Upwelling events over the Yucatan Shelf must have important implications to the marine biota of the region, by bringing colder and nutrient-rich waters from the Caribbean undercurrents all the way to Campeche, and must play a key role in the heat budget of the region which in spring and summer exhibits high atmospheric temperatures (>35°C).  Northerly cold wind burst events are, More data are needed to investigate both issues, which are still open

Acknowledgments

This work was possible thanks to the financial aid of CONACyT grants: Cátedras CONACyT (1912), Ciencia Básica (257075), Apoyo al Fortalecimiento y Desarrollo de la Infraestructura Científica y Tecnológica (270455).  Special thanks to Gabriel May Uc, Julio Uc Medina and Heber Uc González for their fieldwork support in the oceanic surveys, and to the Instituto EPOMEX for all the facilities provided to carry out this work.  
Funding for the development of HyCOM has been provided by the National Ocean Partnership Program and the Office of Naval Research. Data assimilative products using HyCOM are funded by the U.S. Navy. Computer time was made available by the DoD High-Performance Computing Modernization Program. The output is publicly available at https://hycom.org
This project was funded by the United States Department of Energy, National Energy Technology Laboratory, in part, through a site support contract. Neither the United States Government nor any agency thereof, nor any of their employees, nor the support contractor, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United  States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.