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GOES-R ABI and Himawari-8 AHI Training using SIFT

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Presentation on theme: "GOES-R ABI and Himawari-8 AHI Training using SIFT"— Presentation transcript:

1 GOES-R ABI and Himawari-8 AHI Training using SIFT
Raymond K. Garcia, David Hoese, Jordan J. Gerth, Scott S. Lindstrom, Kathleen I. Strabala UW-Madison Cooperative Institute for Meteorological Satellite Studies Timothy J. Schmit NOAA/NESDIS/ASPB Bill Ward NOAA/National Weather Service

2 Satellite Meteorology Madison Wisconsin 2016
SIFT Satellite Information and Familiarization Tool Created to facilitate training of Himawari-8 data in the Pacific Region of the NWS Satellite Meteorology Madison Wisconsin 2016

3 Where has SIFT been used?
NWS Day-1 Ready Training for Guam WFO (Himawari) NWS Training at Honolulu WFO Satellite Liaison Training in Kansas City Graduate Student Training in Madison Satellite Meteorology Madison Wisconsin 2016

4 Satellite Meteorology Madison Wisconsin 2016
System Requirements Compatible with Windows/Linux/Mac Faster I/O the better Does a lot on the Graphics Card 500 Mb (8.5 Gb) workspace needed for 2 km (0.5 km) imagery Sample datasets (pre-projected mercator GeoTIFF files) require up to 1TB of storage. Coming soon: Data in Native Formats! Satellite Meteorology Madison Wisconsin 2016

5 Why is SIFT good for training?
Quick access to multiple bands for visual inspection/comparison Density Diagrams/Scatterplots to compare two channels Easy and seamless zoom and roam capabilities Datasets are pre-selected and loaded Satellite Meteorology Madison Wisconsin 2016

6 AMS Satellite Meteorology Madison Wisconsin 2016
The SIFT Display Area Probe Graphs (Density Diagrams, Bar Graphs) Layers – List of data that are loaded Layer Details AMS Satellite Meteorology Madison Wisconsin 2016

7 Satellite Meteorology Madison Wisconsin 2016
SIFT Example 1 #1 #2 First, just load up one image, then load up all bands for a different time Ask a simple question: Why is Image #2 brighter? Satellite Meteorology Madison Wisconsin 2016

8 SIFT Example 1 Discuss Probe Features of SIFT Tool
0.47 mm, “blue” 0.51 mm, “green” 0.64 mm “red” 0.86 mm, “veggie” 1.6 mm, “cirrus” 2.2 mm, “phase” 3.9 mm, “shortwave IR” 6.2 mm, “high wv” 6.9 mm, “middle wv” 7.3 mm, “low wv” 8.6 mm, “SO2 window” 9.6 mm, “ozone” 10.4 mm, “clean window” 11.2 mm, “window” 12.1 mm, “dirty window” 13.2 mm, “CO2” Visible and near-IR: Reflectance values shown and they increase to the right Discuss Probe Features of SIFT Tool What does this tell you about your scene? Why is Band 5 reflectance small? Why is Band 7 so much warmer? Why is band 13 warmer than band 14? Why is Band 12 Warmer than most other IR bands? Day or Night? Infrared: Brightness temperature shown and they increase to the right

9 SIFT Example 2 Load up all Bands, and create a histogram & density diagram of a region – those are shown below. Explain what you see! Why is there a region of relatively high Band 4 Reflectance? Band 3 Reflectance is mostly small, with a few higher values Conclusion: Mostly clear

10 SIFT Example 2: AHI Band 3 Versus Band 4
AHI Band 3 (0.64 μm) AHI Band 4 (0.86 μm) Easy to toggle between these two to really accentuate the differences Satellite Meteorology Madison Wisconsin 2016

11 Satellite Meteorology Madison Wisconsin 2016
SIFT Example 3 Describe what you see in this Density Diagram (Band 3 v. Band 14) This is an excellent way to make sure the students really do understand the capabilities of each individual band Note there are two distributions: Fairly Warm and Highly Reflective Colder with Increasing Reflectivity Satellite Meteorology Madison Wisconsin 2016

12 Satellite Meteorology Madison Wisconsin 2016
SIFT Example 4a What are the different bands telling you here? Is it day or night? Is it cloudy? Thick clouds? Thin clouds? What do the Water Vapor Bands Tells you? Which two (that’s a hint) bands are most important in describing what’s going on? Satellite Meteorology Madison Wisconsin 2016

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SIFT Example 4b Visible/Near IR Bands Infrared Bands Which Probe Matches Which Scene? Which Two Channels help most? Satellite Meteorology Madison Wisconsin 2016

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SIFT Example 4c Behold the Power of Band 4 in highlighting Land! Reflectivity is much greater Satellite Meteorology Madison Wisconsin 2016

15 At which two channels are you looking?
SIFT Example 5 Cirrus/Ice Band At which two channels are you looking? Visible or Infrared? Veggie Band

16 Satellite Meteorology Madison Wisconsin 2016
Sift Example 5 0.47 mm, “blue” 0.51 mm, “green” 0.64 mm “red” 0.86 mm, “veggie” 1.6 mm, “cirrus” 2.2 mm, “phase” 3.9 mm, “shortwave IR” 6.2 mm, “high wv” 6.9 mm, “middle wv” 7.3 mm, “low wv” 8.6 mm, “SO2 window” 9.6 mm, “ozone” 10.4 mm, “clean window” 11.2 mm, “window” 12.1 mm, “dirty window” 13.2 mm, “CO2” Which probe corresponds to the Ocean Location you just saw? Satellite Meteorology Madison Wisconsin 2016

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Sift Example 5 Of the remaining three probes, which corresponds to this point Satellite Meteorology Madison Wisconsin 2016

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Sift Example 5 Match the Probe on the left to the Scene. Which goes with the ‘x’? Satellite Meteorology Madison Wisconsin 2016

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Sift Example 5 Satellite Meteorology Madison Wisconsin 2016

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SIFT Example 6 15 14 13 Satellite Meteorology Madison Wisconsin 2016

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SIFT Example 6 Satellite Meteorology Madison Wisconsin 2016

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Questions asked in Lab What AHI visible reflectance band is best for detecting/identifying low clouds? What AHI visible reflectance band is best for detecting/identifying high clouds? What AHI thermal infrared band is best for detecting/identifying low clouds? What AHI thermal infrared band is best for detecting/identifying high clouds? What AHI visible reflectance band is best for detecting/identifying land surface features? What AHI thermal infrared band is best for detecting/identifying land surface features? What AHI band or bands are best for detecting/identifying mid atmosphere features? Satellite Meteorology Madison Wisconsin 2016

23 What does this scene represent?
Day or Night? Water or Land? Cloudy or Clear? If cloudy: Thick clouds or Thin? This forces the student to understand how each Band might be used. Visible/Near IR Bands Infrared Bands (This is thin cirrus over land) Satellite Meteorology Madison Wisconsin 2016

24 What’s the chief difference between these two probes?
Satellite Meteorology Madison Wisconsin 2016

25 SIFT Training always referred back to Spectral Response Functions
Why are the channels placed where they are? What can you expect the bands to view given the Spectral Response Functions? Handouts provided to facilitate learning Satellite Meteorology Madison Wisconsin 2016

26 Satellite Meteorology Madison Wisconsin 2016
Advanced Baseline Imager Spectral Bands AHI Band Approximate Central Wavelength (μm) ABI Type Nickname 1 0.47 Visible Blue 2 0.51 Green 3 0.64 Red 4 0.86 Near-Infrared Veggie 1.4 Cirrus 5 1.6 Snow/Ice 6 2.3 2.2 Cloud Particle Size 7 3.9 Infrared Shortwave Window 8 6.2 Upper-level Water Vapor 9 6.9 Mid-level Water Vapor 10 7.3 Lower-level Water Vapor 11 8.6 8.4 Cloud-Top Phase 12 9.6 Ozone 13 10.4 10.3 “Clean” Longwave Window 14 11.2 Longwave Window 15 12.4 12.3 “Dirty” Longwave Window 16 13.3 CO2 Longwave Handout Satellite Meteorology Madison Wisconsin 2016

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AHI Handout Satellite Meteorology Madison Wisconsin 2016

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ABI Handout Satellite Meteorology Madison Wisconsin 2016

29 US Standard Atmosphere (1976) Brightness Temperature Difference
as a result of water vapor (H2O) absorption Why isn’t the window channel here? Satellite Meteorology Madison Wisconsin 2016 Credit: Mat Gunshor, Cong Zhou, Tim Schmit, Allen Huang

30 US Standard Atmosphere (1976) Brightness Temperature Difference
as a result of ozone (O3) absorption Satellite Meteorology Madison Wisconsin 2016 Credit: Mat Gunshor, Cong Zhou, Tim Schmit, Allen Huang

31 Once more: What does this scene represent?
Day or Night? Water or Land? Cloudy or Clear? If cloudy: Thick clouds or Thin? This is a trick question Visible/Near IR Bands Infrared Bands Satellite Meteorology Madison Wisconsin 2016

32 Satellite Meteorology Madison Wisconsin 2016
Questions? Satellite Meteorology Madison Wisconsin 2016


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