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Exploring the Unknown - NASA's History Office

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194<br />

OBSERVING THE EARTH FROM SPACE<br />

. . . gives <strong>the</strong> albedos for various ground covers. Applying <strong>the</strong>se values to Fig. 2, it can be<br />

seen that, except for <strong>the</strong> case of newly fallen snow combined with clouds thicker than<br />

600 meters and <strong>the</strong> case in which <strong>the</strong> background albedo approaches very close to cloud<br />

albedo, 500-ft resolutions are obtainable over a wide range of conditions.<br />

There is one o<strong>the</strong>r factor that might limit contrast and, <strong>the</strong>refore, resolution. This is<br />

aerial haze between <strong>the</strong> camera and <strong>the</strong> ground. As has recently been shown in several<br />

[11] [original placement of “Fig 2—Available contrast with varying cloud and background<br />

albedos”] V-2 photographs, this problem is almost completely solved by use of an infrared<br />

filter in <strong>the</strong> optical system.<br />

Fig. 2—Available contrast with varying cloud and background albedos<br />

From <strong>the</strong> foregoing section we may conclude that, from <strong>the</strong> standpoint of area coverage<br />

and resolution, wea<strong>the</strong>r observations from a satellite are a definite possibility.<br />

[12] Table 5*<br />

SURFACE ALBEDO AND SCENE CONTRAST OF CLOUDS<br />

AGAINST VARIOUS BACKGROUND SURFACES<br />

Ground Surface Albedo + References ±<br />

Fresh snow .80-.93 1, 3, 4<br />

Old snow, sea ice .40-.60 3, 4<br />

Brown soil .32 1<br />

Grass .10-.33 4<br />

Green leaves .25 1<br />

Sandy loam .24 2<br />

Sand .13-/18 3<br />

Asphalt paving .15 2<br />

Dry earth .14 4<br />

Rock .12-.15 4<br />

Moist earth .08-.09 2, 4<br />

Cultivated soil, vegetable .07-.09 3<br />

Smooth sea surface<br />

Solar elev 5 deg .40 3<br />

Solar elev 10 deg .25<br />

Solar elev 20 deg .12<br />

Solar elev 30 deg .06<br />

Solar elev 40 deg .04<br />

Solar elev 50-90 deg .03<br />

* This table was prepared by Dr. R. S. Wehner and is included in <strong>the</strong> RAND general<br />

report on <strong>the</strong> satellite (see footnote 1 . . .).<br />

+ Values of albedo apply to illumination by “white” light or sunlight.<br />

± References:<br />

1. International Critical Tables, 1929 ed., Vol. 5, p. 262.<br />

2. Handbook of Chemistry and Physics, 1942 ed., pp. 2147–2148.<br />

3. H. Landsberg, Handbook of Meteorology, McGraw-Hill Book Company, Inc., New<br />

York, 1945, p. 932.<br />

4. J. Charney, Handbook of Meteorology, McGraw-Hill Book Company, Inc., New<br />

York, 1945, p.296.

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