THE EFFECT OF TROPICAL INSTABILITY WAVES ON CO2 SPECIES DISTRIBUTIONS ALONG THE EQUATOR IN THE EASTERN EQUATORIAL PACIFIC DURING THE 1992 ENSO EVENT

被引:46
作者
FEELY, RA
WANNINKHOF, R
COSCA, CE
MCPHADEN, MJ
BYRNE, RH
MILLERO, FJ
CHAVEZ, FP
CLAYTON, T
CAMPBELL, DM
MURPHY, PP
机构
[1] MONTEREY BAY AQUARIUM RES INST,PACIFIC GROVE,CA 93950
[2] NOAA,ATLANTIC OCEANOG & METEOROL LAB,MIAMI,FL 33149
[3] UNIV S FLORIDA,DEPT MARINE SCI,ST PETERSBURG,FL 33701
[4] UNIV MIAMI,ROSENSTIEL SCH MARINE & ATMOSPHER SCI,DIV MARINE & ATMOSPHER CHEM,MIAMI,FL 33149
关键词
D O I
10.1029/93GL03212
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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, CO2 fugacity, total inorganic carbon, total alkalinity, and pH along the equator were measured from 130-degrees-W to 100-degrees-W during 8-15 May 1992. Concurrent moored measurements of surface currents and temperature were also made at 0-degrees, 110-degrees-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 CO2 species, nitrate and hydrographic parameters at the equator.
引用
收藏
页码:277 / 280
页数:4
相关论文
共 41 条
[1]   HIGH-PRECISION MULTIWAVELENGTH PH DETERMINATIONS IN SEAWATER USING CRESOL RED [J].
BYRNE, RH ;
BRELAND, JA .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1989, 36 (05) :803-810
[2]   PHYTOPLANKTON TAXA IN RELATION TO PRIMARY PRODUCTION IN THE EQUATORIAL PACIFIC [J].
CHAVEZ, FP ;
BUCK, KR ;
BARBER, RT .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1990, 37 (11) :1733-1752
[3]   AN ESTIMATE OF NEW PRODUCTION IN THE EQUATORIAL PACIFIC [J].
CHAVEZ, FP ;
BARBER, RT .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1987, 34 (07) :1229-1243
[4]   PRIMARY PRODUCTION AT 47-DEGREES-N AND 20-DEGREES-W IN THE NORTH-ATLANTIC OCEAN - A COMPARISON BETWEEN THE C-14 INCUBATION METHOD AND THE MIXED LAYER CARBON BUDGET [J].
CHIPMAN, DW ;
MARRA, J ;
TAKAHASHI, T .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1993, 40 (1-2) :151-169
[5]  
CLAYTON TD, IN PRESS DEEP SEA RE
[6]  
COX MD, 1980, J PHYS OCEANOGR, V10, P1168, DOI 10.1175/1520-0485(1980)010<1168:GAPODW>2.0.CO
[7]  
2
[8]   MEANDERS AND LONG WAVES IN EQUATORIAL ATLANTIC [J].
DUING, W ;
HISARD, P ;
KATZ, E ;
MEINCKE, J ;
MILLER, L ;
MOROSHKIN, KV ;
PHILANDER, G ;
RIBNIKOV, AA ;
VOIGT, K ;
WEISBERG, R .
NATURE, 1975, 257 (5524) :280-284
[9]   ACOUSTIC DOPPLER CURRENT PROFILING ALONG THE PACIFIC EQUATOR FROM 95-DEGREES-W TO 165-DEGREES-E [J].
ELDIN, G ;
MORLIERE, A ;
REVERDIN, G .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (09) :913-916
[10]   DISTRIBUTION OF CHEMICAL TRACERS IN THE EASTERN EQUATORIAL PACIFIC DURING AND AFTER THE 1982-1983 EL NINO SOUTHERN OSCILLATION EVENT [J].
FEELY, RA ;
GAMMON, RH ;
TAFT, BA ;
PULLEN, PE ;
WATERMAN, LS ;
CONWAY, TJ ;
GENDRON, JF ;
WISEGARVER, DP .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1987, 92 (C6) :6545-6558