The Earth System Recap Flashcards

1
Q

What does the climate system refer to?

A

An interactive system consisting of the atmosphere, hydrosphere, cryosphere, the land surface and the biosphere.

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2
Q

What is the most unstable and rapidly changing part of the climate system?

A

The atmosphere

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3
Q

Atmospheric processes have a direct impact on human activities…

A

Agriculture, water resources, extreme weather events.

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4
Q

Humans have interacted with atmospheric processes by…

A

Changing land cover, burning fossil fuels and adding important trace gases.

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5
Q

Seasonal differences in climate across the globe are caused by…

A

The spherical shape of the Earth- large N-S temperature differences.
Tilt of the Earth’s axis of rotation (23.5o)

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6
Q

What are the seasons called?

A
September 23 (Autumnal Equinox)
June 22 (Summer Solstice)
March 21 (Vernal Equinox)
December 22 (Winter Solstice)
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7
Q

Wind systems- annual and seasonal variations are caused by…

A

Inequalities in the distribution of solar radiation over the Earth’s surface.
The Earth’s rotation.

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8
Q

Energy surplus at the equator and deficit at the poles leads to…

A

Heat transfers.

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9
Q

What is convection?

A

The dominant process for transferring heat upwards from the Earth’s surface.

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10
Q

What is adiabatic motion?

A

Temperature changes occur with vertical motions in the atmosphere

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11
Q

Why is the atmosphere continually turning?

A

Mass balance dictates that as some air masses rise some must also fall.

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12
Q

Where does atmospheric overturning occur?

A

In the troposhere

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13
Q

Over long timescales the complete Earth–atmosphere system is in thermal equilibrium

A

Heat energy is transferred from the tropics to poles by the north–south circulations in the atmosphere and oceans

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14
Q

What is the dry adiabatic lapse rate?

A

Rate of temperature fall with height in a rising parcel of air (9.8oC per km)

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15
Q

What is the saturated adiabatic lapse rate?

A

Lapse rate in the presence of condensation

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16
Q

What is the coriolis effect?

A
  • Air should move 90° to isobars but is deflected by the
    force of the Earths’ rotation
  • Observations show air flow is almost parallel to the
    isobars (except very near to the surface and at the
    equator)
17
Q

What are geostrophic winds?

A
  • Deflected winds >1km above the surface
  • Speed is proportional to pressure gradient and strength
    of coriolis effect
  • Airflow is anticlockwise around low pressure in the N
    hemisphere and the converse for the S hemisphere
18
Q

3-cell atmospheric circulation model in each hemisphere (controlled by a pressure
gradient force)

A

Hadley cell
Ferrel cell
Polar cell

19
Q

What are jet streams?

A

Fast-moving bands of air embedded in Rossby waves caused by sharp temperature differences (speeds up to 140 kms-1)

20
Q

What is the Subtropical westerly jet stream?

A

Poleward boundary of the tropical Hadley cell
Just below tropopause
In winter it divides around the Tibetan Plateau

21
Q

What is the polar front jet stream?

A

Associated with the warm and cold fronts of temperate-latitude depressions
Considerable day-to-day variation

22
Q

What are Rossby waves?

A

Middle-latitude the atmosphere is highly disturbed (Ferrel cell is largely schematic)
Surface air circulation- irregularly shaped,
eastward-drifting, cyclonic and anticyclonic systems
Higher atmosphere – smooth wave-shaped patterns

23
Q

Why are Rossby waves important?

A

They strongly influence the formation and subsequent

evolution of surface weather features

24
Q

Where do middle-latitude frontal depressions form?

A

Grow rapidly just downwind of upper troughs of

Rossby waves

25
Where do anticyclones form?
Just downwind of upper ridges
26
Rossby waves Differences between the hemispheres Southern temperate-latitudes
Rossby waves could arise anywhere in the middle latitudes due to ocean cover
27
Rossby waves Differences between the hemispheres Northern temperate-latitudes
Preferred locations, because influenced by thermal properties of land and sea and the location of key mountain ranges (Rockies and Himalayas)
28
Summary
1. Energy surplus at the equator and deficit at the poles leads to heat transfers. 2. The large-scale circulation of the atmosphere is organised into cells. 3. Jet streams form at the boundaries of the cells and play a major role in storm development. 4. Jet streams form into standing waves that affect the positions of major air masses.