. is sponsored by the National Science Foundation David Edwards (NCAR) and Arlindo DeSilva (NASA GSFC) with input from the GEO-CAPE SWG CEOS/MACC-II OSSE.

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Presentation transcript:

. is sponsored by the National Science Foundation David Edwards (NCAR) and Arlindo DeSilva (NASA GSFC) with input from the GEO-CAPE SWG CEOS/MACC-II OSSE Workshop A global GEO OSSE activity for GEO-CAPE & CEOS

. Motivation: NASA FY13 Guidance to GEO-CAPE includes the following two points:  2/ Continue to develop and apply OSSE tools to demonstrate the expected impact of the GEO-CAPE atmosphere observations  4/ Continue scientific coordination with complementary Korean and European geosynchronous missions We expect that the GEO-CAPE Global OSSE activity will coordinate with the ongoing Regional and Urban OSSE activity and potentially share people, data and models Current Working Group: David Edwards (Co-Chair, NCAR), Arlindo da Silva (Co-Chair, NASA GSFC/GMAO), Kevin Bowman (JPL), Daven Henze (CU), Peter Zoogman (Harvard) and the GEO-CAPE Regional OSSE Working Group members GEO-CAPE Global OSSE Working Group

. Observation System Simulation Experiments (OSSEs) Observing System Simulation Experiments (OSSEs) have been extensively used by the NWP community in order to help develop and optimize contemporary meteorological satellite instruments OSSEs are now also increasingly used in other fields of earth observation OSSEs assess the impact of hypothetical observations on a model analysis/forecast/inversion and provide a means to generalize on the limited conclusions of case-studies The CEOS/ACC whitepaper A Geostationary Satellite Constellation for Observing Global Air Quality: An International Path Forward called for “(OSSE) cooperation to define, conduct, and analyze common scenarios ….align and extend the ongoing regional studies and to systematically incorporate them into global studies.” Collaboration opportunity between the planned and proposed geostationary Earth orbit (GEO) missions from NASA GEO- CAPE/TEMPO, French MAGEAQ, ESA Sentinel 4, Korean GEMS and Japan

. ECMWF Workshop on Atmospheric Composition OSSEs A CEOS/MACC-II International chemical OSSE Workshop was held at ECMWF in October 2012 attracting 30 participants sharing expertise toward developing common approaches and experiments The meeting aimed at reviewing experience from NWP, reporting on existing work worldwide on OSSEs for "chemical" satellite instruments, discussing best practices and defining needed infrastructure in order to set up reliable experiments Goal: Define experiments to document the impact of GEO instruments alone, together over different parts of the globe, and in conjunction with LEO assets Organizers: J. Al-Saadi (NASA, USA), D. Edwards (NCAR, USA), Y. Kasai (NICT, Japan), V.-H. Peuch (ECMWF, UK), C. H. Song (GIST, Korea) Agenda:  Discussion on what makes a good OSSE  Talks by ECMWF meteorological OSSE experts describing experience and contrasting with chemical OSSEs  Reports on OSSE activities to-date under GEO-CAPE/TEMPO, MAGEAQ, Sentinel 4, Korea GEMS and Japan – primarily GEO  Breakout groups for the OSSE elements: Simulators, Nature/Control runs and Assimilation Highlighted pragmatic approaches: These are computationally expensive experiments requiring a breadth of expertise

. A Chemical Observation System Simulation Experiment (OSSE) for Lowermost Atmosphere CO Nature & Control Runs Instrument Simulator Data Assimilation

. Planned Experiments Regional: Aimed at trade-offs between different instrumentation and observing strategies in regional models – these are funded and in progress in several countries e.g. ESA/ISOTROP Global: Demonstrate value of the CEOS GEO constellation, quantifying regional gains & impact of losing one or more members For practical reasons, OSSEs will be performed using global models at high resolution instead of a regional model, and will be designed to minimize the impact of this assumption Two main categories of OSSE are identified:  Forward problem: What is the impact of a proposed measurement system(s) for improving analysis and forecast of the pollutant distribution?  Inverse problem: How does a proposed measurement system(s) help in constraining the upwind precursor emissions and boundary conditions through adjoint analysis? First step: Consider a primarily tracer study for aerosol and/or CO to investigate the impact of long-range transport; Second Step: Expand this to include ozone chemistry

The Observation Simulator 1. Nature Run Model Required state: 4. Retrieved Products: Radiative Transfer Instrument Description Noise: 2. The Forward Model Simulated signal: Measurement Sensitivity: 2. The Forward Model Simulated signal: Measurement Sensitivity:

. Observation Simulator measurement & retrieval characteristics are represented by the Averaging Kernel (AK) and retrieval error However, running the full Observation Simulator in the OSSE is expensive and very involved The CO and O 3 OSSEs have been simplified by assuming all observations can be represented with a few AK cases and these are used to sample the Nature Run model everywhere/all day But AKs vary a lot…. Retrieval Averaging Kernels Retrieval Averaging Kernels Depend on surface characteristics, temperatures, clouds, aerosol loadings, trace gas loadings, viewing and solar angles Realistic OSSEs need to account for this Spread in CONUS AKs for surface & 500 hPa MOPITT CO Lower tropos. TES-OMI O Pressure (hPa)

. OSSE Development of AK prediction tool OSSE Development of AK prediction tool Evaluation of predicted AKs from multiple regression vs. test case (true) AKs Apply true, predicted and CONUS average AKs to common reference and a priori profiles. Error histograms for CO or O 3 are with respect to the profiles given by the true AKs. See poster and reference: Worden et al., AMTD, Error in O 3 (ppb) Errors in O 3 from using a CONUS average AK Errors in O 3 from using predicted AKs Errors in O 3 for lowermost troposphere Error in CO (ppb) Error in CO from using a CONUS Average AK Number of Observations Errors in CO for lowermost troposphere Errors in CO from using a CONUS average AK Errors in CO from using predicted AKs

.  OSSEs need to account for realistic atmospheric variability: Requires evaluation of NR with observations  OSSEs require realistic variability in measurement simulations generated from NR: Requires incorporation of sensitivities due to cloud, aerosol, trace gases, surface UV-visible reflectivity, and IR emissivity  Simulated retrievals must include realistic range of sensitivities: Requires generation of scene-dependent AKs and errors  OSSEs for relative performance between instruments/viewing scenarios may be more reliable: If comparing a next generation, we need high accuracy and full system evaluation with the existing observing system  NWP experience: OSSE-based decisions have international stakeholders and experiments should be developed as joint global projects. Community ownership and oversight of OSSE capability is also important for maintaining credibility Atmospheric Composition Remote Sensing & Prediction Summary