MJO (Madden-Julian Oscillation) Analysis of the Chlorophyll-a Distribution in Western Waters Bengkulu

2nd International Conference on Tropical and Coastal Region Eco Development 2016

地球科学;生态环境科学

Haryanto, Y.D.^1,2 ; Fitrianti, N.^1 ; Hartoko, A.^2 ; Anggoro, S.^2 ; Zainuri, M.^3

State College of Meteorology Climatology and Geophysics, Jl. Perhubungan 1 No.5 Pondok Aren, Tengerang Selatan

15221, Indonesia^1

Coastal Resource Management, Faculty of Fisheries and Marine Sciences, Diponegoro University, Jl. Imam Bardjo SH No.5, Semarang

50241, Indonesia^2

Department of Marine Science, Faculty of Fisheries and Marine Sciences, Diponegoro University, Jl. Prof.H.Soedharto, SH, Tembalang, Semarang

50275, Indonesia^3

关键词: Conditional probabilities;    Equatorial regions;    High intensity rainfall;    Linear relationships;    Logistics regressions;    Madden-Julian oscillation;    Sea surface temperature (SST);    Temporal distribution;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/55/1/012061/pdf
DOI  :  10.1088/1755-1315/55/1/012061

学科分类：环境科学（综合）

来源: IOP

【 摘 要 】

The global phenomenon Madden-Julian Oscillation (MJO) is one of the dominant oscillation in the equatorial region of the Indian Ocean that oscillates between 30-60 days and experience the process of convection movement from west to east. MJO has a correlation of high intensity rainfall of the area in its path. During his journey eastward, the MJO is influenced by the position of the sun. When the sun in the equatorial MJO moves straight east. Meanwhile, when the position of the sun in the south of the equator, MJO shifted slightly to the south of the equator, known as the propagation of the south-east (south-eastern propagation). When the position of the sun is in the north of the equator, MJO shifted slightly to the north of the equator, known as the propagation of the north-east (north-east of propagation). Waters west of Bengkulu has a huge potential in the fisheries sector, which is situated overlooking the Indian Ocean. The phenomenon MJO influence on rainfall, sea surface temperature, and the concentration of chlorophyll-a. This study aims to look at the temporal distribution of sea surface temperature and chlorophyll- A and decide how MJO relationship with SST and precipitation conditions and increasing the amount of chlorophyll during the phase of the MJO in Bengkulu waters. The dataset used is data of chlorophyll- A which download in oceancolor.gfsc.nasa.gov , sea surface temperature data is used is a model of Kaplan Extended V2, RMM1 index data and RMM2 on www.bom.gov.au and rainfall data of Bengkulu region. The method used is descriptive statistical methods, Conditional Probability and logistics regression. From the above explanation can be said that there is a relationship between the incidence of MJO by the number of chlorophyll-a. Odds the addition of chlorophyll- A have a linear relationship with the duration of the incident MJO in Bengkulu, odds increase the amount of chlorophyll- A in Bengkulu region reaches a threshold value of 0.5, it means that the length occurrence MJO able to identify increasing the number of chlorophyll- A in Bengkulu.