The Development of Agricultural Drought Monitoring and Drought Limit Water Level Assessments for Plateau Lakes in Central Yunnan Based on MODIS Remote Sensing: A Case Study of Qilu Lake

This study focuses on Qilu Lake to study how to mitigate the impacts of seasonal droughts and provide technical support for drought resistance decision-making in low-latitude plateau lake basins. Using the Standardized Precipitation Index (SPI), the Vegetation Condition Index (VCI), and the Temperature Condition Index (TCI) as bases, in this study, the applicability of the vegetation health index (VHI) within the basin is investigated, and the optimal weight distribution between the Vegetation Condition Index (VCI) and the Temperature Condition Index (TCI) in the VHI is determined. The VHI is then applied to analyze the correlation between drought frequency and severity within the basin. The results indicate that the method is most effective in assessing agricultural drought in the Qilu Lake Basin when the VCI and TCI are weighted at a 4:6 ratio, optimizing the VHI’s evaluative performance. The drought limit water levels of lakes are further divided into short- and long-term drought limit water levels. The short-term drought limit water level is divided into the drought warning water level and the drought emergency water level. The drought warning water level (corresponding to moderate drought conditions, with a frequency of P = 75%) ranges from 1794.53 m to 1795.11 m, while the drought emergency water level (corresponding to extreme drought conditions, with a frequency of P = 95%) ranges from 1793.94 m to 1794.31 m. These levels are set to meet the emergency water demand during droughts in the basin. The long-term drought limit water levels are calculated by accumulating the water deficits of various sectors within the watershed under different agricultural drought conditions, based on the short-term drought limit water levels. By setting the drought limit water level using this method, as well as considering the original water regulation capacity of the lake resources, when the watershed experiences drought, the scheduling method based on this drought limit water level can better alleviate the water supply pressure on various sectors in the local area.

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Publication Details

Journal
Sustainability
Published
2025-05-19
DOI
https://doi.org/10.3390/su17104662
Primary Topic
Remote Sensing and Land Use
Type
article
Field-Weighted Citation Impact
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article

The Development of Agricultural Drought Monitoring and Drought Limit Water Level Assessments for Plateau Lakes in Central Yunnan Based on MODIS Remote Sensing: A Case Study of Qilu Lake

Kai Gao, Yanchen Zhou, Jie Ou, Jing Chen et al.
Sustainability
Remote Sensing and Land Use
article

The Development of Agricultural Drought Monitoring and Drought Limit Water Level Assessments for Plateau Lakes in Central Yunnan Based on MODIS Remote Sensing: A Case Study of Qilu Lake

Kai Gao, Yanchen Zhou, Jie Ou, Jing Chen, Shixiang Gu, Jinming Chen
article en

Abstract

This study focuses on Qilu Lake to study how to mitigate the impacts of seasonal droughts and provide technical support for drought resistance decision-making in low-latitude plateau lake basins. Using the Standardized Precipitation Index (SPI), the Vegetation Condition Index (VCI), and the Temperature Condition Index (TCI) as bases, in this study, the applicability of the vegetation health index (VHI) within the basin is investigated, and the optimal weight distribution between the Vegetation Condition Index (VCI) and the Temperature Condition Index (TCI) in the VHI is determined. The VHI is then applied to analyze the correlation between drought frequency and severity within the basin. The results indicate that the method is most effective in assessing agricultural drought in the Qilu Lake Basin when the VCI and TCI are weighted at a 4:6 ratio, optimizing the VHI’s evaluative performance. The drought limit water levels of lakes are further divided into short- and long-term drought limit water levels. The short-term drought limit water level is divided into the drought warning water level and the drought emergency water level. The drought warning water level (corresponding to moderate drought conditions, with a frequency of P = 75%) ranges from 1794.53 m to 1795.11 m, while the drought emergency water level (corresponding to extreme drought conditions, with a frequency of P = 95%) ranges from 1793.94 m to 1794.31 m. These levels are set to meet the emergency water demand during droughts in the basin. The long-term drought limit water levels are calculated by accumulating the water deficits of various sectors within the watershed under different agricultural drought conditions, based on the short-term drought limit water levels. By setting the drought limit water level using this method, as well as considering the original water regulation capacity of the lake resources, when the watershed experiences drought, the scheduling method based on this drought limit water level can better alleviate the water supply pressure on various sectors in the local area.

SustainabilityVol. 17(10)
Yunnan Agricultural University (CN), Changjiang Water Resources Commission (CN), Wuhan University (CN), Yunnan Water Conservancy and Hydropower Survey and Design Institute (CN)
Yunnan Normal University
Openalex Percentile: Top 85%
Remote Sensing and Land Use
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