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OMI Science Team Meeting Helsinki, June 24-27, 2008 Antti Arola. About the status and outlook for OMI Surface UV product. Aapo left FMI about three months ago. - PowerPoint PPT Presentation
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About the status and outlook forOMI Surface UV product
OMI Science Team Meeting
Helsinki, June 24-27, 2008
Antti Arola
Aapo left FMI about three months ago.
Since then, I have been responsible for the scientific development of OMUVB, while Simo Tukiainen
has been responsible for the processing related issues.
Puijo tower measurements
Finnish meteorological institute and Univ. of Kuopio
Current setup of measurements
Ion spectrometerAIS
Gas concentrations (NO-NOx, O3, SO2, CO)GAS
Total particle number concentrationCPC
Aerosol absorptionMAAP
Aerosol particle size distribution (0.25-32 m)ADM
Visibility, precipitationPWD
Weather parameters (T, RH, p, wind 2D)WXT
Aerosol scatteringNM
Cloud condensation nucleus (CCN) concentrationCCNC
Cloud drop size distribution (2-50 m)CDP
Aerosol particle size distribution (7-900 nm)* simultaneously in and out of cloud”
DMPS
DMPS = differential mobility particle sizer; ADM = ambient dust monitor; CPC = condensation particle counter; CDP = cloud droplet probe; CCNC = cloud condensation nuclei counter; NM = nephelometer;MAAP = multi-angle absorption photometer; WXT = weather transmitter; PWD = present weather detector;AIS = Air Ion Spectrometer
AERONET station
• AERONET sites in FinlandHyytiäläKuopioPallasHelsinki_LighthouseSodankylä
• Soon FMI campaign site in India, near Delhi
Provide a long term data set to:• Characterize aerosol optical properties• Validate Satellite & model aerosol retrievals• Synergism with Satellite obs., models sfc net
Satellite observations from A-train
Aqua
CALIPSO CloudSat
PARASOL
Aura
OMI Surface UV Algorithm and Surface UV Products
• Inherits from the TOMS UV algorithm based on look-up-tables made with various radiative transfer models.
• Calculate clear-sky surface UV irradiance
• Define cloud optical depth that gives the measured TOA radiance
• Make cloud correction using the obtained
• Absorbing aerosol correction to be added in the future
• Products:
• Erythemal dose rate both at overpass and at local solar noon (UV Index)
• Erythemal daily dose
• Irradiances at 305, 310, 324 and 380 nm both at overpass and at local solar noon
• The OMI surface UV algorithm is implemented in two separate processing systems: OMI-VFD and Global OMUVB.
OMI Very-Fast-Delivery has been operational since March 2006
OMI data is received by Direct Broadcast in Sodankylä and is processed immediately after each overpass of the Aura satellite. Distribution plots for total column ozone, UV Index and Erythemal daily dose are published within 30 minutes after the overpass at
http://omivfd.fmi.fi/index_eng.html
Global OMUVB product
Processing Status and Data Release
• OMUVB Level 2 V003 reprocessing is on-going. Years 2007 and 2008 are ready, earlier data is in progress.
• Level 2 HDF5-EOS data are available at GES DISC.
• http://disc.gsfc.nasa.gov/Aura/OMI/omuvb_v003.shtml
• AVDC provides OMUVB overpass data for over 100 sites that has been used for validation. New sites can be added ([email protected]).
Tanskanen, A., et al. (2007), Validation of daily erythemal doses from Ozone Monitoring Instrument with ground-basedUV measurement data, J. Geophys. Res., 112, D24S44, doi:10.1029/2007JD008830.
• Brewers in Jokioinen and Sodankylä
• SUV100 network data by National Science Foundation
• Canadian Brewer network data from Meteorological Service of Canada
• Spectral UV data from Lauder and Tokyo
Corr. coeff. = 0.76Slope = 2.4
Arola, A., S. Kazadzis, N. Krotkov, A. Bais, J. Grobner, and J. R. Herman
(2005), Assessment of TOMS UV bias due to absorbing aerosols,
J. Geophys. Res., 110, D23211, doi:10.1029/2005JD005913.
Relationship suggests a correction for the absorbing aerosols:
absb
UVUV
loperationacorrected
*1
)()(
)1(* SSAAODabs
Kinne, S.: Aerosol Direct Radiative Forcing
with an AERONET touch, Atmos. Environ.,
submitted, 2007.
Parameterization allows post-correction of the TOMS operational UV data:
Conclusions• Analog to the TOMS total column ozone time-series the
surface UV time-series are continued with the OMI measurement data applying an algorithm that is similar to the TOMS UV algorithm.
• There is a need to introduce a correction for absorbing aerosols. First step is to include a monthly climatology based on global aerosol models, satellite data, and sunphotometer measurements.
• The validation effort continues, important particularly when changes to the algorithm are applied.