Bezymianny Eruption Captured With ASTER

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******************************************
From: Michael Ramsey <mramsey@xxxxxxxx>
******************************************

Bezymianny volcano (55.9N, 160.6E, ~2900 m elevation) erupted on 11 May
2007 at approximately 14:30 UTC (KVERT report, 2007) and is at Color Code
Yellow (as of 18 May). The Advanced Spaceborne Thermal Emission and
Reflection Radiometer (ASTER), collecting data in an urgent request mode
for the ongoing eruption of nearby Kyluchevskoy volcano, also captured
remarkable images of the initial stages of the Bezymianny eruption. Data
were collected on 12 (daytime) and 13 (nighttime) May, however only data
collected on the 12th are presented here due to heavy cloud cover on the
night of the 13th of June.

A figure has been created and staged at the IVIS website to accompany the 
text: http://ivis.eps.pitt.edu/data/Kamchatka/12May2007_Bezy.pdf


Visible/near infrared (VNIR) observations:

Approximately 40% of the summit region was visible in the 15 m/pixel VNIR
image. A plume of steam and ash was observed trending over 20 km northeast
into the surrounding non-volcanic clouds. It is speculated that ash from
earlier (min-hours) eruptions of Bezymianny was detected over 60 km to the
northeast. It is here where the ash plume mixes with the water-ice plume
from Kyluchevskoy. On the upper southwestern part of the dome, a bright
steam covered area was observed. This region spans ~0.13 km² and is close
to the dome's central summit in an area of persistently active fumaroles.


Shortwave infrared (SWIR) observations:

A strong SWIR thermal anomaly (30 m/pixel) was observed on the upper dome,
near the fumaroles and extended down the southwestern side of the existing
lava dome. The radiance from band 7 (2.26 micrometers) was corrected for
solar reflection by subtracting the non-volcanic background value. From
these data, a maximum derived temperature was found to be ~355 C. These
high pixel-integrated brightness temperatures indicate that a new lava
lobe is being em placed at the surface.


Thermal infrared (TIR) observations:

The brightest thermal anomaly in the TIR (90 m/pixel) was located on the
southwest part of the upper dome in the same area as the SWIR-derived
maximum temperature. A maximum atmospherically-corrected TIR brightness
temperature of 41 C was recorded, which was approximately 49 C above the
non-volcanic background temperature of -8 C.

ASTER will continue to monitor the volcano throughout this phase of
activity. New ASTER day/night data acquisitions are scheduled for the
20/21 May and the 28/29 May and will continue weekly throughout June. In
addition, a field investigation is scheduled for August 2007 to
investigate the surface deposits.


Cited reference:

KVERT report. 17 May 2007.
http://www.avo.alaska.edu/activity/avoreport.php?
view=kaminfo&id=245&type=kaminfo&month=May&year=2007

"The explosive eruption occurred at Bezymianny volcano, probably, from
14:30 till 15:00 UTC on May 11. Clouds obscured the volcano from May 13
till present. According to information by hunters, a large mud flow 200 m
in width moved along the Sukhaya Khapitsa river at Bezymianny volcano area
on May 17. Probably pyroclastic flow deposits caused a mud flow. According
to satellite data, a size of thermal anomaly over the lava dome decreased
from 10-25 pixels (on 8-12 May) till 1-4 pixels (on 15-17 May)."

Adam Carter
ajc44@xxxxxxxx
website: http://www.pitt.edu/~ajc44

Michael Ramsey
mramsey@xxxxxxxx

Shellie Rose
srr13@xxxxxxxx


+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++
Dr. Michael Ramsey, Associate Professor

** sabbatical address (1 May - 31 Aug 2007) **
Alaska Volcano Observatory
U.S. Geological Survey Alaska Science Center
4200 University Drive, room 210
Anchorage, AK 99508
office: 907-786-7111; fax: 907-786-7425
+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++

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