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).

Apr 18, 2023 | frontiersin.org | Lichuan Wu |Jing Ma |Hu Yang

Jiajie Chen1,2, Ronglin Li1,2, Shen Xie1,2, Jiaqi Wei1,2 and Jian Shi1,2*1Frontier Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Physical Oceanography Laboratory, Ocean University of China, Qingdao, China2College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao, ChinaWarm blobs are persistently warmer-than-normal seawaters over the Northeast Pacific (NEP), which cause substantial impacts on marine ecosystems and climate.

Mar 28, 2023 | frontiersin.org | Beijing Normal |Lichuan Wu |Hu Yang |Zhiqiang Gong

1 IntroductionThe Hadley circulation (HC), one of the most significant global circulation cells, is generated when the Earth is heated unevenly by the sun (Hadley, 1735; Bjerknes, 1966). One branch of the HC rises around the equator, while the other two descend at around 30° south and north. i.e., a closed circulation is formed in each hemisphere (Oort and Rasmusson, 1970; Held and Hou, 1980).