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...

Full description

Bibliographic Details
Main Authors: Aulya Rahayu, Marzuki Marzuki, Mutya Vonnisa
Format: Article
Language:English
Published: Universitas Indonesia 2016-12-01
Series:Makara Journal of Science
Subjects:
Online Access:http://journal.ui.ac.id/index.php/science/article/view/6706/3752
id doaj-f1a9e15604824a6fa02f07d2d31a249c
record_format Article
spelling 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
_version_ 1725556168046149632