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: 3,605 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,249
1,260
96
3,605
96
94
HTML: 2,249
PDF: 1,260
XML: 96
Total: 3,605
BibTeX: 96
EndNote: 94
Views and downloads (calculated since 17 Jul 2018)
Cumulative views and downloads
(calculated since 17 Jul 2018)
Total article views: 2,033 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,409
537
87
2,033
87
86
HTML: 1,409
PDF: 537
XML: 87
Total: 2,033
BibTeX: 87
EndNote: 86
Views and downloads (calculated since 24 Apr 2019)
Cumulative views and downloads
(calculated since 24 Apr 2019)
Total article views: 1,572 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
840
723
9
1,572
9
8
HTML: 840
PDF: 723
XML: 9
Total: 1,572
BibTeX: 9
EndNote: 8
Views and downloads (calculated since 17 Jul 2018)
Cumulative views and downloads
(calculated since 17 Jul 2018)
Viewed (geographical distribution)
Total article views: 3,605 (including HTML, PDF, and XML)
Thereof 3,372 with geography defined
and 233 with unknown origin.
Total article views: 2,033 (including HTML, PDF, and XML)
Thereof 1,921 with geography defined
and 112 with unknown origin.
Total article views: 1,572 (including HTML, PDF, and XML)
Thereof 1,451 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...