Irene Ortiz, Ermioni Dimitropoulou, Pierre de Buyl, Nicolas Clerbaux, Javier García-Heras, Amin Jafarimoghaddam, Hugues Brenot, Jeroen van Gent, Klaus Sievers, Evelyn Otero, Parthiban Loganathan, Manuel Soler
{"title":"基于卫星的欧洲上空烟云辐射强迫量化:对航空诱发气候效应的两周分析","authors":"Irene Ortiz, Ermioni Dimitropoulou, Pierre de Buyl, Nicolas Clerbaux, Javier García-Heras, Amin Jafarimoghaddam, Hugues Brenot, Jeroen van Gent, Klaus Sievers, Evelyn Otero, Parthiban Loganathan, Manuel Soler","doi":"arxiv-2409.10166","DOIUrl":null,"url":null,"abstract":"Aviation's non-CO$_2$ effects, especially the impact of aviation-induced\ncontrails, drive atmospheric changes and can influence climate dynamics.\nAlthough contrails are believed to contribute to global warming through their\nnet warming effect, uncertainties persist due to the challenges in accurately\nmeasuring their radiative impacts. This study aims to address this knowledge\ngap by investigating the relationship between aviation-induced contrails, as\nobserved in Meteosat Second Generation (MSG) satellite imagery, and their\nimpact on radiative forcing (RF) over a two-week study. Results show that while\ndaytime contrails generally have a cooling effect, the higher number of\nnighttime contrails results in a net warming effect over the entire day. Net RF\nvalues for detected contrails range approximately from -8 TW to 2.5 TW during\nthe day and from 0 to 6 TW at night. Our findings also show a 41.03% increase\nin contrail coverage from January 24-30, 2023, to the same week in 2024,\naccompanied by a 128.7% rise in contrail radiative forcing (CRF), indicating\ngreater warming from the added contrails. These findings highlight the\nnecessity of considering temporal factors, such as the timing and duration of\ncontrail formation, when assessing their overall warming impact. They also\nindicate a potential increase in contrail-induced warming from 2023 to 2024,\nattributable to the rise in contrail coverage. Further investigation into these\ntrends is crucial for the development of effective mitigation strategies.","PeriodicalId":501166,"journal":{"name":"arXiv - PHYS - Atmospheric and Oceanic Physics","volume":"57 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Satellite-Based Quantification of Contrail Radiative Forcing over Europe: A Two-Week Analysis of Aviation-Induced Climate Effects\",\"authors\":\"Irene Ortiz, Ermioni Dimitropoulou, Pierre de Buyl, Nicolas Clerbaux, Javier García-Heras, Amin Jafarimoghaddam, Hugues Brenot, Jeroen van Gent, Klaus Sievers, Evelyn Otero, Parthiban Loganathan, Manuel Soler\",\"doi\":\"arxiv-2409.10166\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Aviation's non-CO$_2$ effects, especially the impact of aviation-induced\\ncontrails, drive atmospheric changes and can influence climate dynamics.\\nAlthough contrails are believed to contribute to global warming through their\\nnet warming effect, uncertainties persist due to the challenges in accurately\\nmeasuring their radiative impacts. This study aims to address this knowledge\\ngap by investigating the relationship between aviation-induced contrails, as\\nobserved in Meteosat Second Generation (MSG) satellite imagery, and their\\nimpact on radiative forcing (RF) over a two-week study. Results show that while\\ndaytime contrails generally have a cooling effect, the higher number of\\nnighttime contrails results in a net warming effect over the entire day. Net RF\\nvalues for detected contrails range approximately from -8 TW to 2.5 TW during\\nthe day and from 0 to 6 TW at night. Our findings also show a 41.03% increase\\nin contrail coverage from January 24-30, 2023, to the same week in 2024,\\naccompanied by a 128.7% rise in contrail radiative forcing (CRF), indicating\\ngreater warming from the added contrails. These findings highlight the\\nnecessity of considering temporal factors, such as the timing and duration of\\ncontrail formation, when assessing their overall warming impact. They also\\nindicate a potential increase in contrail-induced warming from 2023 to 2024,\\nattributable to the rise in contrail coverage. Further investigation into these\\ntrends is crucial for the development of effective mitigation strategies.\",\"PeriodicalId\":501166,\"journal\":{\"name\":\"arXiv - PHYS - Atmospheric and Oceanic Physics\",\"volume\":\"57 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-09-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"arXiv - PHYS - Atmospheric and Oceanic Physics\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/arxiv-2409.10166\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Atmospheric and Oceanic Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.10166","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Satellite-Based Quantification of Contrail Radiative Forcing over Europe: A Two-Week Analysis of Aviation-Induced Climate Effects
Aviation's non-CO$_2$ effects, especially the impact of aviation-induced
contrails, drive atmospheric changes and can influence climate dynamics.
Although contrails are believed to contribute to global warming through their
net warming effect, uncertainties persist due to the challenges in accurately
measuring their radiative impacts. This study aims to address this knowledge
gap by investigating the relationship between aviation-induced contrails, as
observed in Meteosat Second Generation (MSG) satellite imagery, and their
impact on radiative forcing (RF) over a two-week study. Results show that while
daytime contrails generally have a cooling effect, the higher number of
nighttime contrails results in a net warming effect over the entire day. Net RF
values for detected contrails range approximately from -8 TW to 2.5 TW during
the day and from 0 to 6 TW at night. Our findings also show a 41.03% increase
in contrail coverage from January 24-30, 2023, to the same week in 2024,
accompanied by a 128.7% rise in contrail radiative forcing (CRF), indicating
greater warming from the added contrails. These findings highlight the
necessity of considering temporal factors, such as the timing and duration of
contrail formation, when assessing their overall warming impact. They also
indicate a potential increase in contrail-induced warming from 2023 to 2024,
attributable to the rise in contrail coverage. Further investigation into these
trends is crucial for the development of effective mitigation strategies.