Archive for the ‘Volcanic activity’ Category

Volcanic ash plume from Sarychev Peak eruption

Tuesday, June 16th, 2009
GOES-11 split window IR difference product (10.7 - 12.0 µm)

GOES-11 "split window" IR difference product (10.7 - 12.0 µm)

A series of volcanic eruptions from Sarychev Peak (located in the central Kiril Islands) began on 10-11 June 2009, and GOES-11 “split window” IR difference images (above) showed a good signature of one of the ash plumes (yellow to cyan color enhancement) as it began to move eastward across the North Pacific Ocean on 16 June 2009.

AWIPS images of the MTSAT + GOES-11 IR channel with overlays of the MTSAT high density winds (below) showed the high-altitude flow that was helping the volcanic ash plume features to move southeastward around 40-60 knots (according to the Volcanic Ash Advisories that were issued on 16 June).

GOES-11 is the last of the current GOES series to have the 12.0 µm IR channel on the imager instrument package, which allows the calculation of such a “split window” IR difference product for volcanic ash detection. Once GOES-11 is replaced by either GOES-13 or GOES-14 as the operational GOES-West satellite, the geostationary volcanic ash detection ability will be greatly diminished over the eastern North Pacific Ocean…until the launch of the Advanced Baseline Imagery (ABI) on the GOES-R satellite.

MTSAT + GOES-11 IR images, MTSAT high density winds

MTSAT + GOES-11 IR images, MTSAT high density winds

Yet another Redoubt volcanic eruption

Saturday, April 4th, 2009
GOES-11 visible, 3.9 µm IR, 10.7 µm IR, and IR spilt window difference images

GOES-11 visible, 3.9 µm IR, 10.7 µm IR, and IR "split window difference" images

The Mt. Redoubt volcano in Alaska experienced its 19th explosive event (in a series that began on 23 March) on 04 April 2009. GOES-11 visible, 3.9 µm shortwave IR (IR2), 10.7 µm IR window (IR4), and 10.7-11.0 µm “split window difference” images (above) showed that the southeastward advection of the volcanic plume became increasingly difficult to follow a few hours after the eruption.

However, the volcanic plume likely contained a good deal of water vapor, which made it easier to track on GOES-11 6.7 µm “water vapor channel” imagery (below) as it moved toward and eventually south of 50º N latitude  after about 21:00 UTC.

GOES-11 6.7 µm water vapor images

GOES-11 6.7 µm water vapor images

Images of the MODIS 1.3 µm “cirrus detection channel” at 20:45 and 22:35 UTC (below) exhibited a signal of the leading edge of the volcanic plume as it approached and moved south of 50º N latitude (between 144º W and 142º W longitude). This MODIS near-IR channel is sensitive to particles that are efficient scatterers of light (such as smoke, haze, dust, ash), so these types of airborne particles to show up as slightly brighter features on grayscale-enhanced MODIS “cirrus detection channel” imagery.

Terra and Aqua MODIS near-IR Cirrus detection channel images

Terra and Aqua MODIS near-IR "Cirrus detection channel" images

The extent of the long-range transport of the Redoubt SO2 plume was even more obvious on the AIRS Ozone Monitoring Instrument (OMI) SO2 24-hour composite image for 04 April (below).

OMI SO2 24-hour composite image

AIRS OMI SO2 24-hour composite image