Date post: | 14-Dec-2015 |
Category: |
Documents |
Upload: | malia-isham |
View: | 216 times |
Download: | 0 times |
WP 5 : Clouds & AerosolsWP 5 : Clouds & Aerosols
L.G. Tilstra and P. Stammes
Royal Netherlands Meteorological Institute (KNMI)
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013
Absorbing Aerosol Index (AAI)Absorbing Aerosol Index (AAI)
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (2)
Quality of the official SCIAMACHY Absorbing
Aerosol Index (AAI) level-2 product
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (3)
Absorbing Aerosol Index: version 3.01 versus version 5.02WAbsorbing Aerosol Index: version 3.01 versus version 5.02W
– Totally new algorithm setup
– New look-up tables (pseudo
spherical atmosphere +
including polarisation)
– Better surface height database
– ...
Changes in L1–2 data processor:
version 5.02W is a huge
improvement on version 3.01
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (4)
Scientific product (SC-AAI)
Official product (L2-AAI v5.02W)
Scientific product SC-AAI versus L2-AAI v5.02WScientific product SC-AAI versus L2-AAI v5.02W (2003)(2003)
(grey = sun glint filtering)
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (5)
Scatter plot:
Scientific product SC-AAI versus L2-AAI v5.02WScientific product SC-AAI versus L2-AAI v5.02W (2003)(2003)
Good agreement (in the year 2003)
– Calibration correction SC-AAI
– Degradation correction SC-AAI
– Ozone dependence taken into
account in SC-AAI
– L2-AAI: measurements
“converted” to the (shorter)
integration time of cluster 26
(O2–A band)
Explanation for the differences:
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (6)
Scientific product (SC-AAI)
Official product (L2-AAI)
Scientific product SC-AAI versus L2-AAI v5.02WScientific product SC-AAI versus L2-AAI v5.02W (2011)(2011)
The official L2-AAI is suffering from
a scan-angle dependence
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (7)
Scatter plot:
Scientific product SC-AAI versus L2-AAI v5.02WScientific product SC-AAI versus L2-AAI v5.02W (2011)(2011)
Official product suffers from a strong scan-angle dependence in 2011
colours: scan mirror positions
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (8)
Influence of (scan-angle dependent) instrument degradation:Influence of (scan-angle dependent) instrument degradation:
Global mean reflectance
Global mean residue (AAI)
[no m-factors applied]
[Tilstra et al., JGR 117, 2012]
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (9)
M-factors applied in calculation of L2-AAI:M-factors applied in calculation of L2-AAI:
Global mean residue (AAI)
Current m-factor approach is scan-angle independent; the official L2-AAI product
therefore shows a scan-angle dependence.
Although v5.02W is a large improvement on the previous version, data after 2006
are not to be used without application of necessary corrections by the user.
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (10)
Conclusions:Conclusions:
– The official AAI product of level-2 version 5.02W is a large improvement w.r.t.
the previous version 3.01.
– Instrument degradation has a large impact on the residue. The use of the official
AAI product after 2006 is problematic.
– This is, however, a level-1 issue.
– This issue will be addressed in version 8.x of the level-1 product.
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (11)
Extra slidesExtra slides
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (12)
(A is assumed to be wavelength independent: A340 =
A380)
A. Definition of the residue:
where the surface albedo A for the simulations is such that:
Rayleighmeas
380
340 10
380
34010 log log 100 R
R
R
Rr
)(Rayleigh380
meas380 ARR
The AAI represents the scene colour in the UV
Introduction: Absorbing Aerosol Index (AAI)Introduction: Absorbing Aerosol Index (AAI)
B. Definition of the AAI:
AAI = residue > 0 (and the AAI is not defined where residue < 0)
The AAI can be retrieved over land and sea surfaces, even in the presence of clouds.
no clouds, no aerosols : r = 0
clouds, scattering aerosols : r < 0
absorbing aerosols : r > 0
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (13)
Example of global aerosol distribution recorded by SCIAMACHY:
The “Global Dust Belt”:
Desert Dust Aerosols (DDA)
(dust storms, all year)
AAI from other UV satellite instruments: TOMS, GOME-1, OMI, GOME-2. Combined with
SCIAMACHY there are more than three decades (1978–2012) of AAI data available for
studies of trends in desert dust and biomass burning aerosol.
Biomass Burning Aerosols (BBA)
(dry season, anthropogenic)
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (14)
The “Global Dust Belt”
SCIAvisie Meeting, KNMI, De Bilt, 08-02-2013 (15)
Wavelength Wavelength pair (nm)pair (nm)
Equator Equator crossing crossing
timetime
Pixel size Pixel size (km)(km)
Days needed Days needed for global for global coveragecoverage
Platform / Platform / Operation periodOperation period
GOME–1GOME–1 340 / 380340 / 380 10 : 30 LT10 : 30 LT 320 × 40320 × 40 33ERS-2ERS-2
(1995 – 2003*)(1995 – 2003*)
SCIAMACHYSCIAMACHY 340 / 380340 / 380 10 : 00 LT10 : 00 LT 60 × 3060 × 30 66EnvisatEnvisat
(2002 – 2012)(2002 – 2012)
GOME–2GOME–2 340 / 380340 / 380 09 : 30 LT09 : 30 LT 80 × 4080 × 40 1.51.5MetOp-AMetOp-A
(2006 – present)(2006 – present)
OMIOMI 354 / 388354 / 388 13 : 30 LT13 : 30 LT 13 × 2413 × 24 11AuraAura
(2004 – present)(2004 – present)
AAI products from GOME-1, SCIAMACHY, GOME-2, and OMI:
*GOME-1: loss of global coverage on 22 June 2003 ; instrument retired on 4 July 2011