scholarly journals Wave number-frequency domain properties of coastal sea level response to alongshore wind stress along the west coast of North America 1980–1984

1987 ◽  
Vol 92 (C11) ◽  
pp. 11761 ◽  
Author(s):  
George R. Halliwell ◽  
J. S. Allen
Keyword(s):  
North America ◽  
Sea Level ◽  
West Coast ◽  
Wave Number ◽  
The West ◽  
Coastal Sea ◽  
Number Frequency ◽  
Alongshore Wind Stress ◽  
Alongshore Wind ◽  
Frequency Domain Properties

scholarly journals Alongshore Wind Forcing of Coastal Sea Level as a Function of Frequency

2006 ◽  
Vol 36 (11) ◽  
pp. 2173-2184 ◽  
Author(s):  
Holly F. Ryan ◽  
Marlene A. Noble
Keyword(s):  
United States ◽  
Frequency Response ◽  
Sea Level ◽  
Response Function ◽  
Wind Field ◽  
Frequency Response Function ◽  
The United States ◽  
The West ◽  
Coastal Sea ◽  
Alongshore Wind

Abstract The amplitude of the frequency response function between coastal alongshore wind stress and adjusted sea level anomalies along the west coast of the United States increases linearly as a function of the logarithm (log10) of the period for time scales up to at least 60, and possibly 100, days. The amplitude of the frequency response function increases even more rapidly at longer periods out to at least 5 yr. At the shortest periods, the amplitude of the frequency response function is small because sea level is forced only by the local component of the wind field. The regional wind field, which controls the wind-forced response in sea level for periods between 20 and 100 days, not only has much broader spatial scales than the local wind, but also propagates along the coast in the same direction as continental shelf waves. Hence, it has a stronger coupling to and an increased frequency response for sea level. At periods of a year or more, observed coastal sea level fluctuations are not only forced by the regional winds, but also by joint correlations among the larger-scale climatic patterns associated with El Niño. Therefore, the amplitude of the frequency response function is large, despite the fact that the energy in the coastal wind field is relatively small. These data show that the coastal sea level response to wind stress forcing along the west coast of the United States changes in a consistent and predictable pattern over a very broad range of frequencies with time scales from a few days to several years.

scholarly journals Nonlinear absolute sea-level patterns in the long-term-trend tide gauges of the West Coast of North America

2020 ◽  
Vol 9 (1) ◽  
pp. 382-397
Author(s):  
Alberto Boretti
Keyword(s):  
North America ◽  
Sea Level ◽  
West Coast ◽  
Tide Gauge ◽  
Relative Rate ◽  
Tide Gauges ◽  
The West ◽  
The Absolute ◽  
Long Term Trend

AbstractThe research issue of which are the present relative and absolute rates of rise and accelerations for North America is here addressed. The data of the 20 long-term-trend (LTT) tide stations of the West Coast of North America with more than 80 years of recorded data are shown. The absolute rates of rise are computed by considering the absolute vertical velocity of Global Navigation Satellite System (GNSS) antennas near the tide gauges, and the relative rate of sea-level rise from the tide gauge signals. The 20 LTT stations along the West Coast of North America show an average relative rate of rise of -0.38 mm/yr., an average acceleration of +0.0012 mm/yr2, and an average absolute rate of rise of +0.73 mm/yr. This is the first paper publishing a comprehensive survey of the absolute sea-level rates of rise along the West Coast of North America using the reliable information of relative sea-level rates of rise from LTT tide gauges plus the absolute subsidence rates from different GNSS antennas close to the tide gauge installations.

Altimeter observations of sea-level variability off the west coast of North America

2004 ◽  
Vol 25 (7-8) ◽  
pp. 1303-1306 ◽  
Author(s):  
J. Y. Cherniawsky ◽  
M. G. G. Foreman ◽  
W. R. Crawford ◽  
B. D. Beckley
Keyword(s):  
North America ◽  
Sea Level ◽  
West Coast ◽  
The West ◽  
Sea Level Variability
Sign in / Sign up

Export Citation Format

Share Document