AbstractIn the presence of uncertain initial conditions and soil hydraulic properties, land surface model (LSM) performance can be significantly improved by the assimilation of periodic observations of certain state variables, such as the near-surface soil moisture (θg), as observed from a remote platform. In this paper the possibility of merging observations and the model optimally for providing robust predictions of root-zone soil moisture (θ2) is demonstrated. An assimilation approach that assimilates θg through the ensemble Kalman filter (EnKF) and provides a physics-based update of θ2 is developed. This approach, as with other common soil moisture assimilation approaches, may fail when a key LSM parameter, for example, the saturated hy...
[1] An ensemble Kalman filter for state estimation and a bias estimation algorithm were applied to e...
Satellite-based near-surface (0–2 cm) soil moisture estimates have global coverage, but do not captu...
Model simulated soil moisture fields are often biased due to errors in input parameters and deficien...
Data assimilation techniques have been proven as an effective tool to improve model forecasts by com...
Soil moisture is an important variable for the cycling of water and energy at the catchment/regional...
The linkage between root zone soil moisture and groundwater is either neglected or simplified in mos...
Land surface models are usually biased in at least a subset of the simulated variables even after ca...
This paper aims to investigate how surface soil moisture data assimilation affects each hydrologic p...
International audienceRoot-zone soil moisture constitutes an important variable for hydrological and...
Data assimilation approaches require some type of state forecast error covariance information in ord...
Data assimilation approaches require some type of state forecast error covariance information in ord...
Two data assimilation (DA) methods are compared for their ability to produce an accurate soil ...
Accurate knowledge of soil moisture at the continental scale is important for improving predictions ...
Soil moisture is a crucial meteorological variable to understand land surface and atmospheric proce...
Land surface‐subsurface modeling combined with data assimilation was applied on the Rollesbroich hil...
[1] An ensemble Kalman filter for state estimation and a bias estimation algorithm were applied to e...
Satellite-based near-surface (0–2 cm) soil moisture estimates have global coverage, but do not captu...
Model simulated soil moisture fields are often biased due to errors in input parameters and deficien...
Data assimilation techniques have been proven as an effective tool to improve model forecasts by com...
Soil moisture is an important variable for the cycling of water and energy at the catchment/regional...
The linkage between root zone soil moisture and groundwater is either neglected or simplified in mos...
Land surface models are usually biased in at least a subset of the simulated variables even after ca...
This paper aims to investigate how surface soil moisture data assimilation affects each hydrologic p...
International audienceRoot-zone soil moisture constitutes an important variable for hydrological and...
Data assimilation approaches require some type of state forecast error covariance information in ord...
Data assimilation approaches require some type of state forecast error covariance information in ord...
Two data assimilation (DA) methods are compared for their ability to produce an accurate soil ...
Accurate knowledge of soil moisture at the continental scale is important for improving predictions ...
Soil moisture is a crucial meteorological variable to understand land surface and atmospheric proce...
Land surface‐subsurface modeling combined with data assimilation was applied on the Rollesbroich hil...
[1] An ensemble Kalman filter for state estimation and a bias estimation algorithm were applied to e...
Satellite-based near-surface (0–2 cm) soil moisture estimates have global coverage, but do not captu...
Model simulated soil moisture fields are often biased due to errors in input parameters and deficien...