1. Review of Remote Sensing Fundaments IV Infrared at High Spectral Resolution – Basic Principal & Limitations Allen Huang Cooperative Institute for Meteorological Satellite Studies Space Science & Engineering Center University of Wisconsin-Madison, USA GEOSS Americas/Caribbean Remote Sensing Workshop – Transforming Data into Products 26-30 November 2007 CPTEC/INPE Cachoeira Paulista - São Paulo Materials provided by Elisabeth Weisz, Paul Menzel, Paolo Antonalli, Jun Li, Mat Gunshor and Tim Schmit

2. The road to improved IR sounding using hyperspectral measurements VAS (geo experimental) GOES Sounder (geo operational) GIFTS (geo experimental) (12) (18) (~1600) ??? (geo operational) time (# of spectral bands) VTPR, HIRS (leo operational) CrIS (leo operational) IASI (leo operational) AIRS (leo pseudo-operational) HIS (airborne experimental) IRIS (leo experimental) (~2400) (~8600) IMG (leo experimental) NAST-I (airborne experimental) (~8000) (~6000) (~4000)

3. AIRS 2378 IASI 8461 CrIS 1400 HIRS 19

4. AIRS IR Specification Infrared Spectral Coverage: 3.74  m - 4.61  m[2674 – 2170 cm -1 ] 6.20  m – 8.22  m[1613 – 1217 cm -1 ] 8.80  m – 15.4  m[1136 – 649 cm -1 ] Spectral Resolution: /  =1200 Spatial Coverage:  49.5  around nadir 1.1  (~13.5 km dia) IFOV (Instantaneous Field of View) Sensitivity (NEDT): 0.14 K at 4.2  m 0.20 K from 3.7 to 13.6  m 0.35 K from 13.6 to 15.4  m Power / Mass: 256 W / 166 kg Lifetime: 5 years

5. AIRS Spatial Coverage (1) Swath: 1650 km IFOV: 1.1°  13.5 km http://www-airs.jpl.nasa.gov/

6. AIRS Spatial Coverage (3)

7. AIRS Spectral Coverage IR sounder: 2378 channels spectral ranges: 3.7 - 4.61  m, 6.2 - 8.22  m, 8.8 - 15.4  m;

8. AIRS (Atmospheric Infrared Sounder) & MODIS

9. IASI Scan Characteristics EVOF consists of 2x2 matrix of IFOV 30 EFOV per scan line IFOV size at nadir: 12 km IFOV at edge across/along track: 39/20 km Swath:  48.333 deg Swath width:  1100 km Mean Altitude approx 817 km

10. IASI Spectral Characteristics BandWavenumbers cm -1 Wavelength (  m) 1645.0 - 1210.08.26 - 15.5 21210.0 - 2000.05.0 - 8.26 32000.0 - 2760.03.62 - 5.0 Band 1Band 2Band 3

11. Various Infrared spectral resolutions Standard Atmosphere: 0.2 cm -1 (IASI & NAST-I-like) 0.6 cm -1 (AIRS & CrIS-like) 1.2 cm -1 (CrIS-like) 4.8 cm -1 19.2 cm -1 (current sounder-like) 38.4 cm -1 (imager-like) Jun Li, Mat Gunshor and Tim Schmit

19. Longwave window region

26. Water vapor region

33. Moisture Weighting Functions Pressure (hPa) Advanced Sounder (3074) GOES (18) 1000 100 UW/CIMSS High spectral resolution advanced sounder will have more and sharper weighting functions compared to current GOES sounder. Retrievals will have better vertical resolution.

34. Ultraspectral Infrared Measurement Characteristics - continue Much Enhanced Measurement Information Contents Current - GOESGIFTS ~3 Pieces 10-12 Pieces GOES Vert-Res.: 3-5 Km GIFTS Vert-Res.: 1-2 Km Temperature Sounding

35. Much Enhanced Measurement Information Contents Current - GOES ~2 Pieces8-9 Pieces AIRS/IASI/GIFTS GOES Vert-Res.: 6-8 Km GIFTS Vert-Res.: 2-4 Km Water Vapor Sounding Hyperspectral Infrared Measurement Characteristics

36. Water Vapor Sounding Measurement Vertical Resolution Information Content Hyperspectral Infrared Measurement Characteristics Hyperspectral Filter Radiometer Radiosonde

37. Various Infrared Spectral Absorption Features

68. Infrared Spectral Sounding Profile Sensitivities

77. HeIghtHeIght AbsorptionAbsorption Wavenumber Energy Contribution Weighting Functions

78. Broad Band window CO 2 O3O3 H2OH2O window Samplig of vibrational bands Integration over rotational bands

79. … in Brightness Temperature

80. High Spectral Resolution Samplig over rotational bands

81. Broad Band vs High Spectral

82. Temperature Inversions AIRS (20 July 2002) calculation Sub-Arctic Winter May 2001 S. Pole radiosonde profile used in calculation (0.365 mm H 2 O)

83. Summary (1/2)  Hyperspectral Sounder provides much improved atmospheric information content: Water Vapor (Temp.)

84. Summary (2/2)  Hyperspectral Sounder provides information to detect:  Trace Gases (i.e. O 3 ; CO; CH 4 ; SO 2 ; N 2 O…)  Cloud property (phase, size, optical thickness, concentration ……)  Surface Property/type  Highly accurate radiances for climate study  Validate IR broad band satellite measurments