Elliott M. Sainsbury, R. Schiemann, K. Hodges, A. Baker, L. Shaffrey, Kieran Bhatia, Stella Bourdin
{"title":"低分辨率CMIP6情景ip模型能否提供对未来欧洲后热带气旋风险的洞察?","authors":"Elliott M. Sainsbury, R. Schiemann, K. Hodges, A. Baker, L. Shaffrey, Kieran Bhatia, Stella Bourdin","doi":"10.5194/wcd-3-1359-2022","DOIUrl":null,"url":null,"abstract":"Abstract. Post-tropical cyclones (PTCs) can cause extensive damage across\nEurope through extreme winds and heavy precipitation. With increasing sea\nsurface temperatures, tropical cyclones (TCs) may form and travel further\npoleward and eastward than observed historically. Recent work has\nsuggested that the frequency of intense Europe-impacting PTCs may increase\nsubstantially in the future. Using an objective feature-tracking scheme and TC identification method, we\ntrack and identify the full life cycle of TCs in the North Atlantic in five\nCMIP6 climate models in the historical (1984–2014) period and in the future\nunder the SSP5-85 scenario (2069–2099). These five models are selected based\non their ability to simulate TC frequency similar to observed in the North\nAtlantic, although model deficiencies remain. We find no robust changes in Europe-impacting PTC frequency or intensity in\nthe future. This is because two competing factors – a significant decrease\nin TC frequency of 30 %–60 % and an increase in the proportion of TCs\nreaching Europe – are approximately the same size. The projected increase\nin the proportion of TCs reaching Europe is largely driven by an increase in\nthe likelihood of recurvature and is consistent with projected decreases in\nvertical wind shear and increases in potential intensity along the US East\nCoast in the future. The projected increased likelihood of recurvature is\nalso associated with a shift in TC genesis away from the main development\nregion, where model biases cause very few TCs to recurve. This study\nindicates that large uncertainties surround future Europe-impacting PTCs and\nprovides a framework for evaluating PTCs in future generations of climate\nmodels.\n","PeriodicalId":383272,"journal":{"name":"Weather and Climate Dynamics","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-11-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Can low-resolution CMIP6 ScenarioMIP models provide insight into future European post-tropical-cyclone risk?\",\"authors\":\"Elliott M. Sainsbury, R. Schiemann, K. Hodges, A. Baker, L. Shaffrey, Kieran Bhatia, Stella Bourdin\",\"doi\":\"10.5194/wcd-3-1359-2022\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. Post-tropical cyclones (PTCs) can cause extensive damage across\\nEurope through extreme winds and heavy precipitation. With increasing sea\\nsurface temperatures, tropical cyclones (TCs) may form and travel further\\npoleward and eastward than observed historically. Recent work has\\nsuggested that the frequency of intense Europe-impacting PTCs may increase\\nsubstantially in the future. Using an objective feature-tracking scheme and TC identification method, we\\ntrack and identify the full life cycle of TCs in the North Atlantic in five\\nCMIP6 climate models in the historical (1984–2014) period and in the future\\nunder the SSP5-85 scenario (2069–2099). These five models are selected based\\non their ability to simulate TC frequency similar to observed in the North\\nAtlantic, although model deficiencies remain. We find no robust changes in Europe-impacting PTC frequency or intensity in\\nthe future. This is because two competing factors – a significant decrease\\nin TC frequency of 30 %–60 % and an increase in the proportion of TCs\\nreaching Europe – are approximately the same size. The projected increase\\nin the proportion of TCs reaching Europe is largely driven by an increase in\\nthe likelihood of recurvature and is consistent with projected decreases in\\nvertical wind shear and increases in potential intensity along the US East\\nCoast in the future. The projected increased likelihood of recurvature is\\nalso associated with a shift in TC genesis away from the main development\\nregion, where model biases cause very few TCs to recurve. This study\\nindicates that large uncertainties surround future Europe-impacting PTCs and\\nprovides a framework for evaluating PTCs in future generations of climate\\nmodels.\\n\",\"PeriodicalId\":383272,\"journal\":{\"name\":\"Weather and Climate Dynamics\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-11-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Weather and Climate Dynamics\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5194/wcd-3-1359-2022\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Weather and Climate Dynamics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/wcd-3-1359-2022","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Can low-resolution CMIP6 ScenarioMIP models provide insight into future European post-tropical-cyclone risk?
Abstract. Post-tropical cyclones (PTCs) can cause extensive damage across
Europe through extreme winds and heavy precipitation. With increasing sea
surface temperatures, tropical cyclones (TCs) may form and travel further
poleward and eastward than observed historically. Recent work has
suggested that the frequency of intense Europe-impacting PTCs may increase
substantially in the future. Using an objective feature-tracking scheme and TC identification method, we
track and identify the full life cycle of TCs in the North Atlantic in five
CMIP6 climate models in the historical (1984–2014) period and in the future
under the SSP5-85 scenario (2069–2099). These five models are selected based
on their ability to simulate TC frequency similar to observed in the North
Atlantic, although model deficiencies remain. We find no robust changes in Europe-impacting PTC frequency or intensity in
the future. This is because two competing factors – a significant decrease
in TC frequency of 30 %–60 % and an increase in the proportion of TCs
reaching Europe – are approximately the same size. The projected increase
in the proportion of TCs reaching Europe is largely driven by an increase in
the likelihood of recurvature and is consistent with projected decreases in
vertical wind shear and increases in potential intensity along the US East
Coast in the future. The projected increased likelihood of recurvature is
also associated with a shift in TC genesis away from the main development
region, where model biases cause very few TCs to recurve. This study
indicates that large uncertainties surround future Europe-impacting PTCs and
provides a framework for evaluating PTCs in future generations of climate
models.