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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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 |
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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 |
_version_ |
1810464240027303936 |