Temperature and Heat Flashcards

1
Q

what is temperature?

A
  • a measure of the average velocity of molecules
  • a measure of the potential heat exchange between objects
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2
Q

what is the molecular motion for solids, liquids, and gases/space

A

solids - vibration
liquids - rotation
translation - free movement through space

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3
Q

the higher the temp, the more/less heat being exchanged between objects

A

more

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4
Q

what is heat?

A
  • form of energy capable of being transferred between systems
  • the total molecular motion of a substance
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5
Q

what are the heat transfer mechanisms?

A

conduction - solids
convection - liquids, gases
radiation - needs no medium

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6
Q

What are the temperature scales

A
  • Fahrenheit
    32° = freezing
    212° = boiling
  • Celsius
    0° = freezing
    100° = boiling
  • Kelvin
    0 means absolute zero
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7
Q

How to find temp stats - daily mean, daily range, monthly mean, yearly mean, annual range

A
  • daily mean = (min+max)/2
  • daily range = high - low
  • monthly mean = average of daily means
  • yearly mean = average of monthly means
  • annual range = mean of warmest - coldest month
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8
Q

What are first-order weather stations and how do we fill in the gaps?

A
  • stations that are monitored 24/7 by trained, certified observers (about 270 in US)
  • fill in the gaps with Cooperative Observer Program (COOP)
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9
Q

What are daily temperature cycles governed by and when do the daily highs and lows occur?

A
  • governed by radiation cycles, clouds, moisture, transient air masses
  • daily low usually near sunrise
  • daily high usually mid afternoon
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10
Q

What is the Environmental Temperature Lapse Rate (ELR)?

A

the average lapse rate (6.4°C/1000m)

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11
Q

why is it cooler at night?

A
  1. lower atmospheric pressure
    - gases expand at lower temps
    - as gas expands, molecules and atoms within it more slowly
    - since air temp is just a measure of how fast the molecules in air are moving, the rate of motion is lower
  2. heating takes place at the bottom of the troposphere
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12
Q

what is a temperature inversion?

A

when temperature increases with height
- usually returns to lapse rate after a few hundred feet

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13
Q

what causes temperature inversions?

A
  • normal radiational cooling (on a calm, clear night)
  • cold air drainage
    -synoptic conditions
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14
Q

what are synoptic conditions?

A

the large-scale, general weather patterns and atmospheric conditions over a region

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15
Q

what is the issue with temperature inversions? two examples

A
  • pollution can be trapped
  • Great London Smog and Donora, PA
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15
Q

How does climate change impact temperature inversions?

A

by altering temperature patterns, circulation, and the frequency of extreme weather events

15
Q

what is Q*?

A

net radiation

15
Q

Why is there differential heating of land and water? Which cools faster?

A
  • land warms/cools more rapidly than water
  • land is opaque, no mixing between layers, lower specific heat, and most of the net radiation is used for sensible heat
  • ocean is transparent, there is mixing between layers, higher specific heat, most net radiation used for latent heat transfer
16
Q

what is latent heat?

A

energy gained or lost when a substance changes from one state to another (e.g. when a pot of water is kept boiling, the temperature remains at 100 °C (212 °F) until the last drop evaporates, because all the heat being added to the liquid is absorbed as latent heat of vaporization and carried away by the escaping vapor molecules)

17
Q

what is specific heat?

A

the heat capacity of a substance
- specific heat of water is 5x greater than land’s

18
Q

what is sensible heat?

A

the heat that causes a change in temp of a substance but does not change its phase (e.g. warms water, doesn’t melt ice)