{"title":"评估2050年以前气候变化影响下的里海海平面波动情况","authors":"N. Ivkina, A. Galayeva","doi":"10.54668/2789-6323-2021-100-1-70-77","DOIUrl":null,"url":null,"abstract":"The article considers the possible fluctuation of the Caspian Sea level in the future until 2050, taking into an account the climate changes. For this purpose, possible changes in the river inflow to the sea and meteorological parameters (precipitation, air temperature and evaporation from the water surface) were predicted. Changes in the meteorological parameters were estimated according to two climate scenarios RCP4. 5 and RCP8.5.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"355 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"ASSESSMENT OF FLUCTUATIONS IN THE CASPIAN SEA LEVEL UNDER THE INFLUENCE OF CLIMATE CHANGE FOR THE FUTURE UNTIL 2050\",\"authors\":\"N. Ivkina, A. Galayeva\",\"doi\":\"10.54668/2789-6323-2021-100-1-70-77\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The article considers the possible fluctuation of the Caspian Sea level in the future until 2050, taking into an account the climate changes. For this purpose, possible changes in the river inflow to the sea and meteorological parameters (precipitation, air temperature and evaporation from the water surface) were predicted. Changes in the meteorological parameters were estimated according to two climate scenarios RCP4. 5 and RCP8.5.\",\"PeriodicalId\":256870,\"journal\":{\"name\":\"Hydrometeorology and ecology\",\"volume\":\"355 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Hydrometeorology and ecology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.54668/2789-6323-2021-100-1-70-77\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrometeorology and ecology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.54668/2789-6323-2021-100-1-70-77","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
ASSESSMENT OF FLUCTUATIONS IN THE CASPIAN SEA LEVEL UNDER THE INFLUENCE OF CLIMATE CHANGE FOR THE FUTURE UNTIL 2050
The article considers the possible fluctuation of the Caspian Sea level in the future until 2050, taking into an account the climate changes. For this purpose, possible changes in the river inflow to the sea and meteorological parameters (precipitation, air temperature and evaporation from the water surface) were predicted. Changes in the meteorological parameters were estimated according to two climate scenarios RCP4. 5 and RCP8.5.