- Tropical and Extratropical Cyclones Research
- Ocean Waves and Remote Sensing
- Oceanographic and Atmospheric Processes
- Geological and Geophysical Studies
- Climate variability and models
- Meteorological Phenomena and Simulations
- Remote Sensing and Land Use
- Geological formations and processes
- Coastal and Marine Dynamics
- Fungal Infections and Studies
- Environmental and Agricultural Sciences
Ocean University of China
2021-2025
Sanya University
2025
Qingdao National Laboratory for Marine Science and Technology
2025
Laoshan Laboratory
2024
Abstract Tropical cyclones (TCs) frequently encounter and interact with mesoscale eddies when moving over the ocean, affecting both of their subsequent evolutions. The South China Sea (SCS) suffers most frequent TCs among global oceans contains active eddies. On average, one TC encounters interacts at least eddy during its lifespan in SCS. Using 27‐year satellite data numerical simulations, we examined response feedback to SCS, based on TCs' interaction 183 cyclonic ocean (COEs) 152...
Abstract Typical tropical cyclone (TC) attributes, including translation speed and intensity, have been demonstrated to affect TC intensification via modulating sea surface temperature (SST) cooling effect underneath TCs, while the of storm size is relatively less explored. Using satellite-observed SST during 2004–2021, we examine on TC-induced anomalies (SSTA) in global TC-active oceans (including western north Pacific, eastern Atlantic, southern Indian Ocean, Pacific), compare their...
The upper ocean provides thermal energy to tropical cyclones. However, the impacts of subsurface on cyclogenesis have been largely overlooked. Here, we show that variabilities associated with variation in 26 °C isothermal depth pronounced over global oceans. sea surface wind stress and its curl before are large enough perturb interior down more than one hundred meters due entrainment upwelling. can fluctuate by tens significantly modify heat content. Consequently, temperature anomalies under...
Abstract Tropical cyclones (TCs) often undergo track turning when moving over the ocean. However, influence of on TC‐ocean interactions remains little explored. This study systematically investigates sea surface temperature (SST) cooling and TC intensification during track‐turning stages in global TC‐active basins 1998–2022. Globally, TCs induce stronger SST than straight‐moving (e.g., −1.53°C vs. −1.08°C for categories 1–2), expand area by 40%–110%, greatly reduce asymmetry left‐turning...
Tropical Cyclones (TCs) are devastating natural disasters. Ocean thermal stratification and TC attributes (e.g., translation speed intensity) have been demonstrated to affect intensification via modulating sea surface temperature (SST) cooling effect. Here, we found that both ocean internal tides storm size could intensification. Analyzing decades of global data, here explore the role on TC-induced anomalies (SSTA) in TC-active oceans. Originating from complex interplays between astronomic...
Temporal variations in diurnal internal tides (ITs) and near-inertial waves (NIWs) the southern South China Sea (SCS) are characterized, based on two 13-month moored current observations. Diurnal ITs, dominated by O1 K1, found to exhibit spring–neap cycles of about 14 days significant seasonal variations. The incoherent components explain 54% 56% total energy band, which further complicates its temporal variabilities. As for NIWs, wind input serves as primary source three strong events...
Abstract Tropical cyclone (TC) Freddy traversed the South Indian Ocean (SIO) in 2023, setting a record for longevity and ranking secondly among historical TCs both accumulated energy potential destructiveness. Freddy’s long lifespan benefited from an anomalously strong Mascarene High, which steered westward along its northern flank, thereby pre-venting it encountering cold water areas. In addition to lifespan, we found experienced record-breaking six rapid intensification (RI) events...
Abstract Breaking of internal lee waves generated by flow‐topography interaction is an important driving mechanism for abyssal mixing. By assuming that lee‐wave‐driven mixing a local process, direct measurements in the past mainly focused on water column over rough topography. In this study, non‐local role remote investigated using mooring observations northwestern Philippine Basin and series 2‐dimensional high‐resolution numerical simulations. We find breaking can generate near‐inertial...