AWAN HUJAN DI SERPONG : PENGAMATAN DENGAN BOUNDARY LAYER RADAR

Findy Renggono

Abstract


Kebanyakan kejadian hujan di Serpong, Indonesia (6.4°S, 106.7°E) terjadi setelah lewat tengah hari, walaupun demikian hasil pengamatan dengan penakar hujan otomatis selama 6 tahun menunjukkan adanya puncak hujan di pagi hari. Dari struktur awannya
yang dipantau oleh BLR menunjukkan bahwa awan di pagi hari yang muncul adalah
kebanyakan dari jenis awan Stratiform. Pada tulisan ini akan disajikan kajian statistik dari jenis awan yang muncul di wilayah ini.

Most of the precipitation in Serpong (6.4°S, 106.7°E), Indonesia were occurred in the afternoon, however from the 6 years observation by using automatic rain gauge shows another peak of precipitation in the morning. In this paper, the vertical structure of the
precipitating cloud appeared in this area will be analyzed statistically using the data from Boundary Layer Radar (BLR) observation. The result shows that for the morning precipitation, the occurrence of the stratiform-type clouds were dominant.

Keywords


awan, hujan, radar

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DOI: http://dx.doi.org/10.29122/jstmc.v1i1.2105

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