Trends and Spatiotemporal Patterns of the Meteorological Drought in the Ili River Valley from 1961 to 2023: An SPEI-Based Study
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| Pubblicato in: | Atmosphere vol. 16, no. 1 (2025), p. 43 |
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| Accesso online: | Citation/Abstract Full Text + Graphics Full Text - PDF |
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| 100 | 1 | |a Su, Hang |u College of Resources and Environment, Yili Normal University, Yili 835000, China; <email>220801080@ylnu.edu.cn</email> (S.H.); <email>nejatkasim@126.com</email> (N.K.); <email>20063@ylnu.edu.cn</email> (Z.Z.) | |
| 245 | 1 | |a Trends and Spatiotemporal Patterns of the Meteorological Drought in the Ili River Valley from 1961 to 2023: An SPEI-Based Study | |
| 260 | |b MDPI AG |c 2025 | ||
| 513 | |a Journal Article | ||
| 520 | 3 | |a Drought presents significant challenges in arid regions, influencing local climate and environmental dynamics. While the large-scale climatic phenomena in Xinjiang, northwest China, are well-documented, the finer-scale climatic variability in subregions such as the Ili River Valley (IRV) remains insufficiently studied. This knowledge gap impedes effective regional planning and environmental management in this ecologically sensitive area. In this study, we analyze the spatiotemporal evolution of drought in the IRV from 1961 to 2023, using data from ten meteorological stations. The SPEI drought index, along with Sen’s trend analysis, the Mann–Kendall test, the cumulative departure method, and wavelet analysis, were employed to assess drought patterns. Results show a significant drying trend in the IRV, starting in 1995, with frequent drought events from 2018 onwards, and no notable transition year observed from wet to dry conditions. The overall drought rate was −0.09 per decade, indicating milder drought severity in the IRV compared to broader Xinjiang. Seasonally, the IRV experiences drier summers and wetter winters compared to regional averages, with negligible changes in autumn and milder drought conditions in spring. Abrupt changes in the drying seasons occurred later in the IRV than in Xinjiang, with delays of 21 years for summer, and over 17 and 35 years for spring and autumn, respectively, indicating a lagged response. Spatially, the western plains are more prone to aridification than the central and eastern mountainous regions. The study also reveals significant differences in drought cycles, which are longer than those in Xinjiang, with distinct wet–dry phases observed across multiple time scales and seasons, emphasizing the complexity of drought variability in the IRV. In conclusion, the valley exhibits unique drought characteristics, including milder intensity, pronounced seasonal variation, spatial heterogeneity, and notable resilience to climate change. These findings underscore the need for region-specific drought management strategies, as broader approaches may not be effective at the subregional scale. | |
| 651 | 4 | |a North America | |
| 651 | 4 | |a Africa | |
| 651 | 4 | |a Tien Shan Mountains | |
| 651 | 4 | |a China | |
| 651 | 4 | |a Asia | |
| 653 | |a Autumn | ||
| 653 | |a Climate variability | ||
| 653 | |a Trend analysis | ||
| 653 | |a Environmental management | ||
| 653 | |a Spatiotemporal data | ||
| 653 | |a Drought | ||
| 653 | |a Rivers | ||
| 653 | |a Drying | ||
| 653 | |a Regional planning | ||
| 653 | |a Seasonal variations | ||
| 653 | |a Radiation | ||
| 653 | |a Climate change | ||
| 653 | |a Wavelet analysis | ||
| 653 | |a Heterogeneity | ||
| 653 | |a Variability | ||
| 653 | |a Mountain regions | ||
| 653 | |a Precipitation | ||
| 653 | |a Weather stations | ||
| 653 | |a Regions | ||
| 653 | |a Summer | ||
| 653 | |a Global warming | ||
| 653 | |a Spring | ||
| 653 | |a Arid regions | ||
| 653 | |a River valleys | ||
| 653 | |a Drought index | ||
| 653 | |a Drought patterns | ||
| 653 | |a Humidity | ||
| 653 | |a Drought characteristics | ||
| 653 | |a Seasonal variation | ||
| 653 | |a Trends | ||
| 653 | |a Arid zones | ||
| 653 | |a Biodiversity | ||
| 653 | |a Mountainous areas | ||
| 653 | |a Drought conditions | ||
| 653 | |a Time series | ||
| 653 | |a Valleys | ||
| 653 | |a Patchiness | ||
| 653 | |a Spring (season) | ||
| 653 | |a Temperature | ||
| 653 | |a Water resources | ||
| 653 | |a Spatial heterogeneity | ||
| 653 | |a Local climates | ||
| 700 | 1 | |a Alim Abbas |u College of Resources and Environment, Xinjiang Agriculture University, Urumqi 830052, China; <email>alimabbas@xjau.edu.cn</email> | |
| 700 | 1 | |a Imin, Bilal |u College of Resources and Environment, Yili Normal University, Yili 835000, China; <email>220801080@ylnu.edu.cn</email> (S.H.); <email>nejatkasim@126.com</email> (N.K.); <email>20063@ylnu.edu.cn</email> (Z.Z.); Institute of Ecology and Environment, Yili Normal University, Yili 835000, China | |
| 700 | 1 | |a Kasim, Nijat |u College of Resources and Environment, Yili Normal University, Yili 835000, China; <email>220801080@ylnu.edu.cn</email> (S.H.); <email>nejatkasim@126.com</email> (N.K.); <email>20063@ylnu.edu.cn</email> (Z.Z.); Institute of Ecology and Environment, Yili Normal University, Yili 835000, China | |
| 700 | 1 | |a Zunun, Zinhar |u College of Resources and Environment, Yili Normal University, Yili 835000, China; <email>220801080@ylnu.edu.cn</email> (S.H.); <email>nejatkasim@126.com</email> (N.K.); <email>20063@ylnu.edu.cn</email> (Z.Z.); Institute of Ecology and Environment, Yili Normal University, Yili 835000, China | |
| 773 | 0 | |t Atmosphere |g vol. 16, no. 1 (2025), p. 43 | |
| 786 | 0 | |d ProQuest |t Publicly Available Content Database | |
| 856 | 4 | 1 | |3 Citation/Abstract |u https://www.proquest.com/docview/3159425818/abstract/embedded/ZKJTFFSVAI7CB62C?source=fedsrch |
| 856 | 4 | 0 | |3 Full Text + Graphics |u https://www.proquest.com/docview/3159425818/fulltextwithgraphics/embedded/ZKJTFFSVAI7CB62C?source=fedsrch |
| 856 | 4 | 0 | |3 Full Text - PDF |u https://www.proquest.com/docview/3159425818/fulltextPDF/embedded/ZKJTFFSVAI7CB62C?source=fedsrch |