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Observed Effects of the Northern Hawaiian Islands on Approaching Trade Wind Bands

Observed Effects of the Northern Hawaiian Islands on Approaching Trade Wind Bands PDF Author: Jessica Schauer
Publisher:
ISBN:
Category : Rain and rainfall
Languages : en
Pages : 190

Book Description


Observed Effects of the Northern Hawaiian Islands on Approaching Trade Wind Bands

Observed Effects of the Northern Hawaiian Islands on Approaching Trade Wind Bands PDF Author: Jessica Schauer
Publisher:
ISBN:
Category : Rain and rainfall
Languages : en
Pages : 190

Book Description


The Interaction Between Downslope Flow and Trade-Wind Showers Over the Island of Hawaii During 7-8 August 1990

The Interaction Between Downslope Flow and Trade-Wind Showers Over the Island of Hawaii During 7-8 August 1990 PDF Author: Jeffrey L. Frye
Publisher:
ISBN: 9781423583394
Category : Hawaii
Languages : en
Pages : 105

Book Description
Data from the Hawaiian Rainband Project (HaRP) are used to study the interaction between downslope flow and trade-wind showers over windward sections of the island of Hawaii on 7-8 August 1990. Large-scale conditions produce strong upstream trade-winds of 11 m s-1 which are among the strongest observed during HaRP. In addition, frequent trade-wind showers are responsible for the largest precipitation accumulation between 0300-0700 HST over windward Hawaii during HaRP. The evolution of downslope flow and its interaction with the trade- wind showers under these conditions will be studied in detail. The initiation of downslope flow occurs under dry conditions on the upper slopes by radiative cooling, and then progresses downslope until it arrives over windward lowlands. Here the downslope flow transition is held up by the strong trade winds occurring at the coast. Downslope flow is finally observed over the coast only after a band of rainshowers produces evaporative cooling allowing downslope winds to extend offshore. The evolution of downslope flow afterwards is affected by rainshowers. Vertical mixing associated with rainshowers transports trade- wind momentum into the weak downslope flow layer, replacing westerly winds with strong easterly winds. At the surface, a clear increase in temperature and moist static energy is observed as potentially warmer air aloft mixes with the surface layer. This temporary destruction of downslope flow produces an oscillation of the drainage front from 5-8 km offshore to 10 km inland.

The Effects of the Island of Hawaii on the Trade Winds and the Trade Wind Inversion

The Effects of the Island of Hawaii on the Trade Winds and the Trade Wind Inversion PDF Author: Sheryl Renee Fellbaum
Publisher:
ISBN:
Category : Atmospheric circulation
Languages : en
Pages : 172

Book Description


Scientific and Technical Aerospace Reports

Scientific and Technical Aerospace Reports PDF Author:
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 968

Book Description


Meteorological and Geoastrophysical Abstracts

Meteorological and Geoastrophysical Abstracts PDF Author:
Publisher:
ISBN:
Category : Astrophysics
Languages : en
Pages : 480

Book Description


Journal of the Meteorological Society of Japan

Journal of the Meteorological Society of Japan PDF Author: Nihon Kishō Gakkai
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 452

Book Description


Elementary Meteorology

Elementary Meteorology PDF Author: William Morris Davis
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 392

Book Description


Meteorology for Naval Aviators

Meteorology for Naval Aviators PDF Author: United States. Office of the Chief of Naval Operations
Publisher:
ISBN:
Category : Meteorology in aeronautics
Languages : en
Pages : 228

Book Description


Monthly Weather Review

Monthly Weather Review PDF Author:
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 1020

Book Description


Selected Water Resources Abstracts

Selected Water Resources Abstracts PDF Author:
Publisher:
ISBN:
Category : Water
Languages : en
Pages : 622

Book Description