E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 1 Topics 1.MWs Joint Retrieval of pT, H 2 O, O 3 without CO2MIX as a source of systematic error; MWs Joint.

Slides:



Advertisements
Similar presentations
Institute for Climate and Atmospheric Science SCHOOL OF EARTH AND ENVIRONMENT 3D SLIMCAT Studies of Arctic Ozone Loss Wuhu Feng Acknowledgments: Martyn.
Advertisements

Oxygen: Stratosphere, Mesosphere and Thermosphere Part-3 Chemical Rate Equations Ozone Density vs. Altitude Stratospheric Heating Thermal Conductivity.
Page 1 MIPAS QWG #15, ESRIN, 23-25/01/08 Bianca Maria Dinelli Istituto di Scienze dell'Atmosfera e del Clima CNR (Italy) Enzo Papandrea Massimo Carlotti.
Full Resolution – Reduced Resolution differences E. Papandrea, M. Carlotti, M. Ridolfi, E. Arnone DCFI, University of Bologna, Italy B.M. Dinelli ISAC-CNR,
Using global models and chemical observations to diagnose eddy diffusion.
ACE Linelist Needs for the Atmospheric Chemistry Experiment Chris Boone and Peter Bernath Univ. of Waterloo, Waterloo, Ontario, Canada HITRAN 2006 Conference.
Microwindow Selection for the MIPAS Reduced Resolution Mode INTRODUCTION Microwindows are the small subsets of the complete MIPAS spectrum which are used.
METO 621 Lesson 21. The Stratosphere We will now consider the chemistry of the troposphere and stratosphere. There are two reasons why we can separate.
Page 1 CO2 distribution in stratosphere from MIPAS Bianca Maria Dinelli Istituto di Scienze dell'Atmosfera e del Clima CNR (Italy) Massimo Carlotti Enzo.
Spatial Reduction Algorithm for Numerical Modeling of Atmospheric Pollutant Transport Yevgenii Rastigejev, Philippe LeSager Harvard University Michael.
Page 1 ENVISAT Symposium – Salzburg - Austria 6-10 September 2004 GEO-MTR: A 2-Dimensional Multi Target Retrieval System for MIPAS/ENVISAT Observations.
Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia ASSFTS-13 Toulouse 7-9 Nov 2007 Page 1 Oxford Retrievals of MIPAS Data Anu Dudhia.
Chiara Piccolo and Anu Dudhia Atmospheric, Oceanic and Planetary Physics, Department of Physics, Oxford University, Oxford, UK Predicted.
METO 621 Lesson 24. The Troposphere In the Stratosphere we had high energy photons so that oxygen atoms and ozone dominated the chemistry. In the troposphere.
Page 1 Atmospheric, Oceanic & Planetary Physics, University of Oxford MIPAS QWG9 Florence 01/02 Feb 2006A Dudhia Microwindow Selection for new* Nominal.
Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG12 ESRIN Feb 2007 Page 1 pT Microwindows Anu Dudhia University of.
Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG15 ESRIN Jan 2008 Page 1 Status of Proposed L2 Changes Anu Dudhia.
Atmospheric, Oceanic & Planetary Physics, University of Oxford A Dudhia MIPAS QWG16 Venice Apr 2008 Page 1 Recent MIPAS L2 Data Retrieved at Oxford.
Page 1 ENVISAT SYMPOSIUM - Montreux – 23/27 April 2007 Page 1 Stratospheric Distribution of CO 2 from the MIPAS High-resolution Full Mission Bianca Maria.
Introduction. A major focus of SCOUT-O3 is the tropics and a key issue here is testing how well existing global 3D models perform in this region. This.
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
STRATOSPHERIC CHEMISTRY. TOPICS FOR TODAY 1.Review of stratospheric chemistry 2.Recent trends in stratospheric ozone and forcing 3.How will stratospheric.
CHAPMAN MECHANISM FOR STRATOSPHERIC OZONE (1930) O O 3 O2O2 slow fast Odd oxygen family [O x ] = [O 3 ] + [O] R2 R3 R4 R1.
This Week—Polar Stratospheric Chemistry READING: Chapter 10 of text SPADE Data Analysis Pt 1: Due Tuesday Nov 13.
Atmosphere Carrie Vollmer Topic Troposphere 10 miles (5-16 km) where we live Contains:  Nitrogen – 78%  Oxygen – 21%  Almost all water vapor.
Simple Chemical modeling of ozone sensitivity
Update on paleochemistry simulations Jean-François Lamarque and J.T. Kiehl Earth and Sun Systems Laboratory National Center for Atmospheric Research.
Werner Schmutz, PMOD/WRC Status of the space weather experiments LYRA/PROBA2 and PREMOS/PICARD PMOD/WRC COST 724 project: Short-term variability.
The Odin satellite Swedish led mini-satellite. Cooperation with Canada, Finland, France. Launched in February Design lifetime: 2 years. Circular.
Page 1 MIPAS QWG#12 14/16 February 2007 Retrieval of 15 N/ 14 N isotopic ratio from MIPAS spectra Feasibility of 15 N/ 14 N isotopic ratio profile retrieval.
INTRODUCTION When two or more instruments sound the same portion of atmosphere and observe the same species either in different spectral regions or with.
Pressure Broadening and Spectral Overlap in the Millimeter Wave Spectrum of Ozone International Symposium on Molecular Spectroscopy 65 th Meeting — June.
Page 1ENVISAT Validation Review / GOMOS session - ESRIN – 13th December 2002 ENVISAT VALIDATION WORKSHOP GOMOS Recommendations by the ESL team : Service.
The Atmosphere as a Chemical Reactor OutputsInputs Chemistry Radiation (energy) Biogeochemical Cycling.
IAC ETH, 26 October 2004 Sub-project: Effects of Solar irradiance variability on the atmosphere (steady-state sensitivity study) Progress report (final)
Short term variability of the ozone and other species simulated using LYRA data Tatiana Egorova *, Eugene Rozanov *,**, Werner Schmutz * Ingolf Dammash.
IASI CH 4 Operational Retrieval Feasibility - Optimal Estimation Method Task 1+3: Updates Richard Siddans, Jane Hurley PM2, webex 10 October 2014.
TA11D –Teach About Air Layers Use with BrishLab ES11D Done By: Coach This material is CC by StarMaterials.com.
Constraints on the Production of Nitric Oxide by Lightning as Inferred from Satellite Observations Randall Martin Dalhousie University With contributions.
A new spectroscopic observatory in Créteil to measure atmospheric trace gases in solar occultation geometry C. Viatte, P. Chelin, M. Eremenko, C. Keim,
CHEM /15/12 I.C Strat. Chemistry: Catalytic Ozone Depletion - Catalyst “Families” (HO x, NO x, ClO x ) - Reaction Paths/Cycles (#1, #2, #3) - Sources.
Simulation Experiments for TEMPO Air Quality Objectives Peter Zoogman, Daniel Jacob, Kelly Chance, Xiong Liu, Arlene Fiore, Meiyun Lin, Katie Travis, Annmarie.
METO 621 CHEM Lesson 4. Total Ozone Field March 11, 1990 Nimbus 7 TOMS (Hudson et al., 2003)
Page 1 COST 723 – Opening Workshop - ESTEC March 2004 GEO-MTR: A 2-Dimensional Multi Target Retrieval System for MIPAS/ENVISAT observations Bianca.
Layers of the Atmosphere Layer NameAltitude (km) Temperature change with altitude.
Directions: Choose the correct layer of the atmosphere. Identify the layer that the red star marks.
Night OH in the Mesosphere of Venus and Earth Christopher Parkinson Dept. Atmospheric, Oceanic, and Space Sciences University of Michigan F. Mills, M.
Ozone Budget From: Jacob. Ozone in the Atmosphere Lifetime: –~1 month –Highly variable – dependent on season, latitude, altitude, etc. Background concentrations:
Comparisons of ACE-FTS and PARIS-IR Measurements of Several Trace Gases in the Northern Mid-latitude Atmosphere Dejian Fu, Kaley A. Walker, Keeyoon Sung,
GOME2 Error Study WP 150: Basic SNR column retrieval PM2 10/2001 SNR Basic Column Retrieval R. De Beek, M. Weber,
Free Tropospheric Measurements of Biomass Burning Emissions by the Atmospheric Chemistry Experiment (ACE) Curtis Rinsland, Chris Boone, and Linda Chiou.
SCSL SWAP/LYRA workshop
MIPAS Monitoring at Oxford
Workshop on Air Quality Data Analysis and Interpretation
Nowcasting of neutral and ion composition of the mesosphere:
Dec06 Nominal Mode Chiara Piccolo University of Oxford
EGS-AGU-EUG Joint Assembly, Session AS27, Nice 6-11 April 2003
T. Encrenaz, B. Bézard, T. Fouchet,
Percent of Global GHG Emissions 14%
Structure of the atmosphere
Randall Martin Aaron Van Donkelaar Daniel Jacob Dorian Abbot
Satellite Remote Sensing of Ozone-NOx-VOC Sensitivity
Space-based Diagnosis of Surface Ozone Sensitivity to Anthropogenic Emissions Randall Martin Aaron Van Donkelaar Arlene Fiore.
OZONE PRODUCTION IN TROPOSPHERE
Percent of Global GHG Emissions 14%
Authors: B.Kerridge, R.Siddans, J.Reburn, B.Latter and V.Jay
MIPAS-2D water database and its validation
The Atmosphere.
6.1: Properties of the Atmosphere
Benchmarking of chemical mechanisms
Presentation transcript:

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 1 Topics 1.MWs Joint Retrieval of pT, H 2 O, O 3 without CO2MIX as a source of systematic error; MWs Joint Retrieval of pT, H 2 O, O 3, CO 2 to improve p and CO 2 sensitivity (pT, CO 2 not good as their features are not well separated). 2.Minor species: H 2 O 2 retrieval as an example of specie not yet retrieved.

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 2 PT, H 2 O, O 3 Spectral Range: 685 – 825 cm -1 Q – branches of CO 2 CO 2 line – mixing model has been integrated in the MTR code, these MWs have been sel. to test it

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 3

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 4 PT, H 2 O, O 3, CO 2 Spectral Range: all bands

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 5 We are looking if it is possible to improve CO 2 accuracy.

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 6 H2O2H2O2 OH + O 3 HO 2 + O 2 HO 2 + HO 2 H 2 O 2 + O 2 H 2 O 2 is important as a sink of OH which plays an important role in atmosphere chemistry (OH reacts with CO and CH 4 ) Lifetime OH about 10 seconds Lifetime H 2 O 2 about 1 day H 2 O 2 is created by O 3 Short lifetime

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 7 H 2 O 2 Spectral Range: Band B

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 8 Retrieval can be performed in troposphere – stratosphere regions but not in mesosphere

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 9 Example of a real H 2 O 2 retrieval Blue and red colors = good retrieval ORBIT JUL 2002 No data scan 0, 58,59 Max at 10 mb in eq. regions PSC in south pole

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 10 ORBIT 2081 (from north pole to south pole, day time) Good agreement retrieved and Slimcat model for the Max at 10 mb in eq. regions and minimum below We don’t see the equatorial peak at 200 mb and Slimcat peak is larger Comparison retrieved - Slimcat

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 11 ORBIT 2081 Where ozone has a peak also H 2 O 2 has a peak and where ozone has a minimum again H 2 O 2 has a minimum

E.Papandrea PM4 - Esrin, 5 th Nov 2004 DFCI Page 12 Conclusions New MWs set for joint retrieval pT H 2 O, O 3 without CO 2 error component (to be tested with geofit + line mixing model). New MWs set for joint retrieval pT H 2 O, O 3, CO 2. H 2 O 2 can be retrieved with MIPAS data.