IDEAL STATES OF EQUILIBRIUM IN THE ATMOSPHERE. 



57 



The states of equilibrium represented by these tables are also illustrated by 

 fig. 2, the method of representation being the same as that used in fig. i (p. 45) to 

 illustrate the equilibrium in the sea. 



9 



27/70=1-- 



20000- jo 



10000- 



! 



o- 



I 



4 



I 



I 



-- 100- -- 



200- - = 



-=-- 30O--\ 



00 ZW8*r-0 



wonono 



[,00000 



] sooooo 



tooooo 



100000 



M 

 S 



20000- - 



%--800- -I 



J--900- 

 0-&--1000-- 



t 



% 



I 



5*600- 



50000 - 





4 





10000 JzOoooj 



\O.0002 



-%p.ooas uoooo- 



lOOOO^pooou 



%Ooooi 



- %0.ooos 



~ %>.ooof 



00008 

 ^p0OO9 

 KfiOPJO 



%0.OO12 



<*0.0012Tf 



0- 



* lb 3 



00 S1600-r-0 



-Iff 



10' 



3 50000- 



uoooo- 



30000- 



-78<t O - 



Dry atmosphere in adiabatic equilibrium 



2O00O- 



f 



0.0O127e 



100OO- 



-10- 



-200000 



rJOOOOO joooo- -0,00001 



-moo 



. 100 



---200- 



= --300- -S 



-78V- O -*-00OlS76 



Homogeneous atmosphere. 



10000- = 



- -O.ooat 



zfiooos 



% 



I 



6 



50000- 



UOOOO- 





10000- = 



fo^soo 

 ymooo 



--S00000 

 I200000 



uoooo- 



-100000 



- -0.00001 



20000- - 



- 100- 



- -10000 20000- -00001 



'--20O-- 



Fatl of temperature 0.5 C. per 100 dyn.m. 



E 300-- 1 



-%--UOO I 

 \\-*500~- 1 



-|-- OOO- 

 \ 700-- 1 

 i 800- 



- I- -900 I 



0-E-- lOOO- 



Isothermic atmosphere. 



30000- 



-O.0002 



0O003 



<XXXh% 



- 0.0004 



Fig. 2. States of atmospheric equilibrium. 



