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Characteristics and Trends of Meteorological and Hydrological Drought in the Srepok River Basin

Lam Van Nguyen 1, 2, *
Viet Van Luong 3
Quang Nguyen Xuan Chau 1
  1. Institute of Environment and Resources – Vietnam National University Ho Chi Minh City, Vietnam
  2. Vietnam National University of Forestry – Dong Nai Campus, Vietnam
  3. Industrial University of Ho Chi Minh City, Vietnam
Correspondence to: Lam Van Nguyen, Institute of Environment and Resources – Vietnam National University Ho Chi Minh City, Vietnam; Vietnam National University of Forestry – Dong Nai Campus, Vietnam. Email: [email protected].
Volume & Issue: Vol. 10 No. 1 (2026) | Page No.: 1172-1182 | DOI: 10.32508/stdjsee.v10i1.801
Published: 2026-01-09

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This article is published with open access by Viet Nam National University Ho Chi Minh City, Viet Nam. This article is distributed under the terms of the Creative Commons Attribution License (CC-BY 4.0) which permits any use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited. 

Abstract

Srepok is an important river basin in the Central Highlands region. In recent years, droughts have occurred more frequently, threatening the sustainable development of this region. Therefore, studying the characteristics and trends of droughts is extremely necessary to propose appropriate response solutions. In this study, data from 9 rainfall stations and 1 hydrological station during the period of 1982 - 2022 were used to assess the fluctuations of droughts over time scales. The Mann-Kendall non-parametric test method and Sen slope estimation were applied to analyze the trends. The results show that droughts start from August to November every year, about 2.5 times higher than the remaining months. The duration of droughts ranges from 5 to 15 months, with a median of 7 months. The SPI7 index recorded more severe droughts at a very severe level than SPI3 and SPI5, the most severe drought occurring in 1994. The SSI index also fluctuated strongly, especially in 2014 with SSI5 reaching 37.7. The strongest drought intensity was in 2004 and 2015 with SSI5 reaching 1.7. The SPI tended to increase in the dry season and decrease slightly in the rainy season. Although the period 1982 - 2002 had many droughts at a mild and severe level, the very severe drought tended to increase in the later period. The study shows that combining SPI and SSI to assess drought trends is effective, contributing to optimizing short-term and long-term drought response measures.

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