The GASP product is a retrieval of the Aerosol Optical Depth (AOD) made from the current GOES East visible imagery.

Conus Images

(4km resolution) See below for image descriptions. Left click on JPG's to view. Right click on GEOTIF's to download.

Time (UTC)	GOES AOD	GOES AOD	Time (UTC)	GOES AOD	GOES AOD
Latest	JPG	GEOTIF	12:45	JPG	GEOTIF
13:15	JPG	GEOTIF	13:45	JPG	GEOTIF
14:15	JPG	GEOTIF	14:45	JPG	GEOTIF
15:15	JPG	GEOTIF	15:45	JPG	GEOTIF
16:15	JPG	GEOTIF	16:45	JPG	GEOTIF
17:15	JPG	GEOTIF	17:45	JPG	GEOTIF
18:15	JPG	GEOTIF	18:45	JPG	GEOTIF
19:15	JPG	GEOTIF	19:45	JPG	GEOTIF
20:15	JPG	GEOTIF	20:45	JPG	GEOTIF
21:15	JPG	GEOTIF	21:45	JPG	GEOTIF
22:15	JPG	GEOTIF	22:45	JPG	GEOTIF
23:15	JPG	GEOTIF	23:45	JPG	GEOTIF
00:15	JPG	GEOTIF	00:45	JPG	GEOTIF
01:15	JPG	GEOTIF	01:45	JPG	GEOTIF
02:15	JPG	GEOTIF	02:45	JPG	GEOTIF
03:15	JPG	GEOTIF	03:45	JPG	GEOTIF

Animated Image Loop

 

The latest GASP product can also be viewed through the GASP Internet Map Server.

Imagery Description

• Time (UTC)
• EST = UTC -5, CST = UTC - 6, MST = UTC - 7, PST = UTC - 8
• Latest Image
• The latest GOES image available to the processing system.
• Aerosol Optical Depth (from latest image and most recent surface reflectance retrieval)
• Color scale represents the aerosol optical depth.
• The gray scale in the sunlit portion of the image represents the reflectance of either clouds, sun glint or regions where the retrieval is insensitive to aerosol (e.g., over bright surfaces)
• The thick black line is where the solar zenith angle is 80 degrees.
• The retrieval is not performed at solar zenith angles above 80, so the visible reflectance is provided between 80 and 89 degrees
• Beyond 89 degrees, the IR data (from channel 4) is shown to provide a continuous image.

Method Summary

• A clear sky composite reflectance (background) image is created by selecting the second darkest pixel from the previous 28 days for each observation time.
• The surface reflectance is obtained from the composite background image, using look-up tables calculated with the 6S Radiative Transfer model.
• The Aerosol Optical Depth is estimated using look-up tables from the 6S Radiative Transfer model and the calculated surface reflectance.
• Radiative Transfer calculations assume a continental aerosol model and Lambertian surface.
• Clouds are identified using spatial and spectral tests similar to those developed for CLAVR (Clouds from AVHRR). The AOD is shown only for cloud free pixels.

GASP Team:

Scientists: Shobha Kondragunta, NESDIS/STAR (Originally Ken Knapp)
Operations: George Stephens
Contact Address: SSDFireTeam@noaa.gov