SO2 data and alert service

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Product information

Introduction
 
Slant column density vs.
vertical column density
Geographic regions
Data presentation
and delivery
Solar Zenith Angle
What is the Dobson Unit?
 
Slant column retrieval
Background correction
Reference spectrum
Cloud cover fraction
 
Near-real time service
Criteria for exceptional
SO2 concentrations
 
Air-mass factor using
look-up tables
Air-mass factor using a
chemistry transport model
SO2 column from OMI
 
Time period of
available data
Data format specification
Data and Service
version history
Validation of the
data products
South Atlantic Anomaly
 
Downloading
data & image files
Documentation
References
Acronyms
Acknowledgments


 
NOTE:   This is the OLD product info. Some parts of it are no longer up to date, while other parts are missing -- see the remark on the main product info page.

Cloud cover fraction

As additional service to interpret the SO2 (vertical and slant) column densities, the web pages that show images of the SO2 data also show an image of the cloud cover fraction for the same region, taken from the same instrument. Note that currently there is no cloud screening performed on the data: all SO2 slant column retrieval results are shown as-is.

The same cloud fraction is also used to determine the air-mass factor (AMF) when taking the AMF from look-up tables made with a radiative transfer model in order to compute the SO2 vertical column density. Note that the AMF and thus the vertical column cannot be calculated of the cloud cover fraction is missing.

Cloud fraction Vanuatu on 15 May 2005 For the daily data at orbit (like the image shown here) and at grid coordinates, as well as for the 3-day composites at grid coordinates [GOME-1 and SCIAMACHY only], the cloud cover fraction is presented in the same way and available in the accompanying data files. Monthly averages of the cloud fraction are not made: there is no cloud screening method applied to the SO2 data, so that a monthly average cloud fraction does not provide any useful additional information.

The cloud fraction is a number between zero (clear-sky: no clouds) and one (fully clouded, also known as overcast). For the Volcanic & Air Quality SO2 Services the cloud data is taken from existing data products:

  • For SCIAMACHY data, the cloud fraction is taken from the data files generated by the FRESCO algorithm, which derives the cloud data from the Oxygen A-band (between 758-775 nm). See this page at the TEMIS website for more information and data.

    The FRESCO cloud data is either in "normal mode" or in "snow/ice mode". In the latter case, a cloud fraction of one is assumed with the cloud at ground level when determining the AMF for the SO2 vertical column. In the datafiles, however, the cloud fraction in the "snow/ice mode" is set to '-1', and it is shown in a separate colour in the cloud fraction images (indicated simply as "snow" in the colour bar).

    Note that the FRESCO cloud cover data retrieval stricktly speaking is based on sunlight reflected by a combination of clouds and (reflecting) aerosols: such aerosols are effectively treated as clouds. This means that the FRESCO data product contains a (small) aerosol contribution.

  • For GOME-1 data the FRESCO cloud product is also used; for some details see the SCIAMACHY description above.

  • For OMI data, the cloud fraction is taken from the level-2 data product provided by NASA/NOAA. [reference]

    The "quality flags" of the ground pixel in that data product gives the presence of snow or ice. The following situations are taken to represent the "snow/ice mode": permanent ice, dry snow, and a sea ice concentration of more than 50% -- all other cases are considered to be "normal mode"

  • The GOME-2 SO2 data are generated in near-real time at DLR and that data product contains cloud information based on the OCRA/ROCINN method, developed at DLR. The maps on the web pages show the cloud cover fraction as determined by OCRA. [reference]
 

 


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