Sentences with phrase «condensation point»

Even deep under the condensation point.

H2O's distribution IS governed however by its freezing and condensation point altitudes to the «lower» atmosphere.

It's temperature and altitude that controls the condensation point.

by changing the superheat and subcool numbers higher or lower (by adding or removing freon), you're moving the position of the where the evaporation / condensation point happens further up or down in the evaporator or condenser from top to bottom.

Not exact matches

«It conveys an energetic presence that is neither localized nor enclosed, but radiates from around its point of condensation.»

It would introduce into it a singularity, an irreversible progression, with condensations at its ritical moments, as individual points on a curve.

And the cool thing is that it features plenty of access points for entry, exit, and ventilation, including a large door with a dual - sided zipper to open from the inside or outside, two little doggy doors for your furry friends, and a large window that prevents condensation.

Although most aerosols are carried up by the same atmospheric circulation patterns, their chemical and physical properties determine whether or not they become «cloud condensation nuclei,» which are the points around which droplets form before they become cloud droplets.

Key Terms included: - Water Cycle - Condensation - Transpiration - Groundwater - Cloud - Evaporation - Surface Runoff - Water Vapor - Precipitation - Humidity - Dew Point - Perspiration Folding and playing directions are also included.

I guess I was thinking of the condensation that might cause water to collect in the airspace in an imperfectly sealed container — which, as you point out, doesn't actually mix with the oil, though it still could find its way into the engine easily by accident.

The show features a site - specific version of Center of Form's Condensations, mid-1970s, specially configured for Green Point Projects, New York.

When it reaches a level high enough to cool it to it's «dew point» the water vapour condenses out in the form of clouds and rainfall and the Latent Heat of Condensation is released into the upper part of the atmosphere to accelerate the escape of radiant energy to space.

At the dew point clouds condense out and the latent heat of condensation releases more energy which drives the convection higher.

The regions of large precipitation are determined by the atmospheric circulation: the near - surface atmospheric flow converges near the subsolar point, leading to strong ascending motion and condensation (see Merlis and Schneider (2010) for a detailed discussion).

The only molecule that is constrained outside of gravitational effects is H2O, limited by its condensation and ice points.

The point is, in a glider pilot's world, the evaporation frequently leads to condensation within a few miles laterally and within a mile or even less vertically.

The interesting point to me is not the basics of condensation and latent heat, but how the depth and density of the condensation layer impacts the distribution of that heat.

The local pressure reduction pointed to when condensation reduces volume is instantly offset by mass flowing into the original volume from the surroundings and the energy released is not enough to make the air parcel and the liquid contents lighter than air containing water vapour.

My comprehension is that a rising moist air parcel reduces in temperature and volume gradually, but condensation occurs rather abrupt when the air parcel temperature reaches the dew point.

Condensation can occur all along the rest of the pipe, most strongly at the coldest points.

This paper actually proposes that the sensible heat released by condensation warms the dryer air to a point where it becomes even lighter than air containing water in vapour form.

At this point we can recall that there is a continuity equation and check how our expression for condensation rate relates to it.

«A point which has been increasingly emphasized in M&G's successive expositions of the biotic pump theory, is the «pressure drop» which occurs on condensation.

The actual driver of their «effect» falls apart as the horizontal increases past a point which would cause their «condensation layer» to break apart.

The point being that evaporation starts the initial ascent and adiabatic cooling keeps it going until condensation occurs.

Makarieva et al could now rewrite their paper from the point of view that their previous paper had elicited indignant protestations from everyone that they too had been modeling the same teeny tiny 0.17 % implosion all along, when the reality is that this whole model is completely wrong and that the latent heat of condensation causes a massive 9 % explosion.

Air containing water vapor, cooled to (and under) its dew point, will not undergo homogenous condensation (supersaturation).

The above points describe essentially similar changes as the paper discusses in chapter 2 except for one essential difference: The only source of pressure drop is the ascending movement of air not to the condensation of water.

When you see condensation on the bathroom mirror, you know the dew point of the water vapor in the air is equal to or higher than the surface temperature of the mirror.