Mt. Pinatubo Eruption on June 15, 1991
The second-largest volcanic eruption of the 20th century, and by far the largest eruption to affect a densely populated area, occurred at Mount Pinatubo in the Philippines on June 15, 1991. The eruption produced high-speed avalanches of hot ash and gas, giant mudflows, and a cloud of volcanic ash hundreds of miles across. This animation shows the ozone measurements around Mt Pinatubo reacting to the eruption. That "hole" in the days immediately following the eruption of Pinatubo is due to interference by sulfur dioxide with the retrieval algorithm. There are high amounts of volcanic SO2 in the initial plume from the eruption. These measurements make it look like there was an ozone hole when there was not. Ozone really did decrease in the equatorial zone after the volcanic cloud spread throughout the equatorial zone over the next year or so. Plots of global average ozone show a clear minimum in the two years after the eruption. But that "hole" on June 20th for instance is sulfur dioxide, not an ozone hole.
Mt. Pinatubo Eruption caused Equatorial Ozone Hole
Normal Equatorial Ozone
June 16, 1991 : One day after Mt Pinatubo erupted
June 17, 1991
June 18, 1991
June 19, 1991
June 20, 1991
June 21, 1991
June 21, 1991
June 23, 1991
June 24, 1991
June 25, 1991
August 31, 1991 Subtle equatorial ozone decrease seen in blue
Color Bar
Video slate image reads, "Mt. Pinatubo Eruption effect on Equatorial ozone".
Credits
Please give credit for this item to:
NASA/Goddard Space Flight Center
Scientific Visualization Studio
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Animator
- Lori Perkins (NASA/GSFC)
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Scientists
- Richard McPeters (NASA/GSFC)
- Jay Herman (NASA/GSFC)
Release date
This page was originally published on Tuesday, June 12, 2001.
This page was last updated on Wednesday, May 3, 2023 at 1:58 PM EDT.
Series
This page can be found in the following series:Datasets used
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Ozone [Nimbus-7: TOMS]
ID: 423
Note: While we identify the data sets used on this page, we do not store any further details, nor the data sets themselves on our site.