this event, techniques that exploit the strong absorption of infrared radiation by sulfur dioxide have only recently emerged, allowing scientists to reanalyze old data to track volcanic gas clouds. Using the ultraviolet data collected by the Nimbus 7 Total Ozone Mapping Spectrometer and infrared data collected by the High Resolution Infrared Radiation Sounder (on NOAA's Television Infrared Observation Satellite (TIROS) Operational Vertical Sounder), Carn et al. tracked sulfur dioxide released by Hekla. They find that the eruption emitted about 0.5 to 0.7 teragrams (trillions of grams) of sulfur dioxide, which later split into three distinct clouds, one of which circled the North Pole for 6 days. The others drifted across eastern Russia, Alaska, and Canada. Through this analysis, the authors show that integrated satellite sulfur dioxide measurements may be used to test air parcel trajectory models used for aviation hazard mitigation. This study also highlights the potential impacts of Icelandic volcanic eruptions on the polar atmosphere and Arctic ozone loss.
Title:
Circumpolar transport of a volcanic cloud from Hekla (Iceland)
Authors:
S. A. Carn: Joint Center for Earth Systems Technology (NASA/University of Maryland Baltimore County), University of Maryland Baltimore County, Baltimore, Maryland, U.S.A;
A. J. Prata: Atmosphere and Climate Department, Norwegian Institute for Air Research (NILU), Kjeller, Norway;
S. Karlsdttir: Icelandic Meteorological Office, Reykjavk, Iceland.
Source:
Journal of Geophysical Research-Atmospheres (JGR-D) paper 10.1029/2008JD009878, 2008; http://www.agu.org/journals/pip/jd/2008JD009878-pip.pdf
This paper is "in press".
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