Long-distance radiation of Rossby Waves from the equatorial current system

Author Posting. © American Meteorological Society, 2021. This article is posted here by permission of [publisher] for personal use, not for redistribution. The definitive version was published in Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. Long-distance radiation of Rossby Waves fro...

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Published in:Journal of Physical Oceanography
Main Authors: Farrar, J. Thomas, Durland, Theodore S., Jayne, Steven R., Price, James F.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society 2021
Subjects:
Online Access:https://hdl.handle.net/1912/28620
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/28620 2023-05-15T16:59:27+02:00 Long-distance radiation of Rossby Waves from the equatorial current system Farrar, J. Thomas Durland, Theodore S. Jayne, Steven R. Price, James F. 2021-05-24 https://hdl.handle.net/1912/28620 unknown American Meteorological Society https://doi.org/10.1175/JPO-D-20-0048.1 Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. (2021). Long-distance radiation of Rossby Waves from the equatorial current system. Journal of Physical Oceanography, 51(6), 1947–1966. https://hdl.handle.net/1912/28620 doi:10.1175/JPO-D-20-0048.1 Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. (2021). Long-distance radiation of Rossby Waves from the equatorial current system. Journal of Physical Oceanography, 51(6), 1947–1966. doi:10.1175/JPO-D-20-0048.1 Pacific Ocean Barotropic flows Instability Planetary waves Rossby waves Topographic effects Article 2021 ftwhoas https://doi.org/10.1175/JPO-D-20-0048.1 2022-05-28T23:04:31Z Author Posting. © American Meteorological Society, 2021. This article is posted here by permission of [publisher] for personal use, not for redistribution. The definitive version was published in Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. Long-distance radiation of Rossby Waves from the equatorial current system. Journal of Physical Oceanography, 51(6), (2021): 1947–1966, https://doi.org/10.1175/JPO-D-20-0048.1. Measurements from satellite altimetry are used to show that sea surface height (SSH) variability throughout much of the North Pacific Ocean is coherent with the SSH signal of the tropical instability waves (TIWs) that result from instabilities of the equatorial currents. This variability has regular phase patterns consistent with freely propagating barotropic Rossby waves radiating energy away from the unstable equatorial currents, and the waves clearly propagate from the equatorial region to at least 30°N. The pattern of SSH variance at TIW frequencies exhibits remarkable patchiness on scales of hundreds of kilometers, which we interpret as being due to the combined effects of wave reflection, refraction, and interference. North of 40°N, more than 6000 km from the unstable equatorial currents, the SSH field remains coherent with the near-equatorial SSH variability, but it is not as clear whether the variability at the higher latitudes is a simple result of barotropic wave radiation from the tropical instability waves. Even more distant regions, as far north as the Aleutian Islands off of Alaska and the Kamchatka Peninsula of eastern Russia, have SSH variability that is significantly coherent with the near-equatorial instabilities. The variability is not well represented in the widely used gridded SSH data product commonly referred to as the AVISO or DUACS product, and this appears to be a result of spatial variations in the filtering properties of the objective mapping scheme. This work was supported by NASA Grants NNX13AE46G, NNX14AM71G, and NNX17AH54G. Article in Journal/Newspaper Kamchatka Kamchatka Peninsula Alaska Aleutian Islands Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Pacific Journal of Physical Oceanography
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language unknown
topic Pacific Ocean
Barotropic flows
Instability
Planetary waves
Rossby waves
Topographic effects
spellingShingle Pacific Ocean
Barotropic flows
Instability
Planetary waves
Rossby waves
Topographic effects
Farrar, J. Thomas
Durland, Theodore S.
Jayne, Steven R.
Price, James F.
Long-distance radiation of Rossby Waves from the equatorial current system
topic_facet Pacific Ocean
Barotropic flows
Instability
Planetary waves
Rossby waves
Topographic effects
description Author Posting. © American Meteorological Society, 2021. This article is posted here by permission of [publisher] for personal use, not for redistribution. The definitive version was published in Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. Long-distance radiation of Rossby Waves from the equatorial current system. Journal of Physical Oceanography, 51(6), (2021): 1947–1966, https://doi.org/10.1175/JPO-D-20-0048.1. Measurements from satellite altimetry are used to show that sea surface height (SSH) variability throughout much of the North Pacific Ocean is coherent with the SSH signal of the tropical instability waves (TIWs) that result from instabilities of the equatorial currents. This variability has regular phase patterns consistent with freely propagating barotropic Rossby waves radiating energy away from the unstable equatorial currents, and the waves clearly propagate from the equatorial region to at least 30°N. The pattern of SSH variance at TIW frequencies exhibits remarkable patchiness on scales of hundreds of kilometers, which we interpret as being due to the combined effects of wave reflection, refraction, and interference. North of 40°N, more than 6000 km from the unstable equatorial currents, the SSH field remains coherent with the near-equatorial SSH variability, but it is not as clear whether the variability at the higher latitudes is a simple result of barotropic wave radiation from the tropical instability waves. Even more distant regions, as far north as the Aleutian Islands off of Alaska and the Kamchatka Peninsula of eastern Russia, have SSH variability that is significantly coherent with the near-equatorial instabilities. The variability is not well represented in the widely used gridded SSH data product commonly referred to as the AVISO or DUACS product, and this appears to be a result of spatial variations in the filtering properties of the objective mapping scheme. This work was supported by NASA Grants NNX13AE46G, NNX14AM71G, and NNX17AH54G.
format Article in Journal/Newspaper
author Farrar, J. Thomas
Durland, Theodore S.
Jayne, Steven R.
Price, James F.
author_facet Farrar, J. Thomas
Durland, Theodore S.
Jayne, Steven R.
Price, James F.
author_sort Farrar, J. Thomas
title Long-distance radiation of Rossby Waves from the equatorial current system
title_short Long-distance radiation of Rossby Waves from the equatorial current system
title_full Long-distance radiation of Rossby Waves from the equatorial current system
title_fullStr Long-distance radiation of Rossby Waves from the equatorial current system
title_full_unstemmed Long-distance radiation of Rossby Waves from the equatorial current system
title_sort long-distance radiation of rossby waves from the equatorial current system
publisher American Meteorological Society
publishDate 2021
url https://hdl.handle.net/1912/28620
long_lat ENVELOPE(160.000,160.000,56.000,56.000)
geographic Kamchatka Peninsula
Pacific
geographic_facet Kamchatka Peninsula
Pacific
genre Kamchatka
Kamchatka Peninsula
Alaska
Aleutian Islands
genre_facet Kamchatka
Kamchatka Peninsula
Alaska
Aleutian Islands
op_source Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. (2021). Long-distance radiation of Rossby Waves from the equatorial current system. Journal of Physical Oceanography, 51(6), 1947–1966.
doi:10.1175/JPO-D-20-0048.1
op_relation https://doi.org/10.1175/JPO-D-20-0048.1
Farrar, J. T., Durland, T., Jayne, S. R., & Price, J. F. (2021). Long-distance radiation of Rossby Waves from the equatorial current system. Journal of Physical Oceanography, 51(6), 1947–1966.
https://hdl.handle.net/1912/28620
doi:10.1175/JPO-D-20-0048.1
op_doi https://doi.org/10.1175/JPO-D-20-0048.1
container_title Journal of Physical Oceanography
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