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Atmospheric Infrared Sounder (AIRS) Atmospheric Infrared Sounder - PowerPoint PPT Presentation

National Aeronautics and National Aeronautics and Space Administration Space Administration Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California


  1. National Aeronautics and National Aeronautics and Space Administration Space Administration Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California Atmospheric Infrared Sounder (AIRS) Atmospheric Infrared Sounder (AIRS) Project Status Project Status September 26, 2006 September 26, 2006 T. Pagano T. Pagano AIRS Project Office AIRS Project Office Jet Propulsion Laboratory Jet Propulsion Laboratory 1 1

  2. National Aeronautics and National Aeronautics and Space Administration Space Administration Agenda Agenda Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California  Meeting Agenda/Logistics Meeting Agenda/Logistics   Standard Product Status Standard Product Status   Weather Forecast Improvement Weather Forecast Improvement   Key Science Investigations Key Science Investigations   Science Team and Awards Science Team and Awards   ARIES Future Mission Concept ARIES Future Mission Concept  • Builds on AIRS and MODIS Builds on AIRS and MODIS •  Summary and Conclusions Summary and Conclusions  2 2

  3. National Aeronautics and National Aeronautics and Space Administration Space Administration AIRS/AMSU/HSB Standard Products AIRS/AMSU/HSB Standard Products Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California RMS Requirement Current Estimate Current Estimate RMS Requirement Radiance Products (Level 1B) Radiance Products (Level 1B) AIRS IR Radiance 3%* 3%* AIRS IR Radiance <0.2% <0.2% 20% AIRS VIS/NIR Radiance AIRS VIS/NIR Radiance 20% 10-15% 10-15% 0.25-1.2 K AMSU Radiance AMSU Radiance 0.25-1.2 K 1-2 K 1-2 K 1.0-1.2 K HSB Radiance HSB Radiance 1.0-1.2 K N/A N/A Standard Core Products (Level 2) Standard Core Products (Level 2) Cloud Cleared IR Radiance Cloud Cleared IR Radiance 1.0 K 1.0 K <1.0 K <1.0 K Sea Surface Temperature 0.5 K 0.5 K Sea Surface Temperature 0.8 K 0.8 K Land Surface Temperature 1.0 K 1.0 K Land Surface Temperature TBD (V5) TBD (V5) Temperature Profile 1 K / km 1 K / km Temperature Profile 1K / km 1K / km Humidity Profile 15% / 2 km 15% / 2 km Humidity Profile 15% / 2km 15% / 2km 5% Total Precipitable Water Total Precipitable Water 5% 5% 5% 5% Fractional Cloud Cover Fractional Cloud Cover 5% TBD (V5) TBD (V5) 0.5 km Cloud Top Height Cloud Top Height 0.5 km TBD (V5) TBD (V5) 1.0 K Cloud Top Temperature Cloud Top Temperature 1.0 K TBD (V5) TBD (V5) Ozone Column - - Total Ozone Column 5% 5% Total - - TBD (V5) Ozone Profile TBD (V5) Ozone Profile Carbon Monoxide - - Carbon Monoxide TBD (V5) TBD (V5) Methane - - Methane TBD (V5) TBD (V5) 3 3

  4. National Aeronautics and National Aeronautics and Space Administration Space Administration AIRS Level 3 Products online for V4 AIRS Level 3 Products online for V4 Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California 4 4

  5. National Aeronautics and National Aeronautics and Space Administration Space Administration 3 New Standard Products for Version 5 3 New Standard Products for Version 5 Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California Ozone Profile  • Good sensitivity, but use wisely! • Bian, J., A. Gettelman, H. Chen, and L. L. Pan, Validation of satellite ozone profile retrievals using Beijing ozonesonde data, JGR, in review • Pan, L.L., J.C Wei, C. Barnet, A. Gettelman, W. J. Randel, R. Gao, E.V. Browell, and O. Cooper, Validation of AIRS ozone profile in the upper troposphere and lower stratosphere using airborne in situ measurements, to be submitted. • Monahan, K., L. L. Pan, J. C. Wei, A. McDonald, G. Boderker, Validation of AIRS ozone product using ozonesodes from Lauder, New Zealand and Boulder, USA., in preparation. 2006 Carbon Monoxide Profile  • Well validated; ready for science use. • McMillan, W. W., et al. (2005), Daily global maps of carbon monoxide from NASA's Atmospheric Infrared Sounder, Geophysical Research Letters, 32. L11801 Methane Profile  • Development complete. Limited Validation! • Validation underway by NOAA 5 5

  6. National Aeronautics and National Aeronautics and Space Administration Space Administration AIRS Forecast Improvement AIRS Forecast Improvement Jet Propulsion Laboratory Jet Propulsion Laboratory California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California John LeMarshall (JCSDA) Additional Improvement Using Improved Forecast Prediction All 18 AIRS FOV ’ s 1 in 18 AIRS FOV’s (11 hours total in 6 Days) (6 hours in 6 Days) Northern Hemisphere Northern Hemisphere Preliminary October 2004 * *“This AIRS instrument has provided the most significant increase in forecast improvement in this time range of any other single instrument,” R etired Navy Vice Admiral Conrad C. Lautenbacher, Jr., Ph.D., under secretary of commerce for oceans and atmosphere and NOAA administrator. J. LeMarshall LeMarshall, J. Jung, J. , J. Jung, J. Derber Derber, R. , R. Treadon Treadon, S. Lord, M. Goldberg, W. Wolf, H. , S. Lord, M. Goldberg, W. Wolf, H. J. Liu, J. Joiner, J. Woollen Liu, J. Joiner, J. Woollen, R. , R. Todling Todling, R. , R. Gelaro Gelaro “ “Impact of Atmospheric Infrared Impact of Atmospheric Infrared Sounder Observations on Weather Forecasts” ”, EOS, Transactions, American , EOS, Transactions, American Sounder Observations on Weather Forecasts 6 6 Geophysical Union, Vol. 86 No. 11, March 15, 2005 Geophysical Union, Vol. 86 No. 11, March 15, 2005

  7. National Aeronautics and Good Forecast Impact with L2 using AIRS National Aeronautics and Good Forecast Impact with L2 using AIRS Space Administration Space Administration Jet Propulsion Laboratory Jet Propulsion Laboratory T(p), ), q(p q(p) ) T(p California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California 6 hrs on 4 Day Forecast Oreste Reale: Goddard Laboratory for Atmospheres GEOS-5 by GMAO 7 7

  8. National Aeronautics and AIRS Temperature and Water Vapor Used to National Aeronautics and AIRS Temperature and Water Vapor Used to Space Administration Space Administration Jet Propulsion Laboratory Jet Propulsion Laboratory Study Global Weather Patterns Study Global Weather Patterns California Institute of Technology California Institute of Technology Pasadena, California Pasadena, California Madden Julian Oscillation (MJO) Madden Julian Oscillation (MJO)   NCEP AIRS • • Major Differences in T and Q in lower Major Differences in T and Q in lower troposphere between AIRS and NCEP troposphere between AIRS and NCEP • • Convection preceded by warm and moist Convection preceded by warm and moist anomaly anomaly • • Tian, B., D. E. Waliser, E. Fetzer, B. Tian , B., D. E. Waliser, E. Fetzer, B. Lambrigtsen, Y. Yung, and B. Wang Lambrigtsen, Y. Yung, and B. Wang 2005: Vertical Moist Thermodynamic 2005: Vertical Moist Thermodynamic Structure and Spatial-temporal Evolution Structure and Spatial-temporal Evolution of the Madden-Julian Oscillation in of the Madden-Julian Oscillation in Atmospheric Infrared Sounder Atmospheric Infrared Sounder Observations. J. Atmos Atmos. . Sci Sci Observations. J. Monsoon Interseasonal Interseasonal Waves Waves Monsoon   (MISO) (MISO) • • Larger moisture perturbations compared Larger moisture perturbations compared to ECMWF & NCEP reanalysis. to ECMWF & NCEP reanalysis. • • Boundary-layer moistening ahead of the Boundary-layer moistening ahead of the convection preconditions the northward convection preconditions the northward movement of MISO. movement of MISO. • Positive SST anomaly is the major factor • Positive SST anomaly is the major factor for the BL moistening in this period. for the BL moistening in this period. • Xiouhua Fu, Bin Wang, Li Tao, Satellite • Xiouhua Fu, Bin Wang, Li Tao, Satellite data reveal the 3-D moisture structure of data reveal the 3-D moisture structure of Tropical Intraseasonal Tropical Intraseasonal Oscillation and its Oscillation and its coupling with underlying ocean, Geophys Geophys coupling with underlying ocean, Res. Lett Res. Lett. VOL. 33, L03705, . VOL. 33, L03705, H 2 O Surface Dry Zone doi:10.1029/2005GL025074, 2006 doi:10.1029/2005GL025074, 2006 8 8

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