Javascript must be enabled to continue!
Dynamic Data Assimilation for Improved Streamflow Forecast Using Sensitive Soil Moisture Observations
View through CrossRef
The accuracy of streamflow forecasts is important for efficient
monitoring and mitigation of flood events. Unfortunately, the
uncertainty in the model control variable which includes model
parameters, initial and boundary conditions, propagates through the
model, resulting in the degradation of streamflow forecast. Various
studies in the past have shown the potential of soil moisture
assimilation in hydrological models resulting in the improved forecast.
Further, the efficiency of assimilation is based on the number and the
distribution of observations used. This study proposes a new approach
called Forward sensitivity method (FSM), which operates in two phases.
By running the model and forecast sensitivity dynamics forward in time,
the first phase places the observations at or near where the square of
the forecast sensitivity with respect to the control takes maximum
values. Then using only this subset of observations, the second phase
estimates the unknown elements of the control by solving a resulting
weighted least squares problem. The power of this approach is
demonstrated by assimilating ASCAT soil moisture observations into a
conceptual Two Parameter Model in a medium sized watershed lying in the
Krishna River Basin, India. The model run extends for four monsoon years
from June 2007 to June 2011 and two assimilation scenarios were tested.
The first scenario uses all the observations, whereas, the second uses
only sensitive observations during assimilation and the results were
then compared against open loop simulation (model run without
assimilation). Sensitivity results indicate that observations during
monsoon time alone are sufficient for assimilation purpose, which
accounts for only 37.42 percent of total observations. Also, the
estimation and forecast results show improved streamflow performance
when using only sensitive observations. From the results, it is
concluded that FSM based assimilation can help in reducing the
computation time greatly. Further, this study will be critically helpful
in the places where data availability remains a major problem.
Title: Dynamic Data Assimilation for Improved Streamflow Forecast Using Sensitive Soil Moisture Observations
Description:
The accuracy of streamflow forecasts is important for efficient
monitoring and mitigation of flood events.
Unfortunately, the
uncertainty in the model control variable which includes model
parameters, initial and boundary conditions, propagates through the
model, resulting in the degradation of streamflow forecast.
Various
studies in the past have shown the potential of soil moisture
assimilation in hydrological models resulting in the improved forecast.
Further, the efficiency of assimilation is based on the number and the
distribution of observations used.
This study proposes a new approach
called Forward sensitivity method (FSM), which operates in two phases.
By running the model and forecast sensitivity dynamics forward in time,
the first phase places the observations at or near where the square of
the forecast sensitivity with respect to the control takes maximum
values.
Then using only this subset of observations, the second phase
estimates the unknown elements of the control by solving a resulting
weighted least squares problem.
The power of this approach is
demonstrated by assimilating ASCAT soil moisture observations into a
conceptual Two Parameter Model in a medium sized watershed lying in the
Krishna River Basin, India.
The model run extends for four monsoon years
from June 2007 to June 2011 and two assimilation scenarios were tested.
The first scenario uses all the observations, whereas, the second uses
only sensitive observations during assimilation and the results were
then compared against open loop simulation (model run without
assimilation).
Sensitivity results indicate that observations during
monsoon time alone are sufficient for assimilation purpose, which
accounts for only 37.
42 percent of total observations.
Also, the
estimation and forecast results show improved streamflow performance
when using only sensitive observations.
From the results, it is
concluded that FSM based assimilation can help in reducing the
computation time greatly.
Further, this study will be critically helpful
in the places where data availability remains a major problem.
Related Results
Sequential EnKF Assimilation of Sensitive Soil Moisture Observations to Improve Streamflow Estimation
Sequential EnKF Assimilation of Sensitive Soil Moisture Observations to Improve Streamflow Estimation
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 hydrolo...
Ecological soil physics as section of ecological soil science
Ecological soil physics as section of ecological soil science
Nowadays, there is a general penetration of ecology in other related sciences. Soil science is not an exception. To the evidence of this, the works of soil scientists may serve, th...
Multiscale soil moisture retrievals from microwave remote sensing observations
Multiscale soil moisture retrievals from microwave remote sensing observations
La humedad del suelo es la variable que regula los intercambios de agua, energía, y carbono entre la tierra y la atmósfera. Mediciones precisas de humedad son necesarias para una g...
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...
Skilful Seasonal Streamflow Forecasting Using a Fully Coupled Global Climate Model
Skilful Seasonal Streamflow Forecasting Using a Fully Coupled Global Climate Model
Abstract. The seasonal streamflow forecast (SSF) is a crucial decision-making, planning and management tool for disaster prevention, navigation, agriculture, and hydropower generat...
Rainfall-runoff reaction controlled by soil moisture thresholds in a small Alpine catchment
Rainfall-runoff reaction controlled by soil moisture thresholds in a small Alpine catchment
<p>Since 2009, we have continuously monitored soil moisture in the Eastern Alpine torrent catchment of the Brixenbach (Tyrol, Austria). The measurement network is one...
A Protocol for Establishing Soil Moisture Observations at the Complex Mountainous Region.
A Protocol for Establishing Soil Moisture Observations at the Complex Mountainous Region.
<p>Soil moisture, controlling the fraction of the water between grounds and atmosphere, has been observed from various measurements to understand the hydrological cyc...
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...

