Impact of Sea Surface Temperature and Surface Air Temperature on Maximizing Typhoon Rainfall: Focusing on Typhoon Maemi in Korea

<table class="table-group" id="tab2"><tr><td><table class="table"><tr><td class="thead-hr" colspan="8"><hr/></td></tr><tr class="thead"><td class="align_left">Time</td><td class="align_center">Before 06:00 (11-09-2003)</td><td class="align_center">06:00</td><td class="align_center">12:00</td><td class="align_center">18:00</td><td class="align_center">00:00 (12-09-2003)</td><td class="align_center">06:00</td><td class="align_center">After 06:00 (12-09-2003)</td></tr><tr><td class="thead-hr" colspan="8"><hr/></td></tr><tr><td class="align_left">RH</td><td class="align_center">Original condition</td><td class="align_center">100%</td><td class="align_center">100%</td><td class="align_center">100%</td><td class="align_center">100%</td><td class="align_center">100%</td><td class="align_center">Original condition</td></tr><tr class="table-tr"><td colspan="8"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

<div>Modification of RH in the south boundary condition.</div>

Advances in Meteorology

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Table 2

Table 2: Impact of Sea Surface Temperature and Surface Air Temperature on Maximizing Typhoon Rainfall: Focusing on Typhoon Maemi in Korea 