Evidence map›Paper›PMID 40359423›Full record

ArticlePloS one2025

Analysis of growing season drought characteristics and driving factors for vegetation in the Santun River Irrigation Area in Xinjiang.

Yuxin Wei, Hongfei Tao, Yan Xu, Mahemujiang Aihemaiti, Chunlei Lu, Youwei Jiang, Qiao Li

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Article in PloS one, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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1 · What the graph read from it

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4 · The record

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5 · Who and what money

Authors and funding

7 authors.

Yuxin WeiCollege of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi, China.
Hongfei TaoCollege of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi, China.
Yan XuXinjiang Cold and Arid Regions Water Resources and Ecological Water Conservancy Engineering Research Center (Academician Expert Workstation), Urumqi, China.
Mahemujiang AihemaitiCollege of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi, China.
Chunlei LuChangji Water Conservancy Management Station (Santun River Basin Management Office), Changji, China.
Youwei JiangCollege of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi, China.
Qiao LiCollege of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi, China.ORCID 0000-0002-1514-8572

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Global warming is exacerbating the occurrence of droughts, which have a significant impact on society. Drought is one of the main factors limiting the development of the Santun River Irrigation Area in Xinjiang. Clarifying the driving mechanism and spatial and temporal evolution characteristics of drought in this irrigation area is crucial for ensuring the sustainable development of agriculture. In this paper, the temperature vegetation drought index (TVDI) is used as a drought indicator to analyze the spatial and temporal evolution characteristics of drought in the Santun River Irrigation Area in Xinjiang, as well as to reveal the factors influencing drought using a Geoprobe model. The results show that the mean value of the TVDI in the Xinjiang Santun River Irrigation Area during 19 years was 0. 738, categorizing it as medium drought. During this period, there was an increasing trend of drought in spring and autumn and a decreasing trend of drought in summer. The drought in the irrigation district had strong spatial heterogeneity, and overall, the drought was stronger in the northern part of the region than in the southern part of the region. Over the past 19 years, the light drought areas in the irrigation district shifted to the medium and severe drought classes at a rate of 114.9 km2·10a-1. The combined effect of elevation and temperature had the strongest explanatory power for drought occurrence in the irrigated area, with a q-value of 0.869. The results of this study provide a theoretical basis for drought risk assessment and water resource planning in arid regions, as well as a reference for drought monitoring studies in similar regions.

Indexed as

Agricultural IrrigationDroughtsRiversSeasonsChinaTemperature

Identifiers

PMID40359423
PMCPMC12074591

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.