Presentasi Lengkap Ina Tews English 2014

SIRENS ACTIVATION AND DEACTIVATION

SOP for decision making

Beware

Prepare

alert

out guidance for evacuation

Meteorological CLimatological and Geophysical Agency Indonesia

Active the

Siren

out guidance for evacuation

out guidance for Alertaway from the coast

and rivers

Information Earthquake :there is no tsunami threat

1. From the southern Indo-Australian Plate to infiltrate the Euro-Asian plates in relative terms, the collision zone in the South Indian Ocean Bali (Insecurity First)

2. As a result of the collision of these plates, in North Bali came up active faults (back arc thrust) which is a destructive earthquake in Bali generator (Second Insecurity)

subduction zone

WHERE WE LIVE?

HISTORY TSUNAMI IN BALIHISTORY TSUNAMI IN BALI

? zona rawan ? Tsunami Sumbawa 1977

400 Died

Tsunami Flores 1992

2300 tewas

Tsunami Banyuwangi 1994

300 Died

Prepare=between 0.5m to 3mAlert=below 0.5m

Beware=above 3m

Sirine in Bali

TJ. BENOA

SEMINYAK

KUTA BTDCKEDONGANAN

SANUR

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

TSUNAMI EVACUATION MAP

Sound of INA TEWS sirens

1.ROUTINE TESTheld on 26th every month at 10.00 local time)

2. TSUNAMI

Note :Sirens function is still developing, so it can connected directly through microphone or radio.

thank you for your attention, and Good day

WEB :www.balisafety.baliprov.go.id

EMAIL:[email protected]

Phone (0361) 251177FAX (0361) 263926 / 261238

Sosial Network

Tsunami generating earthquakes typically have

the following characteristics (trigger of Tsunami) :• The location of the epicenter located at sea.• The depth of the epicenter is relatively

shallow, less than 70 km.• It has a large magnitude M> 7.0 SR• The mechanism of the earthquake is a reverse

fault (thrusting fault) and fault down (normal fault)

sea bottom

sea levelWave spread