Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions
The evaluation of the meteorological drought is fundamental for the management of the water resource. One of the most used indices to evaluate the drought is the standardized precipitation index (SPI) due to its practicality and evaluation in a variety of time scales, however, this uses precipitatio...
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MDPI AG
2022-01-01
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Online Access: | https://www.mdpi.com/2073-4433/13/2/236 |
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author | Luis José Cerpa Reyes Humberto Ávila Rangel Luis Carlos Sandoval Herazo |
author_facet | Luis José Cerpa Reyes Humberto Ávila Rangel Luis Carlos Sandoval Herazo |
author_sort | Luis José Cerpa Reyes |
collection | DOAJ |
description | The evaluation of the meteorological drought is fundamental for the management of the water resource. One of the most used indices to evaluate the drought is the standardized precipitation index (SPI) due to its practicality and evaluation in a variety of time scales, however, this uses precipitation as the only variable, depending on the deviations in the precipitation values. This is important when evaluating the SPI, because in some ecosystems close to the equatorial zone, there are very warm periods with low rainfall, in which a large proportion of the data collected by the meteorological stations corresponds to zero. In this research, the SPI was calculated in the Pechelín basin located in Colombia, in which there is zero precipitation in a large proportion of the data, registering zero precipitation in the month of January and February in 67% and 70% respectively. As a result, the SPI values increased to “wet” ranges, only when the amount of data with zero precipitation exceeded half of the total data; this means that the SPI determines wrong values when it is calculated with zero-precipitation data in large proportions. Based on this finding, this study aims to modify the index by typing the distribution (using a correction factor K), finally correcting the SPI values, this correction was called SPI-C. The results indicate that the SPI-C improved the identification of drought, obtaining corresponding values that better represent the high frequency of zero precipitation existing in the study area. |
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issn | 2073-4433 |
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last_indexed | 2024-03-09T22:38:57Z |
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spelling | doaj.art-ae080ed65e8148f182d32fe21b70b5792023-11-23T18:44:22ZengMDPI AGAtmosphere2073-44332022-01-0113223610.3390/atmos13020236Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation ConditionsLuis José Cerpa Reyes0Humberto Ávila Rangel1Luis Carlos Sandoval Herazo2Department of Civil Engineering, Faculty of Engineering, Universidad de Sucre, Sincelejo 700001, ColombiaDepartment of Civil Engineering, Faculty of Engineering, Universidad del Norte, Barranquilla 080001, ColombiaWetlands and Environmental Sustainability Laboratory, Division of Graduate Studies and Research, Tecnológico Nacional de México/Instituto Tecnológico de Misantla, Km 1.8 Carretera a Loma del Cojolite, Misantla 93821, MexicoThe evaluation of the meteorological drought is fundamental for the management of the water resource. One of the most used indices to evaluate the drought is the standardized precipitation index (SPI) due to its practicality and evaluation in a variety of time scales, however, this uses precipitation as the only variable, depending on the deviations in the precipitation values. This is important when evaluating the SPI, because in some ecosystems close to the equatorial zone, there are very warm periods with low rainfall, in which a large proportion of the data collected by the meteorological stations corresponds to zero. In this research, the SPI was calculated in the Pechelín basin located in Colombia, in which there is zero precipitation in a large proportion of the data, registering zero precipitation in the month of January and February in 67% and 70% respectively. As a result, the SPI values increased to “wet” ranges, only when the amount of data with zero precipitation exceeded half of the total data; this means that the SPI determines wrong values when it is calculated with zero-precipitation data in large proportions. Based on this finding, this study aims to modify the index by typing the distribution (using a correction factor K), finally correcting the SPI values, this correction was called SPI-C. The results indicate that the SPI-C improved the identification of drought, obtaining corresponding values that better represent the high frequency of zero precipitation existing in the study area.https://www.mdpi.com/2073-4433/13/2/236SPI settingzero-precipitation periodsmeteorological droughttropical zone |
spellingShingle | Luis José Cerpa Reyes Humberto Ávila Rangel Luis Carlos Sandoval Herazo Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions Atmosphere SPI setting zero-precipitation periods meteorological drought tropical zone |
title | Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions |
title_full | Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions |
title_fullStr | Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions |
title_full_unstemmed | Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions |
title_short | Adjustment of the Standardized Precipitation Index (SPI) for the Evaluation of Drought in the Arroyo Pechelín Basin, Colombia, under Zero Monthly Precipitation Conditions |
title_sort | adjustment of the standardized precipitation index spi for the evaluation of drought in the arroyo pechelin basin colombia under zero monthly precipitation conditions |
topic | SPI setting zero-precipitation periods meteorological drought tropical zone |
url | https://www.mdpi.com/2073-4433/13/2/236 |
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