{"title":"基于issykkul研究站40年观测结果的气候活性大气杂质的变率(42.62n;76.98 e;1640米)和卫星(sbuv)","authors":"M. D. Orozaliev, A. S. Abdyldaev, A. Jumabekov","doi":"10.35803/1694-5298.2021.3.439-448","DOIUrl":null,"url":null,"abstract":"Based on the results of forty years of monitoring of climatically active constituents of the atmosphere at the Issyk-Kul scientific station, a bank of experimental data was obtained, which made it possible to identify specific features in the variability of the ozone layer, greenhouse gases and aerosol components of the atmosphere over the mountainous region of Central Asia. The research results are used to correct existing and develop new models of the atmosphere, which make it possible to predict the state of the ozone layer and climate change, taking into account inland mountain effects that make a significant contribution to the thermodynamic processes of the troposphere-stratosphere.","PeriodicalId":22490,"journal":{"name":"The Herald of KSUCTA, №3, 2021","volume":"34 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-09-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"VARIABILITY OF CLIMATICALLY ACTIVE ATMOSPHERIC IMPURITIES BASED ON THE RESULTS OF 40 YEARS OF OBSERVATIONS ON THE BASIS OF THE ISSYKKUL RESEARCH STATION (42.62N; 76.98E; 1640M) AND ON SATELLITES (SBUV)\",\"authors\":\"M. D. Orozaliev, A. S. Abdyldaev, A. Jumabekov\",\"doi\":\"10.35803/1694-5298.2021.3.439-448\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Based on the results of forty years of monitoring of climatically active constituents of the atmosphere at the Issyk-Kul scientific station, a bank of experimental data was obtained, which made it possible to identify specific features in the variability of the ozone layer, greenhouse gases and aerosol components of the atmosphere over the mountainous region of Central Asia. The research results are used to correct existing and develop new models of the atmosphere, which make it possible to predict the state of the ozone layer and climate change, taking into account inland mountain effects that make a significant contribution to the thermodynamic processes of the troposphere-stratosphere.\",\"PeriodicalId\":22490,\"journal\":{\"name\":\"The Herald of KSUCTA, №3, 2021\",\"volume\":\"34 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-09-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The Herald of KSUCTA, №3, 2021\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.35803/1694-5298.2021.3.439-448\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Herald of KSUCTA, №3, 2021","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.35803/1694-5298.2021.3.439-448","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
VARIABILITY OF CLIMATICALLY ACTIVE ATMOSPHERIC IMPURITIES BASED ON THE RESULTS OF 40 YEARS OF OBSERVATIONS ON THE BASIS OF THE ISSYKKUL RESEARCH STATION (42.62N; 76.98E; 1640M) AND ON SATELLITES (SBUV)
Based on the results of forty years of monitoring of climatically active constituents of the atmosphere at the Issyk-Kul scientific station, a bank of experimental data was obtained, which made it possible to identify specific features in the variability of the ozone layer, greenhouse gases and aerosol components of the atmosphere over the mountainous region of Central Asia. The research results are used to correct existing and develop new models of the atmosphere, which make it possible to predict the state of the ozone layer and climate change, taking into account inland mountain effects that make a significant contribution to the thermodynamic processes of the troposphere-stratosphere.
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