Mesoscale Eddies Influence Coral Reef Environments in the Northwest Gulf of Mexico

Author:

McWhorter J. K.1ORCID,Roman‐Stork H. L.23ORCID,Le Hénaff M.14ORCID,Frenzel H.56ORCID,Johnston M. A.7ORCID,Cornec M.68ORCID,Osborne E.1ORCID

Affiliation:

1. NOAA/OAR/Atlantic Oceanographic & Meteorological Laboratory Miami FL USA

2. Global Science & Technology, Inc. Greenbelt MD USA

3. NOAA/NESDIS/STAR/SOCD Laboratory for Satellite Altimetry College Park MD USA

4. Cooperative Institute for Marine and Atmospheric Studies Rosenstiel School for Marine, Atmospheric, and Earth Science, University of Miami Miami FL USA

5. Cooperative Institute for Climate, Ocean, and Ecosystem Studies University of Washington Seattle WA USA

6. NOAA/OAR/Pacific Marine Environmental Laboratory Seattle WA USA

7. NOAA/NOS/Flower Garden Banks National Marine Sanctuary Galveston TX USA

8. School of Oceanography University of Washington Seattle WA USA

Abstract

AbstractCoral reefs globally are experiencing more frequent and severe warming events due to anthropogenic driven climate change. Subtropical reefs experience more seasonal variability than lower latitude reefs making them typically more resilient to climate change. With relatively stable coral cover in comparison to other global coral reefs, Flower Garden Banks National Marine Sanctuary (FGBNMS) in the Gulf of Mexico is a series of 17 reefs and banks located on the continental shelf‐edge containing a variety of shallow (0–30 m) and mesophotic (30–150 m) coral reef habitats. Here, we use satellite data products to associate open ocean Argo float profiles with eddy features over FGBNMS to study the shelf‐edge reef environment spanning nearly two decades (2003–2022). Satellite data show that FGBNMS is frequently influenced (∼15 days/month) by mesoscale eddies. The upper water column variability (0–25 m) is most influenced by the seasonal mixed layer despite eddy interaction. Subsurface seasonal ranges of temperature and salinity are enhanced or suppressed depending on the influence of eddies in relation to the mixed layer depth. Within the mesophotic zone (0–150 m), the largest range of thermal variability between anticyclonic and cyclonic eddies is between 50 and 150 m upwards of 5°C. However, these observed dynamics will likely change as a result of eddy variability associated with projected warming and Loop Current weakening, leading to increased thermal stress in the future.

Funder

National Oceanic and Atmospheric Administration

National Academies of Sciences, Engineering, and Medicine

Publisher

American Geophysical Union (AGU)

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