Collaborative Innovation Center on Forecast and Evaluation of Meteorological
Disasters (CIC-FEMD), Key Laboratory of Meteorological Disaster, Ministry of
Education (KLME), Joint International Research Laboratory of Climate and
Environment Change (ILCEC), Nanjing University of Information Science &
Technology, Nanjing 210044, China
Joint Innovation Center for Modern Forestry Studies, College of Biology and Environment, Nanjing Forestry University, Nanjing 210037, China
Haiming Xu
Collaborative Innovation Center on Forecast and Evaluation of Meteorological
Disasters (CIC-FEMD), Key Laboratory of Meteorological Disaster, Ministry of
Education (KLME), Joint International Research Laboratory of Climate and
Environment Change (ILCEC), Nanjing University of Information Science &
Technology, Nanjing 210044, China
Jing Ma
Collaborative Innovation Center on Forecast and Evaluation of Meteorological
Disasters (CIC-FEMD), Key Laboratory of Meteorological Disaster, Ministry of
Education (KLME), Joint International Research Laboratory of Climate and
Environment Change (ILCEC), Nanjing University of Information Science &
Technology, Nanjing 210044, China
Ning Shi
Collaborative Innovation Center on Forecast and Evaluation of Meteorological
Disasters (CIC-FEMD), Key Laboratory of Meteorological Disaster, Ministry of
Education (KLME), Joint International Research Laboratory of Climate and
Environment Change (ILCEC), Nanjing University of Information Science &
Technology, Nanjing 210044, China
Collaborative Innovation Center on Forecast and Evaluation of Meteorological
Disasters (CIC-FEMD), Key Laboratory of Meteorological Disaster, Ministry of
Education (KLME), Joint International Research Laboratory of Climate and
Environment Change (ILCEC), Nanjing University of Information Science &
Technology, Nanjing 210044, China
Department of Atmospheric and Environmental Science, University at Albany, State University of New York, Albany, NY 12222, USA
Viewed
Total article views: 4,794 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
3,176
1,474
144
4,794
195
214
HTML: 3,176
PDF: 1,474
XML: 144
Total: 4,794
BibTeX: 195
EndNote: 214
Views and downloads (calculated since 17 Jul 2018)
Cumulative views and downloads
(calculated since 17 Jul 2018)
Total article views: 3,158 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,320
707
131
3,158
180
202
HTML: 2,320
PDF: 707
XML: 131
Total: 3,158
BibTeX: 180
EndNote: 202
Views and downloads (calculated since 24 Apr 2019)
Cumulative views and downloads
(calculated since 24 Apr 2019)
Total article views: 1,636 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
856
767
13
1,636
15
12
HTML: 856
PDF: 767
XML: 13
Total: 1,636
BibTeX: 15
EndNote: 12
Views and downloads (calculated since 17 Jul 2018)
Cumulative views and downloads
(calculated since 17 Jul 2018)
Viewed (geographical distribution)
Total article views: 4,794 (including HTML, PDF, and XML)
Thereof 4,542 with geography defined
and 252 with unknown origin.
Total article views: 3,158 (including HTML, PDF, and XML)
Thereof 3,027 with geography defined
and 131 with unknown origin.
Total article views: 1,636 (including HTML, PDF, and XML)
Thereof 1,515 with geography defined
and 121 with unknown origin.
Net heat flux dominates the frontogenesis of the NPSTF from October to December, while oceanic meridional temperature advection contributes equally as much or even more net heat flux in January and February. The atmosphere is critical to frontogenesis through net heat flux and the Aleutian low, the latter of which benefits meridional temperature advection.
Net heat flux dominates the frontogenesis of the NPSTF from October to December, while oceanic...
