Bigelow— Radiation in the Earth? 8 Atmosphere. 259 



Table 3. 



Evaluation of the equation, 



log C = - 5-960 - 2-220 (A- 4) 

 between the limits A = 4 - 00 and 3*50. 



A 



log C 



A 



log C 



A 



log C 



A 



logC 



4-00 



— 5-960 



3-85 



— 5-627 



3-70 



— 5-294 



3-55 



-4-961 



3-99 



— 5-938 



3-84 



— 5-605 



3-69 



-5-272 



3-54 



-4-939 



3-98 



— 5916 



3-83 



— 5-583 



368 



— 5-250 



3-53 



-4917 



3-97 



— 5-893 



3*82 



— 5-560 



3-67 



— 5-227 



3-52 



— 4-894 



3-96 



— 5-871 



3-81 



— 5-538 



3-66 



— 5-205 



3-51 



— 4-872 



3-95 



— 5-849 



380 



— 5516 



3-65 



— 5-183 



3-50 



— 4-850 



3-94 



— 5-827 



3-79 



— 5-494 



3-64 



— 5-161 





.. 



3-93 



— 5 805 



3-78 



— 5-472 



3-63 



— 5-139 



._ 



_. 



3-92 



— 5-782 



3-77 



— 5449 



3-62 



— 5-116 







.. 



3-91 



— 5-760 



3-76 



— 5-427 



3-61 



-5-094 



-- 



-- 



3-90 



-5-738 



3-75 



— 5-405 



3-60 



-5-072 







3-89 



-5-716 



3-74 



— 5-383 



3-59 



— 5-050 



_. 







3-88 



— 5-694 



3-73 



— 5-361 



3-58 



-5-028 



__ 



__ 



3-87 



— 5-671 



3-72 



— 5-338 



3-57 



— 5-005 



._ 



__ 



3-86 



— 5-649 



3-71 



— 5-316 



3-56 



-4-983 



-- 



-- 



Table 4. — Observed Temperature T. 



z 

 Height 



in 

 meters 



May 5 



July 27 



Sept. 2 



Sept. 7 



Sept. 25 



Sept. 9 



Aug. 29 



July 29 



June 19 



Victoria 



1909 



1908 



1909 



1906 



1907 



1907 



1907 



1907 



1907 



Nyanza 



52° 



52° 



52° 



45° 



35° 



25° 



13° 



13° 



-2° 



0° 



18000 





223-2 

















190-5 



17000 



213-5 



220-5 



_ 



_ 



222-9 



231-1 



_ 



_ 



_ 



197-1 



16000 



222-5 



219-9 



_ 



225-9 



220-2 



227-3 



_ 



_ 



_ 



202 6 



15000 



220-7 



218-3 



- 



219-8 



220-1 



216-8 



203 7* 



205-1* 



203-9* 



206-8 



14000 



219-7 



218-1 



_ 



216-8 



219-9* 



213-4* 



208-4 



209-7 



212-4 



210-8 



13000 



216-9 



216-5 



226-3 



2150* 



220 1 



215-4 



214'1 



214-9 



221-1 



216-0 



12000 



211-3* 



212-7* 



228-1 



223-9 



220-3 



220-4 



220-8 



221-8 



225-8 



222-6 



11000 



2130 



217-4 



228-3 



231-2 



228-1 



227-8 



228-3 



229-4 



237-8 



231-4 



10000 



2214 



225-9 



228-0 



241-4 



236-0 



238-0 



237-3 



237-4 



245-8 



238-9 



9000 



230-5 



233-5 



225-6* 



249 4 



246-0 



246-5 



245-9 



246-7 



253-6 



246 ; 1 



8000 



239-3 



242-2 



230 2 



256-4 



253-7 



255-0 



252-9 



253-1 



260-0 



250-7 



7000 



247-7 



250 6 



237-8 



262-7 



261-1 



262-1 



258-9 



262-1 



266-5 



258-0 



6000 



255-6 



257-4 



246-5 



267-3 



267-4 



267-8 



266-1 



267-8 



272-6 



263-4 



5000 



262-9 



263-5 



250-7 



274-9 



274 



274-9 



272-5 



272-4 



276-9 



269-2 



4000 



267-1 



270-5 



256-7 



279-7 



278-5 



279-3 



276.7 



277-2 



280-9 



274.7 



3000 



272-9 



275-7 



264-1 



287-3 



281-9 



287-1 



282-2 



283-0 



286-5 



280-8 



2500 



275-2 



278-7 



2666 



289-4 



284-5 



290-6 



285-2 



285-8 



287-8 



284-6 



2000 



276-8 



282-5 



268-9 



293-7 



287-1 



293-4 



289-4 



283-9 



290-2 



288-4 



1500 



278-2 



286-3 



272-5 



297-9 



2891 



295-3 



287-5 



286-2 



290-5 



292-4 



1000 



279-7 



290-0 



2755 



301-2 



290-5 



297-8 



291-1 



290-1 



292-7 



296-2 



500 



278 7 



290-4 



278-1 



301-7 



293-5 



297-4 



295-9 



292-7 



296-2 



(1140) 



116 



281-3 



293-3 



283-2 



304-7 



296-5 



303-5 



299-1 



298-1 



300-2 



— 



* Bottom of the isothermal region. 



