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Cadan Plasa

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Mediterranean Marine Heatwaves: Atmospheric Drivers and Ocean Feedback

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By Nikolaos Skliris, Ligin Joseph, Cadan Plasa
| brnw.ch
3.6.1. Major Patterns of Variability The signals presented in are relatively weak, and wind speed anomalies are about as negative after an event as they are before an event, despite the increased LHF signals after an event, which imply strong changes in either the humidity gradient or wind speed. This indicates that this may not be an appropriate method of analysing atmospheric patterns during an MHW event.
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