作者: Edward C. Y. Inn
DOI: 10.1175/1520-0469(1975)032<2375:ACOHIT>2.0.CO;2
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摘要: Abstract The results of absoprtion coefficient measurements HCl in the region 1400 to 2200 A are reported and compared with those previously published. It is concluded that present represent best compromise all should be used for any calculations on photodissociation rate planetary atmospheres.