Polarizing rain types linked to June drought in the Korean peninsula over last 20 years
We observe a notable decreasing trend of June rainfall over the Korean peninsula in recent 20 years. This drought condition is found to be linked to the polarizing trend of rainfall intensity; more non‐rain and drizzle‐like rain, less moderate‐intensity rain, and more heavy rain events. Overall, the...
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| Published in | International journal of climatology Vol. 40; no. 4; pp. 2173 - 2182 |
|---|---|
| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Chichester, UK
John Wiley & Sons, Ltd
30.03.2020
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0899-8418 1097-0088 |
| DOI | 10.1002/joc.6325 |
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| Abstract | We observe a notable decreasing trend of June rainfall over the Korean peninsula in recent 20 years. This drought condition is found to be linked to the polarizing trend of rainfall intensity; more non‐rain and drizzle‐like rain, less moderate‐intensity rain, and more heavy rain events. Overall, the June drought over the Korean peninsula is found to be associated with less occurring moderate‐intensity rain. This feature is interpreted as that the dominant warm‐type heavy rain systems with a medium storm height tends to be less frequent while cold‐type heavy rains characterized by taller storm become more frequent during last 20 years. The northwestward expansion of the North Pacific high in June appears to weaken the continuous moisture supply to the Korean peninsula, which is a main element of forming the warm‐type heavy rain there.
Climatological mean (left) and linear trend (right) for the frequency distribution of storm height normalized by near‐surface radar reflectivities over the Korean domain (June 1998–2017). |
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| AbstractList | We observe a notable decreasing trend of June rainfall over the Korean peninsula in recent 20 years. This drought condition is found to be linked to the polarizing trend of rainfall intensity; more non‐rain and drizzle‐like rain, less moderate‐intensity rain, and more heavy rain events. Overall, the June drought over the Korean peninsula is found to be associated with less occurring moderate‐intensity rain. This feature is interpreted as that the dominant warm‐type heavy rain systems with a medium storm height tends to be less frequent while cold‐type heavy rains characterized by taller storm become more frequent during last 20 years. The northwestward expansion of the North Pacific high in June appears to weaken the continuous moisture supply to the Korean peninsula, which is a main element of forming the warm‐type heavy rain there. We observe a notable decreasing trend of June rainfall over the Korean peninsula in recent 20 years. This drought condition is found to be linked to the polarizing trend of rainfall intensity; more non‐rain and drizzle‐like rain, less moderate‐intensity rain, and more heavy rain events. Overall, the June drought over the Korean peninsula is found to be associated with less occurring moderate‐intensity rain. This feature is interpreted as that the dominant warm‐type heavy rain systems with a medium storm height tends to be less frequent while cold‐type heavy rains characterized by taller storm become more frequent during last 20 years. The northwestward expansion of the North Pacific high in June appears to weaken the continuous moisture supply to the Korean peninsula, which is a main element of forming the warm‐type heavy rain there. Climatological mean (left) and linear trend (right) for the frequency distribution of storm height normalized by near‐surface radar reflectivities over the Korean domain (June 1998–2017). |
| Author | Song, Hwan‐Jin Sohn, Byung‐Ju |
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| CitedBy_id | crossref_primary_10_1016_j_ejrh_2023_101337 crossref_primary_10_1007_s00376_021_1178_8 crossref_primary_10_1093_mnras_stab1971 crossref_primary_10_2151_jmsj_2020_044 crossref_primary_10_1016_j_wace_2022_100490 crossref_primary_10_1007_s13143_019_00170_5 |
| Cites_doi | 10.1038/srep16771 10.1002/joc.2068 10.1038/ncomms7213 10.1175/2009JAMC2266.1 10.1175/1520-0442(2002)015<0386:RSOTAP>2.0.CO;2 10.1007/s00703-005-0125-z 10.1175/JCLI-D-14-00259.1 10.1002/met.1320 10.1175/JCLI-D-14-00464.1 10.1175/JCLI-D-11-00512.1 10.1029/2007GL031977 10.1175/2009JCLI3128.1 10.1007/s13143-017-0032-5 10.1175/JHM560.1 10.1002/2016GL070270 10.1175/MWR-D-14-00184.1 10.1002/joc.4280 10.1175/MWR-D-13-00075.1 10.1155/2017/8598594 10.1002/qj.828 10.1007/s00382-013-1760-6 10.1175/JTECH-D-15-0097.1 10.1007/s00376-016-6136-5 10.2151/jmsj.79.1059 10.1175/JCLI-D-17-0632.1 10.1007/s00382-006-0169-x 10.1002/2016JD025637 10.1007/s13143-018-0006-2 |
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| Notes | Funding information Space Core Technology Development Program, Ministry of Science and ICT, Grant/Award Number: NRF‐2018M1A3A3A02065661; KMA Research and Development Program, Korea Meteorological Administration, Grant/Award Number: 1365003081 This article is published with the permission of the Controller of HMSO and the Queen's Printer for Scotland. |
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| Title | Polarizing rain types linked to June drought in the Korean peninsula over last 20 years |
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