Temperature Flashcards

1
Q

C to F

A

C= 5/9 ( F-32 )

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2
Q

Stevenson screen

What it measures
Height above ground

A

Temp and humidity

1-2m above ground

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3
Q

Radiosonde

What it measures

A

Temp Humidity Pressure

Gps–> wind

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4
Q

Conduction

A

Transfers of energy with contact

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5
Q

Atmosphere heating

A

Sun heats the ground, ground heats the atmosphere

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6
Q

Convection

A

Vertical movement of air

Forced convection windward side
Rotors -> mechanical convection leeward side

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7
Q

Radiation

A

Short waves coming from sun

Ground radiates long waves

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8
Q

Latent heat

A

Melting. Evaporation
Ice Water Vapor
Freezing. Condensation

Left-right: absorption of heat, cooling surrounding

Ice to vapor, heat release temp rise
Vapor to ice, heat absorption, temp decreases

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9
Q

Advection

A

Horizontal movement of air

Wind

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10
Q

Insulation

A

Amount not of solar radiation absorbed per unit area

Equator more because more direct heating
Depends on season, time of the day and latitude

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11
Q

Earth Orbit and tilt

Tilt value
Specific date

A

23.5 inclination

Aphelion 4th of July, furthest 95M km
Perihelion 4th Jan, closest 91M km
Earth rotates at 50.04 degrees/ hour

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12
Q

4 seasons and declination

A

Winter solstice, 21st December, Earth tilts away
Spring equinox, 21st march
Summer solstice, 21st of June
Autumn equinox’ 23rd of September

Declination,angle of sun to the Earth Equator
0 declination: sun right above equator
23.5 max declination, tropic

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13
Q

Retaining heat

A

Heat is the amount of Energy to drive an activity
Calorie: 1 calories is the heat needed to rise 1g of water by 1C

Specific heat, amount of heat needed for same temperature rise
Rock 0.25
Ice: 0.5
Water :1

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14
Q

Diurnal variation or daily variation

Impact of wind

Impact of clouds

A

30 mins after sunrise = coldest
2 hours after local noon= hottest

Wind at night, not as cold
Wind during the day, not as hot

Cloud at night: temperature increases (blanket)
Cloud during the day: colder temperature

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15
Q

Types of temperature inversions

A

Ground inversion: ground cools faster than the air. Air in contact with the ground cools more rapidly, become colder than the layer above.

Valley inversion: flanks cool more rapidly, air sinks

Subsidence: air gets compressed and warms up

Frontal inversion: with the passage of a front

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16
Q

Clearing temperature inversions:

A

Surface heating

Wind