SPI-Based Spatiotemporal Drought over Sri Lanka

Drought is one of the most significant hazards in Sri Lanka. Status of drought in Sri Lanka was assessed using Standardized Precipitation Index (SPI) at 3, 6, and 12 months’ time scales using monthly rainfall (1970 to 2017) data of 54 weather stations. The frequency of drought events was evaluated u...

Full description

Bibliographic Details
Main Authors: N. S. Abeysingha, U. R. L. N. Rajapaksha
Format: Article
Language:English
Published: Hindawi Limited 2020-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2020/9753279
id doaj-6db4a55cd0584f9c86a674a90c85c1da
record_format Article
spelling doaj-6db4a55cd0584f9c86a674a90c85c1da2020-11-25T01:27:03ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172020-01-01202010.1155/2020/97532799753279SPI-Based Spatiotemporal Drought over Sri LankaN. S. Abeysingha0U. R. L. N. Rajapaksha1Department of Agriculture Engineering and Soil Science, Faculty of Agriculture, Rajarata University of Sri Lanka, Anuradhapura, Sri LankaDepartment of Agriculture Engineering and Soil Science, Faculty of Agriculture, Rajarata University of Sri Lanka, Anuradhapura, Sri LankaDrought is one of the most significant hazards in Sri Lanka. Status of drought in Sri Lanka was assessed using Standardized Precipitation Index (SPI) at 3, 6, and 12 months’ time scales using monthly rainfall (1970 to 2017) data of 54 weather stations. The frequency of drought events was evaluated using SPI, and trend of SPI was also detected using the Mann–Kendall (MK) test and Sen’s slope estimator. The result based on SPI identified hydrological years 1975-76, 1982-83, 1986-87, 1988-89, 2000-01, 2001-02, 2013-14, and 2016-17 as drought years for 52, 32, 35, 33, 33, 31, 31, and 31% of tested stations (54), respectively, at annual time scale. Comparison of the SPI at different time scales revealed that more drought events (SPI ≤ −1) occurred during Yala season than Maha cropping season. Considering the Thiessen polygon average rainfall, more frequent drought events occurred in the dry zone (57%) than the wet (49%) and intermediate zone (47%) at the annual time scale. SPI trend results showed greater increase in drought (59% of stations) during Yala seasons as compared to the Maha cropping season (15% of stations) in Sri Lanka.http://dx.doi.org/10.1155/2020/9753279
collection DOAJ
language English
format Article
sources DOAJ
author N. S. Abeysingha
U. R. L. N. Rajapaksha
spellingShingle N. S. Abeysingha
U. R. L. N. Rajapaksha
SPI-Based Spatiotemporal Drought over Sri Lanka
Advances in Meteorology
author_facet N. S. Abeysingha
U. R. L. N. Rajapaksha
author_sort N. S. Abeysingha
title SPI-Based Spatiotemporal Drought over Sri Lanka
title_short SPI-Based Spatiotemporal Drought over Sri Lanka
title_full SPI-Based Spatiotemporal Drought over Sri Lanka
title_fullStr SPI-Based Spatiotemporal Drought over Sri Lanka
title_full_unstemmed SPI-Based Spatiotemporal Drought over Sri Lanka
title_sort spi-based spatiotemporal drought over sri lanka
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2020-01-01
description Drought is one of the most significant hazards in Sri Lanka. Status of drought in Sri Lanka was assessed using Standardized Precipitation Index (SPI) at 3, 6, and 12 months’ time scales using monthly rainfall (1970 to 2017) data of 54 weather stations. The frequency of drought events was evaluated using SPI, and trend of SPI was also detected using the Mann–Kendall (MK) test and Sen’s slope estimator. The result based on SPI identified hydrological years 1975-76, 1982-83, 1986-87, 1988-89, 2000-01, 2001-02, 2013-14, and 2016-17 as drought years for 52, 32, 35, 33, 33, 31, 31, and 31% of tested stations (54), respectively, at annual time scale. Comparison of the SPI at different time scales revealed that more drought events (SPI ≤ −1) occurred during Yala season than Maha cropping season. Considering the Thiessen polygon average rainfall, more frequent drought events occurred in the dry zone (57%) than the wet (49%) and intermediate zone (47%) at the annual time scale. SPI trend results showed greater increase in drought (59% of stations) during Yala seasons as compared to the Maha cropping season (15% of stations) in Sri Lanka.
url http://dx.doi.org/10.1155/2020/9753279
work_keys_str_mv AT nsabeysingha spibasedspatiotemporaldroughtoversrilanka
AT urlnrajapaksha spibasedspatiotemporaldroughtoversrilanka
_version_ 1715767938032599040