As with rainfall, fog duration, and
relative humidity there are significant variations in temperature between the islands.
Not exact matches
We know that
there need to be certain conditions of temperature,
relative humidity, and wind speeds at different altitudes.
«The
relative humidity was 80 percent
there,» Masters says.
And clouds form when 1) the
relative humidity reaches 100 % and 2)
there are sufficient nucleation sites.
Though
there are many caves, only a small number have the best conditions for climate study, including 100 percent
relative humidity, constant temperatures, no cave winds, and the actual stalagmites — free of holes and decay — forming in the cave.
There, we find frozen, in aesthetically serene images, the historical and sociological riots trapped in silent surroundings, embraced by
relative humidity and temperature.
Obviously, in an actual cloud, the
relative humidity is close to 100 %, but at a grid box scale of 100's of km, the mean
humidity — even if
there are quite a few clouds — will be substantially less.
The water vapor feedback (a generally positive feedback)--
there is an roughly exponential increase in saturation water vapor pressure with increasing temperature, and the
relative humidity (at a given vertical level) overall tends not to change a lot globally, though
there will be different regional trends associated with shifting precipitation patterns.
There is a recent study tending to demonstrate that the average
relative humidity is indeed close to constant.
There is a FAQ about this, which describes how to calculate the 2m specific and
relative humidity: http://www.ecmwf.int/en/does-era-40-dataset-contain-near-surface-
humidity-data
With wNA forest loss,
there are significant declines in both precipitation and temperature during the early growing season, however it is the change in the
relative humidity that dominates the observed increase in VPD.
There is a near infinite supply of greenhouse gases available to the atmosphere in the form of water vapor from the ocean to provide the greenhouse effect, but the
relative humidity in the atmosphere is much less than one.
The declining
relative humidity reduces the temperature compared to the model projections so
there is no hot spot.
There is no temperature dependence or vapor pressure dependence except where temperature affects
relative humidity or where vapor pressure affects
relative humidity.
Air in clouds and immediately next to the ocean surface is at or near 100 %
relative humidity, so as temperatures increase the absolute
humidity there also increases.
If you actually look at the data for the last few decades...
there's evidence for rising specific
humidity in the upper troposphere, but we don't have enough data about
relative humidity to say either way.
Given
there is much more water vapour in the lower levels of the atmosphere, the study really found that
there was a decline in overall global
relative humidity when global warming theory suggests it should stay more - or-less stable.
There are supposed to be subtle changes in
relative humidity in different layers and latitudes depending on temperature changes but global warming theory suggests
relative humidity should stay more - or-less stable.
Given
there is much more water vapour in the lower levels of the atmosphere, the study really found that
there was a decline in overall global
relative humidity.
The study found
there was a 1.5 % (percentage points) decline in
relative humidity in the very lower levels of the troposphere and a 1.5 % increase in
relative humidity in the upper layers of the troposphere.
I think the study just confirmed
there are changes in
relative humidity that we do not understand yet.
As I read for example Bony et al. 2006, Soden and Held 2006,
there are in the IPCC dogma four «feedbacks»: increased atmospheric optical thickness due to increased water vapour column amount due to sustained
relative humidity; cloud radiative effects; albedo effects; lapse rate effects.
m day and night 24/365 for the flat earth assumed by Trenberth & Kiehl, above which
there is an apparently stationary sun),
relative humidity, water vapour (H2O), windspeed, etc., plus the all - in Net anthro Forcing of GISS that I used in my last (it does not help your cause if you had actually read my results).
I know very little about tropical dynamics, but have a half - thought question related to the tropical lapse rate: Is
there a simple argument for why the
relative humidity over land is expected to remain fixed?
Isaac — Among unsettled issues is the change in upper tropospheric
humidity with warming — specific humdity increases, but
there is conflicting information as to whether this increase is sufficient to maintain a near - constant
relative humidity (RH — e.g. Minschwaner and Dessler 2004 as compared with Soden et al 2005).
kuhnkat: I was too hasty, in fact at Des Moines
Relative Humidity is highly significant, but negative, and it is average windspeed that
there at least plays no significant role whilst also having a negative impact on mean annual temperature.