where L = latent heat of vaporization, ρ = density of air, qs
= specific humidity at the surface, qr
= specific humidity at a reference height, usually 10m, CDE = empirically measured aerodynamic humidity transfer coefficient (typically around 10 ^ -3 over the ocean), Ur = wind speed at the reference height.
Q
= specific humidity (at surface or on one or more atmospheric levels).
Not exact matches
«Height - resolved measurements of
specific humidity (q) and relative
humidity (RH) are obtained from NASA's satellite - borne Atmospheric Infrared Sounder (AIRS)... The water - vapor feedback implied by these observations is strongly positive, with an average magnitude of λ q
= 2.04 W / m2 / K, similar to that simulated by climate models.»
We know R1 + R2
= R
= εσT ^ 4 We could use a «bulk equation» for L if we knew the air temperature &
specific humidity + wind speed at reference heights.
library (ncdf) ncep500
= open.ncdf («NCEP.nc») ncep500 [1] «file NCEP.nc has 4 dimensions:» [1] «lat Size: 73» [1] «level Size: 1» [1] «lon Size: 144» [1] «time Size: 361» [1] «----------------» [1] «file NCEP.nc has 1 variables:» [1] «short shum [lon, lat, level, time] Longname: Monthly Mean of
Specific Humidity Missval: 32766 ″ nc500
= get.var.ncdf (ncep500) dim (nc500)[1] 144 73 361 nc25SN
= nc500 -LSB-, mean (c (27:47)-RRB-,] dim (nc25SN)[1] 144 361 SN25
= colMeans (nc25SN) x
= 1:361 lmSN25
= lm (SN25 ~ x) summary (lmSN25) acf (residuals (lmSN25)-RRB- $ acf [2][1] 0.5715495 plot (x, SN25, type
=» b», main
=»
Specific Humidity 25S to 25N from 01/1979 to 01/2009 ″, xlab
= «Months Starting at 01/1979 ″, ylab
=» Secific
Humidity», col
=» dark red»)