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TSUNAMI INFORMATION STATEMENT NUMBER 3
NWS PACIFIC TSUNAMI WARNING CENTER EWA BEACH HI
235 PM HST TUE APR 01 2014

TO - CIVIL DEFENSE IN THE STATE OF HAWAII

SUBJECT - TSUNAMI INFORMATION STATEMENT

THIS STATEMENT IS FOR INFORMATION ONLY. NO ACTION IS REQUIRED AT
THIS TIME. HOWEVER... THE TSUNAMI THREAT TO HAWAII IS STILL
BEING EVALUATED.

AN EARTHQUAKE HAS OCCURRED WITH THESE PRELIMINARY PARAMETERS

ORIGIN TIME - 0147 PM HST 01 APR 2014
COORDINATES - 19.8 SOUTH 70.8 WEST
LOCATION - OFF THE COAST OF NORTHERN CHILE
MAGNITUDE - 8.2 MOMENT

EVALUATION

THE PACIFIC TSUNAMI WARNING CENTER HAS ISSUED AN EXPANDING
REGIONAL TSUNAMI WARNING AND WATCH FOR PARTS OF THE PACIFIC
LOCATED CLOSER TO THE EARTHQUAKE. AN EVALUATION OF THE PACIFIC
WIDE TSUNAMI THREAT IS UNDERWAY AND THERE IS A POSSIBILITY THAT
HAWAII COULD BE ELEVATED TO A WATCH OR WARNING STATUS.

IF TSUNAMI WAVES IMPACT HAWAII THEIR ESTIMATED EARLIEST ARRIVAL
TIME IS

0324 AM HST WED 02 APR 2014

We were stationed at pearl sub base and this was one of my fears. That and jaws.

http://pubs.usgs.gov/circ/c1187/

The next wave may be bigger, and the tsunami may last for hours.

Just after 10 p.m. on May 22, 1960, seismologist Jerry Eaton and four companions assembled at the U.S. Geological Survey’s Hawaiian Volcano Observatory on the Island of Hawai’i. Gathering cameras, notebooks, flashlights, and steel measuring tapes, they piled into a Ford station wagon for the 30-mile ride down to Hilo. There they hoped to measure the 1960 Chilean tsunami, which was expected to arrive at about midnight.

The men had good reason to measure this tsunami. Hawai’i had been struck in the past by deadly tsunamis, including ones from Chile in 1837 and 1877 and one from the Aleutian Islands in 1946 that in Hilo alone killed 98 people. Measurements of past tsunamis are commonly used to help identify areas at risk from future tsunamis. Measurements had been made in Hawaii of Aleutian tsunamis, but little was known about the heights of tsunamis from Chile.

In Hilo, Mr. Eaton and his companions stopped to clear their plans with the police and then drove to the Wailuku River Bridge, on the shore of Hilo Bay. They knew that the 1946 Aleutian tsunami had destroyed the bridge there. The men set up an observation post on the new bridge and began measuring the water level beneath it. Just in case, they also planned their own evacuation route, a short sprint to high ground.

Just after midnight, the water under the bridge rose to 4 feet above normal-the first wave of the tsunami had arrived. At 12:46 a.m., the second wave washed under the bridge at a level 9 feet above normal. By 1:00 a.m., the water beneath the bridge had dropped to 7 feet below normal. Mr. Eaton recalls that they then heard an ominous noise, a faint rumble like a distant train, that came from the darkness far out in Hilo Bay. Two minutes later, they began to see the source of the noise, a pale wall of tumbling water, caught in the dim lights of Hilo. The wave grew in height as it moved steadily toward the city, and the noise became deafening.

By 1:04 a.m., the men on the bridge realized that they should run the few hundred feet to high ground. Turning around, they watched the 20-foot-high, nearly vertical front of the wave hit the bridge, and water splashed high into the air. After this wave had passed and they thought it was safe, Mr. Eaton and his companions returned to the bridge and continued to record the water level during several more waves of the tsunami (see diagram below).