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SHADOZ Update: Report to US-Japan TTL Workshop

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Presentation on theme: "SHADOZ Update: Report to US-Japan TTL Workshop"— Presentation transcript:

1 SHADOZ Update: Report to US-Japan TTL Workshop
Anne Thompson, PI – 17 Oct 12

2 SHADOZ Website. http://croc-. gsfc. nasa
SHADOZ Website. Impact Metrics: Hundreds of Citations & Countless AVDC, NDACC Downloads 14 Stations operating Most recent archival paper With 33 Co-I authors: Thompson et al. J Geophys. Res., in press, 2012. = T12

3 Network affiliation ** Ancillary data/UACO variables
Topic of Study Station* Co-I/Sponsor** SHADOZ start year Site start year Network affiliation ** Ancillary data/UACO variables Expected sonde freq./year Long-term Validation / Trends (Data available prior to 1995) Kuala Lumpur Maznorizan bt Mohamad, Malaysian Met. Dept. 1998 1992 26 Watukosek Ninong Komala, LAPAN & Masatomo Fujiwara, Hokkaido Univ. SOWER CFH-water vapor profiles Am. Samoa Bryan Johnson & Samuel J. Oltmans, NOAA 1986 NDACC / GAW Dobson / surface CO2, CH4, CO, CFCs, O3 52 Natal Francis J. Schmidlin, NASA/Wallops & Neusa Paes Leme, INPE 1979 NDACC Brewer Hilo B. Johnson & S. J. Oltmans, NOAA 1982 MLO – Dobson, FTIR, O3 Lidar, CFH-water vapor / surface CO2, CH4, CO, CFCs, O3 Irene G.J.R. Coetzee, S. African Weather Serv. 1999 1990 Dobson La Reunion Françoise Posny, Université de La Réunion SAOZ, O3 Lidar Processes in the FT, TTL, and LS Fiji 1997 San Jose*** Rennie Selkirk, NASA/GSFC & Holger Vömel, GRUAN Lead Center 2006 GRUAN SO2 sondes, CFH-water vapor profiles San Cristobal GRUAN / SOWER Paramaribo Rinus Scheele, KNMI Ascension Is. Francis J. Schmidlin, NASA/Wallops TCCON / GAW Carbon columns / surface CO2, CH4, CO, CFCs Nairobi Bertrand Calpini, MeteoSwiss & John Nguyo, KMD 1996 Dobson, surface O3 Ha Noi H. Gia Hiep, AMO, S. Ogino, JAMSTEC, M. Fujiwara, Hokkaido Univ., & M. Shiotani, RISH 2005 2004 * Colors for stations indicate geographic region: blue-Western Pacific, red-Atlantic/Africa, white-Subtropics, & green-Equatorial Americas ** See Acronyms in Appendix *** Station formerly referred to as Alajuela / Heredia

4 Overview Newer Technical Issues (2012-2016)
SHADOZ proposals in review at NASA – Technical issues affecting site variations (biases) major focus Technical Issues & Progress ( ) Focus on 3 variables (Sensing Solution Type [SST], Instrument type, Pump Correction Factor [PCF]). Resolution & recommendations in JOSIE/WMO Reports (Smit et al., 2007; 2011); Thompson et al., 2007;= T07; Deshler et al., 2008 Current V05 SHADOZ data available Newer Technical Issues ( ) SHADOZ working with WMO/SPARC/IOC consultative process Will reprocessing all SHADOZ data in – recommended ‘homogenization’ to account for variations in background current, instrument and solution type Iterative process may include chamber test: “JOSIE” – 2014 Stay tuned for new issues: radiosonde, ozonesonde technical changes (new ‘state of things’ for network in 15th year!)

5 Implications for SHADOZ
Implications for SHADOZ. Interpretation of Station Biases in Stratospheric Measurement. T07 (not shown) mean total ozone offset relative to *TOMS* - 10 stations 5-7%, range 1-11% low In T12 (below), “re-processing” eliminated Paramaribo offset; 13-site mean offset < 5% relative to *OMI*. Hanoi, KL, Watukosek largest (low sonde) offset.

6 Looking Ahead. How to Address SHADOZ Data Set, from 1998-2012?
Issue illustrated below (from T12). SST change? Work with O3-DQA (WMO/JOSIE) consensus/consultative process in adopting and implementation recommendations Individual Pis to process data. Add meta-data to SHADOZ archive? files?

7 SHADOZ Proposal Table 3 - Summary of Schedule & Deliverables
Timeline SHADOZ PI, Collaborator/Partner Activities for O3S-DQA & SI2N Deliverables, Reporting & Publications April 2012 Sonde Technical Issues in O3S-DQA, Greenbelt Workshop, attended by PI, NASA, NOAA collaborators and Members of the WMO Ozone SAG Processing with first set of Transfer Functions by SHADOZ volunteers. O3S-DQA Report to SI2N Workshop, Columbia, MD. June – Dec. 2012 Preliminary data re-processing at selected stations Transfer function implementation. Re-process SHADOZ data set for stations with instrument, sensor solution changes. Optimize background current correction. (First scheduled: Fiji, Samoa, San Cristóbal) AGU Special Session on O3S-DQA and related sonde technical results: Dec. 2012, San Francisco Jan. – June 2013 Workshop, O3S-DQA Report, Publication preparations for SI2N and UNEP/WMO 2014 Assessment deadline. SHADOZ Deliverable: O3S-DQA Report(s). SHADOZ PI, Collaborators submit 1 or more journal articles for publication. June – Dec. 2013 Workshop: (1) evaluate Transfer Function and other re-processing changes on SHADOZ dataset; (2) Assess needs and protocol for Tropical-JOSIE to be conducted in Re-process all SHADOZ datasets (V06) for self-consistency within given station. Apply Transfer Function as needed. Jan – Dec. 2015 Review Results at WMO-sponsored Workshop. Conduct Tropical-JOSIE at WCCOS, Jülich. Jan. – Dec. 2016 Report at Quadrennial Ozone Symposium. Reprocess & homogenize the SHADOZ Data. Prepare publication(s) for 2018 UNEP/WMO Ozone Assessment. SHADOZ Statistical Analyses, Classifications with LID & SOM, Interannual Variability & Trends 2013 – 2014 Classified profiles on SHADOZ website or link Comparisons of LID & SOM for Ascension, Natal, Irene Prepare journal article, 2014 SHADOZ comparisons with TES Prepare journal article, 2015 Classified profiles for KL, Hilo, Nairobi, Samoa Analyze reprocessed, homogenized data for climate signals, trends Prepare journal article, 2016

8 SHADOZ in SEACIONS/SEAC4RS

9 extras

10 Variables Affecting Ozone Measurement
Variables Affecting Ozone Measurement. Note that Some Affect Entire Profile, Others More Important in Stratosphere or TTL Every sonde launched is a new instrument Pozone = 4.31 x (I- I bg ) x Tpump x PCF (1/F) Calibrated through exposure to low, high ozone amounts. Important variables SST = sonde solution type. KI strength, buffering, eg 0.5%, buffered; 1% buffered, 2% unbuffered; 0.5%, 0.1% buffered, etc Response time, Ibackground determined in pre-launch calibration Pump efficiency correction important above 25 km Instrument manufacturer (“type”), materials Mixing ratio/Partial pressure of ozone = PO3/P(total Atm)

11 Status for SHADOZ, 2004 (in Smit et al. , 2007; Thompson et al
Status for SHADOZ, 2004 (in Smit et al., 2007; Thompson et al., 2007 [T07]). PCF Below

12 Comparisons of 4 SSTs (KI strength) & Manufacturer in Chamber/JOSIE (left) & on Field Test (BESOS) (right), relative to standard uv photometer. (From H. Smit, in Thompson et al., 2010). JOSIE 2000 BESOS 2004 A B OPM = UV Photometer “Standard” used in JOSIE chamber & on BESOS Balloon : 1) Precision and accuracy both 5-10% vs 15% pre-SHADOZ 2) WMO/GAW (World Meteorological Organization/Global Atmospheric Watch) adopted new standards as a result

13 SHADOZ & QUALITY ASSURANCE: UV Photometer & JOSIE-2000 Chamber Tests
Above – JOSIE chamber, 9/ Right -- JOSIE-2000 explains Nairobi high stratospheric ozone bias. Methods tested: Buffer Instrument (1) NOAA/CMDL = Fiji, Samoa, San Cristöbal No SPC (2) NASA/WFF = Ascension/Natal Yes SPC (3) MeteoSwiss/Payerne = Nairobi Yes SPC & Ensci

14 SHADOZ Climatology at Tropical Sites Shows Bias at
Individual Stations – T07 (Left, 98-02); T12 (Right, ) Individual stations show bias in stratospheric profile segment when compared to SHADOZ tropical mean.

15 Emerging Technical Issues (2009)
Background Current (Voemel & Diaz, 2009; Stuebi & Levrat, 2009). Implication for SHADOZ at certain sites. Refer to Solomon et al. 2005, Left Response time – an issue in TTL? (refer to Shiotani/SMILES paper, QOS) – stay tuned New Radiosondes (RS80-> RS92->Imet). DISCOVER-AQ example, Right Third instrument type. SPC stable, ENSCI-> DMT ?? – Time will tell! DISCOVER, DKM


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