Not exact matches
The winds can affect
rates of
evaporation, which cool an
ocean in much the same way as sweating can cool the skin, affecting the amount of heat that moves between the sky and the
ocean.
Warm
oceans produced extensive
evaporation and precipitation, which on the cold continents resulted in extreme snowfall
rates that built up glaciers.
There are some various proposed mechanisms to explain this that involve the surface energy balance (e.g., less coupling between the ground temperature and lower air temperature over land because of less potential for
evaporation), and also lapse
rate differences over
ocean and land (see Joshi et al 2008, Climate Dynamics), as well as vegetation or cloud changes.
Consistent with how I was reading things, pleasantly — barring some cautious hedging I'd made, based on the possibility that salinity could reflect mass changes, either when fresh water was added to the
ocean via glacial melt or impoundment decreases (
ocean mass increase) or via increased
evaporation rates (
ocean mass decrease).
If we isolate the
ocean for diagnosis, there is a rather short list of suspect forcings and feedbacks (ie changes in shortwave reaching
ocean surface possibly from strong negative aerosol feedbacks, net positive
rate change in loss of longwave from the
ocean (which would have implications for the positive WVF), net positive heat loss through
evaporation without balancing compensation (with other implications for positive WVF).
The
rate of
evaporation from the
ocean seems to be increasing as the world warms.
Is it the long - awaited, predicted and scientifically reasonable CO2 fertilization feedback effect on the
oceans» vast biomass of CO2 - consuming cyanobacteria, albeit also driven by the (literally) «shit - loads» of nitrogen compounds the human race is also pumping into the
oceans — thereby shifting sea surface albedos, reducing
evaporation rates and troposphere relative humidities (ringing any bells here, bros)?
If we are to get a real idea of the
rate of tropical convection that drives Hadley cell dynamics and the size of the subtropical high pressure cells we need to measure the
rate of
evaporation from the tropical
ocean.
The
rate of
evaporation from the
ocean is increasing as the world warms.
Since latent heat transport (and surface cooling of the
ocean) must increase in proportion to the
rate of
evaporation, perhaps Wentz et al have identified a reason why the models appear to overstate climate sensitivity: the actual latent cooling increases by about 4 watts per square meter more than the models predict for each degree rise in surface temperature.
The existence of that cooler layer is evidence that the
rate of
evaporation is the primary influence on variability in the
rate of
ocean energy loss (apart from internal
ocean circulation variability which is not relevant here) and it follows that more
evaporation for the same
rate of conduction and radiation (from a stable temperature differential) will send that cooler layer deeper and / or intensify the temperature differential between it and the
ocean bulk below.
Indeed, the faster the
rate of
evaporation the deeper the level of temperature discontinuity will go and / or the larger the temperature differential will be between the cooler layer and the
ocean bulk below.
I have been engaged in a discussion with a young climatology professional who thought that
evaporation from the
ocean surface left behind a residue of surplus energy to warm the
oceans by reducing the
rate of energy release from the
oceans and thus justifying the AGW scenario.
Could an increase in greenhouse gases actually have a cooling effect over water by speeding up the
rate of
evaporation from the
oceans thereby extracting energy faster from the
oceans, speeding up the hydrological cycle and pushing energy faster to space?
Instead the
rate of energy flow from
ocean to air would be primarily governed by the
rate of
evaporation and not by temperature differentials.
So if one increases the
rate of downwelling IR (thereby increasing the
evaporation rate) then the increase in upward energy flow caused by the fall in the temperature of that 1 mm layer will be greater than the decrease in upward energy flow that will result from any reduced temperature differential between the topmost Knudsen layer and the
ocean bulk arising from the application of Fourier's Law.
The
oceans control the background
rate of energy flow from
ocean to air via The Hot Water Bottle Effect and it is the energy flow from
ocean to air (supplemented to a miniscule extent by the greenhouse effect) that drives the
rate of
evaporation by creating varying temperature differentials between sea surface and air at the surface.
Warmer water surfaces from extra downwelling infra red can not cause warming of the
ocean bulk because the
rate of
evaporation increases proportionately to the extra energy available and the latent heat of
evaporation is then taken mostly from the water.It is then no longer available to warm the
ocean bulk.
... The increase in flux is converted by the
ocean surface into an insignificant change in
evaporation rate.
As the world warms, the
rate of
evaporation from our
oceans seems to be increasing, powering ever - stronger storms.
The
rate of
evaporation always increases in proportion to the supply of extra energy to water molecules at the surface or to molecules of air that are in contact with the water surface so that no warming of the
ocean by the air can occur.
As regards a warming of the
ocean skin,
evaporation is a continuous process caused by temperaure, density and pressure (not just temperature) differentials between water and air so that the
rate of
evaporation accelerates when a water surface is warmed such as from the warming effect of extra greenhouse gases (especially if the air is dry).
The
ocean responds by rapidly increasing the surface
evaporation rate by 1.7 W.m - 2, or 2.7 g.hr - 1 of water for ideal «clear sky» conditions.
Water vapor is brought into the atmosphere via
evaporation - the
rate depends on the temperature of the
ocean and air.
v) More CO2 ought theoretically induce faster cooling of the
oceans by increasing
evaporation rates.
I see discussion of
ocean temperature and
evaporation rates without mention of relative humidity effecting
evaporation and heat content.
Instead it is a composite of the
rates of
evaporation and condensation, melting and freezing and thus the average time that a water molecule remains in the air in vapour form, or in the
ocean as a liquid or in ice and snow as a solid.
Stephen Wilde is quite correct in pointing to
evaporation from the
oceans and the
rate of the hydrological cycle as the pre-eminent regulator of surface temperatures on Earth in his conceptual «model.»
Conversely if downwelling IR decreases the
evaporation rate decreases and the heat exchange at the
ocean / atmosphere boundary remains the same.
This is caused by the increased moisture capacity of the atmosphere with increased temperature, as well as warmer
oceans, seas, and rivers, which leads to increased
evaporation rates.
Evaporation rates are increasing over the
oceans, but it's thought to be mostly due to greater windiness.
In fact, one almost certain effect of global warming will be an increase in the
evaporation rate of the
oceans.