4.7 Article Data Paper

An ensemble of 48 physically perturbed model estimates of the 1/8? terrestrial water budget over the conterminous United States, 1980-2015

Journal

EARTH SYSTEM SCIENCE DATA
Volume 15, Issue 7, Pages 2755-2780

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/essd-15-2755-2023

Keywords

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This study presents a dataset simulated from an ensemble of 48 physics configurations of the Noah LSM to estimate terrestrial water budget (TWB) in the United States. The dataset covers the period from 1980 to 2015 at a monthly temporal and 1/8 spatial resolution, including variables such as evapotranspiration, runoff, and terrestrial water storage. Evaluations show that the dataset performs well in reproducing observed water storage and snow water equivalent.
Terrestrial water budget (TWB) data over large domains are of high interest for various hydrological applications. Spatiotemporally continuous and physically consistent estimations of TWB rely on land surface models (LSMs). As an augmentation of the operational North American Land Data Assimilation System Phase 2 (NLDAS-2) four-LSM ensemble, this paper describes a dataset simulated from an ensemble of 48 physics configurations of the Noah LSM with multi-physics options (Noah-MP). The 48 Noah-MP physics configurations are selected to give a representative cross-section of commonly used LSMs for parameterizing runoff, atmospheric surface layer turbulence, soil moisture limitation on photosynthesis, and stomatal conductance.The dataset spans from 1980 to 2015 over the conterminous United States (CONUS) at a monthly temporal resolution and a 1/8(?) spatial resolution. The dataset variables include total evapotranspiration and its constituents (canopy evaporation, soil evaporation, and transpiration), runoff (the surface and subsurface components), as well as terrestrial water storage (snow water equivalent, four-layer soil water content from the surface down to 2 m, and the groundwater storage anomaly). The dataset is available at . Evaluations carried out in this study and previous investigations show that the ensemble performs well in reproducing the observed terrestrial water storage, snow water equivalent, soil moisture, and runoff. Noah-MP complements the NLDAS models well, and adding Noah-MP consistently improves the NLDAS estimations of the above variables in most areas of CONUS. Besides, the perturbed-physics ensemble facilitates the identification of model deficiencies. The parameterizations of shallow snow, spatially varying groundwater dynamics, and near-surface atmospheric turbulence should be improved in future model versions.

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