Change of the global climate regime at the turn of the XX–XXI centuries
Rapid change in the planetary climate regime at the turn of the XX and XXI centuries has been revealed based on the analysis of the observations' data. With respect to the previous climatic regime, evaporation and a latent heat flux have increased from most of the surface of the World Ocean. Re...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | Russian |
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Murmansk State Technical University
2018-03-01
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| Series: | Vestnik MGTU |
| Subjects: | |
| Online Access: | http://vestnik.mstu.edu.ru/show-eng.shtml?art=1938 |
| _version_ | 1819110621285711872 |
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| author | Ponomarev V. I. Dmitrieva E. V. Shkorba S. P. Karnaukhov A. A. |
| author_facet | Ponomarev V. I. Dmitrieva E. V. Shkorba S. P. Karnaukhov A. A. |
| author_sort | Ponomarev V. I. |
| collection | DOAJ |
| description | Rapid change in the planetary climate regime at the turn of the XX and XXI centuries has been revealed based on the analysis of the observations' data. With respect to the previous climatic regime, evaporation and a latent heat flux have increased from most of the surface of the World Ocean. Recent climatic regime in the XXI century is characterized by a significant increase in the number of strong cyclones, storms, sum of precipitation in wet areas with maritime climate. The number of hazardous extreme weather events is mostly increased in the ocean – continent marginal zone, including the Far East of Russia. The increase in precipitation in 2004 and extreme precipitation in 2015–2016 within the catchment of Lake Khanka in the South of the Russian Far East led to a catastrophic spill of this lake. During the first 17 years of the XXI century the number of extreme precipitation and floods in the warm season has increased in most of the marginal zones of Eurasia and North America. Winter snowfall is also amplified in the zone of temperate latitudes over many continental regions. The observed increase in precipitation is caused due to growth in both the water vapour content in the atmosphere over the ocean and the meridional transfer of heat and water vapour. Decrease in rainfall occurs in some continental areas, including the catchment area of Lake Baikal and the reservoirs of the Angara cascade of hydropower plants. |
| first_indexed | 2024-12-22T03:44:38Z |
| format | Article |
| id | doaj.art-caeb1a6f1fdc43b1bc6f7c0c71e91e0c |
| institution | Directory Open Access Journal |
| issn | 1560-9278 1997-4736 |
| language | Russian |
| last_indexed | 2024-12-22T03:44:38Z |
| publishDate | 2018-03-01 |
| publisher | Murmansk State Technical University |
| record_format | Article |
| series | Vestnik MGTU |
| spelling | doaj.art-caeb1a6f1fdc43b1bc6f7c0c71e91e0c2022-12-21T18:40:10ZrusMurmansk State Technical UniversityVestnik MGTU1560-92781997-47362018-03-0121116016910.21443/1560-9278-2018-21-1-160-169Change of the global climate regime at the turn of the XX–XXI centuriesPonomarev V. I. 0Dmitrieva E. V. 1Shkorba S. P. 2Karnaukhov A. A.3V. I. Il'ichev Pacific Oceanological Institute FEB RASV. I. Il'ichev Pacific Oceanological Institute FEB RASV. I. Il'ichev Pacific Oceanological Institute FEB RASV. I. Il'ichev Pacific Oceanological Institute FEB RASRapid change in the planetary climate regime at the turn of the XX and XXI centuries has been revealed based on the analysis of the observations' data. With respect to the previous climatic regime, evaporation and a latent heat flux have increased from most of the surface of the World Ocean. Recent climatic regime in the XXI century is characterized by a significant increase in the number of strong cyclones, storms, sum of precipitation in wet areas with maritime climate. The number of hazardous extreme weather events is mostly increased in the ocean – continent marginal zone, including the Far East of Russia. The increase in precipitation in 2004 and extreme precipitation in 2015–2016 within the catchment of Lake Khanka in the South of the Russian Far East led to a catastrophic spill of this lake. During the first 17 years of the XXI century the number of extreme precipitation and floods in the warm season has increased in most of the marginal zones of Eurasia and North America. Winter snowfall is also amplified in the zone of temperate latitudes over many continental regions. The observed increase in precipitation is caused due to growth in both the water vapour content in the atmosphere over the ocean and the meridional transfer of heat and water vapour. Decrease in rainfall occurs in some continental areas, including the catchment area of Lake Baikal and the reservoirs of the Angara cascade of hydropower plants.http://vestnik.mstu.edu.ru/show-eng.shtml?art=1938changeclimateregimeprecipitationAsia-Pacific regionPacific and Indian OceanslakeKhankaBaikal |
| spellingShingle | Ponomarev V. I. Dmitrieva E. V. Shkorba S. P. Karnaukhov A. A. Change of the global climate regime at the turn of the XX–XXI centuries Vestnik MGTU change climate regime precipitation Asia-Pacific region Pacific and Indian Oceans lake Khanka Baikal |
| title | Change of the global climate regime at the turn of the XX–XXI centuries |
| title_full | Change of the global climate regime at the turn of the XX–XXI centuries |
| title_fullStr | Change of the global climate regime at the turn of the XX–XXI centuries |
| title_full_unstemmed | Change of the global climate regime at the turn of the XX–XXI centuries |
| title_short | Change of the global climate regime at the turn of the XX–XXI centuries |
| title_sort | change of the global climate regime at the turn of the xx xxi centuries |
| topic | change climate regime precipitation Asia-Pacific region Pacific and Indian Oceans lake Khanka Baikal |
| url | http://vestnik.mstu.edu.ru/show-eng.shtml?art=1938 |
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