中国四川盆地1月霾污染的年际变化及其与东南印度、热带太平洋和北太平洋海温的关系

IF 2.8 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Yu Luo, Chao Chen, Pengguo Zhao, Changyan Zhou, Jia Liu, Jing Zhang, Yumeng Zhou, Sixian Cen
{"title":"中国四川盆地1月霾污染的年际变化及其与东南印度、热带太平洋和北太平洋海温的关系","authors":"Yu Luo,&nbsp;Chao Chen,&nbsp;Pengguo Zhao,&nbsp;Changyan Zhou,&nbsp;Jia Liu,&nbsp;Jing Zhang,&nbsp;Yumeng Zhou,&nbsp;Sixian Cen","doi":"10.1002/joc.8897","DOIUrl":null,"url":null,"abstract":"<p>Haze pollution occurs in almost every winter month in the Sichuan Basin, with a higher frequency in January. The interannual and decadal variations of January haze are inconsistent with those in the other winter months, showing a noticeable sub-seasonal variability in haze pollution. The findings of this study indicate that the noticeably higher haze days over the Sichuan Basin in January are closely associated with the simultaneous sea surface temperature (SST) warming in the North Pacific Ocean (NPO) and tropical Pacific Ocean (TPO), and with the SST cooling in the southeastern Indian Ocean (SIO). When the SST in the NPO warms in January, the negative phase of the Arctic Oscillation is stimulated through a high-latitude path, the Middle East jet stream weakens, and the Siberian high weakens, and the Aleutian Low intensifies, indicating that cold air activities are restricted and their paths are eastward. This synoptic situation results in weaker cold air over the Sichuan Basin. Meanwhile, the southern branch of the Rossby wave train from the eastern Pacific Ocean propagates along Western Europe to the East Asian coast, leading to high pressure and anticyclonic circulation anomalies over the Sichuan Basin, resulting in reduced precipitation and more haze days in the Sichuan Basin. When the January SST shows warming in the TPO and cooling in the SIO, prominent anticyclonic anomalies strengthen over the Tibetan Plateau and its downstream regions, weakening the southwesterly warm moisture flow. This situation provides unfavourable conditions for precipitation occurrence, thereby facilitating haze pollution over the Sichuan Basin. Consequently, the January SST anomalies in the NPO, TPO and SIO may be associated with the anomalies of local meteorological elements, which restrict the vertical and horizontal dispersion of haze pollution over the Sichuan Basin in January.</p>","PeriodicalId":13779,"journal":{"name":"International Journal of Climatology","volume":"45 10","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2025-05-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.8897","citationCount":"0","resultStr":"{\"title\":\"Interannual Variability of January Haze Pollution in the Sichuan Basin, China and Its Association With the SSTs Over the Southeastern Indian, Tropical Pacific and North Pacific Oceans\",\"authors\":\"Yu Luo,&nbsp;Chao Chen,&nbsp;Pengguo Zhao,&nbsp;Changyan Zhou,&nbsp;Jia Liu,&nbsp;Jing Zhang,&nbsp;Yumeng Zhou,&nbsp;Sixian Cen\",\"doi\":\"10.1002/joc.8897\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Haze pollution occurs in almost every winter month in the Sichuan Basin, with a higher frequency in January. The interannual and decadal variations of January haze are inconsistent with those in the other winter months, showing a noticeable sub-seasonal variability in haze pollution. The findings of this study indicate that the noticeably higher haze days over the Sichuan Basin in January are closely associated with the simultaneous sea surface temperature (SST) warming in the North Pacific Ocean (NPO) and tropical Pacific Ocean (TPO), and with the SST cooling in the southeastern Indian Ocean (SIO). When the SST in the NPO warms in January, the negative phase of the Arctic Oscillation is stimulated through a high-latitude path, the Middle East jet stream weakens, and the Siberian high weakens, and the Aleutian Low intensifies, indicating that cold air activities are restricted and their paths are eastward. This synoptic situation results in weaker cold air over the Sichuan Basin. Meanwhile, the southern branch of the Rossby wave train from the eastern Pacific Ocean propagates along Western Europe to the East Asian coast, leading to high pressure and anticyclonic circulation anomalies over the Sichuan Basin, resulting in reduced precipitation and more haze days in the Sichuan Basin. When the January SST shows warming in the TPO and cooling in the SIO, prominent anticyclonic anomalies strengthen over the Tibetan Plateau and its downstream regions, weakening the southwesterly warm moisture flow. This situation provides unfavourable conditions for precipitation occurrence, thereby facilitating haze pollution over the Sichuan Basin. Consequently, the January SST anomalies in the NPO, TPO and SIO may be associated with the anomalies of local meteorological elements, which restrict the vertical and horizontal dispersion of haze pollution over the Sichuan Basin in January.</p>\",\"PeriodicalId\":13779,\"journal\":{\"name\":\"International Journal of Climatology\",\"volume\":\"45 10\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2025-05-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.8897\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"International Journal of Climatology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://rmets.onlinelibrary.wiley.com/doi/10.1002/joc.8897\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"METEOROLOGY & ATMOSPHERIC SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Journal of Climatology","FirstCategoryId":"89","ListUrlMain":"https://rmets.onlinelibrary.wiley.com/doi/10.1002/joc.8897","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0

摘要

四川盆地冬季几乎每个月都会出现雾霾污染,以1月份频率较高。1月雾霾的年际和年代际变化与其他冬季月份不一致,雾霾污染表现出明显的亚季节变化。研究结果表明,四川盆地1月份雾霾日数明显增多与北太平洋(NPO)和热带太平洋(TPO)海温同步变暖以及印度洋东南部海温同步变冷密切相关。当1月NPO海温变暖时,高纬路径刺激北极涛动负相,中东急流减弱,西伯利亚高压减弱,阿留申低压增强,表明冷空气活动受限,路径向东。这种天气情况导致四川盆地上空冷空气减弱。同时,东太平洋的罗斯比波列南支沿西欧向东亚海岸传播,导致四川盆地上空出现高压和反气旋环流异常,导致四川盆地降水减少,霾日数增多。这种情况为降水的发生提供了不利条件,从而助长了四川盆地的雾霾污染。因此,NPO、TPO和SIO的1月海温异常可能与局地气象要素异常有关,局地气象要素异常限制了四川盆地1月雾霾污染的垂直和水平扩散。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Interannual Variability of January Haze Pollution in the Sichuan Basin, China and Its Association With the SSTs Over the Southeastern Indian, Tropical Pacific and North Pacific Oceans

Interannual Variability of January Haze Pollution in the Sichuan Basin, China and Its Association With the SSTs Over the Southeastern Indian, Tropical Pacific and North Pacific Oceans

Interannual Variability of January Haze Pollution in the Sichuan Basin, China and Its Association With the SSTs Over the Southeastern Indian, Tropical Pacific and North Pacific Oceans

Interannual Variability of January Haze Pollution in the Sichuan Basin, China and Its Association With the SSTs Over the Southeastern Indian, Tropical Pacific and North Pacific Oceans

Interannual Variability of January Haze Pollution in the Sichuan Basin, China and Its Association With the SSTs Over the Southeastern Indian, Tropical Pacific and North Pacific Oceans

Haze pollution occurs in almost every winter month in the Sichuan Basin, with a higher frequency in January. The interannual and decadal variations of January haze are inconsistent with those in the other winter months, showing a noticeable sub-seasonal variability in haze pollution. The findings of this study indicate that the noticeably higher haze days over the Sichuan Basin in January are closely associated with the simultaneous sea surface temperature (SST) warming in the North Pacific Ocean (NPO) and tropical Pacific Ocean (TPO), and with the SST cooling in the southeastern Indian Ocean (SIO). When the SST in the NPO warms in January, the negative phase of the Arctic Oscillation is stimulated through a high-latitude path, the Middle East jet stream weakens, and the Siberian high weakens, and the Aleutian Low intensifies, indicating that cold air activities are restricted and their paths are eastward. This synoptic situation results in weaker cold air over the Sichuan Basin. Meanwhile, the southern branch of the Rossby wave train from the eastern Pacific Ocean propagates along Western Europe to the East Asian coast, leading to high pressure and anticyclonic circulation anomalies over the Sichuan Basin, resulting in reduced precipitation and more haze days in the Sichuan Basin. When the January SST shows warming in the TPO and cooling in the SIO, prominent anticyclonic anomalies strengthen over the Tibetan Plateau and its downstream regions, weakening the southwesterly warm moisture flow. This situation provides unfavourable conditions for precipitation occurrence, thereby facilitating haze pollution over the Sichuan Basin. Consequently, the January SST anomalies in the NPO, TPO and SIO may be associated with the anomalies of local meteorological elements, which restrict the vertical and horizontal dispersion of haze pollution over the Sichuan Basin in January.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信