Climate Vocab Exam Flashcards

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1
Q

Coriolis Force

A

Causes moving objects to be deflected to the right in the Northern hemisphere, and to the left in the southern hemisphere.

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2
Q

Hygrometer

A

An instrument for measuring atmospheric humidity.

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3
Q

Intertropical Convergence Zone (ITCZ)

A

Three - dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator.

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4
Q

Humidity

A

Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humiditiy is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air. Humidity is the amount of water held in the air.

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5
Q

Continental Tropical Air Mass (CT)

A

A Dry hot air mass in the Summer, and a warm and dry air mass in the winter. A dry hot air mass in the Summer, and a warm and dry air mass in the winter. A Dry hot air mass in the Summer, and a warm and dry air mass in the winter.

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6
Q

Convectional Precipitation

A

It is the type of rain that forms going straight up, and comes straight down. Convectional Precipitation is the type of precipitation that forms going straight up, and comes straight down. Convectional precipitation is the formation of precipitation due to the surface heating an air mass at the ground surface. Convectional Precipitation is the formationof precipitation due to the surface heating of an air mass directly at surface level. Convectional Precipitation is the heating of an air mass directly at surface level. Convectional Precipitation is the surface directly heating the air mass on the surface.

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7
Q

Anticyclone

A

An anti - cyclone High pressure system that rotates in a counter clockwise direction. An Anti Cyclone resembles good weather. An anti - cyclone High pressure system rotates in a counter clockwise direction. An Anti Cyclone resembles good weather. An anti - cyclone High pressure system rotates in a counter clockwise direction. An Anti Cyclone resembles good weather. An anti - cyclone High pressure system rotates counter clockwise. A High Pressure System is good weather.

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8
Q

Hadley Cell

A

Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator. Three dimensional atmospheric air circulation located at roughly 0 to 30 degrees North and South of the Equator.

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9
Q

Isotherm

A

Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure. Isotherm is lines on a map joining equal pressure.

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10
Q

Condensation Nuclei

A

Microscopic particle of dust, smoke or salt that allows for condensation of water vapor to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapor to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapor to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapor to water droplets.

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11
Q

Convergence

A

The Converging of wind horizontally. After this clashing, the wind is then pushed upwards (vertically).

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12
Q

Jet Stream

A

Relatively fast uniform winds concentrated within the upper atmosphere in a narrow band. Relatively fast uniform winds concentrated within the upper atmosphere in a narrow band. Relatively fast uniform winds concentrated within the

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13
Q

Air Pressure

A

Air Pressure is the Atmospheric weight of the air. Air weight is the Atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air. Air Pressure is the atmospheric weight of the air.

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14
Q

Albedo

A

The reflective ability of sunlight. This depends on color and texture. The reflective ability of sunlight. This depends on color and texture. The reflective ability of sunlight. This depends on color and texture. The reflective ability of sunlight. This depends on color and texture. The reflective ability of sunlight. This depends on color and texture.

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15
Q

Climate Controls

A

Macro Scale (Worldwide) forces that affect local weather and climate. Macro Scale (Worldwide) forces that affect local weather and climate. Macro Scale (Worldwide) forces that affect local weather and Climate. Macro Scale (Worldwide) forces that affect local weather and Climate, Macro Scale (Worldwide) forces that affect local weather and Climate. Macro Scale (Worldwide) forces that affect local weather and climate. Macro Scale (Worldwide) forces that affect local weather and climate. Macro Scale (Worldwide) forces that affect local weather and climate.

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16
Q

Climograph

A

A Climograph is a visual representation of annual precipitation and temperatures values at X. A Climograph is a visual representation of annual precipitation and temperatures

17
Q

Doldrums

A

Dolrums means light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light to “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums means Light “no wind” conditions found at the Thermal Equator. Doldrums mean Light “no wind” conditions found at the Thermal Equator. Doldrums mean Light “no wind” conditions found at the Thermal Equator.

18
Q

Air Mass

A

Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets. Microscopic particle of dust, smoke or salt that allows for condensation of water vapour to water droplets.

19
Q

Gulf Stream

A

The Gulf Stream is the warm current that warms northern Europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern Europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe. The Gulf Stream is the warm current that warms northern europe.

20
Q

Latent Heat

A

Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapur turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain. Latent Heat is released when vapour turns into rain.

21
Q

Rossby Wave

A

The Southward Passage of the Polar Jet Stream. The Rossby Wave is the southward passage of the Polar Jet Stream. The Rossby Wave is the Southward Passage of the Polar Jet Stream. The Rossby Wave is the Southward Passage of the Polar Jet Stream. The Rossby Wave is the Southward Passage of the Polar Jet Stream. The Rossby Wave is the Southward Passage of the Polar Jet Stream. The Rossby Wave is the southward passage of the Polar Jet Stream. The Rossby Wave is the southward passage of the Polar Jet Stream. The Rossby Wave is the southward passage of the Polar Jet Stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream. The Rossby Wave is the southward passage of the polar jet stream.