5 YEARS CENTRAL PACIFIC SEA-LEVEL FROM IN-SITU ARRAY, SATELLITE ALTIMETER AND NUMERICAL-MODEL

被引：5

作者：

DONOHUE, KA

WIMBUSH, M

ZHU, XL

CHISWELL, SM

LUKAS, R

MILLER, L

HURLBURT, HE

机构：

[1] UNIV HAWAII,JOINT INST MARINE & ATMOSPHER RES,HONOLULU,HI 96822

[2] NOAA,NOS,GEOSCI LAB,N OES11,SILVER SPRING,MD 20910

[3] USN,RES LAB,BAY ST LOUIS,MS 39529

来源：

ATMOSPHERE-OCEAN | 1994年 / 32卷 / 02期

基金：

美国国家科学基金会; 美国海洋和大气管理局;

关键词：

D O I：

10.1080/07055900.1994.9649509

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

Temporal and spatial features of central equatorial Pacific Ocean sea-level variation appear similar, in measurements from two very different systems (one in the ocean and one carried on a satellite), and in results from a numerical model of the region. In particular, there is an interannual cycle: during El Nino, Kelvin waves appear at the equator, and the sea-surface ridge associated with the equatorial current system shifts southward; in non-El Nino years, instability waves appear at 6-degrees-N (strongest around the end of each calendar year), and the ridge shifts to the north. This three-way comparison gives support to both measurement systems and to the numerical model.

引用

页码：495 / 506

页数：12

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