A major earthquake hit the Aleutian Islands, Alaska, on June 23, 2014.
The earthquake occurred at 51.797°N 178.760°E, 15 miles (24 km) southeast of Little Sitkin Island, Alaska, at a depth of 66.8 miles (107.5km).
The U.S. Geological Survey (
USGS) earlier listed the earthquake at a magnitude of 8 on the Richter scale, but eventually gave the quake a magnitude of 7.9.
Initial tsunami warnings, as reflected by the two NOAA images on the right, were later cancelled, e.g. the
Pacific Tsunami Warning Center in Hawaii said the earthquake’s epicenter was too deep to pose a tsunami threat to its coasts.
Indeed, earthquakes that occur at less depth, i.e. closer to the seafloor, pose a greater tsunami threat, as more energy will enter the sea as kinetic energy pushing up wave height propelled in the form of a tsunami.
Earthquakes that occur at greater depth pose other kinds of threats. When earthquakes hit deep under the sea floor, more energy will translate into shockwaves that can propagate over great distances through the Earth crust, particularly along fault lines.
In this case, the situation is particularly threatening for the Arctic Ocean. As the map below shows, the fault line where this earthquake hit extends through Siberia into the Laptev Sea and was hit by three earthquakes recently:
M 4.9 - East of Severnaya Zemlya
2014-06-22 23:58:24 UTC
Location 78.520°N 125.942°E
Depth 10.00 km (6.21 mi)
M 4.7 - Laptev Sea
2014-06-01 08:52:43 UTC
Location 75.012°N 133.665°E
Depth 10.00 km (6.21 mi)
M 4.8 - 172km N of Deputatskiy, Russia
2014-05-29 05:07:33 UTC
Location 70.844°N 139.761°E
Depth 10.00 km (6.21 mi)
A cluster of earthquakes that recently hit the Aleutian Islands shows up in green in the top right corner op above map. Also note the red dot on the right, respresenting a M 4.1 earthquake that hit the Sea of Okhotsk on June 22, 2014 (at 09:47:47 UTC, location 51.843°N 151.310°E), at a depth of 527.66 km (327.87 mi).
Earthquakes are a major threat for the Arctyic as they can destabilize methane hydrates contained in sediments under the seafloor of the Arctic Ocean.
The situation is the more dangerous given the warm sea water that threatens to enter the Arctic Ocean, as illustrated by the image below.
As the recent NOAA
overview of the climate situation in May 2014 describes, combined average temperature over global land and ocean surfaces reached a record high for May, at 0.74°C (1.33°F) higher than the 20th century average. Across the oceans, the global monthly-averaged sea surface temperature was 0.59°C (1.06°F) higher than the 20th century average, marking the highest May temperature on record. This is further illustrated by the image below.
Meanwhile, the situation hasn't improved, as illustrated by the image below.
The NOAA image below shows sea surface temperature anomalies in the Arctic Ocean on June 23, 2014, with many areas showing anomalies above 8 degrees Celsius.
According to NOAA's Climate Prediction Center, there is about a 70% chance that El Niño conditions will develop during the Northern Hemisphere summer 2014 and an 80% chance it will develop a few months later.
As discussed in earlier posts, the sea ice is already very thin, and while ocean heat is melting the sea ice from beneath, the sun is warming up the ice from above. At this time of year, insolation in the Arctic is at its highest, as Earth reaches its maximum axial tilt toward the sun of 23° 26'. In fact, insolation during the months June and July is higher in the Arctic than anywhere else on Earth, as discussed at this
earlier post.
Feedbacks further accelerate warming in the Arctic, as described in the earlier post
Feedbacks in the Arctic. Temperature rises of the water close to the seafloor of the Arctic Ocean is very dangerous, as heat penetrating sediments there could cause hydrate destabilization, resulting in huge amounts of methane entering the atmosphere over the Arctic Ocean.
In conclusion, the situation is the Arctic is threatening to escalate into runaway warming and urgently requires comprehensive and effective action as discussed at the
Climate Plan blog.
