maheswor Shrestha - Academia.edu (original) (raw)

maheswor Shrestha

Uploads

Papers by maheswor Shrestha

Research paper thumbnail of Development of a land surface model with coupled snow and frozen soil physics

Water Resources Research, 2017

Snow and frozen soil are important factors that influence terrestrial water and energy balances t... more Snow and frozen soil are important factors that influence terrestrial water and energy balances through snowpack accumulation and melt and soil freeze‐thaw. In this study, a new land surface model (LSM) with coupled snow and frozen soil physics was developed based on a hydrologically improved LSM (HydroSiB2). First, an energy‐balance‐based three‐layer snow model was incorporated into HydroSiB2 (hereafter HydroSiB2‐S) to provide an improved description of the internal processes of the snow pack. Second, a universal and simplified soil model was coupled with HydroSiB2‐S to depict soil water freezing and thawing (hereafter HydroSiB2‐SF). In order to avoid the instability caused by the uncertainty in estimating water phase changes, enthalpy was adopted as a prognostic variable instead of snow/soil temperature in the energy balance equation of the snow/frozen soil module. The newly developed models were then carefully evaluated at two typical sites of the Tibetan Plateau (TP) (one snow c...

Research paper thumbnail of Integrated simulation of snow and glacier melt runoff in a distributed biosphere hydrological framework; case studies at Nepal Himalaya and Pakistan Karakoram meso-scale basins

Research paper thumbnail of Development of a land surface model with coupled snow and frozen soil physics

Water Resources Research, 2017

Snow and frozen soil are important factors that influence terrestrial water and energy balances t... more Snow and frozen soil are important factors that influence terrestrial water and energy balances through snowpack accumulation and melt and soil freeze‐thaw. In this study, a new land surface model (LSM) with coupled snow and frozen soil physics was developed based on a hydrologically improved LSM (HydroSiB2). First, an energy‐balance‐based three‐layer snow model was incorporated into HydroSiB2 (hereafter HydroSiB2‐S) to provide an improved description of the internal processes of the snow pack. Second, a universal and simplified soil model was coupled with HydroSiB2‐S to depict soil water freezing and thawing (hereafter HydroSiB2‐SF). In order to avoid the instability caused by the uncertainty in estimating water phase changes, enthalpy was adopted as a prognostic variable instead of snow/soil temperature in the energy balance equation of the snow/frozen soil module. The newly developed models were then carefully evaluated at two typical sites of the Tibetan Plateau (TP) (one snow c...

Research paper thumbnail of Integrated simulation of snow and glacier melt runoff in a distributed biosphere hydrological framework; case studies at Nepal Himalaya and Pakistan Karakoram meso-scale basins

Log In