TEMPERATURE DISTRIBUTION ON EARTH Flashcards by Naveen Kumar

Q

SEASONAL PATTERN

A

DIFFERRENTIATED AMOUNT OF SUNS ENERGY RECEIVED

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Q

RADIATION TRANSFER OF HEAT=———

A

DOESNT NEED MEDIUM

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Q

HEAT TRANFER FROM

A

WITHOUT CONTACT OR MOVEMENT

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Q

INSOLATION

A

SUN RADIATION RECEIVED

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Q

INSOLATION MEASURED

A

SOLAR ENERGY PER SQ CM PERMINUTE

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Q

EARTH RECEIVE—- WAVES

A

SHORTWAVES

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Q

SHORT WAVES

A

VISIBLE AND BELOW THAT

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Q

EARTH RELEASE

A

LONGWAVES

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Q

LONGWAVES

A

MOST INFRARED

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Q

INFRARED

A

USUALLY HEAT

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Q

CONDUCTION

A

MOLECULAR ACTIVITY CONDUCTION

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Q

CONVECTION

A

ACTUAL TRANSFER OF MATTER

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Q

HEAT FROM INTERIOR

A

VOLCANOES

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Q

OCEAN VOLCANO VENT USE

A

CHEMOSYNTHESIS BACTERIA

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Q

OCEAN DEPTH LIVES

A

CHEMOSYNTHESIS BACTERIA

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Q

SCATTERING PARTICLES

A

TOO SMALL

Q

TOO SMALL PARTICLES

A

SCATTER

Q

LARGE PARTICLES>WAVELENGTH

A

REFLECT

Q

DUST

A

REFLECT

Q

GASES

A

SCATTER

Q

ALBEDO

A

SUNLIGHT PROPORTION REFLECTED

Q

ALBEDO OF LAND

A

GREATER THAN SEA

Q

HIGHEST ALBEDO

A

SNOW

Q

LOWEST ALBEDOO

A

BLACK SOIL

SPECIFIC HEAT OF WATER

2.5 TIMES HIGHER THAN LANDMASS

WHY LAND HEATS AND COOLS FASTLY

AVG PENETRATION ONLY UPTO 1M

OCEAN DIURNAL AND ANNUAL TEMP

LOW

TEMP ANOMALY

TEMPERATURE DIFFERENCE BW PLACE AND PARALLEL LATITUDE

TEMPERATURE DIFFERENCE BW PLACE AND PARALLEL LATITUDE

TEMPERATURE ANOMALY

SUNLING SLOPE IN NH

SOUTHERN

SUNLIGHT SLOPE INSH

NORTHERN

SUN SLOPES ARE

DRY

SUN SLOPES ARE DRY BCZ

LOSS OF MOISTURE

SLOPES WITH SUNLIGHT AND IRRIGATION

DENSE HUMAN SETTLEMENT

WHY UK WAR

NORTH ATLANTIC DRIFT

NORMAL LAPSE RATE

1 C FOR EVERY 165 M