Examination of the Expendable Digital Dropsonde–Derived Vertical Velocities from the Tropical Cyclone Intensity (TCI) Experiment

Author:

Nelson T. Connor1,Harrison Lee1,Corbosiero Kristen L.2

Affiliation:

1. Atmospheric Sciences Research Center, University at Albany, State University of New York, Albany, New York

2. Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, Albany, New York

Abstract

Abstract The newly developed expendable digital dropsonde (XDD) allows for high spatial and temporal resolution data collection in tropical cyclones (TCs). In 2015, a total of 725 XDDs were launched into Hurricanes Marty (27–28 September), Joaquin (2–5 October), and Patricia (20–23 October) as part of the Tropical Cyclone Intensity (TCI) experiment. These dropsondes were launched from a NASA WB-57 at altitudes above 18 km, capturing the full depth of the TCs to the tropopause. This study documents the vertical velocity distributions observed in TCI using the XDDs and examines the distributions altitudinally, radially, and azimuthally. The strongest mean or median XDD-derived vertical velocities observed during TCI occurred in the upper levels and within the cores of the three TCs. There was little azimuthal signal in the vertical velocity distribution, likely due to sampling asymmetries and noise in the data. Downdrafts were strongest in Joaquin, while updrafts were strongest in Patricia, especially within the eyewall on 23 October. Patricia also had an impressive low-level (<2 km) updraft that exceeded 10 m s−1 associated with a shallow, overturning, radial circulation in the secondary eyewall.

Funder

Office of Naval Research

Publisher

American Meteorological Society

Subject

Atmospheric Science

Reference53 articles.

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3. Berg, R. , 2016b: National Hurricane Center Tropical Cyclone Report: Hurricane Marty (26–30 September 2015). NHC Rep. EP172015, 17 pp., https://www.nhc.noaa.gov/data/tcr/EP172015_Marty.pdf.

4. Vertical motion characteristics of tropical cyclones determined with airborne Doppler radial velocities;Black;J. Atmos. Sci.,1996

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