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The effect of tropical instability waves on CO 2 species distributions along the equator in the eastern equatorial Pacific during the 1992 ENSO event
Author(s) -
Feely R. A.,
Wanninkhof R.,
Cosca C. E.,
McPhaden M. J.,
Byrne R. H.,
Millero F. J.,
Chavez F. P.,
Clayton T.,
Campbell D. M.,
Murphy P. P.
Publication year - 1994
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/93gl03212
Subject(s) - equator , climatology , sea surface temperature , instability , environmental science , atmospheric sciences , equatorial waves , hydrography , alkalinity , sea surface height , oceanography , geology , latitude , physics , chemistry , geodesy , organic chemistry , mechanics
Tropical instability waves have been shown to have a major impact on the variability of temperature and nutrients along the equatorial wave guide. In order to assess the impact of these features on carbon species distributions during an ENSO event, sea surface temperature, salinity, sigma‐t, nitrate, CO 2 fugacity, total inorganic carbon, total alkalinity, and pH along the equator were measured from 130°W to 100°W during 8–15 May 1992. Concurrent moored measurements of surface currents and temperature were also made at 0°, 110°W. Results indicate that tropical instability waves, with periods of 15 to 20 days and zonal wavelengths of 700–800 km, controlled the observed spatial variability of the CO 2 species, nitrate and hydrographic parameters at the equator.