1,1,1		out1,out2,out3
 259.13440
 236.01870
 209.75790
 207.86090
 207.31050
 221.03530
 233.33480
 243.99810
 253.30600
 261.44590	temperatures for 18 layers and surface
 268.55370
 274.71560
 279.98590
 284.40550
 287.99090
 290.73930
 292.62710
 293.60710
 293.73510

.318,23.00,5.00 		ozone parameters for time<tm3

.318,20.00,3.00 		ozone parameters for time>tm3
4800				tm3

500,60.0,1.0,.0001,2000        So/2,zen. angle,step size,low,run length

6.5,2.5				critical lapse rate, ocean depth

320,640,2000			Carbon Dioxide conc (ppmv) C20,C21,tm2

1.6,3.2,2400			Methane conc (ppmv) C40, C41, tm4

.30,.45,3600			Nitrous Oxide conc (ppmv) N20, N21, tm1

275.0				F-11 conc (pptv)

468.0				F-12 conc (pptv)

0,11				Ac, Cloud layer

.10,8.5 			surface albedo, cloud optical depth

0				Initial time (usually 0)

0				# of step between output

12000				after this time the water vapor content
				of the atmosphere is held fixed

Notes:
*out1,out2,out3 determine if output files 'out1',
'out2', 'out3' are generated see list of output files

*aoz,boz,coz are used in the equation below (see Lacis and Hansen
 1974) to calculate the total ozone amount above level z(i)
 (units are cm-STP)
 uo(i)=(aoz+aoz*exp(-boz/coz))/(1+exp((z(i)-boz)/coz))
 * after the time reaches tm3 the parameters change to the values
 of a1z,b1z,c1z

* Step size of 2.0 days max for good results.  Larger step sizes
can be used but the user should explore the consequences before trusting
the results too much.

* When you get this file the runlength will be set to zero.  We suggest
that you try a 100 day run to see how long it takes on your machine.

* If the critical lapse rate is less than 0.0 the program
uses the moist adiabatic lapse rate as the critical lapse rate

* for carbon dioxide, methane, and nitrous oxide:
the initial concentration of the gas is given, followed by the new
concetration.  The third number is the time in days at which the
concentration of the gas makes the stepwise change from the initial
concentration to the new concentration.  For example, to calculated
the change in surface due to doubling of co2 use 320,640,1200 an
ocean mixed layer depth of 2.5 m and a runlength of 2400 days. After
1200 days equilibrium will be reached with [co2]=320 and then [co2]
will change to 640 ppmv at 1200days and a new equilibrium will be
achieved by 2400 days.