Tropical cyclones (TCs) are expected to intensify in a warming climate as sea surface temperatures (SSTs) rise. Potential intensity (PI), the thermodynamic upper limit on storm strength, has long been used to assess how environmental conditions constrain TC intensity. However, a storm’s realized strength also depends...
Bo-Song Zhang, B. Soden, G. Vecchi et al.· Journal of Climate· 0 citations
Understanding the relationship between the El Niño‐Southern Oscillation (ENSO) phenomenon and North Atlantic tropical cyclone (TC) activity is critical for both seasonal predictions and future projections of TCs. Unfortunately, the satellite observational era (1970‐present) captures too few El Niño events to fully cha...
E. Wallace, Sylvia G. Dee, Andrew Bierbower et al.· Journal of Geophysical Resea...· 0 citations
Marine heatwaves are typically monitored using “foundation” sea surface temperature to ensure a stable climate reference, but this practice neglects the short-lived diurnal extremes occurring within the upper ~10 m of the ocean, where near-surface organisms are exposed and air-sea exchange processes are modulated. Us...
En-Hui Liao, Shiyu Liang, Fengping Wang et al.· Communications Earth & E...· 0 citations
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