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Sequential EnKF Assimilation of Sensitive Soil Moisture Observations to Improve Streamflow Estimation
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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.
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