Drawing lessons - illustrated lesson notes for teachers and students

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The Oil Painter's Bible - chapter 5


As objects recede in space they not only appear to shrink in size, but tend to lose detail, contrast of

values, intensity of color, and their edges appear less distinct the greater the distance from the viewer's

eyes. This is the principle of Atmospheric Perspective. Some writers call it "aerial perspective," but this is

misleading, as the term, "aerial" usually pertains to flying.

The visual alteration of images over

distance is the direct result of "X"

amount of atmosphere between the

eye and the object or plane in view.

The atmosphere contains water vapor

and its own density, which renders it

somewhat less than totally

transparent, adding a certain degree

of whiteness to the air. Light renders

the atmosphere white. The more air

we must look through to view

something, the more atmosphere we

see between it and our eyes, and the

more the image is altered by it.

An optical illusion is created by the

presence of a semitransparent white

between the eye and any color darker

than white, which alters the color in

question in the direction of blue, as

well as lightening the value. This is

precisely why the sky appears to be

blue. The sky's blue is created by the

blackness of space being viewed

through a layer of semitransparent

white atmosphere. The white is the

atmosphere illuminated by the sun.

At night, without the sun's light, the atmosphere is no longer white, and the blackness of space becomes

visible. Note that the sky is always lightest just above the horizon. This is the greatest distance we can see

at ground level, which is where the atmosphere contains the most (white) water vapor and the greatest

density. At the horizon, the density of the atmosphere renders it more opaque, and thus, whiter. As we

look up, we look through thinner air, which is less opaque, and the sky is bluer and darker. This is why

distant objects and planes appear lighter, bluer, and less distinct. The same phenomenon can be produced

with paint. The process is called scumbling and is accomplished by applying a thin veil of white paint

semitransparently over a layer of (dry) darker paint. The optical result in paint is the same as in the air.

Translucent white over black reads bluish, just as light grey smoke against dark trees reads blue. Note that

the same smoke may appear to be brown when a white cloud is behind it, a reverse of the scumble

phenomenon. Dark over light increases apparent warmth. This is the principle at work in glazing, that is,

the application of darker transparent paint over a lighter passage. Glazing and scumbling are discussed at

length in Chapter Six and Chapter Ten.

In painting, atmospheric perspective can be rendered directly, in one step, using opaque paint

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