Base reflectivity at 0.5° showing the passage of Hurricane Harvey's eye well east of the Lower Texas coast. |
Visible satellite as Harvey intensified to a devastating Category 4 hurricane just prior to landfall along the Texas Coastal Bend during the early evening of Aug. 25, 2017 |
Harvey Grazes the Lower Valley and King Ranch High Surf, Overwash, and Some Rain are Fortunate Impacts for the Tip of Texas |
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Overview On the beaches of South Padre Island through Port Mansfield, tide run-up and wave set-up brought water into the dunes, but never breached the sea wall. The steady, northwest track of Harvey allowed winds to quickly shift to the west and northwest, which held back a second high tidal surge and would soon push the tide water back into the Gulf. The strong west/northwest winds did produce wave action that briefly topped docks on the Laguna side of South Padre Island during the afternoon, but no structural flooding or damage was reported. Beach erosion was nil - in fact, most of the beach was fully exposed just 36 hours later. Aerial flights to assess and photograph tidal impacts on all Texas beaches can be found here. Inland, the hope for welcome rainfall was never realized; event total rainfall for the populated Rio Grande Valley was less than 0.5 inch. Sustained (1 or 2 minute persistent) tropical storm force winds only occurred over the open Gulf waters and the northern Laguna Madre mainly north of Port Mansfield - generally, 35 to 45 knots. A peak gust to hurricane force (64 knots, or 74 mph) was observed briefly at NOAA Buoy 42020 about 35 miles east/northeast of Port Mansfield, just before 2 PM on the 25th. Sustained winds 20 to 30 mph with gusts to 35 mph or so were common after the center of Harvey passed northeast of the region. The rare, gusty northwest winds brought a "clean" atmosphere, which led to some beautiful mixes of deep blue sky and fair weather clouds especially by Sunday (August 27). Those same west to northwest winds, which gusted often to 30 to 35 mph by day and calmed by night, compressed the hot atmosphere into near to just over triple-digit heat for most of the Valley during the weekend; McAllen/Miller airport would continue its stretch of 100° high temperatures, reaching 75 for the calendar year by the 29th. Finally, while all of southeast and south central Texas removed the word drought from the vocabulary, abnormally dry to drought conditions intensified a bit across most of the Valley. A preliminary text report of observations of wind, rainfall, storm surge/tide, and more can be found here. |
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Collage of surf and tide photos from South Padre during the morning of Aug. 25. Clockwise, from upper left: Boca Chica beach entrance with a foot or so of water into the dunes, at around 10 AM; City beaches just after noon with water receding quickly from dunes; rough and confused surf at resort beaches at 8 AM; foamy water into the dunes at the resort area around 8 AM. |
Deep blue to indigo sky on morning of August 28th over Brownsville, indicating extremely dry air on the backside of Tropical Cyclone Harvey across Deep South Texas and the Rio Grande Valley |
Rainfall estimated from 7 AM August 25 through 7 AM August 26. Note that there was about 0.25 to 0.5 inches near the coast in a few dying feeder bands prior to this time late on August 24 and early on the 25, and additional isolated showers/storms and bands developed along the Rio Grande in southeast Cameron County during the evening of the 26th. Pattern Matters
As the remains of Harvey awoke from the dead and came free of both the dry air and wind shear that had plagued the system all the way into the Bay of Campeche, the Florida ridge edged farther west and became just dominant enough to provide the steering currents to move the resurrected Harvey on a northwest to north/northwest direction from the central Bay of Campeche. This allowed Harvey to quickly gain latitude while threading the needle of rapid intensification over very high "octane" fuel of 2 to 3° above average Gulf waters. The tightening eye strengthened from Category 2 to Category 4 while cruising by the Lower Texas coast. The rest, of course, is catastrophic history for Texas: Harvey made landfall as a 938 mb intensifying Category 4, leveling older buildings in Rockport, then got "hung" between the competing ridges. Feeder bands of rich tropical moisture dumped two feet to 30 inches of rainfall on Houston on the 26th and 27th, followed by another 12 to 20 inches in the actual swirl around the center of a weakened but still efficient rain-producing Harvey on the 28th and 29th as the cyclone edged off of the middle Texas coast. The final catastrophic chapter will be written in time from Corpus to Beaumont, but for the Valley, the close shave reminded us just how much we walk along the fine line between peril and relief. Steering pattern at around ~18,000 feet that helped strengthen and move Harvey toward the middle Texas coast. Fortunately, the strength of the high pressure ridge west of Florida was able to spin Harvey east of the Lower Texas coast. Unfortunately, that same pattern spun Harvey into the Coastal Bend and would slow the system to a crawl for several days, setting the stage for unprecedented, catastrophic flooding in Southeast Texas |