Lichuan Wu

Jul 12, 2024 | agupubs.onlinelibrary.wiley.com | Biao Zhao |Lichuan Wu |Jun Zhang |Guansuo Wang

Supporting Information References , , , , , & (2017). Nonbreaking wave-induced mixing in upper ocean during tropical cyclones using coupled hurricane-ocean-wave modeling. Journal of Geophysical Research: Oceans, 122(5), 3939–3963. https://doi.org/10.1002/2016jc012219 , & (1977). Tropical cyclone minimum sea level pressure/maximum sustained wind relationship for the Western North Pacific. Monthly Weather Review, 105(4), 421–427.

Jul 10, 2024 | onlinelibrary.wiley.com | Chunyi Wu |Lichuan Wu |Yanhui Zheng |Daxing Zuo

CONFLICT OF INTEREST STATEMENT The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest. REFERENCES , & (2008). Atmospheric warming and the amplification of precipitation extremes. Science, 321(5895), 1481–1484. https://doi.org/10.1126/science.1160787 , & (2022).

May 9, 2024 | rmets.onlinelibrary.wiley.com | Ting Lin |Thomas Stefan Spengler |Anna Rutgersson |Lichuan Wu

1 INTRODUCTION Polar lows (PLs) are intense mesoscale cyclones occurring over the subpolar ice-free oceans with a diameter of 150–600 km and a lifetime ranging from 3 to 36 hours (Condron & Renfrew, 2013; Stoll et al., 2018). When PLs make landfall, they usually pose a threat to marine and coastal socio-economic activities, as they are accompanied by severe weather, such as gale-force winds, heavy snow showers, and intense blizzard events (e.g., Moreno-Ibáñez et al., 2021).