A Meteorological Treatise On the Circulation And Radiation in the Atmospheres of

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8 8799. 4 8724. 6 8750. 0 8742 .
7000 8359. 8 8595. 0 8606. 8 8748. 2 8919. 2 8906. 2 8897. 0 8826. 6 8854. 0 8854. 6 6000 8535. 2 8702. 6 8737. 6 8862. 8 9001. 4 9026. 2 9025. 6 8980 . 5 9015. 7 9000 .
5000 8727. 2 8842 . 8 8892. 2 8993. 6 9119. 0 9137. 4 9158. 6 9141. 0 9166. 4 9177. 0 4000 8940. 8 9023. 6 9061. 5 9138. 4 9261. 0 9287. 8 9297. 4 9291. 6 9350. 8 9349. 0 3000 9165. 4 9217. 6 9234. 4 9310. 4 9405. 0 9433 . 6 9451. 0 9473. 2 9509. 4 9524. 5 2000 9397. 8 9432 .
9461. 2 9490. 8 955
...3. 0 9600. 4 9607. 2 9657. 0 9698. 4 9682. 0 1000 9663. 0 9671. 6 9676. 5 9697. 5 9719. 4 9743 . 6 9770. 8 9776. 8 9793. 3 9781. 4 000 Computed from Tables 29, 31.
TABLE 36 THE HEAT WHICH GIVES RISE TO RADIATION (Qi Q ) z 90 80 70 60 50 40 30 20 10 19000 4694. 2 4581. 1 4451. 2 4253. 8 4064. 2 3800. 2 3350. 6 3270. 0 3079. 6 2853. 1 18000 4449. 3 4331. 0 4195. 5 3982. 7 3794. 3 3514. 3 2990. 1 2944 . 8 2791. 4 2605. 0 17000 4204. 4 4064. 9 3920. 2 3707. 8 3512. 0 3210. 4 2736. 1 2677. 4 2481. 0 2363 .


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