Water rich in suspended matter or shallow with sediments on its bottom appears greenish or blueish cyan in the VIIRS True Colour RGB images. It may appear also brownish.
The image below shows an example. The water of the Adriatic Sea has a very different colour along the Italian coast. Here the water is shallow, the coast is mostly sandy and the rivers bring sediment into the sea.
The Hungarian Lake Balaton and the Lake Neusiedl on the Austrian Hungarian border are shallow and their bottom is sandy/silty. They appear greenish cyan in the following image.
The next image shows the shallow Sea of Azov and the much deeper Black Sea.
The next image shows the region of the Gironde estuary in France. The Garonne river transports sediment into the Atlantic Ocean
The next 2 images show sediment plumes around Mississippi river delta and in East China Sea.
Phytoplankton is a microscopic organisms that live in watery environments. When conditions are right, phytoplankton undergo explosive population growth, creating blooms visible in True Colour RGB images. The next image shows an algae bloom example in in Gulf of Mexico.
• The water reflectivity depends not only on the water characteristics but as well as on the solar and satellite viewing directions. Towards the edge of the swath the colour shades may be brighter, while along the sub-satellite track it might be slightly darker.
• Deep, clean water bodies appear dark blue, almost black in the True Colour RGB, see examples separately.
• If there is high concentration aerosol plume above the sea (such as lofted dust, smoke) the colour of the sea trough the aerosol layer modifies.
• Sea ice appears whitish.
Explanation of the colour of suspended matter rich water in the True Colour RGB (see also the recipe on the left hand side):
The reflectivity of deep, clean water is very low in all three visible channels, so the deep, clean water bodies appear dark blue, almost black
in the True Colour RGB.
In case of suspended matter, the reflectivity values increase. The resulting colour depends on the type and concentration of the sediments.