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Tropical Storm Humberto’s Hybrid Core Revealed By NASA HS3 Mission

September 20, 2013
Image Caption: Dropsonde data from lower and higher levels within Tropical Storm Humberto between Sept. 16 at 1839 UTC and Sept. 17 at 0522 UTC, overlaid on an infrared GOES satellite image of Sept. 17 at 0000 UTC shows temperature (colored circles) and wind barbs at 800 (left) and 400 (right) hPa. Full wind barbs are 10 knots. At 800 hPa, a warm (orange-red colors) core is found at the circulation center ("X"). At 400 hPa, a cold (blue colors) core and circulation center was north-northwest of low level center. Credit: NASA

NASA

NASA’s Global Hawk 872 flew over Tropical Storm Humberto on Sept. 16 and 17 after it was reborn from remnants of its earlier life cycle. Data from NASA 872 showed that the core had a hybrid structure.

NASA’s Global Hawk 872 unmanned aircraft took off at 10:42 a.m. EDT from NASA’s Wallops Flight Facility, Wallops Island, Va., Sept. 16 to investigate newly reformed Tropical Storm Humberto. NASA 872 dispersed dropsondes throughout Humberto and gathered data on the environment of the storm.

A sonde is a device that measures winds, temperature, and humidity. The instrument is called a dropsonde because it is dropped out of the tail of the Global Hawk. The dropsonde is an 11-inch long tube – about the size of the cardboard paper tube for a paper towel roll

HS3 mission scientists at NASA Wallops combined dropsonde data with a satellite image from NOAA’s GOES-East satellite. The dropsonde data, centered on 0000 UTC/8 p.m. EDT Sept. 17, was overlaid over a GOES infrared image and revealed that Humberto was a hybrid storm. “In a typical tropical storm or hurricane, a warm core would be found at most levels,” said Scott Braun, HS3 Mission Principal Investigator from NASA’s Goddard Space Flight Center in Greenbelt, Md. “The structure of Humberto was the result of a union of the tropical storm with an upper-level cold low, so it had a structure that was more of a hybrid of a tropical and extratropical system.”

The image showed temperature at 800 hPa or Hectopascals and 400 hPa. The height of the pressure surfaces varies, but 400 hPa is roughly 7.5 km (24,600 feet) and 800 hPa is about 2.1 km (6,890 feet). The images also showed wind speed and direction using wind barbs.  At 800 hPa, a warm core was found at the center of the circulation while at 400 hPa, a cold core was found with the center of circulation located to the north-northwest of the low level center.

HS3 is a mission that brings together several NASA centers with federal and university partners to investigate the processes that underlie hurricane formation and intensity change in the Atlantic Ocean basin. The HS3 mission will operate in 2013 between Aug. 20 and Sept. 23.

For more information about dropsondes, visit: www.nasa.gov/content/goddard/what-the-heck-is-a-dropsonde/

For more information about NASA’s HS3 mission, visit: www.nasa.gov/HS3

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Source: Rob Gutro, NASA's Goddard Space Flight Center



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