Atmospheric Radiation a Research Conducted At the Allegheny Observatory And At

Frank W Frank Washington Very

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Temperature.
Excess.
Radiation.
o c B Divisions.
+3. U 61. 8 28. 2 + 13. 4 +2. 4 70. 8 37. 2 +17. 3 +4. 0 81. 0 47. 4 +25. 0 +4. 2 90. 9 57. 3 +26. 1 +2. 8 100. 2 66. 6 +32. 6 +2. 0 110. 2 76. 6 +37. 7 The observations may be represented by a straight line passing through the origin and a deflection of 30 div. At excess 63, giving a mean deflection of 0. 476 div. Per degree of excess. The ratios to the deflections of the cooling curve are, as before, about six to one at the middle of the heatin...g curve, where the rate of heating is greatest.
The asbestos in the forward position radiates to the cooler iron of the end-plate, and hence becomes cooler. When withdrawn to the rear the blackened surface of the asbestos absorbs radiation from the hot interior, and is also heated by contact with hotter gas; but, although the copper back is now near a cooler end-plate, the uoucouductivity of asbestos prevents any influ- ence from this cause. The positive differential effect is added to the true gaseous radiation.

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