Global energy budget Flashcards

1
Q

Energy

A

Capacity to do work in the form of motion

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2
Q

Potential Energy

A

PE = massgravityheight
how much something has the potential to create energy

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3
Q

Kinetic Energy

A

K = 0.5(mass*velocity)^2
produced by body in motion

more mass + more velocity = more kinetic energy

atoms always moving

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4
Q

Temperature
definition

A

average speed of atoms or molecules in a substance
measure of kinetic energy

increase in temperatuer = hotter
colder = slower, vibrating, no velocity

Absolute zero theoretically no movement – rare on earth, if at all

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5
Q

Heat Transfer

A

when two substances have a temperature difference between them (difference in KE), heat will always move from warmer to colder object

conduciton
convection
radiation

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6
Q

Conduction

A

Energy transferred through direct contact

the greater the temperature difference, the faster the heat transfer
they vibrate faster

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7
Q

Convection

A

transfer of heat through the mass movement of a liquid or gas

increase in temperature –> increase in movement of molecules (they grow hotter, turn into gas)

less dense - light

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8
Q

Radiation

A

energy transmitted from one substance to another in waves / particles

absorbs into object, one loses energy, other gains energy

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9
Q

Electromagnetic Radiation

A

shorter wavelengths = more energy

all substances emit EMR,

objects produce one wavelength more than others (ex:color)

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10
Q

Stefan-Bloltzmann Law

A

As the temperature of an object increases, more total radiation is emitted each second (exponential)

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11
Q

Wien’s Law

A

As temperature of an object increases, the wavelength at which most of the energy is released will become shorter (more of it)

warmer object = more energy released = shorter wavelength

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12
Q

Solar Radiation

A

produced through nuclear fusion transferred through space
small portion hits earth as shortwave radiation, visible light

6000K

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12
Q

Radiative equilibrium temperature

A

difference in heat energy transferred to the planet and the heat energy lost,
determines the average temperature of Earth

this temperature is cooler than what it actually is

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13
Q

Terrestrial radiation

A

mainly emitted in Infrared
only 288K, not visible to the human eye

some not absorbed

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