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Available Near Real-time Products |
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Description |
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Infrared 11.5 MVIRI spectral channel over black and white background The Thermal Infrared (IR) band is used for imaging by day and by night, and also for determining the temperature of cloud tops and of the ocean's surface. This band corresponds to peak re-emission of radiation from the Earth's surface and atmosphere, according to their temperature. As with the VIS band, the atmospheric gases are fairly transparent in this region. |
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Infrared 11.5 MVIRI spectral channel over color background |
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Visible 0.7 MVIRI spectral channel over black & white background The Visible (VIS) band (0.45 to 1.0 µm) is used for imaging during dayight. This band corresponds to peak solar irradiance; furthermore the atmospheric gases are fairly transparent to incoming and outgoing (reflected) solar radiation in this band. |
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Visible 0.7 MVIRI spectral channel over color background |
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Water Vapour 6.4 MVIRI spectral channel over black and white background The Water Vapour (WV) absorption band (5.7 to 7.1 µm) is used in determining the amount of water vapour in the upper troposphere. It takes advantage of the strong absorption of emitted terrestrial radiation by atmospheric water vapour. In this spectral region, the atmosphere is very opaque if water vapour is present, but transparent if the air is very dry. |
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