Woodworth, Philip L, Maqueda, Miguel A Morales, Roussenov, Vassil M ORCID: 0000-0003-4128-9712, Williams, Richard G
ORCID: 0000-0002-3180-7558 and Hughes, Chris W
ORCID: 0000-0002-9355-0233
(2014)
Mean sea-level variability along the northeast American Atlantic coast and the roles of the wind and the overturning circulation.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 119 (12).
pp. 8916-8935.
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2014-Woodworth_et_al_JGR_WNAtl_Coastal_SL_var.pdf - Published version Download (2MB) |
Abstract
The variability in mean sea level (MSL) during 1950-2009 along the northeast American Atlantic coast north of Cape Hatteras has been studied, using data from tide gauges and satellite altimetry and information from the Liverpool/Hadley Centre (LHC) ocean model, thereby providing new insights into the spatial and temporal scales of the variability. Although a relationship between sea level and the overturning circulation can be identified (an increase of approximately 1.5 cm in MSL for a decrease of 1 Sv in overturning transport), it is the effect of the nearshore wind forcing on the shelf that is found to dominate the interannual sea-level variability. In particular, winds are found to be capable of producing low-frequency changes in MSL ("accelerations") in a narrow coastal band, comparable to those observed by the tide gauges. Evidence is presented supporting the idea of a "'common mode" of spatially coherent low-frequency MSL variability, both to the north and south of Cape Hatteras and throughout the northwest Atlantic, which is associated with large spatial-scale density changes from year to year.
Item Type: | Article |
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Uncontrolled Keywords: | sea-level variability, wind forcing, shelf circulation, meridional overturning circulation |
Subjects: | ?? GC ?? ?? QC ?? |
Depositing User: | Symplectic Admin |
Date Deposited: | 22 Jul 2015 10:36 |
Last Modified: | 16 Dec 2022 00:02 |
DOI: | 10.1002/2014JC010520 |
Related URLs: | |
URI: | https://livrepository.liverpool.ac.uk/id/eprint/2017090 |