Yan Wang, Micha Ruhl, Jian Cao, Wenxuan Hu, Dongming Zhi, Yong Tang, Jinchao Liu
{"title":"英国温室效应变暖使气候带向极地移动,影响全球变化","authors":"Yan Wang, Micha Ruhl, Jian Cao, Wenxuan Hu, Dongming Zhi, Yong Tang, Jinchao Liu","doi":"10.1029/2024JD043219","DOIUrl":null,"url":null,"abstract":"<p>Atmospheric convection is predicted to change in response to anthropogenic global warming, leading to a poleward expansion of the Hadley cells and associated arid climate belts. The magnitude of possible latitudinal change in the position of climate belts is, however, poorly understood. Here, we address this issue based on a case study of the early Toarcian (late Early Jurassic) Oceanic Anoxic Event (T-OAE, ∼183 Ma), one of the most significant global change events of the Phanerozoic, characterized by elevated humidity and major disturbances to terrestrial ecosystems on land. We present new leaf-wax <i>n</i>-alkanes δ<sup>13</sup>C data from the high-paleo-latitude Junggar Basin (northwest China) spanning the T-OAE and develop a time–space framework of plant-fractionation change, from low- to high-paleolatitudes across this time interval. We show that significant latitudinal changes in humidity occurred across the T-OAE (∼10°), likely because of a significant northward expansion of the low-latitude arid belts to mid-paleo-latitudes, and by inference a latitudinal expansion of the Hadley cells. This has important implications for the anthropogenic global warming and its effects on climate belts.</p>","PeriodicalId":15986,"journal":{"name":"Journal of Geophysical Research: Atmospheres","volume":"130 12","pages":""},"PeriodicalIF":3.8000,"publicationDate":"2025-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Toarcian Greenhouse Warming Shifted Climate Belts Poleward With Global Change Implications\",\"authors\":\"Yan Wang, Micha Ruhl, Jian Cao, Wenxuan Hu, Dongming Zhi, Yong Tang, Jinchao Liu\",\"doi\":\"10.1029/2024JD043219\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Atmospheric convection is predicted to change in response to anthropogenic global warming, leading to a poleward expansion of the Hadley cells and associated arid climate belts. The magnitude of possible latitudinal change in the position of climate belts is, however, poorly understood. Here, we address this issue based on a case study of the early Toarcian (late Early Jurassic) Oceanic Anoxic Event (T-OAE, ∼183 Ma), one of the most significant global change events of the Phanerozoic, characterized by elevated humidity and major disturbances to terrestrial ecosystems on land. We present new leaf-wax <i>n</i>-alkanes δ<sup>13</sup>C data from the high-paleo-latitude Junggar Basin (northwest China) spanning the T-OAE and develop a time–space framework of plant-fractionation change, from low- to high-paleolatitudes across this time interval. We show that significant latitudinal changes in humidity occurred across the T-OAE (∼10°), likely because of a significant northward expansion of the low-latitude arid belts to mid-paleo-latitudes, and by inference a latitudinal expansion of the Hadley cells. This has important implications for the anthropogenic global warming and its effects on climate belts.</p>\",\"PeriodicalId\":15986,\"journal\":{\"name\":\"Journal of Geophysical Research: Atmospheres\",\"volume\":\"130 12\",\"pages\":\"\"},\"PeriodicalIF\":3.8000,\"publicationDate\":\"2025-06-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geophysical Research: Atmospheres\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1029/2024JD043219\",\"RegionNum\":2,\"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":"Journal of Geophysical Research: Atmospheres","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2024JD043219","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
Toarcian Greenhouse Warming Shifted Climate Belts Poleward With Global Change Implications
Atmospheric convection is predicted to change in response to anthropogenic global warming, leading to a poleward expansion of the Hadley cells and associated arid climate belts. The magnitude of possible latitudinal change in the position of climate belts is, however, poorly understood. Here, we address this issue based on a case study of the early Toarcian (late Early Jurassic) Oceanic Anoxic Event (T-OAE, ∼183 Ma), one of the most significant global change events of the Phanerozoic, characterized by elevated humidity and major disturbances to terrestrial ecosystems on land. We present new leaf-wax n-alkanes δ13C data from the high-paleo-latitude Junggar Basin (northwest China) spanning the T-OAE and develop a time–space framework of plant-fractionation change, from low- to high-paleolatitudes across this time interval. We show that significant latitudinal changes in humidity occurred across the T-OAE (∼10°), likely because of a significant northward expansion of the low-latitude arid belts to mid-paleo-latitudes, and by inference a latitudinal expansion of the Hadley cells. This has important implications for the anthropogenic global warming and its effects on climate belts.
期刊介绍:
JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.