Back to results

Monterey, California. Naval Postgraduate School

ENSO forced variations of the sea surface temperature and adjusted sea level along the west coast of the United States

Abstract

dc:description.abstract

Daily coastal surface temperature and adjusted sea level data for the period 1955-1988 were used to characterize the surface temperature and adjusted sea level anomalies, and the propagation of features along the west coast of the United States during El Nino-Southern Oscillation (ENSO). The strong ENSO years examined were 1957-58, 1972-73, and 1982-83. Moderate ENSO years used were 1966, 1976, and 1987. To look at regional differences in the signals, the time series of daily coastal surface temperature and adjusted sea level were divided into three distinct regions: the southern region (i.e., Southern California), the central upwelling region (i.e., Central California), and the northern region (i. e., Northern California, Oregon, and Washington). The anomaly series were compared with cross-spectral analysis. Phase speeds and wavenumbers were estimated from the difference in phase between La Jolla and the other stations as a function of frequency band. These were used to characterize the structure of waves associated with the propagation. of the positive surface temperature and adjusted sea level anomalies. These wave characteristics were found to be consistent with coastally trapped internal Kelvin waves, due to their phase speed, wavelength and non-dispersive nature. Phase speeds for frequencies corresponding to 4-20 day periods were 60-100 km/day, based on temperature and sea level. A regression of wavenumber against frequency gives phase speeds of about 65-85 km/day, that is consistent with Kelvin wave theory for typical west coast ocean structure and bathymetry. During ENSO episoddes, strong warm surface temperature anomalies were found to exist along the west coast and were supported by high adjusted sea level anomalies. The use of daily observations was advantageous over traditional monthly data for this analysis.

Degree

thesis:*
Department dc:contributor.department
Oceanography
Grantor dc:publisher
Monterey, California. Naval Postgraduate School
Year dc:date.issued
1993

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Skillman, John B.
Advisors dc:contributor.advisor
  • Schwing, Frank B.
  • Collins, Curtis A.

Rights

dc:rights
Statement dc:rights
  • This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
Language dc:language.iso
en_US

Identifiers

dc:identifier.*
Handle dc:identifier.uri
https://hdl.handle.net/10945/39746
OAI identifier oai:identifier
oai:calhoun.nps.edu:10945/39746

Chain of custody

source
Harvested from
Naval Postgraduate School
Base URL
calhoun.nps.edu/server/oai/request
Last updated
2026-07-27
Source record
OAI-PMH GetRecord
related terms
citation

Skillman, John B.. ENSO forced variations of the sea surface temperature and adjusted sea level along the west coast of the United States. Monterey, California. Naval Postgraduate School, 1993. https://hdl.handle.net/10945/39746