Loop Heat Pipe Anomaly Impacts on GOES-17 ABI Bands 13 & 14

August 26, 2020

2 minute read

What is happening to ABI Band 13?

Users of GOES-17 imagery from ABI Band 13 (Clean Longwave Window IR) should notice the degradation of the imagery as a result of the seasonal loop heat pipe anomaly. A visual representation of the anticipated daily impacts for Band 13 can be found here and in Figure 1, below. A "1" in a cell indicates some degree of degradation in the imagery for a given hour on a given day. The hour of day is at the top along the horizontal axis in UTC. The date is to the left along the vertical axis in ascending order.

Figure 1:  Anticipated impacts for Band 13 from July 24 - September 7

In Figure 1, above, the horizontal axis ranging from 0 to 23 (top) is the hour of the day in UTC
and the vertical axis is the calendar date from July 24 to September 7, 2020 in ascending order.​

 

Operational Impacts from Band 13 Degradation

Band 13 (10.3 µm) is the "Clean Longwave Window IR" band on the ABI. This band is the least sensitive to water vapor absorption compared to the other IR window bands. This results in improved atmospheric moisture corrections, identification and classification of clouds and other features, and cloud top temperature and cloud particle size estimates. Band 13 supports many baseline GOES products, such as Derived Stability Indices and Total Precipitable Water, and RGBs including Day Cloud Phase Distinction, Day Convection, and Simple Water Vapor. One impact of the loop heat pipe anomaly degradation when using Band 13 includes a decreased ability to track convective features during the day/night transition. More information on Band 13 can be found in this quick guide from CIMSS and this article published in the Journal of Operational Meteorology.

 

Impacted Data Products

The table below includes the GOES-17 data products that will be impacted by the degradation of Band 13. A quick guide for each data product is linked in the right column.

Data Product Link to Quick Guide
Derived Stability Indices CIMSS Quick Guide for Derived Stability Indices
Legacy Vertical Moisture and Temperature Profiles CIRA Quick Guide for Legacy Vertical Profiles
Sea Surface Temperature CIRA Quick Guide for Sea Surface Temperature
Total Precipitable Water CIRA Quick Guide for Total Precipitable Water
Air Mass RGB CIRA Quick Guide for Air Mass RGB
Ash RGB CIRA Quick Guide for Ash RGB
Day Cloud Phase Distinction RGB CIRA Quick Guide for Day Cloud Phase Distinction RGB
Day Cloud Convection RGB

CIRA Quick Guide for Day Cloud Convection RGB

Day Convection RGB CIRA Quick Guide for Day Convection RGB
Day Ocean Cloud Convection RGB No Quick Guide Available
Day Snow-Fog RGB CIRA Quick Guide for Day Snow-Fog RGB
Dust RGB CIRA Quick Guide for Dust RGB
Nighttime Microphysics RGB CIRA Quick Guide for Nighttime Microphysics RGB
Simple Water Vapor RGB CIRA Quick Guide for Simple Water Vapor RGB
Sulfur Dioxide (SO2) RGB CIRA Quick Guide for SO2 RGB
Night Fog Difference CIMSS Quick Guide for Night Fog Difference
Split Ozone Brightness Temperature Difference CIMSS Quick Guide for Split Ozone Difference
Split Window Difference CIMSS Quick Guide for Split Window Difference

 

What is happening to ABI Band 14?

Users of GOES-17 imagery from ABI Band 14 (Longwave Window IR) should notice the degradation of the imagery as a result of the seasonal loop heat pipe anomaly. A visual representation of the anticipated daily impacts for Band 14 can be found here and in Figure 2, below. A "1" in a cell indicates some degree of degradation in the imagery for a given hour on a given day. The hour of day is at the top along the horizontal axis in UTC. The date is to the left along the vertical axis in ascending order.

Figure 2:  Anticipated impacts for Band 14 from July 24 - September 7

In Figure 2, above, the horizontal axis ranging from 0 to 23 (top) is the hour of the day in UTC
and the vertical axis is the calendar date from July 24 to September 7, 2020 in ascending order.​

 

Operational Impacts from Band 14 Degradation

Band 14 (11.2 µm) is the traditional "Longwave Window IR" band on the ABI. There is more absorption of energy by water vapor at this wavelength versus Band 13. Brightness temperatures in Band 14 will therefore be cooler than those in Band 13 by an amount that is a function of the amount of moisture in the atmosphere. Band 14 plays a prominent role in many baseline GOES products, such as Fire Detection and Derived Motion Winds, as well as an ingredient to the Ash and Dust RGBs. One impact of the loop heat pipe anomaly degradation when using Band 14 includes a decreased ability to delineate storm-top signatures such as overshooting tops. More information on Band 14 can be found in this quick guide from CIMSS and this article published in the Journal of Operational Meteorology.

 

Impacted Data Products

The table below includes the GOES-17 data products that will be impacted by the degradation of Band 14. A quick guide for each data product is linked in the right column.

Data Product Link to Quick Guide
Aerosol Detection CIMSS Quick Guide for Aerosol Detection
Aerosol Optical Depth CIMSS Quick Guide for Aerosol Optical Depth
Clear Sky Mask CIMSS Quick Guide for Clear Sky Mask
Cloud Optical Depth CIMSS Quick Guide for Cloud Optical Depth
Cloud Particle Size Distribution CIMSS Quick Guide for Cloud Particle Size Distribution
Cloud Top Height CIMSS Quick Guide for Cloud Top Height
Cloud Top Phase CIMSS Quick Guide for Cloud Top Phase
Cloud Top Pressure CIMSS Quick Guide for Cloud Top Pressure
Cloud Top Temperature CIMSS Quick Guide for Cloud Top Temperature
Derived Motion Winds

CIMSS Quick Guide for Derived Motion Winds

Derived Stability Indices CIMSS Quick Guide for Derived Stability Indices
Fire/Hot Spot Characterization CIRA Quick Guide for Fire/Hot Spot Characterization
Land Surface Temperature TOWR-S Quick Guide for Land Surface Temperature
Legacy Vertical Moisture and Temperature Profiles CIRA Quick Guide for Legacy Vertical Profiles
Rainfall Rate/QPE TOWR-S Quick Guide for Rainfall Rate/QPE
Sea Surface Temperature CIRA Quick Guide for Sea Surface Temperature
Total Precipitable Water CIRA Quick Guide for Total Precipitable Water
Ash RGB CIRA Quick Guide for Ash RGB
Dust RGB CIRA Quick Guide for Dust RGB
Split Cloud Phase Brightness Temperature Difference CIMSS Quick Guide for Split Cloud Phase Difference