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Numerical simulation of tropical cyclone storm surge along the Queensland coast.

Material type: TextTextPublication details: [Townsville]: The University, 1987Description: v. (various pagings): ill., maps, plansDDC classification:
  • F 551.4702209943 HAR
Contents:
Subject: This report is one of a series prepared for the Beach Protection Authority, Brisbane, describing the results of an extensive analysis of the tropical cyclone storm surge hazard along the Queensland coast. This report considers the coastal region near Cairns in North Queensland. A numerical hydrodynamic model of the area, which accounts for variations in water depth, shape of the coastline, and the Great Barrier Reef, as well as changes in cyclone path, speed and intensity, was used as the basis for the analysis
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Holdings
Item type Current library Collection Call number Status Date due Barcode
Books Books Australian Emergency Management Library BOOK F551.4702209943 HAR (Browse shelf(Opens below)) Available 004590205
Books Books Australian Emergency Management Library BOOK F551.4702209943 HAR (Browse shelf(Opens below)) Available 004590213
Books Books Australian Emergency Management Library BOOK F551.4702209943 HAR (Browse shelf(Opens below)) Available 004590221
Books Books Australian Emergency Management Library BOOK F551.4702209943 HAR (Browse shelf(Opens below)) Available 004590239
Books Books Australian Emergency Management Library BOOK F551.4702209943 HAR (Browse shelf(Opens below)) Available 005381124

Includes bibliographies

Spiral binding

Part III: Cairns; Pt. VI: Townsville; Pt. VIII: Mackay; Pt. IX: Rockhampton

This report is one of a series prepared for the Beach Protection Authority, Brisbane, describing the results of an extensive analysis of the tropical cyclone storm surge hazard along the Queensland coast. This report considers the coastal region near Cairns in North Queensland. A numerical hydrodynamic model of the area, which accounts for variations in water depth, shape of the coastline, and the Great Barrier Reef, as well as changes in cyclone path, speed and intensity, was used as the basis for the analysis

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