Você procurou por: evaporation (Tcheco - Inglês)

evaporation is greatly increased, from the landmasses.
evaporation is greatly increased, from the landmasses.

to the total amount of evaporation/rainfall worldwide per year:
to the total amount of evaporation/rainfall worldwide per year:

evaporation increases and more heat is lost to space in the upper atmosphere.
evaporation increases and more heat is lost to space in the upper atmosphere.

re: evaporation. its a very good question and represents another shortcoming of the experiment.
re: evaporation. its a very good question and represents another shortcoming of the experiment.

390(radiation) + 24 (thermal) + 78 (evaporation) = 492!
24

loss of heat from evaporation amounts to around 78 w/m or a quarter of the total insolation.
loss of heat from evaporation amounts to around 78 w/m or a quarter of the total insolation.

damorbel - in regards to energy magnitudes of ir, evaporation, and convection, you are unfortunately incorrect.
damorbel - in regards to energy magnitudes of ir, evaporation, and convection, you are unfortunately incorrect.

some figures from the world water council on evaporation from human sources (not abstraction which is much much higher)
some figures from the world water council on evaporation from human sources (not abstraction which is much much higher)

[a complex combination of hydrocarbons obtained from the evaporation of solvent under vacuum from polymerized hydrocarbon resin.
[a complex combination of hydrocarbons obtained from the evaporation of solvent under vacuum from polymerized hydrocarbon resin.

in intermediate years of higher snowfall, the temperatures started to moderate and the lake froze over later, allowing more evaporation and more opportunity for substantial snowfalls.
in intermediate years of higher snowfall, the temperatures started to moderate and the lake froze over later, allowing more evaporation and more opportunity for substantial snowfalls.

my guess for this is that the lake had little ice in december, allowing more evaporation, and the temperatures were periodically cold enough to allow substantial snow and other times rain.
my guess for this is that the lake had little ice in december, allowing more evaporation, and the temperatures were periodically cold enough to allow substantial snow and other times rain.

what i am left wondering is where is the evaporation process being accounted for whilst the measurements of the temperature gradient of the skin layer were being taken, in particular as the cloud cover varied.
what i am left wondering is where is the evaporation process being accounted for whilst the measurements of the temperature gradient of the skin layer were being taken, in particular as the cloud cover varied.

part iii: the temperature relationship between vapour pressure and evaporation rate; pesticide science 13 (1982) 161–168.
part iii: the temperature relationship between vapour pressure and evaporation rate; pesticide science 13 (1982) 161-168.

bear in mind too, that industrial wv emissions include the energy needed to vaporise the water...no heat is required from the atmosphere, unlike 'natural' evaporation.
bear in mind too, that industrial wv emissions include the energy needed to vaporise the water...no heat is required from the atmosphere, unlike 'natural' evaporation.

a good handle on this can be gleaned from a comparison of the water vapour released from cooling towers (and from fossil fuel burning overall) in relation to the overall amount of water vapour produced in the natural evironment by evaporation and precipitation.
a good handle on this can be gleaned from a comparison of the water vapour released from cooling towers (and from fossil fuel burning overall) in relation to the overall amount of water vapour produced in the natural evironment by evaporation and precipitation.

(there are fluctuations in cloud cover patterns, humidity patterns, and evaporation and latent heating and temperature patterns associated with variability in circulation patterns in the atmospheres (which can also contribute to surface albedo fluctuations), so there are both thermal and mechanical (momentum) feedbacks through which circulation patterns cause changes in circulation patterns - but over time there tends to be a predictable statistical description of all that (which is the longer-term climate)...
(there are fluctuations in cloud cover patterns, humidity patterns, and evaporation and latent heating and temperature patterns associated with variability in circulation patterns in the atmospheres (which can also contribute to surface albedo fluctuations), so there are both thermal and mechanical (momentum) feedbacks through which circulation patterns cause changes in circulation patterns - but over time there tends to be a predictable statistical description of all that (which is the longer-term climate)...