aged volcanic clouds n.
Download
Skip this Video
Loading SlideShow in 5 Seconds..
Aged Volcanic Clouds PowerPoint Presentation
Download Presentation
Aged Volcanic Clouds

Loading in 2 Seconds...

play fullscreen
1 / 34

Aged Volcanic Clouds - PowerPoint PPT Presentation


  • 132 Views
  • Uploaded on

A52A-04. Aged Volcanic Clouds. Are they an aviation hazard and why?. Bill Rose, * Patricia Nadeau , Simon Carn Michigan Technological University David Schneider USGS Alaska Volcano Observatory. Aircraft Hazards. Volcanic clouds generally end up in the lower stratosphere

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about 'Aged Volcanic Clouds' - howard-avery


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
aged volcanic clouds

A52A-04

Aged Volcanic Clouds

Are they an aviation hazard and why?

Bill Rose, *Patricia Nadeau, Simon Carn

Michigan Technological University

David Schneider

USGS Alaska Volcano Observatory

aircraft hazards
Aircraft Hazards
  • Volcanic clouds generally end up in the lower stratosphere
  • Commercial aircraft fly at similar altitudes because of low turbulence, few clouds, jet stream winds
  • Volcanic ash advisory centers (VAACs) have the task of advising pilots where hazardous volcanic clouds may be
  • When are volcanic clouds no longer a threat to aircraft?
young volcanic cloud hazards
Young volcanic cloud hazards
  • Engine failure
  • ‘Sandblasting’ of windshield, compressor fan blades, etc.
  • Blockage of fuel nozzles and cooling passages
  • Etching of windshields
    • British Airways Flight 9 to Perth – Galunggung, 1982
    • KLM Flight 867 to Anchorage – Redoubt, 1989
    • 16 damaging encounters – Pinatubo, 1991
    • ~100 encounters 1973-2000 (Guffanti, et al. 2004)
aged volcanic clouds1
“Aged” volcanic clouds
  • Coarse ash falls out of cloud within ~30 minutes
  • Most remaining ash has fallen out of cloud within 24-36 hours
  • Trackable up to 4 days with IR split window, mostly SO2 and sulfate after that
  • Aged = over 2 days old
  • Do they still pose a risk to aircraft?
slide5

Volcanic clouds over western Montana on 7/18/2008 (photo by Margaret Patton, Research Office, Montana Tech of The University of Montana)

Okmok July 12 plume seen from 28,000 ft over Billings, Montana from the cockpit of a commercial passenger flight on the evening of 7/19/2008. (Image courtesy of Bradley Johnson and Alaska Airlines)

kasatochi and okmok
Kasatochi and Okmok

July 12, 2008

August 7, 2008

New cone at Okmok – September 15, 2008

Image courtesy of AVO/USGS

(Photo by Christina Neal)

Kasatochi - October 23, 2008

Image courtesy of Jerry Morris

aircraft encounters
Aircraft encounters
  • Okmok
    • ~28 pilot reports July 18-20 over Northern US and parts of Canada
    • Mentions of visible ash clouds, orange-tinted clouds, smells and throat irritation
  • Kasatochi
    • ~38 pilot reports on/around August 10, Northern US and parts of Canada
    • Mentions of visible ash, brown haze, rapid sky color changes, sulfur smell

* These are likely minimums for total encounters

aircraft encounters1
Aircraft encounters
  • Kasatochi
    • Major airline to Anchorage – brief (few minutes) encounter near Whitehorse, Yukon Terr. No aircraft damage, but ash collected on various parts of plane
    • Regional airline, B737 – problems with pressurization over MacKenzie Valley of Northwest Terr. Following return to Yellowknife, “grey-glittery” coating in wheelwells, ash-type substance in out-flow valve
    • Same aircraft 4 days later, loss of cabin pressure en route to Calgary. Re-routed to Fort McMurray, AB
    • 4 encounters by CARIBIC (aboard Lufthansa flights) instruments over Europe Aug. 15 – Sept. 12
goes visible
GOES - visible

Courtesy of Scott Bachmeier, U. Wisconsin, Madison

slide15

Q

Q

slide19

Q

Q

hekla march 2000
Hekla – March, 2000

SOLVE (ozone study) campaign flight with array of atmospheric sampling instruments, including:

Chemical Ionization Mass Spectrometer

Forward Scattering Spectrometer Probe

Hygrometers

DACOM IR Laser Spectrometer

hekla cloud chemistry
Hekla – cloud chemistry
  • CIMS measured SO2/H2SO4 (gas) ~30,000
  • However, although it wasn’t measured directly, there was probably abundant particulate H2SO4 in the cloud as well

Rose, W. I., et al. (2006), J. Geophys. Res., 111, D20206

hekla cloud chemistry1
Hekla – cloud chemistry

Beyond SO2 and H2SO4, cloud chemistry included many volcanogenic species that could potentially be hazardous to aircraft and passengers

kasatochi cloud encounter
Kasatochi cloud encounter

A-Train views of the Kasatochi cloud on August 10

OMI SO2 - 21:35 UT

CALIPSO Backscatter – 21:28 UT

Solid particles at 11 km alt.

CALIPSO

V-cloud? Ice?

kasatochi cloud encounter1
Kasatochi cloud encounter

Scanning electron photomicrographs of material collected from the leading edge of the wing of a commercial aircraft that encountered the Kasatochi volcanic cloud at around 0100 UTC on August 11, 2008 over the Yukon region.

30 μm

45 μm

50 μm

40 μm

Images courtesy of AVO/USGS. Images were taken on the Environmental Scanning Electron Microscope (ESEM) at the University of Alaska Fairbanks Advanced Instrumentation Laboratory

kasatochi cloud encounter2
Kasatochi cloud encounter

A-Train views of the Kasatochi cloud on August 15

OMI SO2 - 11:55 UT

CALIPSO 2:22 UT

V-cloud

Saharan dust

CARIBIC flight (LH759) - 4:00-6:00 UT – 11.6 km alt.

1850 km

CALIPSO

hekla vs kasatochi
Hekla vs. Kasatochi

Kasatochi cloud encounter in Europe (CARIBIC) found <2.6 - 17.8 ng/m3 of Si, equivalent to 15 - 100 ng/m3 of ash and 243 - 399 ng/m3 of S, equivalent to 500 - 800 ng/m3 of SO2 (Prof. Bengt G. Martinsson Div. Nuclear Physics, Lund University)

These are equivalent to 0.005 to 0.1 μg/m3 ashand 0.1 to 0.25 ppbv of SO2

The much younger Hekla cloud had significantly higher values: 1-10 μg /m3 ashand 1 ppmv SO2

The differences are partly explained by the much greater age of the Kasatochi cloud (8 days vs. 1.5 days for Hekla)

future considerations
Future considerations…

What we know:

What we don’t know:

Locations of SO2 clouds (OMI)

Cloud heights (CALIPSO)

Minor amounts of ash persist for days

Hekla plume components

What are damage/danger thresholds for volcanic cloud constituents? (e.g., SO2 and sulfate)

Effect of exposure time?

Health risks for passengers on board?

  • Need ground tests with companies like Boeing, etc. to establish limits on what is a threat to aircraft
  • More work like CARIBIC
thank you
Thank you

We would like to thank everyone who helped with and contributed to this presentation, including Bengt Martinsson and the CARIBIC project, AVO/USGS, Kristi Wallace, Marianne Guffanti, the SOLVE campaign, and Richard Honrath