If you get a lot of «incoming» it disrupts the polar vortex in the lower stratosphere, and you get a lot of
mixing with warmer air.
Not exact matches
This vapour
mixes with dry
air at the cooling chamber, resulting in the release of
warm, moist
air to the
air in the room.
This means the
warm air can not
mix with colder
air to cool it down.
The researchers found that on windy nights it wasn't possible to measure the cooling effects of the green spaces beyond their boundaries as there was too much turbulent
mixing of the
air; but on calm
warm nights they estimate that a network of green spaces of around 3 - 5 hectares each situated 100 - 150 m apart would provide comprehensive cooling for a city
with a climate and characteristics similar to London.
Zhou says the
warming was caused primarily by vertical
mixing of the
air, rather than as a direct result of friction as
air passes over the turbines» blades: the movement of the turbines is
mixing the cooler ground - level
air with warmer air higher up.
They say the turbines
mix warmer air that sits at their apex
with cooler
air at ground level.
Tornadoes have hit every continent on the planet except Antarctica, but the vast majority of tornadoes hit in the United States — specifically in the south and southeast United States, or «tornado alley,» where cold
air blowing east from the Rocky Mountains can
mix to deadly effect
with warm air blowing north from the Gulf of Mexico.
Here Becker et al. investigated the impact of convective organization on entrainment — a process in which
warm, buoyant parcels of
air become saturated
with moisture; form cumulus clouds; and
mix with cooler, drier parcels of
air.
By contrast, when you breath in your nose, the
air is
warmed, moistened, conditioned and
mixed with nitric oxide, which both kills bacteria and works as a vasodilator on the airways, arteries and capillaries.
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The stable top of the marine layer, a result of the temperature inversion, prevents any dry,
warm air from above the inversion from
mixing with the stratus deck.
As we approached what is known as the Antarctic Boundary line where we crossed into Antarctic waters, the colder
air and water currents from the south
mixed with the
warmer currents of the north causing a thick hazy fog.
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Whilst flowing across the area between the two columns that cold
air does not
warm up by compression despite falling in height because it remains in contact
with stratospheric
air with which it can freely exchange energy by conduction and
mixing.
The
warmer air evaporates more moisture, but it does so across the entire ocean, and this moist
air mixes continually
with the
air above it, so * all * the
air is moister.
The article talks about how the
warm ocean temperatures, when
mixed with cold
air from Canada, quickly create a very powerful storm.
It frequently breaks up during the winter, allowing
warmer air from lower latitudes to
mix with the Arctic
air.
Lake - effect snow happens when moisture from
warmer lake waters
mixes with cold
air coming from the north, causing more than 2 to 3 inches of snow an hour.
Reduced
mixing with relatively
warmer sub-surface waters effectively reduces the thermal mass exposed to the cold Antarctic
air - slightly more ice forms.
The large area of
warm water exposed thereby
warms the
air,
warm air rises, interferes
with trades,
mixes with global circulation, and raises its temperature by half a degree.
Still
air with either little vertical shear and relatively weak
warming of the ground or
with so much vertical shear that turbulence occurs and irreversibly physically
mixes the
air parcels faster than «reversible» adiabatic expansion can keep up favors the «isothermal» pole, although this too is almost never precisely observed.
In moving the heat from the bottom of the tube to the top is causing the lapse rate to become ** more stable ** — cool at the bottom
with warm air above is an inversion which inhibits vertical
mixing!!
In other words, UHI * is the value of the urban - heat - island effect if wind were not reducing it by replacing
warmer air with colder; and NSTI * is the effect of the near - surface temperature inversion if the wind were not
mixing up the
air near the ground
with the
air a little higher up.
However, on windy days, I expect the UHI effect to be vitiated by
mixing of
air from outside the region of the city
with the relatively
warmed air; and I expect the windiness to reduce the stratification of the boundary layer («
mix it up») and thus reduce the cooling effect of the NSTI.
This «counterflow» design will aid in
mixing the
warm air that tends to raise to the top of the chamber
with the cooler
air that will tend to settle on the bottom of the chamber.
The Nature study suggests that global
warming will
mix growing amounts of higher, drier
air with ocean clouds over the course of the century, thinning out the clouds and reducing their cooling effect.
The
warm air rises, stops the trade winds,
mixes with prevailing westerlies, and thereby raises global
air temperature.
They stay
warm because the glass also prevents
mixing with the surrounding
air, but the
air wouldn't be
warm to begin
with if it weren't for trapping infrared.»
You can have a long period of cold
air at the surface
with little turbulent
mixing and little energy transfer, followed by a short period of a
warm surface and lots of turbulence and energy transfer - ending
with a time average of
warm over cold, but a time average of upward energy transfer.
Furthermore, in the absence of such
warming, ocean
mixing would normally be expected to be constantly refreshing the water at the ocean's surface, the place where it meets
with air and dissolves CO2.
I live downwind of topography which in interaction
with the wind
mixes warmer air aloft downwards at night, and my summer minimum temperatures are often 10F
warmer than nearby locations.
Still spinning turbines should create turbulent
mixing of the
warmer air at circa 100M
with the cooler ground surface.