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Infrared Temperature and Water Vapor Sounding

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Title: Infrared Temperature and Water Vapor Sounding


1
Infrared Temperature and Water Vapor Sounding
  • Presented by
  • Chris Barnet

2
Requirement, Science, and Benefit
  • Requirement/Objective
  • Weather Water
  • Increase lead time and accuracy for weather and
    water warnings and forecasts.
  • Increase development, application, and transition
    of advanced science and technology to operations
    and services
  • Climate
  • Reduce uncertainty in climate projections through
    timely information on the forcing and feedbacks
    contributing to changes in the Earths climate.
  • Increase number and use of climate products and
    services to enhance public and private sector
    decision making.
  • Science
  • How can hyper-spectral information be exploited
    to improve accuracy and reduce uncertainty in
    satellite-derived temperature, moisture and trace
    gases?
  • Benefit
  • National Weather Service forecasters and their
    customers
  • Fully exploit temperature and moisture
    information content from hyper-spectral
    instruments.
  • Increase utilization of hyper-spectral
    information in difficult sounding domains (e.g.,
    cloudy scenes)
  • Climate applications
  • Long-term temperature and moisture trends and
    their interaction (water vapor feedback)
  • Long-term monitoring of greenhouse gases (carbon
    dioxide, methane, carbon monoxide).

3
Challenges and Path Forward
  • Science challenges
  • First principles algorithm still has regional
    and time dependent biases as result of null
    space errors between temperature, water vapor,
    and carbon dioxide.
  • Next steps
  • Migration of the AIRS/IASI algorithm to the CrIS
    instrument on NPP
  • Mitigation of biases through algorithm
    improvements.
  • Collaboration with modeling centers to develop
    efficient communication of retrieval vertical
    correlation (averaging functions) and error
    covariance.
  • Transition Path
  • For IASI the transition path is through SPSRB and
    products available via OSDPD.
  • For AIRS the transition path is through the NASA
    AIRS Science team and products are available at
    the NASA data archive.

3
4
Satellite Hyper-spectralInfrared Sounding
Research
  • Research description
  • Hyper-spectral instruments have 1000s of
    channels covering the near and far IR
  • State-of-the-art forward models used to compute
    instrument radiances.
  • Cloud clearing approach removes cloud effects.
  • Simultaneous solution of trace gases improves
    temperature and moisture products
  • Geophysical products derived from cloud cleared
    radiances capture more of the relevant weather
    information and significantly reduces data volume
    .
  • Recent science accomplishments
  • NOAA develops algorithms as part of the
    Atmospheric Infrared Sounder (AIRS) Science Team
    and delivers these to NASA for implementation.
  • AIRS algorithm has been migrated to the
    operational Infrared Atmospheric Sounding
    Interferometer (IASI) processing system.
  • Common algorithm and spectroscopy provides
    consistent products in the am and pm orbits.

IASI spectrum above comprised of 8460 channels
that sample molecular absorption from carbon
dioxide, water, ozone, trace gases. Sounding
algorithms use specific (i.e., select best)
channels to retrieve temperature and other
products.
5
NESDIS OperationalHyper-spectral products
  • STAR led the development and implementation of
    new and improved geophysical products from
    hyper-spectral instruments.
  • Led development of cloud clearing approaches.
  • Led development of deriving surface emissivity.
  • Knowledge of trace gases improves temperature and
    moisture accuracy in difficult sounding regions.
  • ozone absorption affects the temperature
    retrieval.
  • Trace gas products are useful in air-quality and
    climate applications
  • carbon monoxide is a precursor to tropospheric
    ozone which is both pollutant and greenhouse
    gas.
  • Detection of sulfur dioxide from volcanic events
    has enabled hazard condition alerts for air
    travel.
  • Atmospheric carbon products (carbon dioxide,
    methane, and carbon monoxide) are valuable for
    monitoring and understanding the carbon cycle and
    climate.

Product AIRS IASI
Temperature NASA DAAC NCDC/ CLASS
Water vapor NASA DAAC NCDC/ CLASS
Ozone NASA DAAC NCDC/ CLASS
Carbon monoxide NASA DAAC NCDC/ CLASS
Methane NASA DAAC NCDC/ CLASS
Carbon dioxide NOAA NESDIS (experimental) NCDC/ CLASS
Volcanic Sulfur Dioxide Real time flag From NOAA/NESDIS Real time flag From NOAA/NESDIS
Nitric Acid NOAA NESDIS (experimental) NCDC/ CLASS
Nitrous Oxide NOAA NESDIS (experimental) NCDC/ CLASS
6
Recent experiments show potentialvalue of
geophysical products
  • STAR has participated in experiments to
    demonstrating impact of using sounding products
    in operational forecast.
  • Joint Center for Satellite Data Assimilation
    experiments show that cloud cleared radiances
    have positive impact on the global forecast.
  • Use of cloud clear radiances (red) improves 6 day
    forecast by 4 hours relative to assimilation
    with AIRS clear scenes (blue).
  • Univ. Maryland, College Park has used
    experimental temperature and moisture products
    (w/ covariance) in their Kalman Ensemble model
  • AIRS T(p) and q(p) profiles improve zonal and
    meridional winds (blue regions)
  • NASA/Global Modeling and Assimilation Office has
    evaluated AIRS operational products.
  • Use of AIRS T(p) and q(p) profiles with QC
    improves forecast (red vs. black lines) more so
    than assimilating radiances (green)

7
Challenges and Path Forward
  • Science challenges
  • First principles algorithm still has regional
    and time dependent biases as result of null
    space errors between temperature, water vapor,
    and carbon dioxide.
  • Next steps
  • Migration of the AIRS/IASI algorithm to the CrIS
    instrument on NPP
  • Mitigation of biases through algorithm
    improvements.
  • Collaboration with modeling centers to develop
    efficient communication of retrieval vertical
    correlation (averaging functions) and error
    covariance.
  • Transition Path
  • For IASI the transition path is through SPSRB and
    products available via OSDPD.
  • For AIRS the transition path is through the NASA
    AIRS Science team and products are available at
    the NASA data archive.
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