XV. Basic Concepts Flashcards

1
Q

It is the lowermost layer of the atmosphere. The temperature here decreases with an increase in altitude. It is in this layer that essentially all important weather phenomena occur.

A

Troposphere

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2
Q

The term used to describe the temperature decrease in the troposphere.

A

Environmental lapse rate

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3
Q

It is the average value of Environmental lapse rate.

A

6.5°C per kilometer

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4
Q

It is an instrument package that is attached to a balloon and transmits data by radio as it ascends through the atmosphere.

A

Radiosonde

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5
Q

These are found aloft in tropics and not at the poles.

A

Lowest tropospheric temperatures

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6
Q

It is the boundary between the troposphere and the stratosphere

A

Tropopause

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7
Q

It is the second layer of the atmosphere above the troposphere. The temperature at first remains nearly constant to a height of about 20 kilometers before it begins a sharp increase that continues until the stratopause is encountered.

A

Stratosphere

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8
Q

This is the layer where ozone is located.

A

Stratosphere

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9
Q

It is the layer in the stratosphere that absorbs a portion of the radiation from the sun, preventing it from reaching the planet’s surface.

A

Ozone layer

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10
Q

It is the height of Ozone layer above the Earth’s surface.

A

15-30km

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11
Q

It is the boundary between the stratosphere and mesosphere.

A

Stratopause

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12
Q

It is the 3rd layer above the Earth’s surface. The temperatures again decrease with height until at the mesopause, some 80 kilometers above the surface.

A

Mesosphere

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13
Q

It is the average temperature of Mesosphere.

A

-90°C (-130°F)

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14
Q

It is the boundary between mesosphere and thermosphere. The coldest temperatures anywhere in the atmosphere occur at this boundary.

A

Mesopause

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15
Q

It is the fourth layer extends outward from the mesopause and has no well-defined upper limit. It is a layer that contains only a tiny fraction of the atmosphere’s mass. The temperatures again increase, due to the absorption of very shortwave, high-energy solar radiation by atoms of oxygen and nitrogen.

A

Thermosphere

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16
Q

The temperatures in Thermosphere may rise to these extremely high value.

A

More than 1000°C (1800°F)

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17
Q

It extendes from Earth’s surface to an altitude of about 80 kilometers (50 miles). The makeup of the air in this layer is uniform in terms of the proportions of its component gases.

A

Homosphere

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18
Q

It is the very thin atmosphere above 80 kilometers is not uniform, because it has a heterogeneous composition. Here the gases are arranged into four roughly spherical shells, each with a distinctive composition. Lowest layer to highest layer composition: molecular nitrogen (N2) < Oxygen (O) < Helium (He) < Hydrogen (H).

A

Heterosphere

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19
Q

It is the heaviest gas in the atmosphere, that’s why it was in the lowermost layer of the heterosphere.

A

Molecular Nitrogen (N2)

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20
Q

It is the lightest gas, that’s why it is the outermost/highest layer.

A

Hydrogen (H)

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21
Q

It is an electrically charged layer. It is located in the altitude range between 80 to 400 kilometers. It coincides with the lower portions of the thermosphere and heterosphere. The molecules of nitrogen and atoms of oxygen are readily ionized as they absorb high-energy shortwave solar energy. Positively charged ions and negative electrons are most dense in the range of 80 to 400 kilometers, but they can occur as high as 1000 km and as low as 50 km.

A

Ionosphere

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22
Q

It is the layer where Auroras can be found.

A

Ionosphere

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23
Q

It is also called the Northern Lights.

A

Aurora borealis

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24
Q

It is also called the Southern Lights.

A

Aurora australis

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25
Q

It is the scientific study of the atmosphere.

A

Meteorology

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26
Q

It refers to the state of the atmosphere at a given time and place.

A

Weather

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27
Q

It is the weather conditions prevailing in an area in general or over a long period.

A

Climate

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28
Q

It was taken when the Apollo 8 astronauts orbited the Moon for the first time in December 1968.

A

Earthrise

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29
Q

They took the photo of Earthrise in December 1968.

A

Apollo 8

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30
Q

It was taken in December 1972 by the crew of Apollo 17 during the last manned lunar mission.

A

Blue Marble

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31
Q

They took the photo of the Blue Marble in December 1972

A

Apollo 17

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32
Q

It a common boundary where different parts of a system interact.

A

Interface

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33
Q

It is the spinning of Earth on its axis that produces the daily cycle of day and night.

A

Rotation

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34
Q

It refers to Earth’s movement in a slightly elliptical orbit around the Sun.

A

Revolution

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35
Q

It is the distance where the Earth is closest from the Sun

A

Perihelion

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36
Q

Each year, on this day, our planet is about 147.3 million km away from the Sun.

A

January 3

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37
Q

It is the distance where the Earth is farthest from the Sun.

A

Aphelion

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38
Q

Each year, on this day, Earth is about 152.1 million km away from the Sun.

A

July 4

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39
Q

It is the plane of Earth’s orbit around the Sun.

A

Plane of the ecliptic

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40
Q

The inclination of Earth from it’s plane of ecliptic.

A

Inclination of the axis

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41
Q

It is the value of Earth’s tilt.

A

23.5 degrees

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42
Q

“It is the first ““official”” day of summer (Northern Hemisphere). The vertical rays of the Sun strike 23 1/2° north latitude.”

A

Summer solstice

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43
Q

The day in the year that Summer solstice will occur.

A

June 21 or 22

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44
Q

It is the 23 1/2° north latitude located in Northern Hemisphere.

A

Tropic of Cancer

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45
Q

It is the first day of winter in Northern Hemisphere.

A

Winter solstice

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46
Q

The day in the year that Winter solstice will occur.

A

December 21 or 22

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47
Q

It occurs on September 22 or 23 in the Northern Hemisphere.

A

Autumnal (fall) equinox

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48
Q

It occurs on march 21 or 22 in the Northern Hemisphere.

A

Spring (vernal) equinox

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49
Q

It is the boundary separating the dark half of Earth from the lighted half

A

Circle of illumination

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50
Q

It is a measure of the average kinetic energy of the atoms or molecules in a substance.

A

Temperature

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51
Q

It is the energy absorbed by the escaping water vapor molecules

A

Latent heat

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52
Q

It is the heat we can feel and measure with a thermometer

A

Sensible heat

53
Q

It is the annual balance of incoming and outgoing radiation

A

Heat budget

54
Q

It is a natural phenomenon that makes Earth habitable.

A

Greenhouse effect

55
Q

These clouds are high, white, and thin. They form delicate veil-like patches or wisplike strands and often have a feathery appearance.

56
Q

They consist of globular cloud masses that are often described as cottonlike in appearance. Normally, cumulus clouds exhibit a flat base and appear as rising domes or towers.

57
Q

They are best described as sheets or layers (strata) that cover much or all of the sky. Although there may be minor breaks, there are no distinct individual cloud units.

58
Q

“Thin, delicate, fibrous, ice-crystal clouds. Sometimes appear as hooked filaments called ““mares’ tails”” or cirrus uncinus.”

59
Q

Thin sheet of white, ice-crystal clouds that may give the sky a milky look. Sometimes produce halos around the Sun and Moon.

A

Cirrostratus

60
Q

“Thin, white, ice-crystal clouds. In the form of ripples or waves, or globular masses all in a row. May produce a ““mackerel sky.”” Least common of high clouds.”

A

Cirrocumulus

61
Q

“White to gray clouds, often made up of separate globules; ““sheepback”” clouds”

A

Altocumulus

62
Q

“Stratified veil of clouds that is generally thin and may produce very light precipitation. When thin, the Sun or Moon may be visible as a ““bright spot,”” but no halos are produced.”

A

Altostratus

63
Q

Low uniform layer resembling fog but not resting on the ground. May produce drizzle.

64
Q

Soft, gray clouds in globular patches or rolls. Rolls may join together to make a continuous cloud.

A

Stratocumulus

65
Q

Amorphous layer of dark gray clouds. One of the primary precipitation producing clouds.

A

Nimbostratus

66
Q

Dense, billowy clouds often characterized by flat bases. May occur as isolated clouds or closely packed.

67
Q

“These are cumuliform clouds with little vertical extent, common in the summer, that are often referred to as ““fair weather cumulus”””

A

Cumulus humilis

68
Q

It is a low to middle level cloud with some vertical extent of the genus cumulus, larger in vertical development than Cumulus humilis.

A

Cumulus mediocris

69
Q

When the top of the cumulus resembles the head of a cauliflower, it is called cumulus congestus or towering cumulus.

A

Cumulus congestus

70
Q

“Towering cloud, sometimes spreading out on top to form an ““anvil head.”” Associated with heavy rainfall, thunder, lightning, hail, and tornadoes”

A

Cumulonimbus

71
Q

It is a cloud with its base at or very near the ground.

72
Q

These are clouds above 6000 meters.

A

High clouds

73
Q

These are clouds 2000-6000 meters high.

A

Middle clouds

74
Q

These are clouds below 2000 meters high.

A

Low clouds

75
Q

Generally produced by nimbostratus or cumulonimbus clouds. When heavy, size can be highly variable from one place to another. (0.5-5 mm)

76
Q

Small, uniform droplets that fall from stratus clouds, generally for several hours. (<0.5 mm)

77
Q

Droplets large enough to be felt on the face when air is moving 1 meter/second. Associated with stratus clouds. (0.005-0.05 mm)

78
Q

Small, spherical to lumpy ice particles that form when raindrops freeze while falling through a layer of subfreezing air. Because the ice particles are small, any damage is generally minor. It can make travel hazardous. (0.5-5 mm)

79
Q

Produced when supercooled raindrops freeze on contact with solid objects. It can form a thick coating of ice that has sufficient weight to seriously damage trees and power lines. (Layers 1 mm-2 cm thick)

A

Freezing Rain (Glaze)

80
Q

Deposits usually consisting of ice feathers that point into the wind. These delicate frostlike accumulations form as supercooled cloud or fog droplets encounter objects and freeze on contact. (Variable accumulations)

81
Q

The crystalline nature of snow allows it to assume many shapes, including six-sided crystals, plates, and needles. Produced in supercooled clouds where water vapor is deposited as ice crystals that remain frozen during their descent. (1 mm-2 cm)

82
Q

Precipitation in the form of hard, rounded pellets or irregular lumps of ice. Produced in large convective, cumulonimbus clouds, where frozen ice particles and supercooled water coexist. (5-10 cm or larger)

83
Q

”"”Soft hail”” that forms as rime collects on snow crystals to produce irregular masses of ““soft”” ice. Because these particles are softer than hailstones, they normally flatten out upon impact. (2-5 mm)”

84
Q

These are zones between the equator and roughly 30° latitude north and south. These are the low-latitude overturning circulations that have air rising at the equator and air sinking at roughly 30° latitude.

A

Hadley Cell

85
Q

These are regions located at about 30 degrees north and south of the equator. These latitudes are characterized by calm winds and little precipitation. The horse latitudes are located at about 30 degrees north and south of the equator.

A

Horse latitudes

86
Q

“These are the permanent east-to-west prevailing winds that flow in the Earth’s equatorial region. These are also called ““Easterlies”””

A

Trade winds

87
Q

It is the low-pressure zone. This region of ascending moist, hot air is marked by abundant precipitation. It is visible as a band of clouds near the equator.

A

Doldrums, equatorial low or Intertropical Convergence Zone (ITCZ)

88
Q

It is the circulation between 30° and 60° latitude, both Northern and Southern Hemisphere. It is the average motion of air in the mid-latitudes.

A

Ferrel Cell

89
Q

These are prevailing winds that blow from the west at midlatitudes.

A

Westerlies

90
Q

These are relatively narrow bands of strong wind in the upper levels of the atmosphere.

A

Jet streams

91
Q

It is the smallest and weakest cell. It extend from between 60 and 70 degrees, both Northern and Southern Hemisphere, to the poles.

A

Polar Cell

92
Q

These are the dry, cold prevailing winds that blow around the high-pressure areas of the polar highs at the North and South Poles.

A

Polar eaterlies

93
Q

These are the high-pressure zones. In these zones, a subsiding air column produces weather that is normally warm and dry. It is located in the belts about 20° to 35° on either side of the equator, where the westerlies and trade winds originate and go their separate ways.

A

Subtropical highs

94
Q

It is a low-pressure region is situated at about 50° to 60° latitude, in a position corresponding to the polar front. It is a low-pressure convergence zone where the polar easterlies and the westerlies clash. This zone is responsible for much of the stormy weather in the middle latitudes, particularly in the winter.

A

Subpolar low

95
Q

These are areas of high atmospheric pressure around the north and south poles. It exhibit high surface pressure mainly because of surface cooling.

A

Polar highs

96
Q

It refers to a particular wind system that reverses its direction twice each year geostrophic wind. It is the wind that will be blowing parallel to the isobars, when Coriolis force is balanced by the pressure gradient force.

97
Q

It is the boundary between the polar cell and the Ferrel cell around the 60° latitude in each hemisphere.

A

Polar front

98
Q

“It is a belt of powerful upper-level winds that sits atop the polar front. It is also known as ““midlatitude jet stream”””

A

Polar jet stream

99
Q

It is a belt of strong upper-level winds lying above regions of subtropical high pressure. It is a semi permanent jet over the subtropics.

A

Subtropical jet stream

100
Q

It is a climate pattern that describes the unusual warming of surface waters in the eastern tropical Pacific Ocean.

101
Q

It refers to the large-scale cooling of the ocean surface temperatures in the central and eastern equatorial Pacific Ocean.

102
Q

These are tiny solid and liquid particles suspended in the atmosphere.

103
Q

It is amixture of many discrete gases, of which nitrogen and oxygen are most abundant, in which varying quantities of tiny solid and liquid particles are suspended.

104
Q

It is the force exerted by the weight of a column of air above a given point.

A

Air pressure

105
Q

It is the reflectivity of a substance, usually expressed as a percentage of the incident radiation reflected.

106
Q

It is a large cell of low pressure centered over the Aleutian Islands of the North Pacific during the winter.

A

Aleutian Low

107
Q

It is a violent and extremely cold wind, laden with dry snow picked up from the ground

108
Q

The discontinuity at the forward edge of an advancing cold air mass that is displacing warmer air in its path.

A

Cold Front

109
Q

It is a bright, whitish disk centered on the Moon or Sun that results from diffraction when the objects are veiled by a thin cloud layer.

110
Q

It is an area of low atmospheric pressure characterized by rotating and converging winds and ascending air.

111
Q

It is the separation of colors by refraction.

A

Dispersion

112
Q

It is a large cell of low pressure centered over Iceland and southern Greenland in the North Atlantic during the winter.

A

Icelandic Low

113
Q

It is the flow of cold, dense air downslope under the influence of gravity; the direction of this wind’s flow is controlled largely by topography.

A

Katabatic Wind

114
Q

It is an optical effect of the atmosphere caused by refraction in which the image of an object appears displaced from its true position.

115
Q

It is the permanent freezing of the subsoil in tundra regions.

A

Permafrost

116
Q

It is a luminous arc formed by the refraction and reflection of light in drops of water.

117
Q

It is a dry area on the lee side of a mountainrange.

A

Rain Shadow Desert

118
Q

These are shafts of light caused by reflection from ice crystals that extend upward or, less commonly, downward from the Sun when the Sun is near the horizon.

A

Sun Pillar

119
Q

It is the northern coniferous forest; also a name applied to the subarctic climate.

120
Q

It is the sound emitted by rapidly expanding gases along the channel of a lightning discharge.

121
Q

It is a violently rotating column of air attended by a funnelshaped or tubular cloud extending downward from a cumulonimbus cloud.

122
Q

It is the release of water vapor to the atmosphere by plants.

A

Transpiration

123
Q

The parallel of latitude, 23 1/2° north latitude, marking the northern limit of the Sun’s vertical rays.

A

Tropic of Cancer

124
Q

The parallel of latitude, 23 1/2° south latitude, marking the southern limit of the Sun’s vertical rays.

A

Tropic of Capricorn

125
Q

It is a luxuriant broadleaf evergreen forest; also the name given the climate associated with this vegetation.

A

Tropical Rain Forest

126
Q

It is a climate found almost exclusively in the Northern Hemisphere and at high altitudes in many mountainous regions. It is a treeless climatic realm of sedges, grasses, mosses, and lichens dominated by a long, bitterly cold winter.

127
Q

It is the discontinuity at the forward edge of an advancing warm air mass that displaces cooler air in its path.

A

Warm Front

128
Q

It is the air flowing horizontally with respect to Earth’s surface.