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Journal ArticleDOI

Global Observations of Oceanic Rossby Waves

Dudley B. Chelton, +1 more
- 12 Apr 1996 - 
- Vol. 272, Iss: 5259, pp 234-238
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TLDR
The TOPEX/POSEIDON satellite altimeter has detected Rossby waves throughout much of the world ocean from sea level signals with ≲10-centimeter amplitude and ≳500-kilometer wavelength.
Abstract
Rossby waves play a critical role in the transient adjustment of ocean circulation to changes in large-scale atmospheric forcing. The TOPEX/POSEIDON satellite altimeter has detected Rossby waves throughout much of the world ocean from sea level signals with ≲10-centimeter amplitude and ≳500-kilometer wavelength. Outside of the tropics, Rossby waves are abruptly amplified by major topographic features. Analysis of 3 years of data reveals discrepancies between observed and theoretical Rossby wave phase speeds that indicate that the standard theory for free, linear Rossby waves is an incomplete description of the observed waves.

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Citations
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The actual measurements at the tide gauges do not support strongly accelerating twentieth-century sea-level rise reconstructions

A. Parker
TL;DR: The most recent estimation by Hay et al. as mentioned in this paper suggests that the sea level has not risen nor accelerated that much, contrary to what is claimed by reconstructions of the Global Mean Sea Level (GMSL) indicating accelerating sea level rates of rise over a century.
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Divergence and dispersion of global eddy propagation from satellite altimetry

TL;DR: In this paper , the divergence of eddy propagation direction and propagation speed was analyzed using satellite altimetry, leading to a leaf-like full-angle pattern in its overall divergence.
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An ocean model’s response to scatterometer winds

TL;DR: In this article, two simulations of the North Atlantic have been run using the POP ocean model for approximately two and one half years each, one simulation used the 1.25° wind product from ECMWF and the other one used the JPL Quikscat 0.75° gridded product.
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A mechanism for the latitudinal dependence of peak‐spectrum sea surface height variability

TL;DR: In this paper, Lin et al. extended their analysis to high-latitude oceanic basins and to include nonlinear eddy effects, by using a linear wave model and a high-resolution model output from the Earth Simulator (OFES).
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Intraseasonal oscillation in global ocean temperature inferred from Argo

TL;DR: In this paper, the authors studied the intraseasonal oscillation (ISO; 14-97-day periods) of temperature in the upper 2000 m of the global ocean based on Argo observations from 2003-2008.
References
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Journal ArticleDOI

Relation between variations in the intensity of the zonal circulation of the atmosphere and the displacements of the semi-permanent centers of action

TL;DR: The Journal of Marine Research (JMR) as mentioned in this paper is an online peer-reviewed journal that publishes original research on a broad array of topics in physical, biological, and chemical oceanography.
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The 1990–1995 El Niño‐Southern Oscillation Event: Longest on Record

TL;DR: In this article, the authors carried out several statisticaJ tests to assess the likelihood that the recent behavior of the Southern Oscillation (SO) is part of a natural decadal timescae variation.
Journal ArticleDOI

TOPEX/POSEIDON mission overview

TL;DR: The TOPEX/POSEIDON satellite as mentioned in this paper is the first space mission specifically designed and conducted for studying the circulation of the world's oceans and has been making observations of the global oceans with unprecedented accuracy since late September 1992.
Journal ArticleDOI

Forcing of intraseasonal Kelvin waves in the equatorial Pacific

TL;DR: In this article, a model was proposed that suggests an ocean-atmosphere coupling by which zonal advection of SST feeds back to the atmosphere; the model duplicates the steplike advance of warm water and westerly winds across the equatorial Pacific at the onset of the El Nino of 1991-1992.
Journal ArticleDOI

Implicit free‐surface method for the Bryan‐Cox‐Semtner ocean model

TL;DR: In this paper, the surface pressure reformulation of the Bryan-Cox-Semtner global ocean model was further improved by eliminating the rigid-lid approximation in favor of an implicit free-surface method for the barotropic mode.
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