HRD's "Synoptic Flow" experiments use dropwindsondes to gather vertical profiles of wind, temperature, and humidity within 1,000 km of hurricanes. The experiment is typically conducted over the data-sparse oceanic regions of the western Atlantic or Gulf of Mexico roughly 48-72 hours before the projected landfall of a mature hurricane on the coast of the United States. The dropwindsondes define the hurricane's surrounding large-scale flow, particularly in the 300-700 mb middle tropospheric layer - the layer most directly related to tropical cyclone motion.
Key reference:
Burpee, R. W., J. L. Franklin, S. J. Lord, R.E. Tuleya, and S.D. Aberson, 1996: "The impact of Omega dropwindsondes on operational hurricane track forecast models." Bull. Amer. Meteor. Soc., 77, 925-933.
Franklin, J. L., and M. DeMaria, 1992: "The impact of Omega dropwindsonde observations on barotropic hurricane track forecasts." Mon. Wea. Rev., 120, 381-391.
Aberson, S.D., and M. DeMaria, 1994: "Verification of a nested barotropic hurricane track forecast model (VICBAR)." Mon. Wea. Rev., 122, 2804-2815.
Bender, M. A., R. J. Ross, R. E. Tuleya, and Y. Kurihara, 1999: "Improvements in tropical cyclone track and intensity forecasts using the GFDL initialization system" Mon. Wea. Rev., 121, 2046-2061.
Lord, S. J., 1993: "Recent developments in troical cyclone track forecasting with the NMC global analysis and forecasting system." Preprints of the 20th Conference on Hurricanes and Tropical Meteorology, San Antonio, Amer. Meteor. Soc., 290-291.
Hock, T.F., and J.L.Franklin, 1999: "The NCAR GPS dropwindsonde." Bull. American Met. Soc.,80, 407-420.
Aberson, S.D., and J.L.Franklin, 1999: "Impact on hurricane track and intensity forecasts of GPS dropwindsondes observations from the first-season fligs of the NOAA Gulfstream IV jet aircraft." Bull. American Met. Soc.,80, 421-428.
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