Meteorological variables (e.g., air temperature (T2), radiation flux, and precipitation) determine the evolution of glacier mass characteristics. Observations these are not available with adequate spatial coverage spatiotemporal resolution over Tibetan Plateau. Albedo is key factor net determined by land cover snow-related variables. This study focuses on evaluating performance albedo parameter...

In this paper, we compare the efficiency of two models to estimate the surface displacements due to continental water storage (CWS) variations over continental North America. The first model, the monthly North America Land Data Assimilation System Phase 2 Noah (NLDAS2 Noah) is a model of CWS restricted to North America. The second data set, the Global Land Data Assimilation System Noah (GLDAS N...

The impact of several land surface models (LSMs) and microphysics (MP), planetary boundary layer (PBL), schemes on the accuracy simulated brightness temperatures (BTs) from water vapor (WV) sensitive bands was examined via comparison with observations GOES-16 Advanced Baseline Imager. Nine parameterization configurations were evaluated. Analysis revealed that, compared to Thompson MP scheme, Na...

Abstract. Distributed environmental models such as land surface (LSMs) require model parameters in each spatial modeling unit (e.g., grid cell), thereby leading to a high-dimensional parameter space. One approach decrease the dimensionality of space these is use regularization techniques. highly efficient technique multiscale regionalization (MPR) framework that translates high-resolution predi...