lecture 4 air temperature Flashcards

1
Q

conduction

A

is the vertical transfer of heat in soils causing them to warm during the summer and cool in winter.

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2
Q

convection

A

is the principal method of heat transfer in the atmosphere and oceans

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3
Q

Specific heat capacity

A

generally referred to as specific heat) is the amount of heat per unit mass required to raise the temperature of a substance by 1 °C.

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4
Q

Volumetric heat capacity

A

is a measure of how well a substance stores heat and is calculated as specific heat capacity multiplied by density.

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5
Q

Thermal conductivity

A

indicates the rate at which heat flows within a solid, such as soil.
It is determined by the inherent properties of the substance, as well as the temperature gradient that exists between different parts of the substance.

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6
Q

latent heat transfer.

A

when water changes its state from liquid to vapour, it removes stored heat resulting cooler surface, a process know as latent heat transfer.
This is the latent heat of vaporization

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7
Q

latent heat of condensation.

A

When water condenses at a surface, an equivalent amount of energy is released, warming the surface

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