater behaviour in a catenary sequence beneath forest in central Amazonia：I. Comparisons between plateau, slope and valley floor
Soil water storage groundwater central Amazonia plateau valley floor
2009/6/8
Soil water storage was monitored in three landscape elements in the forest (plateau, slope and valley floor) over a 3 year period to identify differences in sub-surface hydrological response. Under th...
Impacts of changes in vegetation cover on soil water heat coupling in an alpine meadow of the Qinghai-Tibet Plateau, China
soil water heat alpine meadow Qinghai-Tibet Plateau
2009/4/28
Alpine meadow is one of the most widespread grassland types in the permafrost regions of the Qinghai-Tibet Plateau, and the transmission of coupled soil water heat is one of the most crucial processes...
Estimating surface fluxes over the north Tibetan Plateau area with ASTER imagery
surface fluxes north Tibetan Plateau area
2009/4/27
Surface fluxes are important boundary conditions for climatological modeling and Asian monsoon system. The recent availability of high-resolution, multi-band imagery from the ASTER (Advanced Space-bor...
The Implication of Heat and Water Balance Changes in a Lake Basin on the Tibetan Plateau
Water Balance Changes Lake Basin Tibetan Plateau
2009/4/13
The numerous lakes found throughout the Tibetan Plateau have a large effect on evaporation from the plateau. We analyzed variation in the water cycle in Yamdrok Yumtso Lake basin under the temperature...