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Author : National Hurricane and Experimental Meteorology Laboratory
Publisher : Unknown
Page : 198 pages
File Size : 53,9 Mb
Release : 1976
Category : Florida Area Cumulus Experiment
ISBN : UIUC:30112104115750
Author : National Hurricane and Experimental Meteorology Laboratory
Publisher : Unknown
Page : 192 pages
File Size : 41,5 Mb
Release : 1977
Category : Florida Area Cumulus Experiment
ISBN : UIUC:30112097119207
Author : United States. Environmental Data Service
Publisher : Unknown
Page : 212 pages
File Size : 48,7 Mb
Release : 1978
Category : Weather control
ISBN : UCSD:31822039164033
Author : Andrew I. Watson
Publisher : Unknown
Page : 238 pages
File Size : 41,6 Mb
Release : 1981
Category : Convection (Meteorology)
ISBN : UIUC:30112104608747
A reliable method is presented for the prediction of convective precipitation in south Florida. Total area diverence is statistically related to area rainfall as derived by radar in a mesoscale region on the order of 1400 sq km. Various network grids and sizes are examined to find the best scale to measure total area divergence. The response of visible clouds to surface convergence is investigated with time-lapse photographs taken in the FACE mesonetwork. One case study of a convective storm complex as measured by Doppler radar and surface pressure data is presented. Finally, vertical adjustment factors are determined for surface winds under varying meteorological conditions and time of day. (Author).
Author : Anonim
Publisher : Unknown
Page : 158 pages
File Size : 40,8 Mb
Release : 2024-06-16
Category : Hurricanes
ISBN : UCSD:31822008873325
Author : Victor Wiggert
Publisher : Unknown
Page : 96 pages
File Size : 48,8 Mb
Release : 1976
Category : Radar meteorology
ISBN : UCSD:31822031474653
Author : Anonim
Publisher : Unknown
Page : 932 pages
File Size : 41,6 Mb
Release : 1987
Category : Meteorology
ISBN : CUB:U183008861125
Author : Michael S. Moss
Publisher : Unknown
Page : 168 pages
File Size : 41,9 Mb
Release : 1977
Category : Hurricane Eloise, 1975
ISBN : UCSD:31822009292814
Extrapolation of the data to the surface yields a stress that agrees very well with that calculated from a diagnostic application of the Deardorff parameterization scheme. The virtual heat flux profile, determined entirely from conventional measurements, is fairly consistent with that observed in the fair weather trade wind regime. From near-surface extrapolated momentum and virtual heat fluxes, a Monin-Obukov length is computed to indicate that the low-layer turbulence is principally shear-induced. This indication is substantiated by the budget of turbulence kinetic energy, which shows an overall predominance of shear over buoyancy production. In the lowest levels there is an approximate balance among shear production, convergence of the vertical transport, and viscous dissipation of the turbulence kinetic energy. At the upper mixed-layer levels, all of the calculable production terms are negligible in comparison with destruction through dissipation.
Author : Anonim
Publisher : Unknown
Page : 1042 pages
File Size : 50,8 Mb
Release : 1976
Category : Aeronautics
ISBN : UVA:X004872601
Author : Patrick T. Gannon
Publisher : Unknown
Page : 100 pages
File Size : 52,8 Mb
Release : 1978
Category : Sea breeze
ISBN : MINN:20000003509862
A two-dimensional numerical sea breeze model that includes radiation and heat budget physics is used to study sea breeze circulations affected by South Florida surface and cloud conditions. Sensitivity experiments show major differences in the intensities and inland penetrations that result from prescribed distributions of surface and cirrus cloud properties. A case study experiment for July 16, 1975, provides a measure of the importance of surface and cumulus cloud properties that were observed or deduced for this one day. Significant differences exist between the model version using a surface heat budget formulation and the version using prescribed thermal forcing. The strength of the sea breeze predicted with the heat budget formulation decreases with increasing initial basic state wind speeds, while the opposite effect occurs with thermal forcing. Soil moisture is the dominant controlling surface property, followed by albedo and thermal inertia. Cirrus clouds can prevent the evolution of the sea breeze when the geometric thickness of cirrus exceeds 2 km. A case study demonstrates the importance of cumulus cloud shielding of the surface from solar radiation. The mesoscale sea breeze convergence zone is seen to evolve adjacent to organized cloud fields, but not necessarily coincident with them. This is an important consideration when sea breeze models are verified with observed cloud fields.
Author : Anonim
Publisher : Unknown
Page : 181 pages
File Size : 41,8 Mb
Release : 1984
Category : Rain and rainfall
ISBN : OCLC:7833041
Author : Anonim
Publisher : Unknown
Page : 340 pages
File Size : 53,8 Mb
Release : 1982
Category : Hail
ISBN : UOM:39015013049872
Author : Anonim
Publisher : Unknown
Page : 334 pages
File Size : 42,9 Mb
Release : 1982
Category : Thunderstorms
ISBN : PSU:000024170505
Author : Anonim
Publisher : Unknown
Page : 2248 pages
File Size : 52,5 Mb
Release : 1978
Category : Government publications
ISBN : UIUC:30112063912759
Author : United States. Superintendent of Documents
Publisher : Unknown
Page : 1228 pages
File Size : 45,7 Mb
Release : 1978
Category : Government publications
ISBN : UCR:31210024274605
February issue includes Appendix entitled Directory of United States Government periodicals and subscription publications; September issue includes List of depository libraries; June and December issues include semiannual index
