observations of volcanic ash by lidar, modis and surface air-quality measurements robin hogan...
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![Page 1: Observations of volcanic ash by lidar, MODIS and surface air-quality measurements Robin Hogan University of Reading Last updated: 18 April 2010](https://reader036.vdocuments.site/reader036/viewer/2022062409/56649f285503460f94c403b5/html5/thumbnails/1.jpg)
Observations of volcanic Observations of volcanic ash by lidar, MODIS and ash by lidar, MODIS and
surface air-quality surface air-quality measurementsmeasurements
Robin Hogan <[email protected]>University of Reading
Last updated: 18 April 2010
![Page 2: Observations of volcanic ash by lidar, MODIS and surface air-quality measurements Robin Hogan University of Reading Last updated: 18 April 2010](https://reader036.vdocuments.site/reader036/viewer/2022062409/56649f285503460f94c403b5/html5/thumbnails/2.jpg)
15 April: 1139 UTC15 April: 1139 UTC
NASA MODIS radiometer
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15 April: 1329 UTC15 April: 1329 UTC
NASA MODIS radiometer
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16 April: 1044 UTC16 April: 1044 UTC
NASA MODIS radiometer
![Page 5: Observations of volcanic ash by lidar, MODIS and surface air-quality measurements Robin Hogan University of Reading Last updated: 18 April 2010](https://reader036.vdocuments.site/reader036/viewer/2022062409/56649f285503460f94c403b5/html5/thumbnails/5.jpg)
16 April: 1224 UTC16 April: 1224 UTC
NASA MODIS radiometer
Stationary colours in the sea (sediment and algae)
x Chilbolton
x CabauwVolcanic ash
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Chilbolton Doppler lidar: 16 AprilChilbolton Doppler lidar: 16 April
Descending volcanic ash?
Vertical velocity shows turbulence in boundary layer and also in ash layer
Mixes into turbulent boundary layer
Background aerosol particles in the boundary layer (0-1 km)
![Page 7: Observations of volcanic ash by lidar, MODIS and surface air-quality measurements Robin Hogan University of Reading Last updated: 18 April 2010](https://reader036.vdocuments.site/reader036/viewer/2022062409/56649f285503460f94c403b5/html5/thumbnails/7.jpg)
Chilbolton Doppler lidar: 16 AprilChilbolton Doppler lidar: 16 April
Descending volcanic ash?
Mixes into turbulent boundary layer
Spherical liquid droplets have very low depolarization Ash is non-spherical
so strongly depolarizing
Background aerosol particles in the boundary layer (0-1 km)
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Chilbolton Doppler lidar: Chilbolton Doppler lidar: 17 April17 April
• Further images at http://www.met.reading.ac.uk/radar/realtime/today.html
Normal aerosol particles in the boundary layer: no further sign of volcanic ash…
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Surface sulphur Surface sulphur dioxidedioxide
Spike due to volcanic ash? Much less that UK air quality objective (1 hr average exceeds 350 g m-3 less than 24 times per year)
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Aerosol particles Aerosol particles (PM10s)(PM10s)
Much less clear sign of ash
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Possible ozone Possible ozone chemistry at chemistry at
Reading Reading (speculative!)(speculative!)
• Further data at http://www.airquality.co.uk/
Possible NO2 source due to volcano?
Converted to NO when sun comes up?NO2 + sunlight NO + O
Large ozone depletion: O3 + NO NO2 + O2
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Ultraviolet EZ-lidar, Cardington Ultraviolet EZ-lidar, Cardington Bedfordshire, 16Bedfordshire, 16thth April April
• http://www.metoffice.gov.uk/corporate/pressoffice/2010/volcano/lidar/• This plot was produced by the University of Manchester, NCAS and FGAM.
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RIVM Caeli lidar, Netherlands, 16RIVM Caeli lidar, Netherlands, 16thth April AprilCourtesy of Arnoud Apituley <[email protected]>Courtesy of Arnoud Apituley <[email protected]>
• This lidar is not operated all the time but has Raman capability• Further images here:
http://cerberus.rivm.nl/lidar/Cabauw/2010/
Volcanic ash just above boundary-layer
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Cabauw EZ-lidar, Netherlands, 16Cabauw EZ-lidar, Netherlands, 16thth April AprilCourtesy of David Donovan, KNMI <[email protected]>Courtesy of David Donovan, KNMI <[email protected]>
Ash appears not to mix into the boundary layer as
it did over Chilbolton…
As over Chilbolton, ash much more depolarizing than ordinary
boundary-layer aerosol
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Cabauw EZ-lidar, Netherlands, 18Cabauw EZ-lidar, Netherlands, 18thth April AprilCourtesy of David Donovan, KNMI <[email protected]>Courtesy of David Donovan, KNMI <[email protected]>
Is this volcanic ash too? Why does it not mix into
the boundary layer?
De Bilt radiosonde put midday boundary-layer top at ~1 km
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Cabauw EZ-lidar, Netherlands, 18Cabauw EZ-lidar, Netherlands, 18thth April AprilCourtesy of David Donovan, KNMI <[email protected]>Courtesy of David Donovan, KNMI <[email protected]>
• Further images: http://www.knmi.nl/~knap/lidar_cabauw/
Another layer coming in?
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ThursdayThursday1515thth, 1329, 1329
Summary from MODIS images
• Icelandic wind from northwest
• Further images: www.sat.dundee.ac.uk
Volcanic ash
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FridayFriday1616thth, 1234, 1234
• Volcano obscured by clouds
Dilute volcanic ash measured over southern England and the Netherlands with lidar, signs of reaching the ground in England
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SaturdaySaturday1717thth, 1317, 1317
• Wind at Iceland from the north
• Volcanic ash heading south behind a cold front
Cold front
Volca
nic a
sh
No depolarizing aerosol observed over Chilbolton or Cabauw
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SundaySunday1818thth, 1222, 1222
• Northerly winds weakening
Is this the ash above the cloud?
Weakening
front
Not much sign in the MODIS image of the depolarizing aerosol observed at Cabauw but could be optically thin