{"title":"气候变化下日本北部及其周边海域线状雨带的气象特征","authors":"Yuta Ohya, Tomohito J. Yamada","doi":"10.2166/hydro.2024.121","DOIUrl":null,"url":null,"abstract":"<div><div data- reveal-group-><div><img alt=\"graphic\" data-src=\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\" path-from-xml=\"hydro-d-23-00121gf01.tif\" src=\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\"/><div>View largeDownload slide</div></div></div><div content- data-reveal=\"data-reveal\"><div><img alt=\"graphic\" data-src=\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\" path-from-xml=\"hydro-d-23-00121gf01.tif\" src=\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\"/><div>View largeDownload slide</div></div><i> </i><span>Close modal</span></div></div><p>In recent years, line-shaped rainbands (LRBs) have increased in Hokkaido, Japan. LRBs caused several flood disasters historically, thus the weather patterns that cause them need to be investigated. This study aimed to understand statistically the relationship between LRBs and weather patterns during the summer months under climate change conditions. Our study investigates the link between LRBs and weather patterns in Hokkaido during July and August, using historical and climate prediction models. With a 2°/4° global temperature rise, LRB occurrences in this region increase by approximately 1.51/2.07 times. The highest occurrences of LRBs correlate with increased water vapor flux from the south and positive pressure anomalies over the Pacific Ocean. Three main weather patterns contribute significantly to LRBs: (1) a nearby low-pressure system, (2) a strengthening Pacific High frontal pattern, and (3) approaching or landing typhoons in Hokkaido. These patterns double the LRB occurrence probability, a trait observed across past and projected climates (+2K and +4K experiments). These are important insights for future flood risk management.</p>","PeriodicalId":54801,"journal":{"name":"Journal of Hydroinformatics","volume":null,"pages":null},"PeriodicalIF":2.2000,"publicationDate":"2024-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Meteorological characteristics of line-shaped rainbands in northern Japan and its surrounding seas under climate change\",\"authors\":\"Yuta Ohya, Tomohito J. Yamada\",\"doi\":\"10.2166/hydro.2024.121\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div data- reveal-group-><div><img alt=\\\"graphic\\\" data-src=\\\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\\\" path-from-xml=\\\"hydro-d-23-00121gf01.tif\\\" src=\\\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\\\"/><div>View largeDownload slide</div></div></div><div content- data-reveal=\\\"data-reveal\\\"><div><img alt=\\\"graphic\\\" data-src=\\\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\\\" path-from-xml=\\\"hydro-d-23-00121gf01.tif\\\" src=\\\"https://iwa.silverchair-cdn.com/iwa/content_public/journal/jh/26/2/10.2166_hydro.2024.121/1/m_hydro-d-23-00121gf01.png?Expires=1712248319&Signature=MBiDDIfBANl5gcv~tx56Jn~TjUdkd53Sw1r0lYohiyDO-cDqWQc5ATJeN9k9TlO939pkTOn3aOFWmBp8b9~0QXkMCUEqgP~cdCFUmI4K4dQ6Taixt83W3Bw0cB0nWK9esBugT~J6SXKT66kp9uK-Ajc3i~rBkRE5HMBTV9rlDJHUg0EVw4xCS0madLwQ28ON0mxSMiO~hVvztcAW5a~Mtf~U~4STezGW~AytqbRsq586E4SI19rLzn0cIa4yEh2YpY6YnH3YC7vwma3olw9VUI8oCUkU9frphzwHpR4W5B-DFlprNjVzR7-1cdWN92MCLn0350S8FiKWuYHXy1csag__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA\\\"/><div>View largeDownload slide</div></div><i> </i><span>Close modal</span></div></div><p>In recent years, line-shaped rainbands (LRBs) have increased in Hokkaido, Japan. LRBs caused several flood disasters historically, thus the weather patterns that cause them need to be investigated. This study aimed to understand statistically the relationship between LRBs and weather patterns during the summer months under climate change conditions. Our study investigates the link between LRBs and weather patterns in Hokkaido during July and August, using historical and climate prediction models. With a 2°/4° global temperature rise, LRB occurrences in this region increase by approximately 1.51/2.07 times. The highest occurrences of LRBs correlate with increased water vapor flux from the south and positive pressure anomalies over the Pacific Ocean. Three main weather patterns contribute significantly to LRBs: (1) a nearby low-pressure system, (2) a strengthening Pacific High frontal pattern, and (3) approaching or landing typhoons in Hokkaido. These patterns double the LRB occurrence probability, a trait observed across past and projected climates (+2K and +4K experiments). These are important insights for future flood risk management.</p>\",\"PeriodicalId\":54801,\"journal\":{\"name\":\"Journal of Hydroinformatics\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":2.2000,\"publicationDate\":\"2024-02-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Hydroinformatics\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://doi.org/10.2166/hydro.2024.121\",\"RegionNum\":3,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Hydroinformatics","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.2166/hydro.2024.121","RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS","Score":null,"Total":0}
Meteorological characteristics of line-shaped rainbands in northern Japan and its surrounding seas under climate change
View largeDownload slide
View largeDownload slide
Close modal
In recent years, line-shaped rainbands (LRBs) have increased in Hokkaido, Japan. LRBs caused several flood disasters historically, thus the weather patterns that cause them need to be investigated. This study aimed to understand statistically the relationship between LRBs and weather patterns during the summer months under climate change conditions. Our study investigates the link between LRBs and weather patterns in Hokkaido during July and August, using historical and climate prediction models. With a 2°/4° global temperature rise, LRB occurrences in this region increase by approximately 1.51/2.07 times. The highest occurrences of LRBs correlate with increased water vapor flux from the south and positive pressure anomalies over the Pacific Ocean. Three main weather patterns contribute significantly to LRBs: (1) a nearby low-pressure system, (2) a strengthening Pacific High frontal pattern, and (3) approaching or landing typhoons in Hokkaido. These patterns double the LRB occurrence probability, a trait observed across past and projected climates (+2K and +4K experiments). These are important insights for future flood risk management.
期刊介绍:
Journal of Hydroinformatics is a peer-reviewed journal devoted to the application of information technology in the widest sense to problems of the aquatic environment. It promotes Hydroinformatics as a cross-disciplinary field of study, combining technological, human-sociological and more general environmental interests, including an ethical perspective.