On 20 march, 2010 a new eruption of the volcan Eyjafjallajökull (Island) occurred, after 87 years of inactivity. On 14 April explosive activity begun, producing a plume reaching 8000 m of altitude. The ash plume rapidly reached continental Europe in the next days. The plume was soon detected by means of LIDARs in several European countries (Switzerland, France, Germany, Romania, etc.).
On 19 April the plume was first detected in Italy by means of LIDAR at IFAC CNR and by means of in-situ instrument at ISAC-CNR Mount Cimone station.
For an overview of volcanic ash related problems click here (Wikipedia)
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As shown in this snapshot of the depolarization plot produced by the INO acquisition software, the plume resulted very weak and was evidenced at 2000-3000 m altitude just because of its characteristic depolarization (<10%). The day was quite cloudy and thus the number of valid data above 1000 m altitude was limited. The cloud was above the PBL and its vertical structure resulted quite irregular. In the afternoon, a strong convective activity occurred, resulting into an upward shift of the cloud and its vertical spreading.
At sunset, the presence of volcanic dust was visible at the naked eye because of its charcteristic, reddish blur:
Galliano di Mugello (Florence, Italy), sunset, 19 April 2010
HYSPLIT trajectory analysis for 20 April, 00 UTC: |
NAAPS MODIS aerosol concentrations for April 20 |
... and a final INO picture of the period 18-22 April 2010! Several PBL structures above Florence are also evidenced
On 18 May 2010 in the evening we started observing a depolarizing structure between 3000 and 4000 m altitude. The weak structure differentiated into several layers between 1000 and 4500 m on May 19, each showing different depolarization. On May, 20 the event decreased in intensity in the morning, but a mixing of volcanic dust with PBL aerosols was apparently occurring in the late morning.
In the plot, several hours show low clouds/rain which prevented a good observation of the cloud. Steps in the raw signal are just due to changes of laser power with time.
Massimo Del Guasta - National Institute of Optics (INO) - National Research Council | Via Madonna del Piano, 10 - 50019 Sesto Fiorentino - Firenze, Italy | Tel (office): +39-055-5226423 - Tel (laboratory) +39-055-5226424 | Email: Massimo Del Guasta | Web: www.ino.it | sito ottimizzato per una risoluzione minima di 1024x768 e firefox