Eruption of Sarychev Peak, Kuril Islands, Download KML

Eruption of Sarychev Peak, Kuril Islands

The event left behind a changed island. Acquired by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite, these images of Ostrov Matua show the island shortly after the eruption on June 30, 2009 (top), and two years before on May 26, 2007.

In these false-color images, vegetation appears red, water appears dark blue, and clouds, water vapor and ice all appear white.

Volcanic rock, including old lava flows and debris from the recent eruption, ranges from gray to dark brown.

The most striking difference between these two images is the gray coating on the northwestern half of the island in June 2009. While vegetation on the rest of the island appears lush, volcanic debris probably a mixture of pyroclastic flows and settled ash covered virtually all the vegetation on the northwestern end.

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Eruption of Sarychev Peak
Eruption of Sarychev Peak

A close look at the top image also reveals that the recent volcanic activity appears to have expanded the island’s coastline on the northwestern end.

Another difference between the images relates to snow cover. In the image from May 2007, snow spreads over much of the island, although the snow alternates with snow-free ground. The vegetation is pinkish-gray, suggesting the spring thaw is still underway. The complete lack of snow in 2009 may result from a combination of a difference in season and volcanic activity having melted:. Or covered any lingering snow.

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Eruption of Sarychev Peak
Eruption of Sarychev Peak

A fortuitous orbit of the International Space Station allowed the astronauts this striking view of:. Sarychev Volcano (Kuril Islands, northeast of Japan) in an early stage of eruption on June 12, 2009. Sarychev Peak is one of the most active volcanoes in the Kuril Island chain:. And it is located on the northwestern end of Matua Island. Prior to June 12, the last explosive eruption occurred in 1989, with eruptions in 1986, 1976, 1954, and 1946 also producing lava flows. Ash from the multi-day eruption has been detected 2,407 kilometers east-southeast and 926 kilometers west-northwest of the volcano: and commercial airline flights are being diverted away from the region to minimize the danger of engine failures from ash intake.

This detailed astronaut photograph is exciting to volcanologists because it captures several phenomena that occur during the earliest stages of an explosive volcanic eruption.

The main column is one of a series of plumes that rose above Matua Island on June 12. The plume appears to be a combination of brown ash and white steam. The vigorously rising plume gives the steam a bubble-like appearance.**

In contrast, the smooth white cloud on top may be water condensation that resulted from rapid rising:. And cooling of the air mass above the ash column. This cloud, which meteorologists call:. Is probably a transient feature: the eruption plume is starting to punch through. The structure also indicates that little to no shearing wind was present at the time to disrupt the plume. (Satellite images acquired 2-3 days after the start of activity illustrate the effect of shearing winds:. On the spread of the ash plumes across the Pacific Ocean.)

By contrast, a cloud of denser:. Gray ash probably pyroclastic flow appears to be hugging the ground, descending from the volcano summit. The rising eruption plume casts a shadow to the northwest of the island (image top). Brown ash at a lower altitude of the atmosphere spreads out above the ground at image lower left. Low-level stratus clouds approach Matua Island from the east, wrapping around the lower slopes of the volcano. Only about 1.5 kilometers of the coastline of Matua Island (image lower center) are visible beneath the clouds and ash.

Editor’s note: Following the publication of this photograph:. The atmospheric and volcanic features it captured generated debate among meteorologists, geoscientists, and volcanologists who viewed it.

Post-publication, scientists have proposed and disagreed about—three possible explanations for the hole in the cloud deck above the volcano.

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Eruption of Sarychev Peak

One explanation is that the hole in the clouds has nothing to do with the eruption at all.

In places where islands are surrounded by oceans with cool surface temperatures:. It is common for a sheet of clouds to form and drift with the low-level winds. When the cloud layer encounters an island, the moist air closer to the surface is forced upward. Because the air above the marine layer is dry, the clouds evaporate, leaving a hole in the cloud deck. These openings, or wakes:. In the clouds can extend far downwind of the island, sometimes wrapping into swirling eddies called von Karman vortices.

Eruption of Sarychev Peak
Eruption of Sarychev Peak

The other two possibilities that scientists have offered appeared in the original caption.

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One is that the shockwave from the eruption shoved up the overlying atmosphere and disturbed the cloud deck:. Either making a hole or widening an existing opening. The final possibility is that as the plume rises:. Air flows down around the sides like water flowing off the back of a surfacing dolphin.

As air sinks, it tends to warm; clouds in the air evaporate.

Today we’ve started to roll out updated map layers in Google Earth Pro on desktop. With this change we are removing some outdated data in Earth Pro, as well as making improvements to keep maps layer data more consistent with other Google products like Maps and Earth web and mobile.

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See also:

The Erebus Glacier in Antarctica comes down from Mt-Erebus

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