{"title":"北半球中纬度地区平流层北极涡旋与地表气温之间的关系","authors":"Xue Ran, Dingzhu Hu, Yang Zhang, Mei-Chen Liu","doi":"10.1007/s13351-024-3072-7","DOIUrl":null,"url":null,"abstract":"<p>It is known that different relationships exist between the strength and displacement of the stratospheric polar vortex (SPV), and the surface air temperature (SAT) patterns in Eurasia and North America, but the mechanisms behind these relationships remain unclear, especially on an interannual timescale. Based on empirical orthogonal function (EOF) analysis using NCEP reanalysis data over 1958–2018, this study attempts to ascertain the relationship between the SPV intensity and displacement over the Arctic and the SATs in the midlatitudes of the Northern Hemisphere. Our results indicate that a strengthened SPV corresponds to an SAT increase in Eurasia and a decrease in eastern North America and Greenland. When the SPV is shifted towards Eurasia, however, a corresponding SAT increase occurs in both North America and Eurasia, with a larger increase in North America than in Eurasia. Specifically, a strengthened SPV tends to correspond to a positive North Atlantic Oscillation-like circulation in the troposphere with negative geopotential height (GH) anomalies in Greenland and eastern North American continent and positive GH anomalies to the north of 45°N in Eurasia, which corresponds to lower SATs in North America than in Eurasia. However, when the SPV shifted towards Eurasia, it was accompanied by a positive Pacific/North American-like pattern with a deepened Aleutian low, which corresponds to the increasing SATs in North America. These tropospheric circulation changes are related to the response of tropospheric planetary wave activity to the SPV. A strengthened SPV corresponds to the weakening of tropospheric planetary wave-1 waves, which is accompanied by a negative GH in North America but a positive GH in Eurasia. If the SPV shifted towards Eurasia, the tropospheric planetary wave-1 (-2) waves strengthened (weakened), and the combined effects of the planetary wave-1 and wave-2 waves would cause positive GH anomalies in both Eurasia and North America.</p>","PeriodicalId":48796,"journal":{"name":"Journal of Meteorological Research","volume":"2 1","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-03-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Relationship between the Stratospheric Arctic Vortex and Surface Air Temperature in the Midlatitudes of the Northern Hemisphere\",\"authors\":\"Xue Ran, Dingzhu Hu, Yang Zhang, Mei-Chen Liu\",\"doi\":\"10.1007/s13351-024-3072-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>It is known that different relationships exist between the strength and displacement of the stratospheric polar vortex (SPV), and the surface air temperature (SAT) patterns in Eurasia and North America, but the mechanisms behind these relationships remain unclear, especially on an interannual timescale. Based on empirical orthogonal function (EOF) analysis using NCEP reanalysis data over 1958–2018, this study attempts to ascertain the relationship between the SPV intensity and displacement over the Arctic and the SATs in the midlatitudes of the Northern Hemisphere. Our results indicate that a strengthened SPV corresponds to an SAT increase in Eurasia and a decrease in eastern North America and Greenland. When the SPV is shifted towards Eurasia, however, a corresponding SAT increase occurs in both North America and Eurasia, with a larger increase in North America than in Eurasia. Specifically, a strengthened SPV tends to correspond to a positive North Atlantic Oscillation-like circulation in the troposphere with negative geopotential height (GH) anomalies in Greenland and eastern North American continent and positive GH anomalies to the north of 45°N in Eurasia, which corresponds to lower SATs in North America than in Eurasia. However, when the SPV shifted towards Eurasia, it was accompanied by a positive Pacific/North American-like pattern with a deepened Aleutian low, which corresponds to the increasing SATs in North America. These tropospheric circulation changes are related to the response of tropospheric planetary wave activity to the SPV. A strengthened SPV corresponds to the weakening of tropospheric planetary wave-1 waves, which is accompanied by a negative GH in North America but a positive GH in Eurasia. If the SPV shifted towards Eurasia, the tropospheric planetary wave-1 (-2) waves strengthened (weakened), and the combined effects of the planetary wave-1 and wave-2 waves would cause positive GH anomalies in both Eurasia and North America.</p>\",\"PeriodicalId\":48796,\"journal\":{\"name\":\"Journal of Meteorological Research\",\"volume\":\"2 1\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-03-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Meteorological Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1007/s13351-024-3072-7\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"METEOROLOGY & ATMOSPHERIC SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Meteorological Research","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s13351-024-3072-7","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
摘要
众所周知,平流层极地涡旋(SPV)的强度和位移与欧亚大陆和北美洲的地表气温(SAT)模式之间存在不同的关系,但这些关系背后的机制仍不清楚,尤其是在年际时间尺度上。本研究利用 1958-2018 年的 NCEP 再分析数据,基于经验正交函数(EOF)分析,试图确定北极上空 SPV 强度和位移与北半球中纬度地区 SAT 之间的关系。我们的研究结果表明,SPV 的加强对应于欧亚大陆 SAT 的增加和北美东部及格陵兰岛 SAT 的减少。然而,当 SPV 向欧亚大陆移动时,北美和欧亚大陆的 SAT 都会相应增加,但北美的增幅大于欧亚大陆。具体来说,SPV 的增强往往与对流层中类似北大西洋涛动的正向环流相对应,格陵兰岛和北美大陆东部出现负的位势高度(GH)异常,而欧亚大陆北纬 45°以北出现正的位势高度异常,这与北美比欧亚大陆更低的 SAT 相对应。然而,当 SPV 向欧亚大陆移动时,伴随着阿留申低纬度加深的类似太平洋/北美的正模式,这与北美洲 SAT 的增加相对应。这些对流层环流变化与对流层行星波活动对 SPV 的响应有关。SPV 的加强对应于对流层行星波-1 的减弱,这伴随着北美洲负的 GH,而欧亚大陆正的 GH。如果 SPV 向欧亚大陆移动,对流层行星波-1(-2)就会增强(减弱),行星波-1 和行星波-2 的综合效应将导致欧亚大陆和北美洲出现正的 GH 异常。
Relationship between the Stratospheric Arctic Vortex and Surface Air Temperature in the Midlatitudes of the Northern Hemisphere
It is known that different relationships exist between the strength and displacement of the stratospheric polar vortex (SPV), and the surface air temperature (SAT) patterns in Eurasia and North America, but the mechanisms behind these relationships remain unclear, especially on an interannual timescale. Based on empirical orthogonal function (EOF) analysis using NCEP reanalysis data over 1958–2018, this study attempts to ascertain the relationship between the SPV intensity and displacement over the Arctic and the SATs in the midlatitudes of the Northern Hemisphere. Our results indicate that a strengthened SPV corresponds to an SAT increase in Eurasia and a decrease in eastern North America and Greenland. When the SPV is shifted towards Eurasia, however, a corresponding SAT increase occurs in both North America and Eurasia, with a larger increase in North America than in Eurasia. Specifically, a strengthened SPV tends to correspond to a positive North Atlantic Oscillation-like circulation in the troposphere with negative geopotential height (GH) anomalies in Greenland and eastern North American continent and positive GH anomalies to the north of 45°N in Eurasia, which corresponds to lower SATs in North America than in Eurasia. However, when the SPV shifted towards Eurasia, it was accompanied by a positive Pacific/North American-like pattern with a deepened Aleutian low, which corresponds to the increasing SATs in North America. These tropospheric circulation changes are related to the response of tropospheric planetary wave activity to the SPV. A strengthened SPV corresponds to the weakening of tropospheric planetary wave-1 waves, which is accompanied by a negative GH in North America but a positive GH in Eurasia. If the SPV shifted towards Eurasia, the tropospheric planetary wave-1 (-2) waves strengthened (weakened), and the combined effects of the planetary wave-1 and wave-2 waves would cause positive GH anomalies in both Eurasia and North America.
期刊介绍:
Journal of Meteorological Research (previously known as Acta Meteorologica Sinica) publishes the latest achievements and developments in the field of atmospheric sciences. Coverage is broad, including topics such as pure and applied meteorology; climatology and climate change; marine meteorology; atmospheric physics and chemistry; cloud physics and weather modification; numerical weather prediction; data assimilation; atmospheric sounding and remote sensing; atmospheric environment and air pollution; radar and satellite meteorology; agricultural and forest meteorology and more.