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Studies of Advanced Baseline Sounder (ABS) for Future GOES Jun Li + Timothy J. Allen Huang+ W. +CIMSS, UW-Madison.

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Presentation on theme: "Studies of Advanced Baseline Sounder (ABS) for Future GOES Jun Li + Timothy J. Allen Huang+ W. +CIMSS, UW-Madison."— Presentation transcript:

1 Studies of Advanced Baseline Sounder (ABS) for Future GOES Jun Li + Timothy J. Schmit @ Allen Huang+ W. Paul Menzel @ @NOAA/NESDIS/ORA +CIMSS, UW-Madison ITSC-XII, Feb.27 - Mar.05, 2002, Lorne, Victoria, Australia UW-Madison

2 More than 5 years of high spectral measurements from polar orbits: - AIRS (Atmospheric InfraRed Sounder) - IASI (Infrared Atmospheric Sounding Interferometer) - CrIS (Crosstrack Infrared Sounder) Approximately 5 years of high spectral, spatial and temporal measurements from geostationary orbit: - GIFTS (Geostationary Imaging Fourier Transform Spectrometer) 30 years of filter wheel technology in geostationary orbit: - VAS and GOES Sounder 40 years since the first interferometer flown in space to study the weather: IRIS (Infrared Radiation Interferometer Spectrometer) ABS is scheduled to be on GOES-R in 2012 The time is right to update the GOES sounder! The technology is mature. The need is documented.

3 Limitations of Current GOES Sounders –scan conflicts between oceans vs CONUS (regional vs hemispheric) –low vertical resolution for moisture, temperature –eclipse and related outages

4 User Requirements Current (1999) NWS Thresholds Resolutions - Temporal: The ‘sounding disk’ in 1 hour - Spectral : from 3.7-15.4 µm at 0.6 to 2.5 cm -1 resolution (similar to spectral performance of polar interferometers - CrIS) - Spatial: 10 km horizontal resolution for independent observation Accuracies 1 degree K temperature; 10% relative humidity Applications - Nowcasting - Short-range weather forecasting - Longer-range numerical weather prediction

5 User Requirements

6 Sounder Comparison Coverage RateCONUS/hrSounding Disk/hr Horizontal Resolution - Sampling Distance10 km10 km Vertical resolution~3 km 1 km Accuracy Temperature2 deg. K 1 deg. K Humidity20%10% CurrentRequirement

7 Areas within 62 degrees local zenith angle from GOES-East and GOES-West sub- satellite points are indicated. Threshold coverage rate calls for the 62 arc region, excluding half of over-lap, to be scanned each hour. Current GOES -E and -W sounder hourly coverage is also shown. Spatial Coverage

8 GOES-12 Sounder -- Cloud Top Pressure

9 GOES-12 Imager -- Cloud Top Pressure

10 Geostationary Sounders (# of channels) VAS (experimental) GOES Sounder (operational) GIFTS (experimental) (12) (18) (~1600) Advanced Baseline Sounder (operational) time

11 Spectral coverage of the proposed ABS’, ABS, GIFTS and the current GOES radiometer sounder ABS:

12 Spectral widthsSpectral resolutions ABS 3-band: 650 -1200 cm -1 0.625 1210-1740 cm -1 1.25 2150-2720 cm -1 2.5 ABS’ 2-band: 650 -1200 cm -1 0.625 1650-2250 cm -1 0.625

13 Noise vectors used for the ABS simulations ABS’

14 Is a new 2-band ABS’ comparable to a traditional 3- band ABS for Temperature? UW/CIMSS

15 Is a new 2-band ABS’ comparable to a traditional 3- band ABS for Moisture? UW/CIMSS

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17 ABS’ LW 650 - 1200 cm**-1

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20 00 and 12 UTC only. Land-based CONUS locations.

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23 12 UTC. Land-based CONUS location. 12 UTC Land-based CONUS location

24 Detection of Temperature Inversions Possible with Interferometer The detection of inversions is critical for severe weather forecasting. Combined with improved low-level moisture depiction, critical ingredients for night-time severe storm development over the Plains can be monitored. Knowing if there is an inversion can also help improve the profiles estimates. Spikes down - Cooling with height Spikes up - Heating with height Texas Ontario Brightness Temperature (K) (low-level inversion) (No inversion) GOES Wavenumber (cm -1 )

25 Cloud-Top Information Future GOES -- simulating the Advanced Baseline Sounder (ABS) performance

26 Summary The information from CrIS-like three spectral bands is close to that from GIFTS- like two spectral bands. The Advanced Baseline Sounder overcomes existing instrument limitations. Geostationary interferometer will resolve high temporal and vertical fluctuations of moisture that are not resolved by current in-situ or satellite measurements. Only geostationary interferometer observes critical meteorological parameters (temperature, moisture, clouds, winds) with necessary temporal, spatial and vertical resolutions to support future Nowcasting, Short-range weather forecasting, and Longer-range numerical weather prediction. Technology is mature and meteorological need is documented. Time is right to update geostationary sounding instruments. Advanced Sounder will provide required high spectral resolution measurements.


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