Sari, Qurnia Wulan and Utari, Putri Adia and Setiabudidaya, Dedi and Yustian, Indra and Siswanto, Eko and Iskandar, Iskhaq (2019) Surface chlorophyll-a variations in the Southeastern Tropical Indian Ocean during various types of the positive Indian Ocean Dipole events. International Journal of Remote Sensing, 41 (1). pp. 171-184. ISSN 13665901, 01431161
Preview |
Text
1.c.1.12. Q1-Surface chlorophyll a variations in the Southeastern Tropical Indian Ocean during various types of the positive Indian Ocean Dipole events-Journal Remote Sensing 2019 -plus SJR.pdf Download (3MB) | Preview |
Abstract
Surface chlorophyll-a (chl-a) variation in the Southeastern Tropical Indian Ocean (SETIO) shows di!erent patterns in response to the various types of the Indian Ocean Dipole (IOD) events. Thirteen years of remotely sensed surface chl-a data from the Moderate- resolution Imaging Spectroradiometer (MODIS) were used to eval- uate interannual surface chl-a variation in the SETIO. During the period of analysis (January 2003-December 2015), there were three canonical positive IOD (pIOD) and four pIOD Modoki events. It is found that the spatial patterns of surface chl-a variation were coherent with the pattern of surface wind anomaly, and the sea surface temperature anomaly (SSTA). During canonical pIOD events, high chl-a concentrations were observed in the vicinity of the Sunda Strait and along the coast of western tip of the Java Island around the Cilacap region. Meanwhile, during pIOD Modoki event, surface chl-a concentration was relatively higher and dis- tributed wider than those observed during canonical pIOD event. The analysis shows that relatively weak upwelling event indicated by a deep isothermal layer depth (ILD) during pIOD Modoki events combined with thin barrier layer thickness (BLT) and deep mixed layer provides a favourable condition for an increase in surface chl- a in the SETIO region. Meanwhile, strong upwelling as indicated by shallow ILD combined with thick BLT and shallow mixed layer prevents surface chl-a to increase during canonical pIOD events.
| Item Type: | Article |
|---|---|
| Subjects: | Q Science > Q Science (General) > Q1-295 General |
| Divisions: | 11-Postgraduates Study > 95029-Environmental Science (S3) |
| Depositing User: | Dr Indra Yustian |
| Date Deposited: | 19 Nov 2021 03:24 |
| Last Modified: | 19 Nov 2021 03:24 |
| URI: | http://repository.unsri.ac.id/id/eprint/57453 |
Actions (login required)
 |
View Item |