Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5

Local climate effects of Tibetan Plateau Ozone Valley (OVTP) were investigated by numerical simulations using Community Atmosphere Model version 5.1.1 (CAM5). After a 20-year spin-up period, two additional 10-year experiments were conducted. CAM5 was driven by monthly mean climatological ozone in co...

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Main Authors: Zhenkun Li, Hao Qin, Dong Guo, Shunwu Zhou, Ying Huang, Yucheng Su, Linwei Wang, Yang Sun
Format: Article
Language:English
Published: Wiley 2017-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2017/9383495
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author Zhenkun Li
Hao Qin
Dong Guo
Shunwu Zhou
Ying Huang
Yucheng Su
Linwei Wang
Yang Sun
author_facet Zhenkun Li
Hao Qin
Dong Guo
Shunwu Zhou
Ying Huang
Yucheng Su
Linwei Wang
Yang Sun
author_sort Zhenkun Li
collection DOAJ
description Local climate effects of Tibetan Plateau Ozone Valley (OVTP) were investigated by numerical simulations using Community Atmosphere Model version 5.1.1 (CAM5). After a 20-year spin-up period, two additional 10-year experiments were conducted. CAM5 was driven by monthly mean climatological ozone in control experiment (CE) and OVTP in the sensitivity experiment (SE) was removed from May to September. After the removal of OVTP, South Asian High (SAH) becomes more robust and colder from June to August, especially in June. The reason for enhancement of SAH is that removal of OVTP increasing ozone in 200–30 hPa leads to significant enhancement of longwave and shortwave radiative heating rate in SAH region in June, and then enhancement of horizontal divergence resulting from the radiative warming leads to strengthening of SAH influenced by the Coriolis force, while the colder SAH is primarily caused by dynamic processes. Adiabatic expansion and ascending movement mainly bring about temperature decrease in SAH after OVTP removal, but the thermodynamic process related to radiative heating offsets part of the cooling response.
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institution Kabale University
issn 1687-9309
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language English
publishDate 2017-01-01
publisher Wiley
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series Advances in Meteorology
spelling doaj-art-21095e23623a4ac2abe0d25a72795e292025-02-03T01:23:15ZengWileyAdvances in Meteorology1687-93091687-93172017-01-01201710.1155/2017/93834959383495Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5Zhenkun Li0Hao Qin1Dong Guo2Shunwu Zhou3Ying Huang4Yucheng Su5Linwei Wang6Yang Sun7Shanghai Climate Center, Shanghai 200030, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, ChinaShanghai Public Meteorological Service Center, Shanghai 200030, ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, ChinaLocal climate effects of Tibetan Plateau Ozone Valley (OVTP) were investigated by numerical simulations using Community Atmosphere Model version 5.1.1 (CAM5). After a 20-year spin-up period, two additional 10-year experiments were conducted. CAM5 was driven by monthly mean climatological ozone in control experiment (CE) and OVTP in the sensitivity experiment (SE) was removed from May to September. After the removal of OVTP, South Asian High (SAH) becomes more robust and colder from June to August, especially in June. The reason for enhancement of SAH is that removal of OVTP increasing ozone in 200–30 hPa leads to significant enhancement of longwave and shortwave radiative heating rate in SAH region in June, and then enhancement of horizontal divergence resulting from the radiative warming leads to strengthening of SAH influenced by the Coriolis force, while the colder SAH is primarily caused by dynamic processes. Adiabatic expansion and ascending movement mainly bring about temperature decrease in SAH after OVTP removal, but the thermodynamic process related to radiative heating offsets part of the cooling response.http://dx.doi.org/10.1155/2017/9383495
spellingShingle Zhenkun Li
Hao Qin
Dong Guo
Shunwu Zhou
Ying Huang
Yucheng Su
Linwei Wang
Yang Sun
Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5
Advances in Meteorology
title Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5
title_full Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5
title_fullStr Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5
title_full_unstemmed Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5
title_short Impact of Ozone Valley over the Tibetan Plateau on the South Asian High in CAM5
title_sort impact of ozone valley over the tibetan plateau on the south asian high in cam5
url http://dx.doi.org/10.1155/2017/9383495
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