Difference between revisions of "100415 IcelandVolcanicErruption Data"
From Earth Science Information Partners (ESIP)
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== Models == | == Models == | ||
* [http://meteo.gc.ca/eer/vaac/viewData_e.html?product=current&data=20100414-1537Z_Eyjafjoll_mldp0_42_48.png Montreal Volcanic Ash Advisory Models] | * [http://meteo.gc.ca/eer/vaac/viewData_e.html?product=current&data=20100414-1537Z_Eyjafjoll_mldp0_42_48.png Montreal Volcanic Ash Advisory Models] | ||
− | * [http://www.grapevine.is/Home/ReadArticle/Eruption-News-Roundup Danish Model predicting ash transport] | + | * [http://www.grapevine.is/Home/ReadArticle/Eruption-News-Roundup Danish Model predicting ash transport] |
− | + | * [http://www.dmu.dk/Luft/Luftforurenings-modeller/Vulkansky.htm National Environmental Research Institute Denmark] The graphics show the amount of air pollution from ground level until 20 km height on a relative scale, where red is the most polluted. The difference between the colours is a factor 10. NERI has assumed that the volcano has emitted the plume to a height of 5-7 km. Please note that the model works in UTC-time. Central European summertime = UTC + 2 hours. | |
+ | http://www2.dmu.dk/atmosphericenvironment/Vulkansky/dreameu_ani.gif | ||
== Satellites == | == Satellites == |
Revision as of 11:50, April 18, 2010
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Models
- Montreal Volcanic Ash Advisory Models
- Danish Model predicting ash transport
- National Environmental Research Institute Denmark The graphics show the amount of air pollution from ground level until 20 km height on a relative scale, where red is the most polluted. The difference between the colours is a factor 10. NERI has assumed that the volcano has emitted the plume to a height of 5-7 km. Please note that the model works in UTC-time. Central European summertime = UTC + 2 hours.
Satellites
- MODIS Satellite Image - 4/15 - shared by marksteward 'Pic of ash cloud spreading from Iceland north of UK http://bit.ly/ber3Hp #volcano #ashtag #nasa'
- From EUMETSAT: Time Series Satellite Image of Plume moving
- Twitpic Courtesy of NEODAAS/University of Dundee
Surface Observations