{"title":"CMIP6 对北印度洋表面潜热通量的预测","authors":"Pravat Rabi Naskar, Mrutyunjay Mohapatra, Gyan Prakash Singh","doi":"10.1007/s00704-024-05114-2","DOIUrl":null,"url":null,"abstract":"<p>This study has been undertaken to predict the Surface Latent Heat Flux (SLHF) over the North Indian Ocean (NIO) in the future period (2020–2099) under different emission scenarios. For this 12 Coupled Model Inter-comparison Project 6 (CMIP6), Global Climate Models (GCMs) SLHF and ERA5 SLHF data have been used. It is observed that the SLHF is going to increase in the far future (2060–2099) under all emission scenarios probably due to higher warming. In the near future (2020–2059) particularly in the first half (2020–2039) a clear fall in the SLHF is noticed. It is also observed that the SLHF rise under the Shared Socioeconomic Pathways 5 (SSP5) is more than that under the SSP2 in the far future due to higher warming. Seasonal variation of the SLHF depicts that under SSP5 in the far future, the rise in the SLHF is the maximum in MAM. The rise of the SLHF in the far future can be attributed to the rise in the SST over the NIO but the reason for the fall of the SLHF in the first half of the near future is not clear.</p>","PeriodicalId":22945,"journal":{"name":"Theoretical and Applied Climatology","volume":"24 1","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-07-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"CMIP6 projections of surface latent heat flux over the North Indian Ocean\",\"authors\":\"Pravat Rabi Naskar, Mrutyunjay Mohapatra, Gyan Prakash Singh\",\"doi\":\"10.1007/s00704-024-05114-2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>This study has been undertaken to predict the Surface Latent Heat Flux (SLHF) over the North Indian Ocean (NIO) in the future period (2020–2099) under different emission scenarios. For this 12 Coupled Model Inter-comparison Project 6 (CMIP6), Global Climate Models (GCMs) SLHF and ERA5 SLHF data have been used. It is observed that the SLHF is going to increase in the far future (2060–2099) under all emission scenarios probably due to higher warming. In the near future (2020–2059) particularly in the first half (2020–2039) a clear fall in the SLHF is noticed. It is also observed that the SLHF rise under the Shared Socioeconomic Pathways 5 (SSP5) is more than that under the SSP2 in the far future due to higher warming. Seasonal variation of the SLHF depicts that under SSP5 in the far future, the rise in the SLHF is the maximum in MAM. The rise of the SLHF in the far future can be attributed to the rise in the SST over the NIO but the reason for the fall of the SLHF in the first half of the near future is not clear.</p>\",\"PeriodicalId\":22945,\"journal\":{\"name\":\"Theoretical and Applied Climatology\",\"volume\":\"24 1\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-07-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Theoretical and Applied Climatology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1007/s00704-024-05114-2\",\"RegionNum\":4,\"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":"Theoretical and Applied Climatology","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s00704-024-05114-2","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
CMIP6 projections of surface latent heat flux over the North Indian Ocean
This study has been undertaken to predict the Surface Latent Heat Flux (SLHF) over the North Indian Ocean (NIO) in the future period (2020–2099) under different emission scenarios. For this 12 Coupled Model Inter-comparison Project 6 (CMIP6), Global Climate Models (GCMs) SLHF and ERA5 SLHF data have been used. It is observed that the SLHF is going to increase in the far future (2060–2099) under all emission scenarios probably due to higher warming. In the near future (2020–2059) particularly in the first half (2020–2039) a clear fall in the SLHF is noticed. It is also observed that the SLHF rise under the Shared Socioeconomic Pathways 5 (SSP5) is more than that under the SSP2 in the far future due to higher warming. Seasonal variation of the SLHF depicts that under SSP5 in the far future, the rise in the SLHF is the maximum in MAM. The rise of the SLHF in the far future can be attributed to the rise in the SST over the NIO but the reason for the fall of the SLHF in the first half of the near future is not clear.
期刊介绍:
Theoretical and Applied Climatology covers the following topics:
- climate modeling, climatic changes and climate forecasting, micro- to mesoclimate, applied meteorology as in agro- and forestmeteorology, biometeorology, building meteorology and atmospheric radiation problems as they relate to the biosphere
- effects of anthropogenic and natural aerosols or gaseous trace constituents
- hardware and software elements of meteorological measurements, including techniques of remote sensing