Well, orchids are notoriously difficult to raise — they require very
specific humidity levels, fertilization, and light (as I can attest to firsthand).
Not exact matches
Still, Hess cautioned, some exotics require special care: Reptiles need certain
levels of temperature and
humidity that vary according to the animal, and birds require specially - formulated diets
specific to the type of bird.
I think you now are trying to prove something that (as Ten Hoeve et al say) is quite «understandable» and something that at a basic
level nobody would disagree with (certainly while relative /
specific humidity remains outwith the discussion).
And
specific humidity has been increasing at all
levels of the troposphere (IPCC AR4 3.4)(the stratosphere too, but that is a somewhat separate issue).
Q =
specific humidity (at surface or on one or more atmospheric
levels).
Global rainfall increases typically cause an overall reduction of
specific humidity (q) and relative
humidity (RH) in the upper tropospheric
levels of the broader scale surrounding convection subsidence regions.
Here, here, and here are
specific humidity time plots for the tropics (25N to 25S, globally) for the 700mb, 500mb and 400mb
levels, respectively.
Problem number two is the
specific humidity of the 300mb
level, shown here.
The 2009 State of the Climate Report of the US National Oceanic and Atmospheric Administration (NOAA) tells us that climate change is real because of rising surface air temperatures since 1880 over land and the ocean, ocean acidification, sea
level rise, glaciers melting, rising
specific humidity, ocean heat content increasing, sea ice retreating, glaciers diminishing, Northern Hemisphere snow cover decreasing, and so many other lines of evidence.
Does anyone know why the only surface
humidity field from the ERA - Interim dataset is 2m dew point and not the more commonly used fields of
specific humidity and / or relative
humidity (which are also available as pressure
level fields)?
However, the strength of the correlation between
specific humidity variations and the temperature variations at the same
level appears to be strongly height dependent.
Overall, the variations of
specific humidity correlate positively at all
levels with the temperature variations at the same
level.
Daily mean NCEP / NCAR reanalysis data are used as atmospheric forcing, i.e., 10 - m surface winds, 2 - m surface air temperature (SAT),
specific humidity, precipitation, evaporation, downwelling longwave radiation, sea
level pressure, and cloud fraction.
The decreasing
specific humidity (especially at 300 and 400 mb
levels) almost totally offsets the GHE of increasing CO2 content.
It's worth noting that
specific humidity at the tropopause follows solar activity
levels, not the rise of co2.
The latter effect acts to reduce CO2 sensitivity by increasing the aerosol - sensitive SW tau, increasing both cloud density and cover, decreasing upper tropospheric
specific humidity and INCREASING SW albedo and will increasingly do so as the atmospheric
level of CO2 rises!
The latter effect acts to reduce CO2 sensitivity by increasing the aerosol - sensitive SW tau, increasing both cloud density and cover, decreasing upper tropospheric
specific humidity and SW albedo and will increasingly do so as the atmospheric
level of CO2 rises!
There is increasing
specific humidity at the lower
levels, some decline in higher
levels but the weighted average is constant.
It is also not surprising that the Tibetan plateau
specific humidity at this pressure
level is considerably higher than the zonal mean (3.5 - 4 times larger during the summer).
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»)