GOES-18 Interleave Testing - Has ended. GOES-West data now supplied from operational GOES-17 satellite.
GOES-18 expected to become operational GOES-West in January 2023. See GOES-18 Interleave Testing for more information.
30 Jan 2023 - 18:49 EST
30 Jan 2023 - 23:49 UTC
GOES-East Full Disk - Day Cloud Phase
2 hour loop - 12 images - 10 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.
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2140 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2150 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2200 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2210 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2220 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2230 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2240 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2250 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2300 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2310 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2320 UTC
Day Cloud Phase - Show phase of cooling cloud tops - 30 Jan 2023 - 2330 UTC
This RGB will be phased out around 1 Feb 2023 and will be replaced by the Day Night Cloud Micro Combo RGB.
This RGB is used to evaluate the phase of cooling cloud tops to monitor convective initiation, storm growth, and decay. It can also be used to identify snow on the ground. The Day Cloud Phase Distinction RGB takes advantage of cloud reflectance differences between the visible and near infrared channels and temperature variances between land and clouds in the infrared to provide increased contrast between background surfaces and phases of clouds (i.e., water vs. ice). Due to its reliance on visible bands 2 and 5, it is only usable during daylight hours. This RGB composite was developed by the Japan Meteorological Agency (JMA) for Himawari-8. Interpretation is still under investigation.