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Department of Oceanography

Estimating the upper ocean vertical temperature structure from surface temperature as applied to the southern Benguela

Abstract

dc:description.abstract

Underwater Sound Velocity Profiles (SVP) are used throughout the world by their respective navies for submarine and surface vessel strategic operations and exercises. Together with the sonar equations, the sound velocity profiles are of paramount importance to solve underwater sound detectability problems as they provide insight into the highly variable sound transmission loss. Oceanographic records of sea temperature-depth profiles are ordinarily incorporated into a sonar propagation model to determine the sound level at any point (range and depth). The ability to predict these environmental conditions with a defined level of confidence and accuracy significantly increases the situational awareness to in-theatre naval operators and fleet planners. The hypothesis in this thesis is that thermal characteristics of the water column in the southern Benguela can be numerically modeled and deduced from a single Sea Surface Temperature (SST) value, if provided with sufficient historic temperature-depth profiles for that region. For operational use, the SST would ideally be provided from near real time remotely sensed satellite derived data.

Degree

thesis:*
Grantor dc:publisher.institution
Department of Oceanography
Year dc:date.issued
2012

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Wainman, Carl Kevin

Rights

Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/11427/10915
OAI identifier oai:identifier
oai:open.uct.ac.za:11427/10915

Chain of custody

source
Harvested from
University of Cape Town
Base URL
open.uct.ac.za/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
related terms
citation

Wainman, Carl Kevin. Estimating the upper ocean vertical temperature structure from surface temperature as applied to the southern Benguela. Department of Oceanography, 2012. http://hdl.handle.net/11427/10915