Statistical Properties of Cloud Propagation over Sumatra during CPEA-I
Cloud propagation over Sumatra and the surrounding area (10°S-10°N, 70°-120°E) during the Coupling Processes in the Equatorial Atmosphere-I (CPEA-I) campaign (10 April to 9 May 2004) was tracked using brightness temperature (Tb) data from the GOES-9 satellite. The cloud tracking was based on three-d...
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doaj-f1a9e15604824a6fa02f07d2d31a249c2020-11-24T23:25:46ZengUniversitas IndonesiaMakara Journal of Science2339-19952356-08512016-12-0120418119210.7454/mss.v20i4.6706Statistical Properties of Cloud Propagation over Sumatra during CPEA-IAulya Rahayu0Marzuki Marzuki1Mutya Vonnisa2Department of Physics, Faculty of Mathematics and Natural Science, Universitas Andalas, Padang 25163, Indonesia Department of Physics, Faculty of Mathematics and Natural Science, Universitas Andalas, Padang 25163, IndonesiaDepartment of Physics, Faculty of Mathematics and Natural Science, Universitas Andalas, Padang 25163, IndonesiaCloud propagation over Sumatra and the surrounding area (10°S-10°N, 70°-120°E) during the Coupling Processes in the Equatorial Atmosphere-I (CPEA-I) campaign (10 April to 9 May 2004) was tracked using brightness temperature (Tb) data from the GOES-9 satellite. The cloud tracking was based on three-dimensional data with a threshold of Tb < 210 K. During the campaign, westward-moving clouds were more dominant than eastward-moving systems, with a ratio of approximately 4:1. This characteristic coincided with the dominant easterly wind aloft. Most clouds propagated with a speed varying between 4 and 35 m/s, with a mean value of 13.7 m/s. If the westward and eastward propagations were separated, the average duration, speed, and span of the westward (eastward) moving clouds are 7.7 (5.8 h), -14.5 (9.8 m/s), and 435.5 (187.1 km), respectively. The characteristics of cloud propagation during the CPEA-I were influenced by environmental factors such as relative humidity, temperature, the vertical movement of air, and wind shear. Such factors interacted with the inactive and active phases of the Madden-Julian Oscillation.http://journal.ui.ac.id/index.php/science/article/view/6706/3752brightness temperaturecloud propagationMadden-Julian OscillationSumatra |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Aulya Rahayu Marzuki Marzuki Mutya Vonnisa |
spellingShingle |
Aulya Rahayu Marzuki Marzuki Mutya Vonnisa Statistical Properties of Cloud Propagation over Sumatra during CPEA-I Makara Journal of Science brightness temperature cloud propagation Madden-Julian Oscillation Sumatra |
author_facet |
Aulya Rahayu Marzuki Marzuki Mutya Vonnisa |
author_sort |
Aulya Rahayu |
title |
Statistical Properties of Cloud Propagation over Sumatra during CPEA-I |
title_short |
Statistical Properties of Cloud Propagation over Sumatra during CPEA-I |
title_full |
Statistical Properties of Cloud Propagation over Sumatra during CPEA-I |
title_fullStr |
Statistical Properties of Cloud Propagation over Sumatra during CPEA-I |
title_full_unstemmed |
Statistical Properties of Cloud Propagation over Sumatra during CPEA-I |
title_sort |
statistical properties of cloud propagation over sumatra during cpea-i |
publisher |
Universitas Indonesia |
series |
Makara Journal of Science |
issn |
2339-1995 2356-0851 |
publishDate |
2016-12-01 |
description |
Cloud propagation over Sumatra and the surrounding area (10°S-10°N, 70°-120°E) during the Coupling Processes in the Equatorial Atmosphere-I (CPEA-I) campaign (10 April to 9 May 2004) was tracked using brightness temperature (Tb) data from the GOES-9 satellite. The cloud tracking was based on three-dimensional data with a threshold of Tb < 210 K. During the campaign, westward-moving clouds were more dominant than eastward-moving systems, with a ratio of approximately 4:1. This characteristic coincided with the dominant easterly wind aloft. Most clouds propagated with a speed varying between 4 and 35 m/s, with a mean value of 13.7 m/s. If the westward and eastward propagations were separated, the average duration, speed, and span of the westward (eastward) moving clouds are 7.7 (5.8 h), -14.5 (9.8 m/s), and 435.5 (187.1 km), respectively. The characteristics of cloud propagation during the CPEA-I were influenced by environmental factors such as relative humidity, temperature, the vertical movement of air, and wind shear. Such factors interacted with the inactive and active phases of the Madden-Julian Oscillation. |
topic |
brightness temperature cloud propagation Madden-Julian Oscillation Sumatra |
url |
http://journal.ui.ac.id/index.php/science/article/view/6706/3752 |
work_keys_str_mv |
AT aulyarahayu statisticalpropertiesofcloudpropagationoversumatraduringcpeai AT marzukimarzuki statisticalpropertiesofcloudpropagationoversumatraduringcpeai AT mutyavonnisa statisticalpropertiesofcloudpropagationoversumatraduringcpeai |
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