Panting
allows evaporation of water and heat across the moist surfaces of the lungs, tongue, and surfaces within the mouth.
Not exact matches
If you've got it, flaunt it — and your hair will remain perfect until the excess energy you used powering two hair dryers will hasten the world's expenditure
of fossil fuels to the point where we can no longer afford the electricity to power hair dryers, and instead resort into walking into darkened caves full
of bats and
allowing the collective heat
of their tiny nocturnal bodies to hasten the
evaporation of our surplus hair
water.
Cooler night temperatures also
allow the scanner to stay cool and minimize the
evaporation of water from the surface during the scanning procedure.
Drip irrigation — plastic tubing to
water the trees» roots — would minimize the amount
of water lost to
evaporation and seepage into sandy soils,
allowing trees to prosper in areas that are parched today.
% due to eruption 9.5 % (assuming the average thickness
of melted ice was 1 meter, and not
allowing for any
of the heat being lost to warming the 4 km thick sea
water column, or air, or
evaporation)
The increased area
of warm
water on the surface
allows the tropical Pacific Ocean to discharge more heat than normal into the atmosphere through
evaporation.
The persistent upwelling
of cold
water in the eastern tropical Pacific would have reduced cloud cover there, via reduced oceanic
evaporation, and thus
allowed more
of the sun's energy to enter the tropical ocean - this would have aided the ocean warming process, as generally the case when the tropical ocean is cooler - than - normal.
* When it's warmer, the
evaporation of water speeds up,
allowing the ground to heat up faster, which then evaporates more
water in a vicious cycle which continues until meaningful rain stops it.
The oceans and seas absorb the heat from the atmosphere and redistribute it through the means
of water currents, and atmospheric processes, such as
evaporation and the reflection
of light
allow for the cooling and warming
of the overlying atmosphere.
Notable among these are Wentz et al. (2007), who suggest that the IPCC has failed to
allow for two - thirds
of the cooling effect
of evaporation in its evaluation
of the
water vapor - feedback; and Spencer (2007), who points out that the cloud - albedo feedback, regarded by the IPCC as second in magnitude only to the
water - vapor feedback, should in fact be negative rather than strongly positive.
For example, the root system
of forest trees facilitates both storage and extraction
of moisture from soil; biogenic aerosols produced by trees control the intensity
of water vapor condensation over the forest; the large height
of trees determines the vertical temperature gradient under the canopy, keeping soil
evaporation under biotic control; tall trees are also essential for surface friction that does not
allow extremely high wind velocities to develop.