Notice:
Starting December 3, 2024, visitors to GOES.NOAA.GOV will be redirected
to the STAR
GOES Imagery site. If you have any questions about this change
or need assistance, please contact OSPO
User Services.
7 Dec 2024 - 08:51 EST
7 Dec 2024 - 13:51 UTC
GOES-East CONUS - Derived Motion Winds
1 hour loop - 12 images - 5 minute update
To enlarge, pause animation & click the image. Hover over popups to zoom. Use slider to navigate.
While GOES animation code will not run on older Internet Explorer browsers,
they work in the newest versions of Microsoft Edge. If you are using
Internet Explorer, please try a different browser: Chrome, Firefox, Safari, or
MS Edge are all supported.
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1031 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1046 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1101 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1116 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1131 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1146 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1201 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1216 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1231 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1246 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1301 UTC
Derived Motion Winds - Derived Motion Winds - 07 Dec 2024 - 1316 UTC
Derived Motion Winds key:
Red barbs: High level winds: 100 - 400mb, altitude approximately 23,000 - 46,000 ft. (7-14 km)
Cyan barbs: Mid-level winds: 400 - 700mb, altitude: approximately 10,000 - 23,000 ft. (3 - 7 km)
Yellow barbs: Low-level winds: > 700mb, altitude: approximately < 10,000 ft. (< 3 km)
Derived Motion Wind Vectors (DMW) are produced using sequential ABI images and as such they can provide important information about winds at different levels during asynoptic times. Areas of wind shear or jet maxima can be identified. Wind Vectors are computed using both visible and infrared (including water vapor) imagery. DMWs are used to identify regions of strong winds or wind shear to confirm model forecasts and/or to anticipate the result of strong winds or shear.