Dang! CNN
Tsunami advisories lifted in US after waves hit Tonga following volcanic
eruption
An underwater volcano in the South Pacific erupted violently on Saturday,
causing tsunamis to hit Hawaii, Japan, and Tonga's largest island, Tongatapu
-- sending waves flooding into the capital.
The
Hunga-Tonga-Hunga-Ha'apai volcano, about 30 kilometers (18.6 miles) southeast of Tonga's Fonuafo'ou island,
first erupted on Friday and a second time on Saturday around 5:26 p.m. local
time, according to CNN affiliate Radio New Zealand (RNZ).
The eruptions sent a plume of ash, gas and steam 20 kilometers (12.4 miles)
into the air, according to RNZ. Satellite imagery showed a massive ash cloud
and shockwaves spreading from the eruption. Ash was falling from the sky in
the Tonga capital, Nuku'alofa, Saturday evening and phone connections were
down.
The eruption caused a severe tsunami on Tongatapu, where the
capital is located, with waves flowing onto coastal roads and flooding
properties on Saturday.
There's a satellite video of the explosion at the link which is just stunning. A slightly less awesome, but at least embeddable one:
The explosion sent a tsunami out over the whole Pacific region,
including the US Lori Dengler at the Eureka Time Standard:
An unprecedented tsunami from the Tonga Islands
In the 74-year history of US tsunami warning centers, there had never been a
volcanic-generated tsunami worthy of issuing a bulletin about. The software
for sending alerts is predicated on an earthquake source and the warning
center folks had to put something in the earthquake magnitude field in order
to send it out.
Normally, the earthquake triggers the tsunami alerting
process. An audible alert goes off and computer screens flash in the tsunami
warning centers whenever an earthquake above a certain magnitude occurs and
that initiates the analysis and bulletin dissemination. For US earthquakes, it
typically takes five minutes or less to get an initial bulletin out. If the
earthquake is further away, that initial bulletin may take 10 minutes.
This
morning, the first tsunami bulletin from the National Tsunami Warning Center
was issued at 3 a.m. PST. It was a statement — an earthquake of M1 had
occurred in the Tonga Islands area at 8:27 p.m PST the day before and
“Earthquakes of this size are known to generate tsunamis potentially dangerous
to coasts outside the source region.” At 4:53 a.m. bulletin #2 announces that
a Tsunami Advisory is in effect for all the US and Canadian West Coast and
Alaska. The Pacific Tsunami Warning Center issued similar advisories for
Hawaii. This time the volcanic source was included, and Ryan at the NWS deemed
it worthy of waking me up.
. . .
By the time the US tsunami centers
issued their first bulletin, the tsunami was approaching Hawaii. By the time I
got my computer up and running, I could pull up coastal tide gauges and
underwater deep pressure data and watch the tsunami progressing across the
Pacific.
After
an hour or two, it became clear to me that this tsunami looked very different
than typical earthquake caused ones. It was particularly evident on the DART
instruments. Beginning in the late 1990s, NOAA began deploying pressure
sensors on the ocean floor. These instruments now called DART, are located in
deep water far from coastal topography so that they can measure the true
tsunami signal unaffected by coastal amplification. They are an important tool
in the warning arsenal for forecasting likely tsunami heights.
I
have looked at a lot of DART graphs for earthquake tsunamis. They tend to
start out with larger amplitudes and then decay and disappear over the next
hour. Today’s tsunami is lasting much longer on the deep-sea instruments –
four hours now and still counting. We don’t know for sure yet why it is
lasting so long – whether it has to do with the eruption itself or complex
interaction with the sea floor. But it likely means that today’s tsunami will
last even long than usual, and my guess is that I will still be seeing traces
in a few days.
On the California coast, Port Luis recorded
the highest water level so far – at just over 4 feet with Crescent City a
close second at 3.9.

The vulnerability of Crescent City to tsunamis has been well known since the Good Friday 1964 quake in Alaska led to the flooding, damage and death in Crescent City. Apparently, the hydrography nearby helps to bring out the best in them.
The signal of the tsunami was also easily visible in the Aleutian Islands:
But even more than the tsunamis, which beyond Tonga, seem to have had only minor consequence, I wonder about the effect of this eruption on the climate in the medium term.
Large volcanic eruptions have been observed to have strong cooling impacts on the whole earth several times in recorded history, and down through geologic time. In recent events, it was considered to be the result of sulfate aerosols blocking sunlight.
Well, several cubic kilometers of sulfate laden seawater just had a violent encounter with a whole lot of hot lava. Just sayin.'