amfic third progress meeting mariliza koukouli & dimitris balis laboratory of atmospheric...
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AMFIC third progress meeting
MariLiza Koukouli & Dimitris Balis Laboratory of Atmospheric PhysicsAristotle University of Thessaloniki
Task 3.1: Validation of satellite-retrieved aerosol properties over a wide range of geolocations over Europe and China using ground-based results from the AERONET network.
Task 3.2: Validation of satellite-retrieved aerosol properties over the city of Thessaloniki using a dedicated ground-based Brewer spectrophotometer.
Task 3.3: Validation of satellite-retrieved SO2 pollution fields over a wide range of geolocations over Europe and China where ground-based Brewer spectrophotometers exist.
Task 3.4: Validation of the satellite-retrieved SO2 pollution fields over the city of Thessaloniki using the coincident to the satellite overpass ground-based Brewer spectrophotometers measurements.
Task 3.5: Validation of satellite-retrieved tropospheric O3 slant columns over selected Chinese and European stations that include ozone sondes.
Work package 3: Validation of aerosol properties, SO2 and O3 amounts
Task 3.1: Validation of satellite-retrieved aerosol properties over a wide range of geolocations over Europe and China using ground-based results from the AERONET network.
With Anu-Maija Sundström, Pekka Kolmonen and Gerrit de Leeuw
Aeronet data http://aeronet.gsfc.nasa.gov AERONET provides globally
distributed observations of spectral aerosol optical depth (AOD), inversion products, and precipitable water in diverse aerosol regimes. Aerosol optical depth data are computed for three data quality levels: Level 1.0 (unscreened), Level 1.5 (cloud-screened), and Level 2.0 (cloud-screened and quality-assured).
AOD at 675nm & associated Angstrom Exponent
AATSR data provided by FMI AODs from AATSR are at
555, 659 & 1060nm. Data given for a 5km radius
from the ground-based station.
27 European stations from AATSR for year 2006 with an average of 10 days of measurements per station.
6 China stations from AATSR analysis for one month in 2007 and three months in 2008, same issue as above was encountered.
Europe
Moldova: station possibly plagued by sulfate aerosols due to well-established SO2 pollution.
Crete: station often affected by absorbing dust aerosol due to Saharan storms that plague the island.
All 27 European stations
China
China: dirty pollution, fine mode and neutral aerosol, coarse mode.
China: sulphate type, fine mode and mineral type, coarse mode
Conclusions – suggestions for the near future More data from AATSR? -> infrastructure is
ready and waiting! Collaborate on the deliverable with FMI?
Task 3.2: Validation of satellite-retrieved aerosol properties over the city of Thessaloniki using a dedicated ground-based Brewer spectrophotometer.
Koukouli, et al., Investigation of the negative trend in the MODIS Aerosol Optical Depth over the Southern Balkans, submitted to Atmospheric Environment, 2009
Task 3.3: Validation of satellite-retrieved SO2 pollution fields over a wide range of geolocations over Europe and China where ground-based Brewer spectrophotometers exist.
With Jos van Geffen and Michel Van Roozendael
MaxDOAS in Beijing
Southern latitudes around Beijing, 100km
Northern latitudes around Beijing, 100km
All latitudes around Beijing, 100km
Investigating further into the South-North gradient issue
Task 3.4: Validation of the satellite-retrieved SO2 pollution fields over the city of Thessaloniki using the coincident to the satellite overpass ground-based Brewer spectrophotometers measurements.
Koukouli, et al., SO2 atmospheric loading revealed through ground-based and satellite measurements, International Conference On Space Technology, August 2009.
Task 3.5: Validation of satellite-retrieved tropospheric O3 slant columns over selected Chinese and European stations that include ozonesondes.
With Ronald van der A, Olaf Tuinder and Jacob van Peet
Ozonesonde sites around the globe
The datasets GOME-2 : tropospheric O3 profiles
provided from 01.05.2007 to 31.12.2008 Ground-based: 29 ozonesonde stations
have coincident measurements within the GOME2 time frame. Since so few data points exist, all available ozonesondes are used in this study. The ozonesondes provide high resolution
vertical ozone profiles.
The methodology First comparison: 1. The height of the tropopause is found, in
order to integrate the ozonesonde vertical profile into a tropospheric ozone column [TOC].
2. The two quantities are then directly compared, i.e. the GOME-2 TOC to the ozonesonde integrated TOC.
This comparison will be called : without AK treatment
The methodology Second comparison:1. The ozonesonde profile is convolved into a new
profile using the apriori ozone profile and averaging kernels that were used in the GOME-2 analysis as follows: X’OZONESONDE = XAPRIORI + AK * [XOZONESONDE-XAPRIORI]
2. This convolved profile is then integrated up to the tropopause level to a new TOC.
3. The new convolved TOC is compared to the GOME-2 TOC.
This comparison will be called : with AK treatment
Comparing tropopause levels for four different ozonesondes: 21-EDMONTON, 221-LEGIONOWO , 242-PRAHA , 308-MADRID
Typical example – Hohenpeissenberg
Without AK treatment With AK treatment
Mean difference 10%, no common variability.
Mean difference 30%, common variability.
Dependency on the latitude & SZA.
Without AK treatment With AK treatment
Dependency on the distance from ground-station & on the tropopause height.
Without AK treatment With AK treatment
O3-Saf GOME2 validation of tropospheric O3 profilesUTLS consistent overestimationWork of: Andy Delcloo, Royal Meteorological Institute of Belgium
Conclusions - I No dependency on cloud parameters, total
ozone, distance from ground-based station.
Some dependency on solar zenith angle with smaller angles giving less satellite overestimation.
Strong dependency of final convolved ozonesonde TOC on the apriori & averaging kernel.
Comparing the apriori and the convolved ozonesonde TOC for all data points
20 0 7.8 20 0 8 20 0 8 .2 20 0 8 .4 20 0 8 .6 20 0 8 .8 20 0 9
0
20
40
60
8 0
10 0
Apriori
Convolved Ozonesonde
Comparing the GOME-2 and the convolved ozonesonde TOC for all data points
20 0 7.8 20 0 8 20 0 8 .2 20 0 8 .4 20 0 8 .6 20 0 8 .8 20 0 9
0
20
40
60
8 0
10 0
GOME-2
Convolved Ozonesonde
Dependency of convolved ozonesonde TOC on apriori used
20 40 60 8 0 10 0A pr ior i
20
40
60
8 0
10 0
Ozo
nes
on
de
con
volv
ed
Equation Y = 0.657* X + 11.909Num ber of data points used = 632
Average X = 46.4657 & Average Y = 42.454R-squared = 0.671
0 20 40 60 8 0G O M E 2
20
40
60
8 0
10 0
Ozo
nes
on
de
con
volv
ed
Equation Y = 0.401 * X + 27.784Num ber of data points used = 632
Average X = 36.574&Average Y = 42.454R-squared = 0.150
Conclusions - II Another main problem seem to be the
number of measurements in total.
Conclusions – Next steps New averaging kernel treatment to allow
the convolved ozonesonde profile to approach the original ozonesonde profile and not follow the apriori profile shape.
More months of data which will improve the statistics and permit the assessment of both satellite and ground-based measurements.
Status of Work package 3: Validation of aerosol properties, SO2 and O3 amounts
Task 3.1: Validation of satellite-retrieved aerosol properties over a wide range of geolocations over Europe and China using ground-based results from the AERONET network.
Task 3.2: Validation of satellite-retrieved aerosol properties over the city of Thessaloniki using a dedicated ground-based Brewer spectrophotometer.
Task 3.1: Work in progress.
Task 3.2: Work in progress [completed for MODIS data].
Status of Work package 3: Validation of aerosol properties, SO2 and O3 amounts
Task 3.3: Validation of satellite-retrieved SO2 pollution fields over a wide range of geolocations over Europe and China where ground-based Brewer spectrophotometers exist.
Task 3.4: Validation of the satellite-retrieved SO2 pollution fields over the city of Thessaloniki using the coincident to the satellite overpass ground-based Brewer spectrophotometers measurements.
Task 3.3: Completed.
Task 3.2: Completed.
Status of Work package 3: Validation of aerosol properties, SO2 and O3 amounts
Task 3.5: Validation of satellite-retrieved tropospheric O3 slant columns over selected Chinese and European stations that include ozone sondes.
Task 3.5: Work in progress.