The influence of assimilating leaf area index in a land surface model on global water fluxes and storages

<p>Vegetation plays a fundamental role not only in the energy and carbon cycles but also in the global water balance by controlling surface evapotranspiration (ET). Thus, accurately estimating vegetation-related variables has the potential to improve our understanding and estimation of the dyn...

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Main Authors: X. Zhang, V. Maggioni, A. Rahman, P. Houser, Y. Xue, T. Sauer, S. Kumar, D. Mocko
Format: Article
Language:English
Published: Copernicus Publications 2020-07-01
Series:Hydrology and Earth System Sciences
Online Access:https://hess.copernicus.org/articles/24/3775/2020/hess-24-3775-2020.pdf
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author X. Zhang
V. Maggioni
A. Rahman
P. Houser
Y. Xue
T. Sauer
S. Kumar
D. Mocko
author_facet X. Zhang
V. Maggioni
A. Rahman
P. Houser
Y. Xue
T. Sauer
S. Kumar
D. Mocko
author_sort X. Zhang
collection DOAJ
description <p>Vegetation plays a fundamental role not only in the energy and carbon cycles but also in the global water balance by controlling surface evapotranspiration (ET). Thus, accurately estimating vegetation-related variables has the potential to improve our understanding and estimation of the dynamic interactions between the water, energy, and carbon cycles. This study aims to assess the extent to which a land surface model (LSM) can be optimized through the assimilation of leaf area index (LAI) observations at the global scale. Two observing system simulation experiments (OSSEs) are performed to evaluate the efficiency of assimilating LAI into an LSM through an ensemble Kalman filter (EnKF) to estimate LAI, ET, canopy-interception evaporation (CIE), canopy water storage (CWS), surface soil moisture (SSM), and terrestrial water storage (TWS). Results show that the LAI data assimilation framework not only effectively reduces errors in LAI model simulations but also improves all the modeled water flux and storage variables considered in this study (ET, CIE, CWS, SSM, and TWS), even when the forcing precipitation is strongly positively biased (extremely wet conditions). However, it tends to worsen some of the modeled water-related variables (SSM and TWS) when the forcing precipitation is affected by a dry bias. This is attributed to the fact that the amount of water in the LSM is conservative, and the LAI assimilation introduces more vegetation, which requires more water than what is available within the soil.</p>
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spelling doaj.art-adc81cc3f88c4ce2859fd92f6ac2d2e42022-12-21T23:58:43ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382020-07-01243775378810.5194/hess-24-3775-2020The influence of assimilating leaf area index in a land surface model on global water fluxes and storagesX. Zhang0V. Maggioni1A. Rahman2P. Houser3Y. Xue4T. Sauer5S. Kumar6D. Mocko7Department of Civil, Environmental and Infrastructure Engineering, George Mason University, Fairfax, VA 20771, USADepartment of Civil, Environmental and Infrastructure Engineering, George Mason University, Fairfax, VA 20771, USADepartment of Civil, Environmental and Infrastructure Engineering, George Mason University, Fairfax, VA 20771, USADepartment of Civil, Environmental and Infrastructure Engineering, George Mason University, Fairfax, VA 20771, USADepartment of Civil, Environmental and Infrastructure Engineering, George Mason University, Fairfax, VA 20771, USADepartment of Civil, Environmental and Infrastructure Engineering, George Mason University, Fairfax, VA 20771, USAHydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAHydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA<p>Vegetation plays a fundamental role not only in the energy and carbon cycles but also in the global water balance by controlling surface evapotranspiration (ET). Thus, accurately estimating vegetation-related variables has the potential to improve our understanding and estimation of the dynamic interactions between the water, energy, and carbon cycles. This study aims to assess the extent to which a land surface model (LSM) can be optimized through the assimilation of leaf area index (LAI) observations at the global scale. Two observing system simulation experiments (OSSEs) are performed to evaluate the efficiency of assimilating LAI into an LSM through an ensemble Kalman filter (EnKF) to estimate LAI, ET, canopy-interception evaporation (CIE), canopy water storage (CWS), surface soil moisture (SSM), and terrestrial water storage (TWS). Results show that the LAI data assimilation framework not only effectively reduces errors in LAI model simulations but also improves all the modeled water flux and storage variables considered in this study (ET, CIE, CWS, SSM, and TWS), even when the forcing precipitation is strongly positively biased (extremely wet conditions). However, it tends to worsen some of the modeled water-related variables (SSM and TWS) when the forcing precipitation is affected by a dry bias. This is attributed to the fact that the amount of water in the LSM is conservative, and the LAI assimilation introduces more vegetation, which requires more water than what is available within the soil.</p>https://hess.copernicus.org/articles/24/3775/2020/hess-24-3775-2020.pdf
spellingShingle X. Zhang
V. Maggioni
A. Rahman
P. Houser
Y. Xue
T. Sauer
S. Kumar
D. Mocko
The influence of assimilating leaf area index in a land surface model on global water fluxes and storages
Hydrology and Earth System Sciences
title The influence of assimilating leaf area index in a land surface model on global water fluxes and storages
title_full The influence of assimilating leaf area index in a land surface model on global water fluxes and storages
title_fullStr The influence of assimilating leaf area index in a land surface model on global water fluxes and storages
title_full_unstemmed The influence of assimilating leaf area index in a land surface model on global water fluxes and storages
title_short The influence of assimilating leaf area index in a land surface model on global water fluxes and storages
title_sort influence of assimilating leaf area index in a land surface model on global water fluxes and storages
url https://hess.copernicus.org/articles/24/3775/2020/hess-24-3775-2020.pdf
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