Yu Luo , Changchun Xu , Zhiyi Li , Lin Li , Qian Wang , Qiyue Zhang
{"title":"过去20年,亚洲季风对西风带的协同增强加剧了中亚干旱地区的干旱趋势","authors":"Yu Luo , Changchun Xu , Zhiyi Li , Lin Li , Qian Wang , Qiyue Zhang","doi":"10.1016/j.gr.2025.08.021","DOIUrl":null,"url":null,"abstract":"<div><div>As global warming intensifies, understanding the interactions between the westerlies and Asian monsoons becomes increasingly crucial for predicting regional climate change and managing water resources effectively. However, current knowledge regarding how these atmospheric systems influence dry-wet climate change (DWCC) in Arid Central Asia (ACA) remains insufficient. This study examines the long-term trends in DWCC and evaluates the individual and combined impacts of the westerlies and Asian monsoons on ACA from 1940 to 2022, using the Standardized Precipitation Evapotranspiration Index (SPEI) and atmospheric circulation data. Results indicate that the summer climate in ACA has generally become slightly drier over the past 80 years, with a notable increased in aridity beginning in the 1990s. Spatially, ACA exhibits contrasting dry-wet trends from the southeast to the northwest, with drier areas becoming drier and wetter areas becoming wetter. The influence of Asian monsoons on DWCC in Northern Xinjiang (NX), the Tianshan Mountain area (TM) and the Central Desert (CD) surpasses that of the westerlies. Over the past two decades, as the westerlies weakened, the correlation between the summer SPEI and both the East Asian Monsoon Index (EMI) and South Asian Monsoon Index (SMI) increased, suggesting a growing influence of monsoonal systems. Specifically, the East Asian monsoon (above 700 hPa) and South Asian monsoon (below 700 hPa) demonstrate enhanced effects. The interactive effects between the westerlies and Asian monsoons on DWCC are more pronounced than the influence of either system alone or in combination with a third. Particularly under conditions of weak (strong) westerlies and strong (weak) monsoons, the climate in ACA tends to become drier (wetter). Overall, the increasing synergy between the westerlies to monsoons has accelerated the aridification process in ACA over the past two decades.</div></div>","PeriodicalId":12761,"journal":{"name":"Gondwana Research","volume":"149 ","pages":"Pages 337-350"},"PeriodicalIF":7.2000,"publicationDate":"2025-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Synergistic enhancement of Asian monsoons to westerlies intensifies the drying trend of arid Central Asia over the last 20 years\",\"authors\":\"Yu Luo , Changchun Xu , Zhiyi Li , Lin Li , Qian Wang , Qiyue Zhang\",\"doi\":\"10.1016/j.gr.2025.08.021\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>As global warming intensifies, understanding the interactions between the westerlies and Asian monsoons becomes increasingly crucial for predicting regional climate change and managing water resources effectively. However, current knowledge regarding how these atmospheric systems influence dry-wet climate change (DWCC) in Arid Central Asia (ACA) remains insufficient. This study examines the long-term trends in DWCC and evaluates the individual and combined impacts of the westerlies and Asian monsoons on ACA from 1940 to 2022, using the Standardized Precipitation Evapotranspiration Index (SPEI) and atmospheric circulation data. Results indicate that the summer climate in ACA has generally become slightly drier over the past 80 years, with a notable increased in aridity beginning in the 1990s. Spatially, ACA exhibits contrasting dry-wet trends from the southeast to the northwest, with drier areas becoming drier and wetter areas becoming wetter. The influence of Asian monsoons on DWCC in Northern Xinjiang (NX), the Tianshan Mountain area (TM) and the Central Desert (CD) surpasses that of the westerlies. Over the past two decades, as the westerlies weakened, the correlation between the summer SPEI and both the East Asian Monsoon Index (EMI) and South Asian Monsoon Index (SMI) increased, suggesting a growing influence of monsoonal systems. Specifically, the East Asian monsoon (above 700 hPa) and South Asian monsoon (below 700 hPa) demonstrate enhanced effects. The interactive effects between the westerlies and Asian monsoons on DWCC are more pronounced than the influence of either system alone or in combination with a third. Particularly under conditions of weak (strong) westerlies and strong (weak) monsoons, the climate in ACA tends to become drier (wetter). Overall, the increasing synergy between the westerlies to monsoons has accelerated the aridification process in ACA over the past two decades.</div></div>\",\"PeriodicalId\":12761,\"journal\":{\"name\":\"Gondwana Research\",\"volume\":\"149 \",\"pages\":\"Pages 337-350\"},\"PeriodicalIF\":7.2000,\"publicationDate\":\"2025-09-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Gondwana Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1342937X25002862\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Gondwana Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1342937X25002862","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Synergistic enhancement of Asian monsoons to westerlies intensifies the drying trend of arid Central Asia over the last 20 years
As global warming intensifies, understanding the interactions between the westerlies and Asian monsoons becomes increasingly crucial for predicting regional climate change and managing water resources effectively. However, current knowledge regarding how these atmospheric systems influence dry-wet climate change (DWCC) in Arid Central Asia (ACA) remains insufficient. This study examines the long-term trends in DWCC and evaluates the individual and combined impacts of the westerlies and Asian monsoons on ACA from 1940 to 2022, using the Standardized Precipitation Evapotranspiration Index (SPEI) and atmospheric circulation data. Results indicate that the summer climate in ACA has generally become slightly drier over the past 80 years, with a notable increased in aridity beginning in the 1990s. Spatially, ACA exhibits contrasting dry-wet trends from the southeast to the northwest, with drier areas becoming drier and wetter areas becoming wetter. The influence of Asian monsoons on DWCC in Northern Xinjiang (NX), the Tianshan Mountain area (TM) and the Central Desert (CD) surpasses that of the westerlies. Over the past two decades, as the westerlies weakened, the correlation between the summer SPEI and both the East Asian Monsoon Index (EMI) and South Asian Monsoon Index (SMI) increased, suggesting a growing influence of monsoonal systems. Specifically, the East Asian monsoon (above 700 hPa) and South Asian monsoon (below 700 hPa) demonstrate enhanced effects. The interactive effects between the westerlies and Asian monsoons on DWCC are more pronounced than the influence of either system alone or in combination with a third. Particularly under conditions of weak (strong) westerlies and strong (weak) monsoons, the climate in ACA tends to become drier (wetter). Overall, the increasing synergy between the westerlies to monsoons has accelerated the aridification process in ACA over the past two decades.
期刊介绍:
Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.