Key Laboratory for Aerosol-Cloud-Precipitation of China
Meteorological Administration, Nanjing University of Information Science and
Technology, Nanjing, China
School of Atmospheric Physics, Nanjing University of Information
Science and Technology, Nanjing, China
Gordon G. Shepherd
Centre for Research in Earth and Space Science, York University,
Toronto, Canada
Yuanhe Tang
School of Science, Xi'an University of Technology, Xi'an, China
Lingbing Bu
Key Laboratory for Aerosol-Cloud-Precipitation of China
Meteorological Administration, Nanjing University of Information Science and
Technology, Nanjing, China
School of Atmospheric Physics, Nanjing University of Information
Science and Technology, Nanjing, China
Zhen Wang
Key Laboratory for Aerosol-Cloud-Precipitation of China
Meteorological Administration, Nanjing University of Information Science and
Technology, Nanjing, China
School of Atmospheric Physics, Nanjing University of Information
Science and Technology, Nanjing, China
Viewed
Total article views: 1,478 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
904
492
82
1,478
54
82
HTML: 904
PDF: 492
XML: 82
Total: 1,478
BibTeX: 54
EndNote: 82
Views and downloads (calculated since 28 Feb 2017)
Cumulative views and downloads
(calculated since 28 Feb 2017)
We find double-layer structure events with percentages of 10.32 and 7.25 % compared to total PMCs events, and the mean distances between two peaks are 3.06 and 2.73 km for the NH and SH respectively using SOFIE data from 2007 to 2014. By analysis of the background temperature and water vapour residual profiles, we conclude that the lower layer is a reproduced one formed at the bottom of the upper layer. These structures have close relationships with temperature enhancements and GWs.
We find double-layer structure events with percentages of 10.32 and 7.25 % compared to total...