East Asian heatwaves driven by Arctic-Siberian warming
Abstract This study investigates the contributing factors of East Asian heatwaves (EAHWs) linked to the Arctic-Siberian Plain (ASP) over the past 42 years (1979–2020). EAHWs are mainly affected by two time scales of variabilities: long-term externally forced and interannual variabilities. The extern...
| Published in: | Scientific Reports |
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| Main Authors: | , , , , |
| Format: | Article |
| Language: | English |
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Nature Portfolio
2022-10-01
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| Online Access: | https://doi.org/10.1038/s41598-022-22628-9 |
| _version_ | 1852692170796957696 |
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| author | Jeong-Hun Kim Seong-Joong Kim Joo-Hong Kim Michiya Hayashi Maeng-Ki Kim |
| author_facet | Jeong-Hun Kim Seong-Joong Kim Joo-Hong Kim Michiya Hayashi Maeng-Ki Kim |
| author_sort | Jeong-Hun Kim |
| collection | DOAJ |
| container_title | Scientific Reports |
| description | Abstract This study investigates the contributing factors of East Asian heatwaves (EAHWs) linked to the Arctic-Siberian Plain (ASP) over the past 42 years (1979–2020). EAHWs are mainly affected by two time scales of variabilities: long-term externally forced and interannual variabilities. The externally forced EAHWs are attributed to the increasing global warming trend, while their interannual variability is related to the circumglobal teleconnection (CGT) and the ASP teleconnection patterns. In addition to the CGT, the Rossby wave energy originating from the ASP propagates to East Asia through the upper troposphere, amplifying the EAHWs. The stationary high pressure in the ASP is generated by vorticity advection in the upper troposphere. Enhanced surface radiative heating and evaporation on the ASP surface increase the specific humidity and temperature, amplifying the thermal high pressure via positive water vapor feedback. Thermal high-pressure amplified by land–atmosphere interactions in the ASP during the peak summer season leads to EAHWs by the propagation of stationary Rossby wave energy. The results indicate that our enhanced understanding of the ASP teleconnection can improve forecasting of the EAHWs not only on a sub-seasonal time scale but also in future projections of global climate models. |
| format | Article |
| id | doaj-art-e2f32a1205fe43d5b46b2b91d3c86156 |
| institution | Directory of Open Access Journals |
| issn | 2045-2322 |
| language | English |
| publishDate | 2022-10-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| spelling | doaj-art-e2f32a1205fe43d5b46b2b91d3c861562025-08-19T21:24:10ZengNature PortfolioScientific Reports2045-23222022-10-0112111110.1038/s41598-022-22628-9East Asian heatwaves driven by Arctic-Siberian warmingJeong-Hun Kim0Seong-Joong Kim1Joo-Hong Kim2Michiya Hayashi3Maeng-Ki Kim4Department of Atmospheric Sciences, Kongju National UniversityDivision of Atmospheric Sciences, Korea Polar Research InstituteDivision of Atmospheric Sciences, Korea Polar Research InstituteEarth System Division, National Institute for Environmental StudiesDepartment of Atmospheric Sciences, Kongju National UniversityAbstract This study investigates the contributing factors of East Asian heatwaves (EAHWs) linked to the Arctic-Siberian Plain (ASP) over the past 42 years (1979–2020). EAHWs are mainly affected by two time scales of variabilities: long-term externally forced and interannual variabilities. The externally forced EAHWs are attributed to the increasing global warming trend, while their interannual variability is related to the circumglobal teleconnection (CGT) and the ASP teleconnection patterns. In addition to the CGT, the Rossby wave energy originating from the ASP propagates to East Asia through the upper troposphere, amplifying the EAHWs. The stationary high pressure in the ASP is generated by vorticity advection in the upper troposphere. Enhanced surface radiative heating and evaporation on the ASP surface increase the specific humidity and temperature, amplifying the thermal high pressure via positive water vapor feedback. Thermal high-pressure amplified by land–atmosphere interactions in the ASP during the peak summer season leads to EAHWs by the propagation of stationary Rossby wave energy. The results indicate that our enhanced understanding of the ASP teleconnection can improve forecasting of the EAHWs not only on a sub-seasonal time scale but also in future projections of global climate models.https://doi.org/10.1038/s41598-022-22628-9 |
| spellingShingle | Jeong-Hun Kim Seong-Joong Kim Joo-Hong Kim Michiya Hayashi Maeng-Ki Kim East Asian heatwaves driven by Arctic-Siberian warming |
| title | East Asian heatwaves driven by Arctic-Siberian warming |
| title_full | East Asian heatwaves driven by Arctic-Siberian warming |
| title_fullStr | East Asian heatwaves driven by Arctic-Siberian warming |
| title_full_unstemmed | East Asian heatwaves driven by Arctic-Siberian warming |
| title_short | East Asian heatwaves driven by Arctic-Siberian warming |
| title_sort | east asian heatwaves driven by arctic siberian warming |
| url | https://doi.org/10.1038/s41598-022-22628-9 |
| work_keys_str_mv | AT jeonghunkim eastasianheatwavesdrivenbyarcticsiberianwarming AT seongjoongkim eastasianheatwavesdrivenbyarcticsiberianwarming AT joohongkim eastasianheatwavesdrivenbyarcticsiberianwarming AT michiyahayashi eastasianheatwavesdrivenbyarcticsiberianwarming AT maengkikim eastasianheatwavesdrivenbyarcticsiberianwarming |
