+ All Categories
Home > Documents > AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES...

AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES...

Date post: 26-Jul-2020
Category:
Upload: others
View: 1 times
Download: 0 times
Share this document with a friend
13
AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES AND SAOZ TOTAL OZONE IN THE SOUTHERN TROPICS J.-P. Pommereau (1) , F. Goutail (1) , C. Clerbaux (1) , A. Pazmino (1) , A. Frihi (1) , C. Lerot (2) , M. Van Rozendael (2) (1) LATMOS, CNRS and University of Versailles Saint Quentin, Guyancourt, France (2) BIRA-IASB, Brussels, Belgium ATMOS Heraklion June 8-12 2015 1
Transcript
Page 1: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES AND SAOZ TOTAL

OZONE IN THE SOUTHERN TROPICS

J.-P. Pommereau(1), F. Goutail(1), C. Clerbaux(1), A. Pazmino(1), A. Frihi(1), C. Lerot(2), M. Van Rozendael(2)

(1) LATMOS, CNRS and University of Versailles Saint Quentin, Guyancourt, France

(2) BIRA-IASB, Brussels, Belgium

ATMOS Heraklion June 8-12 2015 1

Page 2: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

SATELLITES overpasses above SAOZ stations GOME2 CCI (2007-12), SCIAMACHY (2002-11), TOMS 1995-2005, NPP

(2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15)

SAOZ

• Zenith sky at twilight 86-91° SZA, Visible Chappuis bands

• Version 2 retrieval following NDACC working group recommendations (daily Air Mass Factors from TOMS V8 ozone profiles climatology)

• Data cleaned for thick clouds and rainfall from SAOZ O4 and H2O.

OZONE MEASUREMENTS

ATMOS Heraklion June 8-12 2015 2

Page 3: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

• GOME2, TOMS, SCIA : 2% seasonality <2012 • Seasonality decrease after 2012 • Negative peaks in the SH summer

SCIA CCI

GOME 2 CCI

TOMS

Satellite-SAOZ monthly mean (1)

ATMOS Heraklion June 8-12 2015

Page 4: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

• OMI-T, OMI-D, 1.6% seasonality <2012, OMI-CCI 2.4% • Seasonality reduction with all satellites after 2012

• Negative peaks in SH summer on OMI-T and OMI-CCI OMI

OMI-TOMS

OMI-DOAS

OMI-CCI

Satellite-SAOZ monthly mean (2)

ATMOS Heraklion June 8-12 2015

Page 5: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

IASI

SBUV

NPP

• Seasonality prior to 2012: IASI 2.6%, SBUV 2.2% • Reduced on all satellites after 2012

• Negative peaks of 3-4% on IASI, 1% on NPP, OMI-T, OMI-CCI, absent on SBUV

Satellite-SAOZ monthly mean (3)

ATMOS Heraklion June 8-12 2015

Page 6: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

SBUV-SAOZ

ATMOS Heraklion June 8-12 2015

DAILY SBUV-SAOZ IN 2013 < ± 1%

Page 7: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

All Satellite-SAOZ monthly mean corrected for mean biases

ATMOS Heraklion June 8-12 2015

SEASONALITY OF VARIABLE AMPLITUDE • max in 2007, 2009, 2010 • decrease after 2012 • of less than ± 0.5% after 2013

Page 8: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

All Satellite-SAOZ monthly mean corrected for mean biases

ATMOS Heraklion June 8-12 2015

NEGATIVE PEAKS (smaller Satellites or larger SAOZ) • every SH summer

• on individual year only • on IASI, OMI-T, OMI-CCI, NPP, SCIA-CCI and GOME-2 CCI

• absent in SBUV, OMI-D

Page 9: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

Discussion

1. Seasonality

• Since in phase on all satellites and reducing simultaneously after 2012, must come from SAOZ

• SAOZ instrument installed in 1998. No change identified since

then.

• Same SAOZ V3 retrieval procedure applied to all data

• SAOZ AMF derived from mean TOMS V8 ozone profile zonal climatology between 15°-25°S, interpolated at 20.9°S.

AMF variations not properly taken into account ??

ATMOS Heraklion June 8-12 2015

Page 10: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

Reunion Island

Equivalent Latitude seasonality

ITCZ near Reunion in SH summer, shifted to northern tropics in the SH winter

Equivalent latitude seasonality at Reunion Island

Difference % between Air Mass Factor calculated at 21° and 25°S.

Satellite-SAOZ seasonaility due to equivalent latitude change ?

ATMOS Heraklion June 8-12 2015

Smaller AMF in the summer if southern equivalent latitude taken into account

Page 11: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

2. Satellite-SAOZ minima

Dumile 3 Jan

Bejisa 3 Jan

Haliba 9 Mar

• SAT-SAOZ minima coincident with Hurricane on the same month • Hurricane days removed from SAOZ from detection of H2O and O4 peaks

• Hurricane signature on IASI, OMI-T, OMI-CCI and NPP •

• Satellites cleansing procedure for high clouds in the tropics requires improvement.

Gamede 25 Fev

Gelane 22 Feb

Fanele 21 Jan

Diwa 5 Mar

Ernest 22 Mar

Gaël 1 Fev

Giovanna 13 Feb

Hondo 28 Feb

ATMOS Heraklion June 8-12 2015

Dumile 3 Jan

Bejisa 3 Jan

Haliba 9 Mar

Bansi 11 Jan

Page 12: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

3. Equivalent latitude at 475 K (altitude of maximum ozone concentration)

ATMOS Heraklion June 8-12 2015

• High variability of Eq Lat seasonality (but no direct correlation with Sat-SAOZ O3 seasonality)

• Equivalent latitude slow increase at 475K • Is it enough for explaining the change of Sat-SAOZ

ozone seasonality after 2012?

Page 13: AMPLITUDE AND ORIGIN OF DIFFERENCE BETWEEN SATELLITES …seom.esa.int/atmos2015/files/presentation15.pdf · (2012-15), SBUV (1995-14), OMI-TOMS (2005-15), OMI-DOAS (2005-15) SAOZ

CONCLUSIONS

• Difference between Satellites and SAOZ of similar shape with all satellites but of variable amplitude

• Seasonality could be coming from ignorance of seasonal change of equivalent latitude in AMF calculations

• Perturbations of satellite measurements by hurricanes high clouds not

properly identified in IASI, OMI-T, OMI-CCI, NPP, SCIA, GOME2

• Slow increase of Reunion Island Equivalent Latitude

PERSPECTIVE • Improved detection and correction for very high clouds in satellite data

• Improved Air Mass Factor calculations

ATMOS Heraklion June 8-12 2015


Recommended