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Evaluation of Noah Frozen Soil Parameterization for Application to a Tibetan Meadow Ecosystem
Publisher: American Meteorological Society
Abstract: his study evaluates the Noah land surface model (LSM) in its ability to simulate water and heat exchanges over frozen ground in a Tibetan meadow ecosystem. A comprehensive dataset including in situ micrometeorological and ...
Assessment of Roughness Length Schemes Implemented within the Noah Land Surface Model for High-Altitude Regions
Publisher: American Meteorological Society
Abstract: urrent land surface models still have difficulties with producing reliable surface heat fluxes and skin temperature (Tsfc) estimates for high-altitude regions, which may be addressed via adequate parameterization of the ...
CORRIGENDUM
Publisher: American Meteorological Society
Influence of Organic Matter on Soil Hydrothermal Processes in the Tibetan Plateau: Observation and Parameterization
Publisher: American Meteorological Society
Augmentations to the Noah Model Physics for Application to the Yellow River Source Area. Part I: Soil Water Flow
Publisher: American Meteorological Society
Abstract: his is the first part of a study focusing on evaluating the performance of the Noah land surface model (LSM) in simulating surface water and energy budgets for the high-elevation source region of the Yellow River (SRYR). ...
Augmentations to the Noah Model Physics for Application to the Yellow River Source Area. Part II: Turbulent Heat Fluxes and Soil Heat Transport
Publisher: American Meteorological Society
Abstract: his is the second part of a study on the assessment of the Noah land surface model (LSM) in simulating surface water and energy budgets in the high-elevation source region of the Yellow River. Here, there is a focus on ...
Effects of Roughness Length Parameterizations on Regional-Scale Land Surface Modeling of Alpine Grasslands in the Yangtze River Basin
Publisher: American Meteorological Society
Abstract: urrent land surface models (LSMs) tend to largely underestimate the daytime land surface temperature for high-altitude regions. This is partly because of underestimation of heat transfer resistance, which may be resolved ...