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
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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...
