Javascript must be enabled to continue!
Sequential EnKF Assimilation of Sensitive Soil Moisture Observations to Improve Streamflow Estimation
View through CrossRef
Comparison of ensemble-based state and parameter estimation methods for
soil moisture data assimilation The use of accurate streamflow estimates
is widely recognized in the hydrological field. However, due to the
model’s structural error, they often yield suboptimal streamflow
estimates. Past studies have shown that soil moisture assimilation
improves the performance of the hydrological model which often results
in enhanced model estimates. Due to this reason, it is widely studied in
the hydrological field. However, the efficiency of the assimilation
largely relies on the correct placement of the observation into the
model. Ingesting futile observations often results in the degradation of
model performance. On the contrary, performing assimilation only at
those time steps when the assimilating variable is sensitive to the
model output may yield desirable output. Further, it will avoid the
assimilation of spurious observations. In this view, this study proposes
a new approach where sensitivity-based sequential assimilation is
performed on a conceptual Two Parameter Model (TPM). To demonstrate this
approach, ASCAT soil moisture observations are assimilated into TPM
using Ensemble Kalman Filter (EnKF) sequential approach. At first, the
temporal evolution of the soil moisture sensitivity with respect to
streamflow is established. Later, at those time steps when the soil
moisture is sensitive, EnKF assimilation is performed. For this purpose,
a moderately sized catchment in the Krishna basin, India is selected as
the study area. Model calibration and validation are performed between
2000 to 2006 and 2007 to 2011 respectively. Model run without
assimilation is considered as open-loop simulation. Streamflow
simulation after assimilation showed a significant improvement when
compared against the open-loop simulation. KGE value increased from 0.70
to 0.79 and PBIAS value reduced from 18.31 to 1.80. The highlighting
factor is that only 39% of the total observations were used during the
assimilation process. The initial results are encouraging and looks that
the proposed approach shall be highly useful at those locations where
data availability for assimilation purpose is a serious concern.
Title: Sequential EnKF Assimilation of Sensitive Soil Moisture Observations to Improve Streamflow Estimation
Description:
Comparison of ensemble-based state and parameter estimation methods for
soil moisture data assimilation The use of accurate streamflow estimates
is widely recognized in the hydrological field.
However, due to the
model’s structural error, they often yield suboptimal streamflow
estimates.
Past studies have shown that soil moisture assimilation
improves the performance of the hydrological model which often results
in enhanced model estimates.
Due to this reason, it is widely studied in
the hydrological field.
However, the efficiency of the assimilation
largely relies on the correct placement of the observation into the
model.
Ingesting futile observations often results in the degradation of
model performance.
On the contrary, performing assimilation only at
those time steps when the assimilating variable is sensitive to the
model output may yield desirable output.
Further, it will avoid the
assimilation of spurious observations.
In this view, this study proposes
a new approach where sensitivity-based sequential assimilation is
performed on a conceptual Two Parameter Model (TPM).
To demonstrate this
approach, ASCAT soil moisture observations are assimilated into TPM
using Ensemble Kalman Filter (EnKF) sequential approach.
At first, the
temporal evolution of the soil moisture sensitivity with respect to
streamflow is established.
Later, at those time steps when the soil
moisture is sensitive, EnKF assimilation is performed.
For this purpose,
a moderately sized catchment in the Krishna basin, India is selected as
the study area.
Model calibration and validation are performed between
2000 to 2006 and 2007 to 2011 respectively.
Model run without
assimilation is considered as open-loop simulation.
Streamflow
simulation after assimilation showed a significant improvement when
compared against the open-loop simulation.
KGE value increased from 0.
70
to 0.
79 and PBIAS value reduced from 18.
31 to 1.
80.
The highlighting
factor is that only 39% of the total observations were used during the
assimilation process.
The initial results are encouraging and looks that
the proposed approach shall be highly useful at those locations where
data availability for assimilation purpose is a serious concern.
Related Results
Adaptive covariance hybridization for coupled climate reanalysis
Adaptive covariance hybridization for coupled climate reanalysis
<p>Because of their very heavy computational burden, climate prediction systems that use ensemble data assimilation methods can afford only a few tens of members. Sam...
An Iterative Ensemble Kalman Filter for Data Assimilation
An Iterative Ensemble Kalman Filter for Data Assimilation
Abstract
The ensemble Kalman filter (EnKF) is a subject of intensive investigation for use as a reservoir management tool. For strongly nonlinear problems, however, ...
Large-scale Soil Moisture Monitoring: A New Approach
Large-scale Soil Moisture Monitoring: A New Approach
Soil moisture is a critical factor for understanding the interactions and feedback between the atmosphere and Earth's surface, particularly through energy and water cycles. It also...
Soil Moisture Retrieval Over Agricultural Fields Using Synthetic Aperture Radar (SAR) Data
Soil Moisture Retrieval Over Agricultural Fields Using Synthetic Aperture Radar (SAR) Data
Soil moisture is vital for agricultural fields as it determines water availability for crops, directly affecting plant growth and productivity. It regulates nutrient uptake, root d...
Estimating top-soil moisture at high spatiotemporal resolution in a highly complex landscape
Estimating top-soil moisture at high spatiotemporal resolution in a highly complex landscape
Soil moisture is a critical variable in precision agriculture, hydrological modeling, and environmental monitoring, influencing crop productivity, irrigation planning, hydrological...
Textural Image-Based Feature Prediction Model for Stochastic Streamflow Synthesis
Textural Image-Based Feature Prediction Model for Stochastic Streamflow Synthesis
Abstract
To address the challenge of obtaining reliable streamflow data for water resource management, this paper develops an encoding scheme to transform a streamflow time...
Parameterization of soil evaporation and coupled transport of moisture and heat for arid and semiarid regions
Parameterization of soil evaporation and coupled transport of moisture and heat for arid and semiarid regions
Soil moisture is an important parameter in numerical weather forecasting and climate projection studies, and it is extremely important for arid and semiarid areas. Different from t...
El Niño-Southern Oscillation (ENSO) controls on mean streamflow and streamflow variability in Central Chile
El Niño-Southern Oscillation (ENSO) controls on mean streamflow and streamflow variability in Central Chile
<p>Understanding hydrological extremes is becoming increasingly important for future adaptation strategies to global warming. Hydrologic extremes affect food security...

