Drought forecasting using artificial neural networks and time series of drought indices

Abstract Drought forecasting is a critical component of drought risk management. The paper describes an approach to drought forecasting, which makes use of Artificial Neural Network (ANN) and predicts quantitative values of drought indices—continuous functions of rainfall which measure the degree of...

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Published in:International Journal of Climatology
Main Authors: Morid, Saeid, Smakhtin, Vladimir, Bagherzadeh, K.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2007
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.1498
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spelling crwiley:10.1002/joc.1498 2024-09-15T18:23:57+00:00 Drought forecasting using artificial neural networks and time series of drought indices Morid, Saeid Smakhtin, Vladimir Bagherzadeh, K. 2007 http://dx.doi.org/10.1002/joc.1498 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1498 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1498 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 27, issue 15, page 2103-2111 ISSN 0899-8418 1097-0088 journal-article 2007 crwiley https://doi.org/10.1002/joc.1498 2024-08-30T04:09:52Z Abstract Drought forecasting is a critical component of drought risk management. The paper describes an approach to drought forecasting, which makes use of Artificial Neural Network (ANN) and predicts quantitative values of drought indices—continuous functions of rainfall which measure the degree of dryness of any time period. The indices used are the Effective Drought Index (EDI) and the Standard Precipitation Index (SPI). The forecasts are attempted using different combinations of past rainfall, the above two drought indices in preceding months and climate indices like Southern Oscillation Index (SOI) and North Atlantic Oscillation (NAO) index. A number of different ANN models for both EDI and SPI with the lead times of 1 to 12 months have been tested at several rainfall stations in the Tehran Province of Iran. The best models in both cases have been found to include, among the others, a corresponding drought index value from the same month of the previous year. Both best models have the R 2 values of 0.66‐0.79 for a lead time of 6 months, but it is also shown that the EDI forecasts are superior to those of the SPI for all lead times and at all rainfall stations. The better performance of the EDI model is illustrated by its more accurate prediction of the overall pattern of ‘dry’ and ‘wet’ conditions. The structure of the model inputs (previous rain and drought indices) does not vary with the lead time, which makes the models very convenient for the operational purposes. The final forecasting models can be utilized by drought early warning systems, which are emerging in Iran at present. Copyright © 2007 Royal Meteorological Society Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library International Journal of Climatology 27 15 2103 2111
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Drought forecasting is a critical component of drought risk management. The paper describes an approach to drought forecasting, which makes use of Artificial Neural Network (ANN) and predicts quantitative values of drought indices—continuous functions of rainfall which measure the degree of dryness of any time period. The indices used are the Effective Drought Index (EDI) and the Standard Precipitation Index (SPI). The forecasts are attempted using different combinations of past rainfall, the above two drought indices in preceding months and climate indices like Southern Oscillation Index (SOI) and North Atlantic Oscillation (NAO) index. A number of different ANN models for both EDI and SPI with the lead times of 1 to 12 months have been tested at several rainfall stations in the Tehran Province of Iran. The best models in both cases have been found to include, among the others, a corresponding drought index value from the same month of the previous year. Both best models have the R 2 values of 0.66‐0.79 for a lead time of 6 months, but it is also shown that the EDI forecasts are superior to those of the SPI for all lead times and at all rainfall stations. The better performance of the EDI model is illustrated by its more accurate prediction of the overall pattern of ‘dry’ and ‘wet’ conditions. The structure of the model inputs (previous rain and drought indices) does not vary with the lead time, which makes the models very convenient for the operational purposes. The final forecasting models can be utilized by drought early warning systems, which are emerging in Iran at present. Copyright © 2007 Royal Meteorological Society
format Article in Journal/Newspaper
author Morid, Saeid
Smakhtin, Vladimir
Bagherzadeh, K.
spellingShingle Morid, Saeid
Smakhtin, Vladimir
Bagherzadeh, K.
Drought forecasting using artificial neural networks and time series of drought indices
author_facet Morid, Saeid
Smakhtin, Vladimir
Bagherzadeh, K.
author_sort Morid, Saeid
title Drought forecasting using artificial neural networks and time series of drought indices
title_short Drought forecasting using artificial neural networks and time series of drought indices
title_full Drought forecasting using artificial neural networks and time series of drought indices
title_fullStr Drought forecasting using artificial neural networks and time series of drought indices
title_full_unstemmed Drought forecasting using artificial neural networks and time series of drought indices
title_sort drought forecasting using artificial neural networks and time series of drought indices
publisher Wiley
publishDate 2007
url http://dx.doi.org/10.1002/joc.1498
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1498
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1498
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology
volume 27, issue 15, page 2103-2111
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.1498
container_title International Journal of Climatology
container_volume 27
container_issue 15
container_start_page 2103
op_container_end_page 2111
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