World’s population is
increasing day by day. It will be making water management very
critical issue. It has become absolutely necessary to find the
solution for effective water management. Many techniques are
available for effective water management based on the observed data
analysis. Most of the techniques are statistical which are based on
collection of data and analysing this data with the help of designing
a computational model. For designing the computational model various
mathematical and statistical techniques has been used based on state
variable equations.
A computational model contains
numerous variables that characterise the system being studied.
Simulation is done by adjusting these variables and observing how the
changes affect the outcomes predicted by the model. The results of
model simulations help researchers make predictions about what will
happen in the real system that is being studied in response to
changing conditions.
Data assimilation is the process
by which observations are incorporated into a computer model of a
real system. Data assimilation is very important concept of applied
mathematics which is used in most of the application areas from
signal processing to weather forecasting.
THE BEST ESTIMATE WE CAN MAKE OF
ANY PHENOMENON IS PROVIDED BY COMBINING OUR KNOWLEDGE FROM THE
PREDICTION AND THE MEASUREMENT.
Predicting something is very
hard problem. For solving this problem we need to develop the
computational model for future prediction. But only mathematical
model cannot give the accurate and significant results. The model
should be evolved over time and real world observations should be
incorporated into the model to measure the efficiency of the
mathematical model. If there are errors in the model means the
distraction of the model from the actual observational values, then
that errors should be corrected. So we need to incorporate the
observations in the model over the period of time.
The figure shows the process of
Data Assimilation.
The purpose of data assimilation is to provide better estimates than can be obtained by only the data or model. Now the question arises why do we assimilate data? The answer is to make a prediction of future pesticides, nutrients and water need to the crop, for this we want to begin with the state of the agricultural field as close to the real field as possible. To understand previous pattern in variability, we want to make the field simulation as close to reality as possible.
Test(1)=A set of soil moisture
estimates made by math equations for time=1
Tobs(1)=A set of soil moisture
measured in real field at time=1
This is assumed to be “Truth”
Difference=Tobs(1)-Test(1)
Test(2)=
Tobs(1)+R*Difference+math,
where R includes
a) Information on errors
b) How to distribute the observed
soil moisture to nearby points.
Methods of Model Updating
Input:
corrects model input forcing errors or replaces model-based forcing
with observations, thereby improving the model’s predictions;
State:
corrects the state or storage of the model so that it comes closer
to the observations (state estimation, data assimilation in the
narrow sense);
Parameter:
corrects or replaces model parameters with observational information
(parameter estimation, calibration);
Error correction:
correct the model predictions or state variables by an observed time
integrated error term in order to reduce systematic model bias.
Assimilating moisture data will
also cause other variables used for the estimates. The goal is to minimise some measure of difference between the model and the data.
There are two types of DA
intermittent data assimilation schemes and continuous assimilation
schemes. In intermittent DA data is assimilate after fixed amount of
time on a regular schedule, the model is initialised, and a new
short-term forecast is made. In continuous assimilation schemes, data
is inserted whenever it becomes available. Incremental insertion of
data is used over time.
Comparison of prediction with
observations is the heart of data assimilation techniques. By
comparing we know that the model is close to the truth values.
Modeling
the behavior of agro ecosystems is, therefore, of great help since it
allows the definition of management strategies that maximize (crop)
production while minimising the environmental impacts. Remote sensing
can support such modeling by offering information on the spatial and
temporal variation of important canopy state variables which would be
very difficult to obtain otherwise.
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