# The Impact of Hurricanes on the Oceanographic Conditions in the Exclusive Economic Zone of Cuba

## TL;DR

This study analyzes satellite data to assess how hurricanes affect sea surface temperature and chlorophyll-a levels in Cuba's EEZ, revealing weak cooling effects and increased chlorophyll post-storm, with spatial heterogeneity.

## Contribution

It provides a detailed multi-scale analysis of hurricane impacts on oceanographic conditions in Cuba's EEZ, highlighting mechanisms behind chlorophyll-a changes.

## Key findings

- Hurricanes caused weak SST cooling, mostly under -1°C.
- Post-storm chlorophyll-a increased significantly in the first two weeks.
- Island Mass Effect was 89% higher after hurricanes.

## Abstract

In this work, we analysed the satellite-based responses of sea surface temperature (SST) and chlorophyll-a (chl-a) concentration in the waters of the Exclusive Economic Zone (EEZ) of Cuba to hurricanes that crossed the EEZ between 1998 and 2016. We considered two spatial scales to capture the spatially heterogeneous nature of the effects of hurricanes. A first more fine-grained one where we considered 120 km radius disks centered at every consecutive hurricane position within the EEZ (scale 1) and a second more coarse grained one enclosing the entire EEZ (scale 2). We conclude that the hurricanes induced a weak cooling since 75 and 85% of the SST anomalies at scale 1 and 2, respectively, were smaller than -1{\deg}C. The cooling was mainly caused by the wind, inducing mixing and/or upwelling of subsurface cool waters. The maximum chl-a responses were recorded in the first and second post-storm weeks, with 60% ranging between -0.01 and 0.04 mg m$^{-3}$ at scale 1, and between -0.07 and 0.02 mg m$^{-3}$ at scale 2. During those post-storm weeks SST and chl-a anomalies were 18 and 44% higher at scale 1 than at scale 2, respectively. We argue that the transport of chl-a from the deep chlorophyll maximum and/or the rich coastal waters are the dominant mechanisms determining the post-storm chl-a response in the EEZ. We also found that the magnitude of the Island Mass Effect in the EEZ after the passage of the hurricanes was 89% higher than before its passage.