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    Guo-yue Niu

    The presence of ice in soil dramatically alters soil hydrologic and thermal properties. Despite this important role, many recent studies show that explicitly including the hydrologic effects of soil ice in land surface models degrades the... more
    The presence of ice in soil dramatically alters soil hydrologic and thermal properties. Despite this important role, many recent studies show that explicitly including the hydrologic effects of soil ice in land surface models degrades the simulation of runoff in cold regions. This paper addresses this dilemma by employing the Community Land Model version 2.0 (CLM2.0) developed at the National
    Groundwater interacts with soil moisture through the exchanges of water between the unsaturated soil and its underlying aquifer under gravity and capillary forces. Despite its importance, groundwater is not explicitly represented in... more
    Groundwater interacts with soil moisture through the exchanges of water between the unsaturated soil and its underlying aquifer under gravity and capillary forces. Despite its importance, groundwater is not explicitly represented in climate models. This paper developed a simple groundwater model (SIMGM) by representing recharge and discharge processes of the water storage in an unconfined aquifer, which is added as a single integration element below the soil of a land surface model. We evaluated the model against the Gravity Recovery and Climate Experiment (GRACE) terrestrial water storage change (DeltaS) data. The modeled total water storage (including unsaturated soil water and groundwater) change agrees fairly well with GRACE estimates. The anomaly of the modeled groundwater storage explains most of the GRACE DeltaS anomaly in most river basins where the water storage is not affected by snow water or frozen soil. For this reason, the anomaly of the modeled water table depth agree...
    In this study, we simulated and analyzed the monthly variations of stable water isotopes in different reservoirs at Manaus, Brazil, using the Community Land Model (CLM) that incorporates stable isotopic effects as a diagnostic tool for... more
    In this study, we simulated and analyzed the monthly variations of stable water isotopes in different reservoirs at Manaus, Brazil, using the Community Land Model (CLM) that incorporates stable isotopic effects as a diagnostic tool for understanding stable water isotopic processes, filling the observational data gaps and predicting hydrometeorological processes. The simulation results show that the δ18O values in precipitation,
    The Technical Notes series provides an outlet for a variety of NCAR Manuscripts that contribute in specialized ways to the body of scientific knowledge but that are not suitable for journal, monograph, or book publication. Reports in this... more
    The Technical Notes series provides an outlet for a variety of NCAR Manuscripts that contribute in specialized ways to the body of scientific knowledge but that are not suitable for journal, monograph, or book publication. Reports in this series are issued by the NCAR scientific divisions. Designation symbols for the series include: EDD–Engineering, Design, or Development Reports Equipment descriptions, test results, instrumentation, and operating and maintenance manuals. IA–Instructional Aids Instruction manuals, ...
    The Community Land Model is the land component of the Community Climate System Model (CCSM). CLM3 exhibited significant energy and water biases resulting from deficiencies in hydrological processes. In this presentation, we will describe... more
    The Community Land Model is the land component of the Community Climate System Model (CCSM). CLM3 exhibited significant energy and water biases resulting from deficiencies in hydrological processes. In this presentation, we will describe a suite of improvements to the representation of hydrologic processes in the model that have been developed in collaboration with the research community that utilizes CLM. The modifications are broad and extend throughout the model. Modifications that direcly affected hydrologic processes include new surface data sets based on Moderate Resolution Imaging Spectroradiometer products, new parameterizations for canopy integration, canopy interception, frozen soil, soil water availability, soil evaporation, a TOPMODEL-based model for surface and subsurface runoff, a groundwater model for determining water table depth, Richard's equation solution, organic soil, and snow processes (snow cover fraction and vegetation burial, aerosol deposition) . The results from a set of offline simulations comparing several versions of CLM will be presented and compared against observed data for runoff, river discharge, soil moisture, and total water storage to assess the performance of the new model. Among the most significant improvements are improved partitioning of global evapotranspiration (ET) which result in wetter soils, less plant water stress, increased transpiration and photosynthesis, and an improved annual cycle of total water storage. The new model, CLM4, provides the basis for improved large-scale modeling and study of energy, water, and biogeochemical (carbon and nitrogen) cycles.