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  1. GOES Image Viewer. Click on a region to view images and animations for that region. Coverage area depictions are approximate.

    • CONUS

      CONUS - GOES Imagery Viewer - NOAA / NESDIS / STAR

    • Full Disk

      Full Disk - GOES Imagery Viewer - NOAA / NESDIS / STAR

    • Caribbean

      Caribbean - GOES Imagery Viewer - NOAA / NESDIS / STAR

    • Pacific

      Pacific - GOES Imagery Viewer - NOAA / NESDIS / STAR

  2. 14 sty 2016 · Atlantic Tropical Water Vapor: GOES East. VIEW LOOP. Atlantic Tropical Channels: GOES East. More Tropical Atlantic Images & Loops. Note: Imagery and loops on this site are intended for informational purposes only, they are not considered "operational".

  3. Atlantic Tropical: Water Vapor Loop. Note: Imagery and loops on this site are intended for informational purposes only, they are not considered "operational". This web site should not be used to support operational observation, forecasting, emergency, or disaster mitigation operations, either public or private.

  4. 3 dni temu · The single water vapor band on GOES-13 contained a mixture of water vapor features over many levels of the troposphere, but GOES-16 enables us to focus on water vapor in the upper troposphere (band 8), the middle troposphere (band 9), or the lower troposphere (band 10).

  5. This page supplies satellite images and loops from GOES-16, GOES-18, and Himawari-9 geostationary satellites for the Atlantic, Pacific, and Indian oceans, including visible, infrared (IR) and water vapor (WV) bands. Floaters provide imagery centered on tropical cyclones and disturbances.

  6. Central Atlantic Water Vapor Loop: GOES East. Note: Imagery and loops on this site are intended for informational purposes only, they are not considered "operational". This web site should not be used to support operational observation, forecasting, emergency, or disaster mitigation operations, either public or private. ...

  7. www.nesdis.noaa.gov › imagery › interactive-mapsWater Vapor Imagery | NESDIS

    The 7.3 µm “Lower-level water vapor” band typically senses farthest down into the mid-troposphere in cloud-free regions. It is used to track lower tropospheric winds, identify jet streaks, monitor severe weather potential, estimate lower-level moisture, identify regions where the potential for turbulence exists, highlight volcanic plumes ...

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