Atmosphere Flashcards

1
Q

Earth’s axis of rotation and the plane of ecliptic are…

A

parallel

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2
Q

axial tilt

A

angle of Earth’s axis of rotation

  • relative to the normal to the orbital plane
  • 23.4 degrees
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3
Q

obliquity (of tilt)

A
  • change in axial tilt
  • 22 to 24.5 degrees
  • period of 41 000 years
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4
Q

axial precission

A

wobbling caused by gravitational attraction

  • gravitational attraction from Sun and Moon
  • period of 100 000 years
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5
Q

Aphelion

A
  • furthest from the sun (Summer in NH)

- July 4

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6
Q

Periphelion

A
  • closest to sun (Winter NH)

- Jan 4

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7
Q

Earth’s Oscillation Period and Shape

A
  • oscillates between circle and ellipse

- period of 100 000 years

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8
Q

Earth’s Atmosphere Size

A

480 km

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9
Q

Atmosphere Formation

A
  • planet cooled at surface
  • dense material went to the center
  • lighter materials flowed to top -> created layers
  • gases from inside out gassed the atmosphere (volcanic eruptions and collisions)
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10
Q

Volcanic Outgassing

A
  • lots of water (50-60%)
  • quarter CO2 (24%)
  • sulfur, 13% etc.
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11
Q

Formation of the Ozone

A
  • O2 is produced, UV radiation splits to create ozone (O3)

- ozone layer also created (UV shield)

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12
Q

Main Reason for Seasons:

A

tilt!!

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13
Q

Modern Atmosphere Composition

A

-70% N2
-21% Oxygen
-Ar 1%
-CO2 0.04%
….

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14
Q

Thermosphere

A
  • 80 - 550 km
  • N, O, and smaller particles in Ionosphere absorb radiation from the sun
  • become electrically charged
  • absorbs cosmic rays (gamma, x, shorter)
  • gases are layered by weight (gravity)
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15
Q

Lower layers of Thermosphere

A
  • 0-80 km
  • chemically uniform mix of gases
  • absorbs UV rays
  • H20y variations near surface
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16
Q

Density of Atmosphere

A
  • density and pressure DECREASES with altitude
  • troposphere contains 90% of mass
  • above 50 km. 0.001% of mass
17
Q

Heterosphere (80-?)

A
  • 80 km to 500 km
  • 0.001% of mass
  • distinct layers of gas due to gravity
18
Q

Homosphere

A
  • 0 km to 80 km
  • uniformly mixed
  • ozone layer
19
Q

Thermosphere (temperature)

A
  • 80 km to 480 km (thermopause)
  • temperature INCREASES with altitude
  • no heat conduction, high energy solar radiation
20
Q

Mesosphere (temperature)

A
  • 50 km to 80 km

- temperature DECREASES with altitude (-90 C)

21
Q

Stratosphere (temperature)

A
  • 18 km to 50 km
  • temperature INCREASES with altitude
  • from -57 C to 0 C at stratopause
  • absorption of UV by ozone
22
Q

Troposphere (temperature)

A
  • surface to 18 km
  • decreases with altitude
  • normal lapse rate of 6.5 degrees C /km