首页> 外文会议>Asian conference on remote sensing;ACRS >INDONESIAN RAINFALL DIURNAL CYCLE ANALYSIS USING SATELLITE DATA: A CASE STUDY IN JAVA ISLAND AND SURROUNDING AREAS
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INDONESIAN RAINFALL DIURNAL CYCLE ANALYSIS USING SATELLITE DATA: A CASE STUDY IN JAVA ISLAND AND SURROUNDING AREAS

机译:利用卫星数据进行印尼降雨日循环的分析:以爪哇岛和周边地区为例

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Precipitation is one element of climate that mostly studied in Indonesia because it has a very high diversity both temporal (time) as well as spatial (place). The diurnal cycle is one of the important factors in the occurrence of rain in the islands of Indonesia that have an impact on regional rainfall patterns in Indonesia. The diurnal cycle of precipitation is an essential component of the tropical climate and one of the predominant components of atmospheric variations. The aims of this research were to determine and analyze the spatial patterns and the characteristics of rainfall diurnal cycle in Java Island and the surrounding areas (Java Island, Java Sea and Indian Ocean) using remote sensing data. In this study, data from Tropical Rainfall Measuring Mission satellite (TRMM) Precipitation Radar level 2A25 and wind data from National Centers for Environmental Prediction (NCEP) for 5 years period from 2007 to 2011 are used. The results of this research are the spatial patterns of daily rainfall in Java Island and the surrounding areas are different between land and sea. In the land, rain generally occur in the afternoon (12.00 to 18.00 LT), whereas in the ocean (the Java Sea and Indian Ocean) generally occur at midnight and noon (00.00 to 12.00 LT). The characteristics of rainfall diurnal cycle in Java Island and the surrounding areas are effected by land-sea physical properties, day-night cycle and by land-sea location.
机译:降水是印度尼西亚主要研究的气候要素之一,因为它在时间(时间)和空间(地点)方面都有很高的多样性。昼夜周期是印度尼西亚岛屿降雨发生的重要因素之一,这对印度尼西亚的区域降雨模式有影响。降水的昼夜周期是热带气候的重要组成部分,也是大气变化的主要组成部分之一。这项研究的目的是利用遥感数据确定和分析爪哇岛及其周边地区(爪哇岛,爪哇海和印度洋)的降雨日周期的空间格局和特征。在这项研究中,使用了2007年至2011年这5年期间热带雨量测量任务卫星(TRMM)降水雷达2A25级的数据和国家环境预测中心(NCEP)的风数据。这项研究的结果是爪哇岛每天降雨的空间格局,而陆地和海洋周围的地区是不同的。在陆地上,降雨通常发生在下午(中午12:00至18.00 LT),而在海洋(爪哇海和印度洋)中通常在午夜和正午(LT 00.00至12.00 LT)发生。爪哇岛及周边地区降雨的昼夜周期特征受陆海物理特性,昼夜周期和陆海位置的影响。

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