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GOES-R 9.6 um (Channel 12)

GOES-R ABI Fact Sheet Band 12 (“Ozone” Infrared Band)

The “need to know” Advanced Baseline Imager reference guide for the NWS forecaster

By: The Cooperative Institute for Meteorological Satellite Studies (CIMSS)

 

The “ozone” band at 9.6 μm will provide information both day and night about the dynamics of the atmosphere near the tropopause with high spatial and temporal resolutions. For clear (cloud-free) scenes of view, this band is cooler than the IR window bands because of absorption due to ozone. In general, larger amounts of ozone cause more cooling relative to the the nominal surface emission. A high temporal and spatial ozone product derived from the 9.6 μm band may give some indications to clear-air turbulence in certain situations associated with tropopause folding. A similar band is available on today’s geostationary sounders. In fact, similar ozone-sensitive bands are on many geostationary imagers around the globe. Product generation will be key for estimating the ozone signature; stated another way, this band alone does not provide total column ozone, but must be computed using other spectral bands. More information can be found in the AWG ATBD on Total Ozone. This band/product can also be compared to upper-level potential vorticity. Band 12 is part of the “air mass” red-green-blue (RGB) composite and the non-baseline total column ozone product.
Source: Schmit et al., 2005 in BAMS, and the ABI Weather Event Simulator (WES) Guide by CIMSS.

 

Figure 1: The Advanced Himawari Imager (AHI) 9.6 μm ozone band image for Typhoon Maysak from March 31, 2015, at 06 UTC. Credit: CIMSS and JMA

 

In a Nutshell:
GOES-R ABI Band 12 (approximately 9.6 μm central, 9.4 μm to 9.8 μm)
Similar to MODIS Band 30, SEVIRI Band 8, AHI Band 12
Available on current GOES sounder
Nickname:
"Ozone" infrared band
Availability:
Both day and night
Primary Purpose:
Total column ozone
Uses Similar to:
None

Table 1: Overview of the 9.6 μm channel

 

Figure 2: The GOES sounder Total Column Ozone product depicted mesoscale ozone features on February 25, 2001. Small changes in ozone gradient (from yellow to green) were visible on the western edge of a developing cyclone, which propagated eastward with the cyclone. A Pacific Landfalling Jets Experiment flight encountered severe turbulence while passing though the fine features highlighted in the ozone images. These gradients are not visible in Band 12 images. Credit: CIMSS.

 

Did You Know?: While the future capability product is called total column ozone, there is very limited sensitivity to surface levels of ozone, especially when using a spectrally broad band. When the ABI was first designed, there was a high-spectral resolution infrared sensor (the ABS: Advanced Baseline Sounder) on the GOES-R series. The advanced geostationary sounder, later called the Hyperspectral Environmental Suite (HES) was removed in 2006, predominately because of budgetary issues. High spectral resolution infrared observations allow for improved vertical resolution of retrieved quantities such as temperature and moisture profiles. In addition, these IR observations allow for estimating other traces gases, such as SO2 from volcanoes.

 

GOES-R Baseline Product Used?
Aerosol Detection  
Aerosol Optical Depth  
Clear Sky Mask  
Cloud & Moisture Imagery x
Cloud Optical Depth  
Cloud Particle Size Distribution  
Cloud Top Phase  
Cloud Top Height  
Cloud Top Pressure  
Cloud Top Temperature  
Hurricane Intensity  
Rainfall Rate / QPE  
Legacy Vertical Moisture Profile x
Legacy Vertical Temperature Profile x
Derived Stability Indices x
Total Precipitable Water x
Downward Shortwave Radition: Surface  
Reflected Shortwave Radiation: TOA  
Derived Motion Winds  
Fire / Hot Spot Characterization  
Land Surface Temperature  
Snow Cover  
Sea Surface Temperature  
Volcanic Ash: Detection & Height  
Radiances x

Table 2: List of GOES-R baseline products that use the 9.6 μm channel

 

Carven's Corner: Beyond ozone, water vapor absorption also occurs in this band. This makes Band 12 somewhat complicated to use, because the horizontal distribution of ozone and water vapor varies across the globe (there is an ozone hole in the southern hemisphere). The brightness temperature will generally increase with less water vapor, less ozone, or an increase in air temperature in the layer where water vapor or ozone resides.
Compared to other bands, Band 12 will show cloud top temperatures at the tropopause in tropical environments with temperatures somewhat higher than other bands. This is because temperatures increase with height in the stratosphere, where the majority of ozone resides. This ozone partially obscures the cloud (and entire troposphere) in this spectral range.In lieu of Band 12, a difference between two water vapor channels, Band 8 and Band 10, is effective at locating stratospheric intrusions that may better depict the evolution of extratropical cyclones.
Carven Scott is the ESSD Chief in NWS Alaska Region and a former SOO

 

Figure 3: The weighting function (or contribution function) represents the layer(s) of the atmosphere where the radiation sensed by the instrument originated. The plot above shows the weighting function of the ozone band on the ABI. The clear-sky calculated brightness temperature does not include the presence of clouds. The weighting function peaks both in the stratosphere and near the surface. Credit: CIMSS

 

Tim's Topics: The ozone band on the ABI was added in the early formulation stages, suggested by those in both NOAA and NASA. The thermal infrared ozone channel on ABI can provide information about turbulence and wind shear near the tropopause which is important to aviation. In 2003, Art Neuendorffer, then of NOAA NESDIS, noted the “channel [spectral width] allows for a strong quasi-linear signal over a broad range of ozone values (and secant angles) while being relatively insensitive to variations in filter function.” This band was based on Europe’s Meteosat Second Generation (MSG) SEVIRI and the current GOES sounders, first launched in 2002 and 1994, respectively.
Tim Schmit is a research meteorologist with NOAA NESDIS in Madison, Wisconsin.

 

ABI Band Approximate Central Wavelength (µm) Band Nickname Type Nominal Sub Satellite Pixel Spacing (km)
11 8.4 "Cloud-top phase" band IR 2.0
12 9.6 "Ozone" Window IR 2.0

Table 3: Comparison of GOES-R channels

 

Further reading
ABI Bands Quick Information Guides: http://www.goes-r.gov/education/ABI-bands-quick-info.html
GOES Sounder Total Column Ozone: http://cimss.ssec.wisc.edu/goes/rt/viewdata.php?product=o3_us
CIMSS Satellite Blog post: http://cimss.ssec.wisc.edu/goes/blog/archives/16395
CIMSS Satellite Blog post: http://cimss.ssec.wisc.edu/goes/blog/archives/15047
Total Ozone ATBD: http://www.goes-r.gov/products/ATBDs/option2/AAA_Ozone_V2.0_no_color.pdf
EUMETSAT: http://oiswww.eumetsat.org/IPPS/html/MSG/RGB/AIRMASS/
GOES-R COMET training: http://www.goes-r.gov/users/training/comet.html  
AHI Weighting Functions: http://cimss.ssec.wisc.edu/goes/wf/AHI/
GOES-R acronyms: http://www.goes-r.gov/resources/acronyms.htm

 

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