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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Main Author: | |
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Format: | Theses |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/30081 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | 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. |
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