If the top of a radiator feels
cooler than the bottom then it probably needs bleeding to get rid of trapped air.
Not exact matches
One of my friends had an «old family recipe» for whiskey sours, and though it wasn't much more
than combining
bottom - shelf whiskey with juice concentrate (in a Gatorade
cooler no less), it always hit the spot.
My baby's
bottom always stayed
cooler in cotton
than any other material or disposables; I live in the tropics so staying
cool is important.
Common examples include the fact that liquid water expands on
cooling below 4 C, which is responsible for lakes freezing from the top rather
than the
bottom.
I am more
than happy to share with you my favorite street wear looks featuring these
cool denim
bottoms.
If you do struggle with any of puzzles, there's a handy hint button at the
bottom of the screen with an appropriate
cool - down timer, however I found that I was rarely stuck on anything more
than a few moments.
Double check the substance in question, if you realize that it is nothing more
than sludgy build - up in the
cooling system (you will notice it on the
bottom of the radiator cap and in the coolant overflow tank) and the vehicle has a Dexcool brand coolant in it, this is caused by air being introduced to the coolant system.
The
bottom rocker cover fin on the sides has also become larger
than before in order to improve the flow of air towards the radiators and improve
cooling.
The new Kindle Fire is packed with a horde of
cool features at a surprisingly low price, and
bottom line (short of a few idiosyncrasies) it's a boon for the book enthusiast, the tablet novice, and the student who needs / wants more
than just a textbook reader.
The pool is small, more to dunk and get
cool than anything else, but the ocean is easily accessible — we would spent afternoons on the dock at the
bottom of the stairs.
The layering of paint seems to engage more
than one palette; orange and magenta peak out of the
bottom of the composition, but are obscured by a haze of
cool white that occupies the majority of the image.
The paint on side A will clearly be burnt even a bit more
than from A alone, creeping up from the green
cool temperature
bottom in the middle, against the temperature gradient, when you also start heating the rod at B.
This warming is less
than it will ultimately be, because the
cool ocean surface holds back the warming — allowing more energy loss out the
bottom than will ultimately be the case.
* & & * — if the stratosphere were optically thick and warmed at the
bottom even if the whole experiences net
cooling, then the stratospheric feedback adds to the initial TRPP forcing, and the end result could require warming below TRPP to change the flux at TRPP to an amount greater
than the TRPP after stratospheric adjustment, because of the additional warming that would occur in the (lower) stratosphere.
-------- * & & * — if the stratosphere were optically thick and warmed at the
bottom even if the whole experiences net
cooling, then the stratospheric feedback adds to the initial TRPP forcing, and the end result could require warming below TRPP to change the flux at TRPP to an amount greater
than the TRPP after stratospheric adjustment, because of the additional warming that would occur in the (lower) stratosphere.
The anomolous expansion of liquid water with
cooling at temperatures less
than 4 °C, means that the
bottom of a frozen garden pond can remain relatively warm, if it is deep enough.
Since the deeper waters are very isolated from the surface and several degrees
cooler than the surface waters, this means that the 3 oC heating of the surface can not be caused by the (
cooler)
bottom waters.
Not that Fred Staples will be back, but from the EPA Endangerment Response to Comments document: «For example, as a disproof of the greenhouse effect, the paper by Gerlich and Tscheuschner presents the example of a pot of water, noting that the
bottom of the pot will be
cooler if it is filled with water
than if it is empty.
The
bottom surface
cools and the top surface warms, even if the
bottom is already
cooler than the top, and the stairs aren't doing anything but freely moving along between.
Hell, the KE will be greater as well, because you'll have to integrate once you figure out what is, and this too will get a much bigger addition from differentially warming the dense
bottom than you lose from
cooling the not - so - dense top, I think.
Thawing permafrost also delivers organic - rich soils to lake
bottoms, where decomposition in the absence of oxygen releases additional methane.116 Extensive wildfires also release carbon that contributes to climate warming.107, 117,118 The capacity of the Yukon River Basin in Alaska and adjacent Canada to store carbon has been substantially weakened since the 1960s by the combination of warming and thawing of permafrost and by increased wildfire.119 Expansion of tall shrubs and trees into tundra makes the surface darker and rougher, increasing absorption of the sun's energy and further contributing to warming.120 This warming is likely stronger
than the potential
cooling effects of increased carbon dioxide uptake associated with tree and shrub expansion.121 The shorter snow - covered seasons in Alaska further increase energy absorption by the land surface, an effect only slightly offset by the reduced energy absorption of highly reflective post-fire snow - covered landscapes.121 This spectrum of changes in Alaskan and other high - latitude terrestrial ecosystems jeopardizes efforts by society to use ecosystem carbon management to offset fossil fuel emissions.94, 95,96
Weyl (1968), speculating that the «temporary stagnation» of the
bottom water would end because of warming by the interior heat of the Earth; the role of glacial meltwater suppressing North Atlantic Deep Water production was also pioneered by Worthington (1968); a neat explanation of the entire circulation in terms of water evaporating from the North Atlantic more
than from the
cooler North Pacific was indicated by Warren (1983).
The
bottom is indeed
cooler than the top.
Now the sun would be expected to set up an undisturbed gradient from cold at the
bottom to warm at the top but it does not because upward radiation from the surface plus energy drawn upwards by evaporation at the surface creates a layer 1 mm deep near the surface (the subskin) which is 0.3 C
cooler than the water below it.
For example, average overnight temperatures can be significantly
cooler at the
bottom of a valley
than at higher elevations.