Chapter 2: Energy Flashcards

1
Q

Define ‘Albedo’.

A

The reflectivity of the surface of a planet.

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2
Q

Define ‘Blackbody radiator’.

A

A (hypothetical) perfect radiator of light that absorbs all light that strikes it and reflects none; its light output depends only on its temperature.

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3
Q

Define ‘Celsius temperature scale’.

A

The temperature scale in which the zero reference point is the freezing temperature of water at surface atmospheric pressure and the boiling point of water is assigned a temperature of 100 degrees Celsius.

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4
Q

Define ‘Conduction’.

A

The means by which heat is transmitted through solids without deforming the solids. Moves from one object to an adjacent object through the transfer of kinetic energy.

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5
Q

Define ‘Convection’.

A

The process by which hot, less dense materials rise upwards, being replaced by cold, dense, downward flowing material to create a convection current.

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6
Q

Define ‘Degradation (of energy)’.

A

The transformation of energy into a form that is less useful, or less available for work.

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7
Q

Define ‘Electromagnetic radiation’.

A

A self-propagating electric and magnetic wave, such as light, radio, UV, or infrared radiation; all types travel at the same speed and differ in wavelength or frequency, which relates to the energy.

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8
Q

Define ‘Energy’. How can it be added/removed from a system?

A

The capacity to do work. It can be added/removed typically by work done to or by the system, or by heat flow.

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9
Q

Define ‘Energy cycle’.

A

The flow of energy from the external and internal sources of the planet, that drives the cycles of the Earth system.

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10
Q

Define ‘Entropy’.

A

A measure of disorganization. Entropy increases as the usefulness/ability to do work decreases. Absolute zero K would hypothetically result in zero entropy.

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11
Q

Define ‘Fission’.

A

Controlled radioactive transformation.

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12
Q

Define ‘Fusion (of nuclei)’.

A

The merging of the nuclei of lightweight chemical elements, particularly H, to form heavier elements such as He and C.

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13
Q

Define ‘Geothermal gradient’.

A

The rate of increase of temperature downward in the Earth. It varies from site to site and is less pronounced under the continents than under ocean basics, where the crust is thinner.

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14
Q

Define ‘Gradients’.

A

A measure of the vertical drop over a given horizontal distance. (Definition in back of book, perhaps not appropriate to chapter)
Alternatively, the flow of something down a gradient from higher concentration to low.

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15
Q

Define ‘Gravity’.

A

The mutual physical attraction between any two masses, such as Earth and the Moon.

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16
Q

Define ‘Greenhouse effect’.

A

The property of the Earth’s atmosphere by which long wavelength heat rays from the Earth’s surface are trapped or reflected back by the atmosphere.

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17
Q

Define ‘Heat’.

A

Al so known as thermal energy. The energy of a body due to the motions of its atoms. Temperature is the measure of that motion.

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18
Q

Define ‘Kelvin temperature scale’.

A

The absolute temperature scale in which the foundation is the point where entropy is zero.

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19
Q

Define ‘Kinetic energy’.

A

Energy that is expressed in the movement of matter.

20
Q

Define ‘Luminosity’.

A

The total amount of energy radiated outward each second by the Sun or any other star.

21
Q

Define ‘Potential energy’.

A

The energy stored in a system.

22
Q

Define ‘Power’.

A

The amount of work done per unit time.

23
Q

Define ‘Radiation’.

A

Transmission of heat energy through the passage of electromagnetic waves.

24
Q

Define ‘Radiatively active gas’.

A

Gases in the lower part of the atmosphere that absorb outgoing radiation, thus preventing the radiactive loss of heat.

25
Q

Define ‘Radiogenic heat’.

A

Heat energy produced by the spontaneous breakdown, or decay, of radioactive elements.

26
Q

Define ‘Reflection’.

A

The bouncing of a wave off the surface between two media.

27
Q

Define ‘Spectrum’.

A

A group of electromagnetic rays arranged in order of increasing or decreasing wavelength.

28
Q

Define ‘Star’.

A

A large spherical mass of ionized gas that radiates heat as a result of thermonuclear reactions in its core.

29
Q

Define ‘Stratospheric ozone layer’.

A

The region of the stratosphere within which ozone (O3) absorbs radiation in the short-wavelength region of the electromagnetic radiation spectrum.

30
Q

Define ‘Temperature’.

A

A measure of the average kinetic energy of all the atoms in a body. A measure of heat/thermal energy.

31
Q

Define ‘Terrestrial energy’.

A

Also known as Geothermal energy, it is heat energy drawn from the Earth’s internal heat.

32
Q

Define ‘Tide’.

A

The twice-daily rise and fall of the ocean surface resulting from the gravitation attraction of the Moon and Sun.

33
Q

Define ‘Work’.

A

The addition or subtraction to the internal energy of a system.

34
Q

Define ‘Thermodynamics’. What are the three laws?

A

The set of natural laws that govern the transfer of energy from one body to another.

  1. In a system of constant mass, the energy involved in any physical or chemical change is neither created nor destroyed, but merely changed from one form to another.
  2. Energy always changes from a more useful, more concentrated for to a less useful, less concentrated form.
  3. Postulates the existence of the state of absolute zero, in which all molecular motion would cease and entropy would disappear.
35
Q

What are some forms of energy?

A

Thermal, chemical, nuclear, mechanical, gravitational, radiant or electromagnetic, electrical, sound, and motion.

36
Q

What are the three fundamental mechanisms of heat transfer?

A

Conduction, convection, and radiation.

37
Q

The Sun is a star, in which nucleosynthesis occurs by fusion. The Sun produces most of its energy by thermo- nuclear reactions in which hydrogen protons fuse to form helium. During the fusion process, some mass is converted to energy. Each individual fusion reaction produces only a tiny amount of energy, but such an enormous amount of hydrogen fuel is continuously converted to helium that the Sun’s overall luminosity is huge. Only a tiny fraction of the total energy emitted by the Sun reaches Earth; even so, a __ percent increase or decrease would have a significant impact on climate.

A

1 %. In text says 1 K.

38
Q

What are the equations used to describe light and what are the types of radiation in the electromagnetic spectrum?

A

c=(frequency)(gamma) and E=h(frequency)

Radio->Infrared->Visible->UV->X-ray->Gamma

39
Q

What are the six layers of the Sun?

A

The Sun has six concentric layers: the core, in which the nuclear fusion reactions occur; the radiative layer, across which energy from the core moves by radiation; the convective layer, across which energy moves by convection; the photosphere, an intensely turbulent zone which emits the light that reaches Earth; the chromosphere, a transparent, low-density layer of very hot gas; and the corona, a zone of even lower density gas than the chromosphere.

40
Q

The Sun’s spectral curve matches that of a blackbody radiator emitting at __, the average temperature of the photosphere. The peak is at a wavelength of __, in the visible part of the electromagnetic spectrum. Gases in Earth’s atmosphere selectively absorb some wavelengths from the solar radiation as it passes through on its way to the surface. Notably, ozone absorbs radiation in the very short- wavelength, ultraviolet portions of the spectrum.

A

5800 K

5x10^-7 m

41
Q

What is the temperature of Earth’s core?

A

~5000 degrees Celsius.

42
Q

Heat flow from the interior to the surface is greatest in locations with volcanic activity. Heat reaches the bottom of the lithosphere primarily by ___, and passes through the lithosphere primarily by __. Slow convection currents of solid rock deep in Earth’s interior provide the driving force behind plate tectonics, in addition to generating volcanic eruptions.

A

convection

conduction

43
Q

What are some of the sources of Earth’s internal energy?

A

Radiogenic heat from the spontaneous decay of naturally occurring radioactive elements; accretionary heat from the collision and accretion of particles during the formation of Earth; tidal heat generated by the distortions of body tides; and gravitational and latent heat of crystallization associated with core formation.

44
Q

The total amount of energy flowing into Earth’s energy budget is more than 174,000 terawatts (or 174,000 1012 watts). Solar radiation dominates the flow of energy into Earth’s energy budget, at __ percent of the total. The second most powerful source, at 23 terawatts or ___ percent of the total, is Earth’s internal heat energy. Tidal energy accounts for approximately 3 terawatts, or ___ percent of the total.

A
  1. 985 %
  2. 013 %
  3. 002 %
45
Q

About ___ percent of incoming solar radiation is reflected back to space as a result of the planet’s albedo.

A

40 %

46
Q

Earth, a lower-temperature radiator than the Sun, has a peak at a wavelength of ___, in the infrared part of the electromagnetic spectrum. Earth’s outgoing radiation is selectively absorbed by radiatively active gases, notably water vapor and carbon dioxide. This causes the greenhouse effect, in which some outgoing radiation from the thermal portion of the spectrum is retained near the surface, forming a “blanketing” layer of warmed air.

A

1x10^-5 m

47
Q

What are some energy sources used by humans and where do they come from?

A

Fossil fuels, by far the main source of energy for modern industrial society, come from the ancient remains of plants and animals; they are an expression of stored solar energy. Wind energy, wave energy, and biomass energy are also secondary expressions of solar radiation. Geothermal energy comes from Earth’s internal heat sources. Tidal and hydroelectric energy come from the kinetic energy of water. Nuclear energy is produced by controlled fission of radioactive isotopes.