The relationship between monsoon and sea surface temperature in the western part of Aceh Waters, Indonesia

被引：2

作者：

Imanullah, I. ^{[1
]}

Sofyan, S. ^{[2
]}

Sugianto, S. ^{[3
]}

Haditiar, Y. ^{[4
]}

Rizal, S. ^{[4
,5
]}

机构：

[1] Univ Syiah Kuala, Grad Sch Integrated Coastal Resource Management, Banda Aceh 23111, Indonesia

[2] Univ Syiah Kuala, Fac Agr, Dept Agribusiness, Banda Aceh 23111, Indonesia

[3] Univ Syiah Kuala, Fac Agr, Dept Soil Sci, Banda Aceh 23111, Indonesia

[4] Univ Syiah Kuala, Grad Sch Math & Appl Sci, Banda Aceh 23111, Indonesia

[5] Univ Syiah Kuala, Fac Marine & Fisheries, Dept Marine Sci, Banda Aceh 23111, Indonesia

来源：

2ND ICFAES 2019 INTERNATIONAL CONFERENCE ON FISHERIES, AQUATIC AND ENVIRONMENTAL SCIENCES 2019 IN CONJUNCTIONS WITH THE 6TH ASI 2019 ANNUAL CONFERENCE OF THE ASIAN SOCIETY OF ICHTHYOLOGIST 2019 | 2019年 / 348卷

关键词：

FISHING GROUND LOCATIONS;

D O I：

10.1088/1755-1315/348/1/012066

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

The western part of Aceh waters is part of the eastern Indian Ocean. This waters is a dynamic region where there is differences in sea surface temperature (SST) and significant chlorophyll a concentrations between the southwest (SW) monsoon (June-September) and the northeast (NE) monsoon (December-February). Analysis of SST and chlorophyll-a concentration were used to determine upwelling events in the region. We found that SST in the NE monsoon is lower than that of in the SW monsoon.

引用

页数：7

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