REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG
The occurence of precipitation in Bandung region can be generated from repeatedly formed <br /> <br /> convective clouds in one diurnal cycle, this events also can be detected as multiple rain peak <br /> <br /> during a day. In satellite and radar imagery, the formation of n...
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id-itb.:300812018-03-15T13:55:18ZREGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG FITRIANI (NIM: 22415004), RACHMY Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/30081 The occurence of precipitation in Bandung region can be generated from repeatedly formed <br /> <br /> convective clouds in one diurnal cycle, this events also can be detected as multiple rain peak <br /> <br /> during a day. In satellite and radar imagery, the formation of new convective cell after <br /> <br /> dissipation stage of predecessors cell around or in the same location indicates a regeneration <br /> <br /> process in these activity. The evolution of daily convective activity were analyzed during <br /> <br /> February - May 2017. The rainfall events that determined using cumulative distribution <br /> <br /> function (CDF) with highest percentages of daily precipitation will be likely to have local <br /> <br /> precipitation with multiple peak. The convective cloud activity initiate in northern Bandung <br /> <br /> then rapidly increased during the day. The regeneration of precipitationg cloud in this study <br /> <br /> are classified into three types based on the number of convective cloud regeneration <br /> <br /> indications, propagation path of convective cloud regeneration and convective cloud intensity <br /> <br /> relative to their predecessors. text |
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The occurence of precipitation in Bandung region can be generated from repeatedly formed <br />
<br />
convective clouds in one diurnal cycle, this events also can be detected as multiple rain peak <br />
<br />
during a day. In satellite and radar imagery, the formation of new convective cell after <br />
<br />
dissipation stage of predecessors cell around or in the same location indicates a regeneration <br />
<br />
process in these activity. The evolution of daily convective activity were analyzed during <br />
<br />
February - May 2017. The rainfall events that determined using cumulative distribution <br />
<br />
function (CDF) with highest percentages of daily precipitation will be likely to have local <br />
<br />
precipitation with multiple peak. The convective cloud activity initiate in northern Bandung <br />
<br />
then rapidly increased during the day. The regeneration of precipitationg cloud in this study <br />
<br />
are classified into three types based on the number of convective cloud regeneration <br />
<br />
indications, propagation path of convective cloud regeneration and convective cloud intensity <br />
<br />
relative to their predecessors. |
format |
Theses |
author |
FITRIANI (NIM: 22415004), RACHMY |
spellingShingle |
FITRIANI (NIM: 22415004), RACHMY REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG |
author_facet |
FITRIANI (NIM: 22415004), RACHMY |
author_sort |
FITRIANI (NIM: 22415004), RACHMY |
title |
REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG |
title_short |
REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG |
title_full |
REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG |
title_fullStr |
REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG |
title_full_unstemmed |
REGENERATION OF PRECIPITATING CONVECTIVE CLOUDS IN BANDUNG |
title_sort |
regeneration of precipitating convective clouds in bandung |
url |
https://digilib.itb.ac.id/gdl/view/30081 |
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1821995627993628672 |