Simultaneously, thin high clouds above the snow-covered mountains are easily visible in red and yellow tones. (2/2)

Over such areas, due to a higher contrast between the dust and the sea surface, a dust event that might appear less pronounced in the Dust RGB, becomes more apparent in the True Color RGB, which is also aided by higher spatial resolution. (3/3)

With the Sun low in the east, picking up dust signal in visible channels is enhanced by the forward scattering from dust particles. In the True Color RGB, dust can be easily spotted, especially over areas such as sea surface, that is absorbing more in the visible spectrum (2/3)