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Journal ArticleDOI

Hurricane Hilda, 1964 II. Structure and Budgets of the Hurricane on October 1, 1964

Harry F. Hawkins, +1 more
- 01 Sep 1968 - 
- Vol. 96, Iss: 9, pp 617-636
TLDR
In this paper, the authors used data from five levels (900 to 180 mb) to depict the structure of a mature hurricane and derived estimates of the drag coefficient under hurricane conditions from a different formulation, utilizing the momentum budget in the inflow layer.
Abstract
Aircraft data from five levels (900 to 180 mb.) are used to depict the structure of a mature hurricane. Horizontal analyses, vertical cross sections, and various budgets, which have been prepared from the research flight data only, are presented. New estimates of the drag coefficient under hurricane conditions are derived from a different formulation-utilizing the momentum budget inthe inflow layer.

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Citations
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The JRA-25 Reanalysis

TL;DR: A long-term global atmospheric reanalysis, named "Japanese 25-year Reanalysis (JRA-25) was completed using the Japan Meteorological Agency (JMA) numerical assimilation and forecast system.
Journal ArticleDOI

Reduced drag coefficient for high wind speeds in tropical cyclones

TL;DR: It is found that surface momentum flux levels off as the wind speeds increase above hurricane force, contrary to surface flux parameterizations that are currently used in a variety of modelling applications, including hurricane risk assessment and prediction of storm motion, intensity, waves and storm surges.
Journal ArticleDOI

Air-sea bulk transfer coefficients in diabatic conditions

TL;DR: In this paper, the bulk transfer coefficients of the sea surface have been estimated based on the Owen-Thomson theory on the transfers of heat and mass between a rough surface and the flow above it.
Journal ArticleDOI

The Maximum Potential Intensity of Tropical Cyclones

TL;DR: In this paper, a thermodynamic approach to estimate the maximum potential intensity (MPI) of tropical cyclones is described and compared with observations and previous studies, which requires an atmospheric temperature sounding, SST, and surface pressure; including the oceanic feedback of increasing moist entropy associated with falling surface pressure over a steady SST.
Journal ArticleDOI

Wind-stress coefficients over sea surface from breeze to hurricane

TL;DR: The empirical formula proposed recently relating wind-stress coefficient to wind velocity, C10 = (0.8 + 0.065 U10) × 10−3, appears to be applicable even in hurricanes as discussed by the authors.
References
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Journal ArticleDOI

Mean soundings for the west indies area

TL;DR: Mean aerological data for the West Indies area have been prepared from ten-year records for three stations Mean monthly height, temperature and relative humidity data are tabulated for constant pressure surfaces More detailed information, including density, potential temperature and specific humidity, is shown for the mean annual and the mean hurricane season soundings as mentioned in this paper.
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Observed Ocean Conditions and Hurricane Hilda, 1964

TL;DR: In this article, a 7-day cruise was conducted over the area where hurricane winds had been observed, using the GUS III of the Galveston Biological Laboratory of the Bureau of Commercial Fisheries.
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A study of the filling of hurricane donna (1960) over land

TL;DR: The processes which resulted in the filling of a tropical cyclone over land have been investigated in this paper, where the eddy fluxes of latent and sensible heat and the dissipation of kinetic energy at the earth's surface have been computed for a 3-day period.
Journal ArticleDOI

An analysis of hurricane cleo (1958) based on data from research reconnaissance aircraft

TL;DR: In this article, the structure of hurricane Cleo (1958) is presented, based on observations of wind, temperature, pressure, humidity, clouds, and precipitation obtained from three research reconnaissance aircraft of the National Hurricane Research Project.
Journal ArticleDOI

Budget of angular momentum and energy in tropical cyclones

TL;DR: In this article, the surface stress in tropical storms is computed as a function of the radius, from mean wind data in the troposphere, and the absolute angular momentum budget is carried by the symmetrical part of the circulation near the core, and that the asymmetrical part contributes up to 50 per cent at a distance of 6 deg lat from the center.
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