Identification of Mesoscale Convective Complex (MCC) phenomenon with image of Himawari 8 Satellite and WRF ARW Model on Bangka Island (Case Study: 7-8 February 2016)

5th Geoinformation Science Symposium 2017

地球科学;计算机科学

Rinaldy, Nanda^1 ; Saragih, Immanuel J. A.^1 ; Wandala Putra, Agie^2 ; Redha Nugraheni, Imma^1 ; Wijaya Yonas, Banu^1

Indonesian School of Meteorology, Climatology and Geophysics, STMKG, Indonesia^1

Agency for Meteorology, Climatology and Geophysics, Indonesia^2

关键词: Cloud temperature;    Himawari 8;    Mesoscale convective complexes;    Mesoscale Convective System;    Meteorological observation;    Meteorological station;    Satellite image datas;    WRF ARW;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/98/1/012002/pdf
DOI  :  10.1088/1755-1315/98/1/012002

学科分类：计算机科学（综合）

来源: IOP

【 摘 要 】

Based on monitoring on 7th and 8th February 2016 there has been a flood that occurred due to heavy rainfall in a long time in some areas of Bangka Island. Mesoscale Convective Complex (MCC) is one type of Mesoscale Convective System (MCS). Previous research on MCC mentions that MCC can cause heavy rain for a long time. This study aims to identify the phenomenon of MCC in Bangka Island both in the satellite imagery and the output of the model. In addition, this study was also conducted to determine the effect of MCC on the weather conditions in Bangka Island. The study area in this research is Bangka Island with Pangkalpinang Meteorological Station as the centre of research. The data used in this research are FNL (Final Analysis) data from http://rda.ucar.edu/, Satellite Image of Himawari-8 IR1 Channel from BMKG, and meteorological observation data (synoptic and radiosonde) from Pangkalpinang Meteorological Station. The FNL data is simulated using the WRF-ARW model, verified using observation data and then visualized using GrADS. The results of the analysis of Himawari-8 satellite image data showed that two MCCs occurred on 7th and 8th February 2016 on Bangka Island and the MCC was nocturnal, which appeared at night which then continued until extinction in the morning the next day. In a peak cloud temperature review with the coordinates of Pangkalpinang Meteorological Station (-2,163 N 106,137 E) when 1stMCC and 2ndMCC events ranged from -60°C to -80°C. The result of WRF-ARW model output analysis shows that MCC area has high humidity value and positive vertical velocity value which indicates the potential of heavy rain for a long time.