Sentences with phrase «as water vapor when»

Not exact matches

Rather, when the fullness of time is reached, there is a qualitative transformation, as in the case of the acorn becoming an oak, or water brought to boiling point becoming vapor, or instinct becoming reflection, or molecular increase becoming cellular.
Ever since 2005, when NASA's Cassini orbiter found plumes of water vapor spilling out of cracks in the south pole of Saturn's icy moon Enceladus, researchers have sought to learn more about the moon's mysterious interior as a possible abode for extraterrestrial life.
This effect makes the atmosphere act somewhat like a blanket that becomes thicker when amounts of water vapor, carbon dioxide and other greenhouse gases, such as methane and nitrous oxide, increase.
Rime forms when droplets of water vapor deposit directly as ice on surfaces.
When the water enters the atmosphere as vapor, it leaves the salt behind.
As this water moves through rocks, it dissolves salt compounds and pushes through fractures in the overlying ice to form reservoirs closer the moon's surface, where it is expelled into space when the outermost layer of the crust cracks open and the resulting depressurization of these reservoirs causes water vapor and ice particles to shoot out in the observed plumes.
• Clouds form because cold air doesn't hold as much water as warm air • Clouds are made of water vapor • Clouds always predict rain • Rain falls when clouds become too heavy and the rain drips out or bursts the cloud open • Rain comes from holes in clouds, sweating clouds, funnels in clouds, melted clouds • Lightning never strikes the same place twice • Thunder occurs when two clouds collide • Clouds block wind and slow it down • Clouds come from somewhere above the sky • Clouds are made of smoke How does the 5E model facilitate learning?
(PS regarding Venus — as I have understood it, a runaway water vapor feedback would have occured when solar heating increasing to become greater than a limiting OLR value (Simpson - Kombayashi - Ingersoll limit — see http://chriscolose.wordpress.com/2010/08/23/climate-feedbacks-part-1/ — although I should add that at more «moderate» temperatures (warmer than today), stratospheric H2O increases to a point where H escape to space becomes a significant H2O sink — if that stage worked fast enough relative to solar brightening, a runaway H2O case could be prevented, and it would be a dry (er) heat.
Re 9 wili — I know of a paper suggesting, as I recall, that enhanced «backradiation» (downward radiation reaching the surface emitted by the air / clouds) contributed more to Arctic amplification specifically in the cold part of the year (just to be clear, backradiation should generally increase with any warming (aside from greenhouse feedbacks) and more so with a warming due to an increase in the greenhouse effect (including feedbacks like water vapor and, if positive, clouds, though regional changes in water vapor and clouds can go against the global trend); otherwise it was always my understanding that the albedo feedback was key (while sea ice decreases so far have been more a summer phenomenon (when it would be warmer to begin with), the heat capacity of the sea prevents much temperature response, but there is a greater build up of heat from the albedo feedback, and this is released in the cold part of the year when ice forms later or would have formed or would have been thicker; the seasonal effect of reduced winter snow cover decreasing at those latitudes which still recieve sunlight in the winter would not be so delayed).
But the boiling point of heavy water, as well as heavy oxygen water (H2O ^ 18 rather than H2O ^ 16) are higher than that of normal water, and are found in water vapor in the atmosphere at lower concentrations when the global temperature is low.
when there are so many other gases such as methane and water vapor that are equally or more important and forget the input by the sun and ocean currents
CO2 and WATER VAPOR are influenced by the environment in other words as the oceans go so do hey despite man's contribution which is fractional when compared to natural processes.
When a moisture reservoir is located on the exterior of a wall assembly it can act as a source of water that can migrate by a process called vapor diffusion.
When petroleum is burned, some energy is required to separate the molecules into individual atoms, but much more energy is given back as the carbon and hydrogen atoms combine with oxygen to give carbon dioxide and water vapor.
As with petroleum, some energy is required to separate the molecule into separate atoms, but the energy is more than returned when the carbon and hydrogen burn to form carbon dioxide and water vapor respectively.
Many skeptics including myself believed that the rising side of the AMDO was being counted as anthropogenic and that when the falling side arrived this would show that positive feedback from water vapor is a myth and sensitivity is the 1.1 C that modtrans predicts.
Latent heat is in the air when there's water vapor in the air, 2260 kiloJoules for each kilogram, as a matter of fact.
It is becoming apparent that the warming of clouds that is used as a point to prove «back - radiation» from water vapor is not from water vapor (single water molecules) but instead is from the micro-droplets within the clouds which then act as gray bodies when radiating, spreading the energy into all IR bands.
When the convective processes of the atmosphere remove enough water vapor from the oceans to drop sea levels and build polar ice caps, as has happened many times before, the top 35 meters of the oceans where climate models assume the only thermal mixing occurs, must heat up cold ocean water that comes from depths below the original 35 meter depth, removing vast more amounts of heat from the earth's surface and atmosphere.
As if sweltering heat weren't bad enough, Europeans also suffered through a higher - than - normal number of days with dangerous smog levels that year.6 Smog — with ground - level ozone as the main component — forms when sunlight reacts with chemicals such as volatile organic compounds, carbon monoxide, nitrogen oxides, and water vapoAs if sweltering heat weren't bad enough, Europeans also suffered through a higher - than - normal number of days with dangerous smog levels that year.6 Smog — with ground - level ozone as the main component — forms when sunlight reacts with chemicals such as volatile organic compounds, carbon monoxide, nitrogen oxides, and water vapoas the main component — forms when sunlight reacts with chemicals such as volatile organic compounds, carbon monoxide, nitrogen oxides, and water vapoas volatile organic compounds, carbon monoxide, nitrogen oxides, and water vapor.
The Equilibrium Climate Sensitivity (ECS) The Economist refers to is how much Earth temperatures are expected to rise when one includes fast feedbacks such as atmospheric water vapor increase and the initial greenhouse gas forcing provided by CO2.
H2O or water in 100 x more common as a vapor in the atmoshere, and 40x as common when measured by weight.
So why should climatologists rig up a water vapor release, when just as easily they could have had the initial CO2 release more CO2?
I looked at it as potential and it does tend to provide the right range of wind velocity though when water vapor actually decides to condense and precipitate is a bit iffy.
In the Arctic, however, when the Arctic Ocean freezes, there is comparatively little other ocean in the neighborhood to serve as an alternate reservoir that can supply water vapor that will reach the northern landmasses before precipitation elsewhere.
[1975] Greenland, which is a small Antarctica, a polar landmass entirely surrounded by water, has an ocean to the south that remains as a vapor reservoir even when the ocean to the north freezes, so it retains its ice cap.
When that air finds a surface, such as a cold duct boot, at a temperature below the dew point, the water vapor just can't help itself.
They are overwhelmed when water turns to vapor or to ice, releasing and absorbing vast amounts of heat energy as CO2 can not possibly do.
When temperatures rise there may be more water vapor evaporated into the Atmosphere and that may result in more clouds and, if clouds have a net cooling effect (as I think they do) that may reduce the rate of incoming shortwave radiation and thus reduce incoming energy rates such that the temperatures will not rise as high.
It's kind of like considering water vapor as a gas expanding into more space that it is given when it is warmer because the condensation level rises higher.
Air masses are more mobile than the ocean waters, and when they move to a cooler region, the water vapor condenses as rain or snow, leaving the heat energy in the atmossphere.
The shape of the CO2 band is such that, once saturated near the center over sufficiently small distances, increases in CO2 don't have much affect on the net radiative energy transfer from one layer of air to the other so long as CO2 is the only absorbing and emitting agent — but increases in CO2 will reduce the LW cooling of the surface to space, the net LW cooling from the surface to the air, the net LW cooling of the atmosphere to space (except in the stratosphere), and in general, it will tend to reduce the net LW cooling from a warmer to cooler layer when at least one of those layers contains some other absorbing / emitting substance (surface, water vapor, clouds) or is space)
The only sense in which your argument for a negative water cycle feedback makes much sense is if you are grouping together cloud and water vapor effects in such a feedback (which I guess is not unreasonable when you refer to it as «water cycle» but becomes confusing when you refer to it as «water vapor feedback»).
When coupled with the new images from both the Calipso and CloudSat, there now exists a possible 3D view of the atmosphere and a clear indication that we really may not understand the adiabatic character of water vapor nearly as well as had been indicated in the past.
When you said «What we KNOW is that CO2 is a greenhouse gas, much less important than water vapor,», you don't understand, or won't understand, AGW; as somebody said, a stressed denier.
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