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International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072
© 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 424
RAINFALL-RUNOFF MODELING USING ARTIFICIAL NEURAL NETWORK
TECHNIQUE
---------------------------------------------------------------------***---------------------------------------------------------------------
Abstract - Artificial neural networks(ANNs)areamongthe
most sophisticated empirical models available and have
proven to be especially good in modelling complex systems.
Their ability to extract relationsbetweeninputsandoutputsof
a process, without the physics being explicitly provided to
them, theoretically suits the problem of relating rainfall to
runoff well, since it is a highly nonlinear andcomplexproblem.
The goal of this investigation was to develop rainfall-runoff
models for the river Jhelum catchment that are capable of
accurately modelling the relationships between rainfall and
runoff in a catchment. It is for this reason that ANN technique
was tested as R-R models on a data set from the upper Jhelum
catchment in Jammu and Kashmir, India. Two types of ANN
models viz. Back Propagation networks (BPN) and Radial
Basis function (RBF) were developed and tested for this data
and later their performance was checked by different
statistical parameters like coefficient of determination R2 and
root mean squared error (RMSE).
Key Words: Back Propagation network, Radial Basis
function network, Modeling, Artificial neural network.
1. INTRODUCTION
Hydrologic engineering design and management purposes
require information about runoff from a hydrologic
catchment. In order to predict this information, the
transformation of rainfall on a catchment to runoff from it
must be modeled. One approach to this modeling issue is to
use empirical Rainfall-Runoff (R-R) models. Empirical
models simulate catchment behaviour by parameterization
of the relations that the model extracts from sample input
and output data. Artificial Neural Networks (ANNs) are
models that use dense interconnection of simple
computational elements, known as neurons, in combination
with so-called training algorithms to make their structure
(and therefore their response) adapt to information that is
presented to them. ANNs have analogies with biological
neural networks, such as nervous systems. ANNs are among
the most sophisticated empirical models available and have
proven to be especially good in modeling complex systems.
Their ability to extract relations between inputsandoutputs
of a process, without the physics being explicitlyprovided to
them, theoretically suits the problem of relating rainfall to
runoff well, since it is a highly nonlinear and complex
problem. The goal of this investigation was to prove that
ANN models are capable of accurately modeling the
relationships between rainfall and runoff in a catchment.An
existing software tool in the Matlab environment was
selected for design and testing of ANNs on the data set. A
special algorithm (the back propagation algorithm) was
programmed and incorporated in this tool. This algorithm
was expected to ease the trial-and-error efforts for finding
an optimal network structure. The ANN type that was used
in this investigation is the so-called static multilayer feed
forward network. The main conclusion that can be drawn
from this investigation is that ANNs are indeed capable of
modeling R-R relationships. In the present study Multiple
Linear Regression technique was employed on the
normalized data using MS Excel. The analysis of variance
was done and R2, root mean squared error (RMSE) were
computed. The MLR model was validated by plotting the
predicted discharge v/s actual discharge curve for years
2010-2013 (about 20% data).
2. STUDY AREA
The present study was carried out in the upper Jhelum
catchment. The study area spatially lies between 33°21′54″
N to 34° 27′ 52″ N latitude and 74° 24′ 08″ E to 75° 35′ 36″ E
longitude with a total area of 8600.78 sq.kms (Figure.1). It
covers almost all the physiographic divisions of the Kashmir
Valley and is drained by the most important tributaries of
river Jhelum. Srinagar city which is the largest urban centre
in the valley is settled on both the sides of Jhelum River and
is experiencing a fast spatial growth. Physical features of
contrasting nature can be observed in the study area that
ranges from fertile valley floor to snow-clad mountains and
from glacial barren lands to lush green forests.
Fig -1: Location map of study area
Lateef Ahmad Dar
Dept of Civil Engineering, National Institute of Technology Srinagar, J&K, India.
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072
© 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 425
3. DATA
The discharge data at Padshahibagh gauging station from
1991-2013 was obtained from the irrigation and flood
control department, Kashmir and the precipitationdata was
procured from the Indian meteorological department(IMD)
and National climate data centre (NCDC). The data sets for
the years 2001-2009 were used for
development/calibrating/training the models and these
models were validated for various data sets achieved for
2010-2013.
4. ARTIFICIAL NEURAL NETWORK (ANN)
Artificial Neural Networks (ANNs) are networks of simple
computational elements that are able to adapt to an
information environment. This adaptation is realised by
adjustment of the internal network connections through
applying a certain algorithm. Thus, ANNsareabletouncover
and approximate relationships thatarecontainedinthedata
that is presented to the network. ANN applications are
becoming more and more popular since the resurgence of
these techniques in the last part of the1980’s.Sincetheearly
1990’s, ANNs have been successfully used in hydrology
related areas, one of which is Rainfall-Runoff (R-R)
modelling [after Govindaraju, 2000]. The application of
ANNs as an alternative modelling tool in this field, however,
is still in its nascent stages. The reason for modelling the
relation between precipitationona catchmentandthe runoff
from it is that runoff information is needed for hydrologic
engineeringdesignandmanagementpurposes[Govindaraju,
2000]. However, as Tokar and Johnson [1999] state, the
relationship between rainfall and runoff is one of the most
complex hydrologic phenomena to comprehend. This is due
to the tremendous spatial and temporal variability of
watershed characteristicsandprecipitationpatterns,and the
number of variables involvedinthemodellingofthe physical
processes. The network is able to intelligently change its
internal parameters, so that the target output signal is
approximated. This way the relationshipsbetweentheinput
and output variable are parameterised in the model
structure and the ANN can make an output prediction based
on new input. ANNs have proven to be especially good in
modelling complex and non-linear systems.Otherimportant
merits of these techniques aretheshortdevelopmenttimeof
ANN models, their flexibility and the fact that no great
expertise in a certain field is needed in order to be able to
apply ANN techniques in this field. The present study is
under taken develop rainfall-runoff model in river Jhelum.
Artificial Neural Network Techniqueswill beusedtodevelop
the rainfall runoff models, to predict the runoffdischargesat
Padshahi Bagh station. A predictive analysis is used to
determine the predictors which influence the runoff. After
the model development the runoff at the Padshahi-Bagh
station could then be predicted. Neural Network Tool Box of
MATLAB was used to develop Artificial Neural Network
Models for Rainfall-RunoffmodelinginRiverJhelum.Various
types of neural networks Viz. BPN and RBF were developed.
The BPN was optimized for the number of neurons in the
hidden layer by changing the number of neurons in the
hidden layer. AIC and BIC criteria was employed on various
BPN models which led to the selection of two BPN networks
with 6 and 10 neurons in the hidden layer. These networks
are represented as BPN 6N and BPN 10N in this study
respectively. The predicted vs. actual discharges were
developed curves were drawn for all the neural network
models and there by models werevalidatedforabout20%of
the data. Various statistical indices like R2 and RMSE were
computed for comparing these models. Based on these
statistical indices, the artificial neural networksprovedto be
better than MLR. Among various ANN models, RBF with
RMSE=0.046 and R2=0.937 emerged to be the best suited
model for the prediction. The models developed were then
used to developed two individual hydrographs and all the
models predicted flood hydrograph to a good extent butRBF
networks with RMSE=0.016 and R2=0.976 again proved to
be quite impressive as per the overall performance .
5. RESULTS AND DISCUSSIONS
The number of neurons in the hidden layer is a very
complicated task in finalizing the network architecture.This
can be done by trial and error analysis. We have to finalize
the number of hidden layers and the number of neurons in
the hidden layers. The hidden layers in the network were
fixed to one. Hence we start with one neuron in the hidden
layer and increase it every time after training the network.
The observed Vs predicted runoffs for various number of
neurons in the hidden layer is shown in figure 6.10 to 6.13.
Results of BPN network with 6 neurons in the hidden layer
and BPN network with 10 neurons in the hidden layer are
shown in Figure 4 and Table 1.After carrying out regression
and validating the data the value of R2 and RMSE for
different parameters werecalculatedasshownintable1and
table 2:
Fig -2: Dialogue box showing the training performance
of RBF network.
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072
© 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 426
Fig -3: Dialogue box showing training performance
of BPN network.
Fig -4: Observed vs. predicted discharge, P(t-1) to P(t-5)
for BPN network.
Table -1: Goodness of fit for the effect of no. of previous
day input rainfall parameters.
Fig -5: Observed vs. predicted discharge, P(t-1) to P(t-5)
for RBF network.
Table -2: Statistical indices of RBF model for various
inputs.
NETWORK INPUTS RMSE R-SQUARE
RBF
P(t-1) 0.097 0.912
P(t-1)…P(t-
5)
0.046 0.937
The statistical analysis shows that the performance of this
network increases as the number rainfall inputs increase
from one to five i.e. from p(t-1) to p(t-1)....p(t-5).
3. CONCLUSIONS
From the values of R2 and RMSE it was observed that radial
basis function networks (RBF) were able to predict the
runoff more accurately than Back propagation networks
(BPN). BPN network performed better when thenumbersof
neurons in the hidden layer were increased upto 10. On
increasing the number of neurons further, the network
showed no considerable improvement in performance. The
radial function model (RBF) gave better resultscomparedto
BPN networks with RMSE = 0.046 and was able to predict
the stream at the Padshahi-Bagh station more accurately
than the other networks.
REFERENCES
[1] Amari, S., Murata, N., Muller, K. R., Finke, M., and Yang,
H.H. (1997). Asymptotic statistical theory of overtraining
and cross-validation.IEEETransactionsonNeural Networks,
8(5): p 985-996.
[2]Champion, H. G. and Seth, S. K. (1968): A Revised Survey
of the Forest Types of India. ManagerofPublications,Govt.of
India, New Delhi, pp. 404
NETWORK INPUTS RMSE R-SQUARE
Back
propagation
network
6 neurons.
P(t-1) 0.521 0.776
P(t-
1)…P(t-5)
0.245 0.856
Back
propagation
network
10 neurons.
P(t-1) 0.342 0.814
P(t-
1)…P(t-5)
0.132 0.891
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072
© 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 427
[3]Dibike, Y. B. Solomatine, D.P.2000“Riverflowforecasting
using artificial neural networks” Physics and Chemistry of
the Earth (B), Vol. 26, No. 1, pp. 1-7, Elsevier Science B.V.
[4]Fahlman, Scott E. Lebiere, Christian 1991 “The Cascade-
Correlation Learning Architecture” School of Computer
Science, Carnegie Mellon University
[5]Govindaraju, Rao S. 2000 “Artificial neural networks in
hydrology I: preliminary concepts” Journal of Hydrologic
Engineering, Vol. 5, No. 2, pp. 115-123, ASCE.
[6]Govindaraju, Rao S. 2000 “Artificial neural networks in
hydrology II: hydrologic applications” Journal of Hydrologic
Engineering, Vol. 5, No. 2, pp. 124-137, ASCE.
[7]Halff, A. H. Halff, H. M. Azmoodeh, M. 1993 “Predicting
from rainfall using neural networks” Proceedings of
Engineering Hydrology, pp. 760-765, ASCE.
[8]Krajewski, W. F.Cuykendal, R. R. 1992 “Rainfall
forecasting in space and time using a neural network”
Journal of Hydrology, Vol. 137, pp. 1-37,ElsevierScience B.V.
[9]Meher-Homji, V. M. (1971): The Climate of Srinagar and
its Variability. Geog. Rev. Ind., 33, (1): 1-14.
[10] Mehnaza Akhter, Ahanger Manzoor Ahmad (2017)
Climate Modeling of Jhelum River Basin - A Comparative
Study. Environ Pollut Climate Change 1: 110.
[11] Mehnaza Akhter (2017) Application of ANN for the
Hydrological Modeling. International Journal forResearchin
Applied Science & Engineering Technology (IJRASET),
Volume 5 Issue VII, July 2017
[12]Sridhar, S.P.(1996). Synthesis of artificial neural
networks using genetic algorithms. thesis submitted to
Indian institute of technology, New Delhi, India.
[13]Tokar, A. Sezin Johnson, Peggy A. 1999 “Rainfall-runoff
modelling using artificial neural networks” Journal of
Hydrologic Engineering, Vol. 4, No. 3, pp. 232-239, ASCE.

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Rainfall-Runoff Modeling using Artificial Neural Network Technique

  • 1. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072 © 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 424 RAINFALL-RUNOFF MODELING USING ARTIFICIAL NEURAL NETWORK TECHNIQUE ---------------------------------------------------------------------***--------------------------------------------------------------------- Abstract - Artificial neural networks(ANNs)areamongthe most sophisticated empirical models available and have proven to be especially good in modelling complex systems. Their ability to extract relationsbetweeninputsandoutputsof a process, without the physics being explicitly provided to them, theoretically suits the problem of relating rainfall to runoff well, since it is a highly nonlinear andcomplexproblem. The goal of this investigation was to develop rainfall-runoff models for the river Jhelum catchment that are capable of accurately modelling the relationships between rainfall and runoff in a catchment. It is for this reason that ANN technique was tested as R-R models on a data set from the upper Jhelum catchment in Jammu and Kashmir, India. Two types of ANN models viz. Back Propagation networks (BPN) and Radial Basis function (RBF) were developed and tested for this data and later their performance was checked by different statistical parameters like coefficient of determination R2 and root mean squared error (RMSE). Key Words: Back Propagation network, Radial Basis function network, Modeling, Artificial neural network. 1. INTRODUCTION Hydrologic engineering design and management purposes require information about runoff from a hydrologic catchment. In order to predict this information, the transformation of rainfall on a catchment to runoff from it must be modeled. One approach to this modeling issue is to use empirical Rainfall-Runoff (R-R) models. Empirical models simulate catchment behaviour by parameterization of the relations that the model extracts from sample input and output data. Artificial Neural Networks (ANNs) are models that use dense interconnection of simple computational elements, known as neurons, in combination with so-called training algorithms to make their structure (and therefore their response) adapt to information that is presented to them. ANNs have analogies with biological neural networks, such as nervous systems. ANNs are among the most sophisticated empirical models available and have proven to be especially good in modeling complex systems. Their ability to extract relations between inputsandoutputs of a process, without the physics being explicitlyprovided to them, theoretically suits the problem of relating rainfall to runoff well, since it is a highly nonlinear and complex problem. The goal of this investigation was to prove that ANN models are capable of accurately modeling the relationships between rainfall and runoff in a catchment.An existing software tool in the Matlab environment was selected for design and testing of ANNs on the data set. A special algorithm (the back propagation algorithm) was programmed and incorporated in this tool. This algorithm was expected to ease the trial-and-error efforts for finding an optimal network structure. The ANN type that was used in this investigation is the so-called static multilayer feed forward network. The main conclusion that can be drawn from this investigation is that ANNs are indeed capable of modeling R-R relationships. In the present study Multiple Linear Regression technique was employed on the normalized data using MS Excel. The analysis of variance was done and R2, root mean squared error (RMSE) were computed. The MLR model was validated by plotting the predicted discharge v/s actual discharge curve for years 2010-2013 (about 20% data). 2. STUDY AREA The present study was carried out in the upper Jhelum catchment. The study area spatially lies between 33°21′54″ N to 34° 27′ 52″ N latitude and 74° 24′ 08″ E to 75° 35′ 36″ E longitude with a total area of 8600.78 sq.kms (Figure.1). It covers almost all the physiographic divisions of the Kashmir Valley and is drained by the most important tributaries of river Jhelum. Srinagar city which is the largest urban centre in the valley is settled on both the sides of Jhelum River and is experiencing a fast spatial growth. Physical features of contrasting nature can be observed in the study area that ranges from fertile valley floor to snow-clad mountains and from glacial barren lands to lush green forests. Fig -1: Location map of study area Lateef Ahmad Dar Dept of Civil Engineering, National Institute of Technology Srinagar, J&K, India.
  • 2. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072 © 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 425 3. DATA The discharge data at Padshahibagh gauging station from 1991-2013 was obtained from the irrigation and flood control department, Kashmir and the precipitationdata was procured from the Indian meteorological department(IMD) and National climate data centre (NCDC). The data sets for the years 2001-2009 were used for development/calibrating/training the models and these models were validated for various data sets achieved for 2010-2013. 4. ARTIFICIAL NEURAL NETWORK (ANN) Artificial Neural Networks (ANNs) are networks of simple computational elements that are able to adapt to an information environment. This adaptation is realised by adjustment of the internal network connections through applying a certain algorithm. Thus, ANNsareabletouncover and approximate relationships thatarecontainedinthedata that is presented to the network. ANN applications are becoming more and more popular since the resurgence of these techniques in the last part of the1980’s.Sincetheearly 1990’s, ANNs have been successfully used in hydrology related areas, one of which is Rainfall-Runoff (R-R) modelling [after Govindaraju, 2000]. The application of ANNs as an alternative modelling tool in this field, however, is still in its nascent stages. The reason for modelling the relation between precipitationona catchmentandthe runoff from it is that runoff information is needed for hydrologic engineeringdesignandmanagementpurposes[Govindaraju, 2000]. However, as Tokar and Johnson [1999] state, the relationship between rainfall and runoff is one of the most complex hydrologic phenomena to comprehend. This is due to the tremendous spatial and temporal variability of watershed characteristicsandprecipitationpatterns,and the number of variables involvedinthemodellingofthe physical processes. The network is able to intelligently change its internal parameters, so that the target output signal is approximated. This way the relationshipsbetweentheinput and output variable are parameterised in the model structure and the ANN can make an output prediction based on new input. ANNs have proven to be especially good in modelling complex and non-linear systems.Otherimportant merits of these techniques aretheshortdevelopmenttimeof ANN models, their flexibility and the fact that no great expertise in a certain field is needed in order to be able to apply ANN techniques in this field. The present study is under taken develop rainfall-runoff model in river Jhelum. Artificial Neural Network Techniqueswill beusedtodevelop the rainfall runoff models, to predict the runoffdischargesat Padshahi Bagh station. A predictive analysis is used to determine the predictors which influence the runoff. After the model development the runoff at the Padshahi-Bagh station could then be predicted. Neural Network Tool Box of MATLAB was used to develop Artificial Neural Network Models for Rainfall-RunoffmodelinginRiverJhelum.Various types of neural networks Viz. BPN and RBF were developed. The BPN was optimized for the number of neurons in the hidden layer by changing the number of neurons in the hidden layer. AIC and BIC criteria was employed on various BPN models which led to the selection of two BPN networks with 6 and 10 neurons in the hidden layer. These networks are represented as BPN 6N and BPN 10N in this study respectively. The predicted vs. actual discharges were developed curves were drawn for all the neural network models and there by models werevalidatedforabout20%of the data. Various statistical indices like R2 and RMSE were computed for comparing these models. Based on these statistical indices, the artificial neural networksprovedto be better than MLR. Among various ANN models, RBF with RMSE=0.046 and R2=0.937 emerged to be the best suited model for the prediction. The models developed were then used to developed two individual hydrographs and all the models predicted flood hydrograph to a good extent butRBF networks with RMSE=0.016 and R2=0.976 again proved to be quite impressive as per the overall performance . 5. RESULTS AND DISCUSSIONS The number of neurons in the hidden layer is a very complicated task in finalizing the network architecture.This can be done by trial and error analysis. We have to finalize the number of hidden layers and the number of neurons in the hidden layers. The hidden layers in the network were fixed to one. Hence we start with one neuron in the hidden layer and increase it every time after training the network. The observed Vs predicted runoffs for various number of neurons in the hidden layer is shown in figure 6.10 to 6.13. Results of BPN network with 6 neurons in the hidden layer and BPN network with 10 neurons in the hidden layer are shown in Figure 4 and Table 1.After carrying out regression and validating the data the value of R2 and RMSE for different parameters werecalculatedasshownintable1and table 2: Fig -2: Dialogue box showing the training performance of RBF network.
  • 3. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072 © 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 426 Fig -3: Dialogue box showing training performance of BPN network. Fig -4: Observed vs. predicted discharge, P(t-1) to P(t-5) for BPN network. Table -1: Goodness of fit for the effect of no. of previous day input rainfall parameters. Fig -5: Observed vs. predicted discharge, P(t-1) to P(t-5) for RBF network. Table -2: Statistical indices of RBF model for various inputs. NETWORK INPUTS RMSE R-SQUARE RBF P(t-1) 0.097 0.912 P(t-1)…P(t- 5) 0.046 0.937 The statistical analysis shows that the performance of this network increases as the number rainfall inputs increase from one to five i.e. from p(t-1) to p(t-1)....p(t-5). 3. CONCLUSIONS From the values of R2 and RMSE it was observed that radial basis function networks (RBF) were able to predict the runoff more accurately than Back propagation networks (BPN). BPN network performed better when thenumbersof neurons in the hidden layer were increased upto 10. On increasing the number of neurons further, the network showed no considerable improvement in performance. The radial function model (RBF) gave better resultscomparedto BPN networks with RMSE = 0.046 and was able to predict the stream at the Padshahi-Bagh station more accurately than the other networks. REFERENCES [1] Amari, S., Murata, N., Muller, K. R., Finke, M., and Yang, H.H. (1997). Asymptotic statistical theory of overtraining and cross-validation.IEEETransactionsonNeural Networks, 8(5): p 985-996. [2]Champion, H. G. and Seth, S. K. (1968): A Revised Survey of the Forest Types of India. ManagerofPublications,Govt.of India, New Delhi, pp. 404 NETWORK INPUTS RMSE R-SQUARE Back propagation network 6 neurons. P(t-1) 0.521 0.776 P(t- 1)…P(t-5) 0.245 0.856 Back propagation network 10 neurons. P(t-1) 0.342 0.814 P(t- 1)…P(t-5) 0.132 0.891
  • 4. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 04 Issue: 11 | Nov -2017 www.irjet.net p-ISSN: 2395-0072 © 2017, IRJET | Impact Factor value: 6.171 | ISO 9001:2008 Certified Journal | Page 427 [3]Dibike, Y. B. Solomatine, D.P.2000“Riverflowforecasting using artificial neural networks” Physics and Chemistry of the Earth (B), Vol. 26, No. 1, pp. 1-7, Elsevier Science B.V. [4]Fahlman, Scott E. Lebiere, Christian 1991 “The Cascade- Correlation Learning Architecture” School of Computer Science, Carnegie Mellon University [5]Govindaraju, Rao S. 2000 “Artificial neural networks in hydrology I: preliminary concepts” Journal of Hydrologic Engineering, Vol. 5, No. 2, pp. 115-123, ASCE. [6]Govindaraju, Rao S. 2000 “Artificial neural networks in hydrology II: hydrologic applications” Journal of Hydrologic Engineering, Vol. 5, No. 2, pp. 124-137, ASCE. [7]Halff, A. H. Halff, H. M. Azmoodeh, M. 1993 “Predicting from rainfall using neural networks” Proceedings of Engineering Hydrology, pp. 760-765, ASCE. [8]Krajewski, W. F.Cuykendal, R. R. 1992 “Rainfall forecasting in space and time using a neural network” Journal of Hydrology, Vol. 137, pp. 1-37,ElsevierScience B.V. [9]Meher-Homji, V. M. (1971): The Climate of Srinagar and its Variability. Geog. Rev. Ind., 33, (1): 1-14. [10] Mehnaza Akhter, Ahanger Manzoor Ahmad (2017) Climate Modeling of Jhelum River Basin - A Comparative Study. Environ Pollut Climate Change 1: 110. [11] Mehnaza Akhter (2017) Application of ANN for the Hydrological Modeling. International Journal forResearchin Applied Science & Engineering Technology (IJRASET), Volume 5 Issue VII, July 2017 [12]Sridhar, S.P.(1996). Synthesis of artificial neural networks using genetic algorithms. thesis submitted to Indian institute of technology, New Delhi, India. [13]Tokar, A. Sezin Johnson, Peggy A. 1999 “Rainfall-runoff modelling using artificial neural networks” Journal of Hydrologic Engineering, Vol. 4, No. 3, pp. 232-239, ASCE.