To enlarge, pause animation & click the image. Hover over popups to zoom. Use slider to navigate. Apparent 'jumps' in the animation occur due to adjustments to reflect storm movement.
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Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1420 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1430 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1440 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1520 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1530 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1600 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1630 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1640 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1700 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1720 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1730 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1740 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1750 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1800 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1810 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1850 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1900 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1930 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 1950 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 2000 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 2100 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 2130 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 2150 UTC
Band 15 - 12.3 µm - Dirty Longwave Window - IR - 29 Jun 2019 - 2200 UTC
12.3 µm - "Dirty" Longwave IR Window Band - 2 km resolution - Band 15 at 12.3 µm offers nearly continuous monitoring for numerous applications, though usually through a split window difference with a cleaner window channel. These differences can better estimate low-level moisture, volcanic ash, airborne dust/sand, sea surface temperature, and cloud particle size.