Castaway Jose Salvador: Blame the Tehuantepecer?
By Surfline/Buoyweather Chief Meteorologist Mark Willis
By now you have likely seen the media coverage of Jose Salvador’s story. If not, Jose is the famous shark fisherman that washed up on the shores of the Marshall Islands just days ago. It is estimated that he spent the last ~13 months at sea, but we don’t know for sure. When the Buoyweather meteorology team heard the news that Jose encountered strong north winds that blew him off course after departing from Paredon Viejo (within the Gulf of Tehuantepec), we immediately thought of one thing: The infamous “Tehuantepecer”.
What is a “Tehuantepecer”?
Simply put, a “Tehuantepecer” is one of the most amazing displays of wind in the world. The term is used to describe a phenomenon that brings a narrow area of strong northerly winds to the Gulf of Tehuantepec. These wind events occur when cold fronts from the Gulf of Mexico allow northerly winds to funnel through the 40-km wide Chivela Pass, a narrow gap in the Sierra Madre Mountains in southeastern Mexico.
The “gap flow” associated with a Tehuantepecer typically produces around 12 gale force (greater than or equal to 34kts) wind events in the Gulf of Tehuantepec each cold season, most of which occur between November and March. In addition, there are typically around 6 storm force (greater than or equal to 50kts) events each year (Brennan et al., 2010).
Archived Weather Charts during the Dates in Question
Every meteorologist loves looking at chart archives during past weather events, especially when they start getting media attention like this situation. So, we decided to take a gander at Buoyweather’s historical chart archives during the two time frames that continue to be quoted in the media in reference to when the fishermen went missing: November 17-19, 2012 or December 21, 2012.
November 17-19, 2012: “Tehuantepecer 1”
Our archives suggest that a low end “Tehuantepecer” event occurred during this time. A strong area of high pressure that built south from the eastern half of the United States and through the Gulf of Mexico led to a narrow area of 25-35kt N winds through the Gulf of Tehuantepec during November 17-19, 2012. This was also confirmed by ASCAT satellite observed winds. Buoyweather wave data suggests that the N winds produced very short period, steep waves in the 10-15ft range during this time. In addition, a Gale Warning (issued by the National Hurricane Center’s Tropical Analysis and Forecast Branch or NHC TAFB) was in effect for this area during this time.
December 21, 2012: “Tehuantepecer 2”
Archived weather charts during the second date of interest (December 21, 2012) revealed an even stronger “Tehuantepecer” event. This event was associated with a strong area of high pressure (~1033mb) that built over South Texas behind a cold front that pushed through the Gulf of Mexico. The further south position of the post-frontal high-pressure system was key in making this event stronger than “Tehuantepecer 1” in November. While satellite observations were not readily available in this region on the 21st, Buoyweather chart archives suggested that an area of strong gale to low end storm force winds (40-50kt) were blowing through the Gulf of Tehuantepec during this time. In addition, NHC TAFB had a Storm Warning in effect on the 21st.
Did a “Tehuantepecer” lead to Jose Salvador’s Mayday?
Well, we don’t know for sure and we may never know the answer to that question. However, we are fairly confident that there were potentially very dangerous “Tehuantepecer” North wind events that occurred on both November 17-19, 2012 and December 21, 2012. These events are enough to impact any mariner, especially the storm force event on the 21st.
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