STUDI VARIABILITAS KEJADIAN SIKLON TROPIS SERTA HUBUNGANNYA DENGAN EL NIÃO-SOUTHERN OSCILLATION (ENSO) DAN INDIAN OCEAN DIPOLE (IOD) DI PERAIRAN SEKITAR INDONESIA
This final project describes the period, frequency, intensity and also the trajectory of tropical cyclone events near Indonesian Waters which consist of Western North Pasific Ocean, Northern Indian Ocean, and Southern Indian Ocean for 32 years from 1977 untill 2008 based on Joint Typhoon Warni...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/11742 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | This final project describes the period, frequency, intensity and also the trajectory of
tropical cyclone events near Indonesian Waters which consist of Western North Pasific Ocean,
Northern Indian Ocean, and Southern Indian Ocean for 32 years from 1977 untill 2008 based
on Joint Typhoon Warning Center (JTWC) annual report. This study is correlated with the El
Niño-Southern Oscillation (ENSO) events based on sea surface temperature anomalies ENSO
index in Niño-3.4 as well as Indian Ocean Dipole Mode (IODM) events based dipole mode
index in Indian Ocean.
Cross correlation analysis between number of tropical cyclones and ENSO/dipole
mode index was used to observe the relevance between ENSO/IODM and tropical cyclone
frequencies. Tropical cyclone initial position analysis was also used to investigate trajectories
change during El Niño/
In Western North Pasific, there is a tendency where the intense tropical cyclone events
(category 3 untill 5) more (less) frequent during El Niño (
La Niña/dipole mode periods.
La Niña) periods that indicated from
the positive significant correlations (r > 0.7) between number of intense tropical cyclone with
ENSO index. There is also negative significant correlation (r < -0.4) between number of
tropical storms that show the tendency more (less) frequent tropical storms during El Niño (La
Niña) periods. Tropical cyclone formation shifted more to east at 140o
E along with decrease
of tropical cyclone formations in 120o
E-140o
E region during El Niño periods, conversely
happen during La Niña periods. In Northern Indian Ocean there is negative significant
correlations (r < -0.2) between dipole mode index and number of tropical cyclones that
indicated the increase number of tropical cyclones during negative dipole periods. There is no
significant correlations (|r| < 0.1) between dipole mode index and number of tropical cyclones
in Southern Indian Ocean that cause by different occurance period. |
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