SEASONAL VARIABILITY OF THE INDONESIAN THROUGHFLOW FROM A VARIABLE-GRID GLOBAL OCEAN MODEL

被引：0

作者：

Wang Yong-gang ^{[1
,2
,3
]}

Fang Guo-hong ^{[2
]}

Wei Ze-xun ^{[2
]}

Chen Hai-ying ^{[2
]}

Wang Xin-yi ^{[2
]}

机构：

[1] Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China

[2] State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sci & Numer Modeling, Qingdao 266061, Peoples R China

[3] Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China

来源：

JOURNAL OF HYDRODYNAMICS | 2004年 / 16卷 / 05期

基金：

中国国家自然科学基金;

关键词：

Indonesian throughflow; seasonal variability; global ocean circulation model;

D O I：

暂无

中图分类号：

O3 [力学];

学科分类号：

08 ; 0801 ;

摘要：

The objective of this study is to model the mean and seasonal mass transport of the Pacific to Indian Ocean throughflow using variable-grid global Ocean General Circulation Model (OGCM) with fine grid (1 degrees/6) covering the area from 20 S to 60 degrees N and from 98 E to 156 E. The computations show that Indonesian Throughflow (ITF) mass transport, computed as a sum of through-strait transport, has maximum transport in Sept. (17. 5Sv) and minimum transport in Jan. (9. 5Sv). The annual mean ITF transport amounts to 14. 5Sv. Twenty-two percent of this transport passes through Lombok Strait. Sixty-five percent of this transport passes through Timor Passage. Semi-annual variability is apparent in Lombok and Ombai Straits while annual variability is apparent in Timor Passage.

引用

页码：525 / 532

页数：8

共 22 条

[1] Indonesian Throughflow in a coupled climate model and the sensitivity of the heat budget and deep overturning [J].

Banks, HT .

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2000, 105 (C11) :26135-26150

[2] Shallow throughflow variability in the outflow straits of Indonesia [J].

Chong, JC ;

Sprintall, J ;

Hautala, S ;

Morawitz, WL ;

Bray, NA ;

Pandoe, W .

GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (01) :125-128

[3]

Fang GH, 2004, ACTA OCEANOL SIN, V23, P23

[4] Interbasin freshwater, heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model [J].

Fang, GH ;

Wei, ZX ;

Choi, BH ;

Wang, H ;

Fang, Y ;

Li, W .

SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2003, 46 (02) :149-161

[5] MEASUREMENTS WITHIN THE PACIFIC INDIAN OCEANS THROUGHFLOW REGION [J].

FIEUX, M ;

ANDRIE, C ;

DELECLUSE, P ;

ILAHUDE, AG ;

KARTAVTSEFF, A ;

MANTISI, F ;

MOLCARD, R ;

SWALLOW, JC .

DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1994, 41 (07) :1091-1130

[6] THE WESTERN EQUATORIAL PACIFIC - A WATER MASS CROSSROADS [J].

FINE, RA ;

LUKAS, R ;

BINGHAM, FM ;

WARNER, MJ ;

GAMMON, RH .

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1994, 99 (C12) :25063-25080

[7]

Gordon AL, 1999, J PHYS OCEANOGR, V29, P198, DOI 10.1175/1520-0485(1999)029<0198:TSOTIS>2.0.CO

[8]

[9] A diagnostic study of the Indonesian Throughflow [J].

Lebedev, KV ;

Yaremchuk, MI .

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2000, 105 (C5) :11243-11258

[10]

LEETMAA A., 1995, MON WEA REV, V110, P1863

← 1 2 3 →