I'm going to approach this very naively, to try to quantify the contribution of humidity and temperature
External Quote:
Where:
P = dry pressure, ~1000mb
T = temperature, ~300k [27C]
e = water vapour partial pressure ~40mb
Now for a start, that's from a page on radio wave propagation, so there might be problems right there, but continuing.
What's the magnitude of the effects over the few feet directly above the lake surface? Lake was at 22°C (295K) Air was at 14C (287K), pressure is about 1000, and I'm assuming that varies very little
Water vapor partial pressure, let say for now it varies from 100%RH at the surface of the lake to 50% RH above it.
RH = Actual Vapor Pressure/Saturation Vapor Pressure as a %
Using this calculator:
http://www.srh.noaa.gov/epz/?n=wxcalc_vaporpressure
Saturation Vapor Pressure at 22C (water level) is 26.5mb
Saturation Vapor Pressure at 14C (few feet up) is 16mb, 50% of that is 8mb
So taking those two extremes, at water level:
N = 77.6*1000/295+3.73*10^5*26.5/295^2
N = 263 + 113.6 = 376.6
In the air, varying humidity and temperature
N=77.6*1000/287+3.73*10^5*8/287^2
N = 270.3 + 36.2= 306.5 (decrease in N as we rise, so bend down)
If we just vary humidity:
N=77.6*1000/295+3.73*10^5*8/295^2
N = 263 + 34.3 = 297.3 (bigger decrease in N as we rise, so bend down)
If we just vary temperature:
N =77.6*1000/287+3.73*10^5*26.5/287^2
N =270.4 + 120.0 = 390.4 (increase in N as we rise, so bend up).
I'm assuming the first P term has the water vapor partial pressure factored in, and is not actually the dry pressure.
Of course, we
can't just vary humidity, so the actual meaning of these numbers (if any) is rather dubious. For a start, if the air humidity is 50%, then will it actually be 100% just above the lake surface?
Interesting stuff, but probably ultimately irrelevant to the outcome of the experiment.
However, the laser
does bend up, which would seem to suggest the humidity was not a factor, unless I've got something backwards.