The Influence of Madden–Julian Oscillation on Local-Scale Phenomena over Indonesia during the Western North Pacific and Australian Monsoon Phases

Ida Pramuwardani, H. Hartono, S. Sunarto, A. Sopaheluwakan
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引用次数: 5

Abstract

In this study, geographical Madden–Julian oscillation (MJO) propagation in association with precipitation rate was obtained using lag correlation applied to empirical orthogonal function (EOF) analysis modes 1 and 2 of filtered MJO data. The precipitation rate over Indonesia was provided at day -10 through day +10 in five-day steps during the December, January, and February (DJF) Western North Pacific (WNP) and July, August and September (JAS) Australian (AU) monsoon phases. Connection with local atmospheric factors was then sought through comparison of local precipitation, represented by 3-hourly precipitation, and dynamical processes, represented by multilevel wind, at seven locations across Indonesia. The results show a global MJO contribution toward local-scale phenomena in Tangerang, Surabaya, and Makassar during the DJF-WNP monsoon phase and in Padang, Medan, Surabaya, Makassar, and Kupang during the JAS-AU monsoon phase. Meanwhile, a lack of MJO contribution toward local factors is presumably due to other local through wider atmospheric-scale phenomena which are suspected to have more influence, particularly in Medan, Padang, Manado, and Kupang during the DJF-WNP monsoon phase, and in Manado and Tangerang during the JAS-AU monsoon phase. This research uses a dataset of 15-year series of daily and three-hourly Tropical Rainfall Measuring Mission (TRMM) (3B42 V7 derived) measurements, 850 hPa zonal wind measurements from 30-year reanalysis data from the ERA-Interim reanalysis dataset, and a 15-year series of 12-hourly observational soundings data from seven stations of the Indonesian Meteorological Climatological and Geophysical Agency (BMKG).
北太平洋西部和澳大利亚季风相期间马登-朱利安涛动对印尼局地尺度现象的影响
本研究利用滞后相关性对滤波后MJO数据的经验正交函数(EOF)分析模式1和模式2进行分析,得到MJO的地理传播与降水率的关系。在12月、1月和2月(DJF)西北太平洋(WNP)和7月、8月和9月(JAS)澳大利亚(AU)季风阶段,印度尼西亚的降水率在-10天到+10天以5天的步骤提供。然后,通过比较印度尼西亚七个地点的当地降水(以3小时降水为代表)和动力过程(以多层风为代表),寻求与当地大气因素的联系。结果表明,全球MJO对DJF-WNP季风期丹格朗、泗水和望加锡以及JAS-AU季风期巴东、棉兰、泗水、望加锡和古邦的局地尺度现象有贡献。同时,MJO对局地因子的贡献不足可能是由于其他局地通过更广泛的大气尺度的现象被怀疑具有更大的影响,特别是在DJF-WNP季风阶段在棉兰、巴东、万鸦老和古邦,以及在JAS-AU季风阶段在万鸦老和Tangerang。本研究使用了15年的每日和3小时热带降雨测量任务(TRMM) (3B42 V7衍生)测量数据,850 hPa纬向风测量数据来自ERA-Interim再分析数据集的30年再分析数据,以及印度尼西亚气象气候和地球物理局(BMKG) 7个站点的15年12小时观测探测数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.10
自引率
0.00%
发文量
11
审稿时长
15 weeks
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