Snow on the ground as well as ice over mountains, frozen lakes and sea ice appear cyan in the Natural Colour RGB images.
In the Natural Colour RGB, the cyan colour of snow and ice on the earth surface results from a strong reflection of short wave solar radiation (see the green arrows on the left hand image). The more homogenous the snow/ice cover is, the brighter the cyan colour will be. Snow and ice on mountains (see the image below) will therefore be depicted in a stronger cyan colour than snowy surfaces on ground which are often disrupted by vegetation.
The Natural Colour RGB from early May 2013 shows sea ice at the northernmost part of the Gulf of Bothnia as well as over the lake of Ladoga and Onega (red arrows). Depending on how much melted water is mixed to the ice sheet, the cyan colour range goes from bright (no water) to dark cyan when much of the ice sheets has melted or when the ice sheeld is broken by areas with open water.
Explanation of the colours of snow and ice over land and ice over seas in the Natural Colour RGB (see also the recipe on the left side):
• Radiation mesured by the SEVIRI instrument of MSG in channel 1 (0.6 micron) and channel 2 (0.8 micron) contributes much more to the Natural Colour RGB than radiation measured in channel 3 (1.6 micron). Solar radiation is strongly absorbed by snow and ice crystals at 1.6 micrometer while it is strongly reflected in both visible channels 0.6 and 0.8 micrometer. Cyan is resulting from a mixture of blue and green.