眼高差について(日本航海学会第10回講演会)
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概要
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Supposing that dips depend on the temperature at the observer Tn and the one just above the sea-surface, we have obtained the heat conductivity of the lower atmosphere by observing the timely variation of dips. As the results we have got the order of magnitude of b^2D as 2×10^<-2>〜3×10^<-2> hour^<-1>
- 社団法人日本航海学会の論文
- 1954-04-10