General Circulation Flashcards

1
Q

Geneal Circulation

A

What conditions (winds, pressure, precipitation, temperature) look like if we average over long periods of time, and over large areas

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2
Q

Typical winds

A

Easterly in the tropics

Westerly in mid-latitudes

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3
Q

Distribution of precipitation

A

Persistent rain near the equator and in mid-latitude “storm tracks” and clear skies in the subtropics

The relationships between average wind patterns and pressure patterns and upward and downward air motions

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4
Q

Three-cell model of the ATM

A

Polar cell (cold, sinking air near the pole spreads equatorward at the surface)

Ferrel cell (rising motion in the mid-latitude “storm tracks”

  • Polar jet aloft associated with large horizontal temperature gradient (thermal wind)
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5
Q

Jet streams becomes unstable =>

A

starts getting wavy

wavy ==> mid-latitude cyclones

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6
Q

Conservation of Angular Momentum:

A

Unless acted upon by some force, the angular momentum of a parcel of air does not change

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7
Q

Thermal Wind

A

A horizontal change in temprature causes wind speed to increase with height

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8
Q

Subtropical Jet

A

Conservation of angular momentum

Problem: jet would be way too fast, and becomes unstable. Waves start to form on the jet

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9
Q

Polar / Mid-latitude Jet:

A

Strong temperature difference between tropics and high-latitudes => strong jet

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10
Q

Poleward transport of energy

A

Without this transport of eneergy the poles would be much colder and the tropics much warmer

Poleward energy transport is accomplished by both the atmosphere and the oceans

The region of maximum energy transport liew between latitudes 30 degrees and 60 degrees

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11
Q

Thermohaline Circulation

A

Water sinks in the North Atlantic and Antarctic, fills the deep ocean around the globe

Returns to surface in Indian, Pacific, and Southern Oceans, and returns to the Atlantic

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12
Q

Thermo:

A

warm water loses heat as it moves N. in the Atlantic

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13
Q

Haline

A

Evaporation causes water to become more salty as it moves North

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14
Q

Thermohaline

A

Water is more dense as it moves toward the North Atlantic

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15
Q

Key Features of the Tropical Pacific Mean State

A
  1. Easterly winds
  2. Thermocline close to surface in East
  3. Cold(er) water in East - Cold Tongue
  4. Warm(er) water in West - Warm Pool
  5. Rainfall in West
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16
Q

Thermocline

A

Large vertical temperature difference that seperates warm surface water from colder, denser sub-surface water

slopes upward toward the east

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17
Q

Tropical Pacific normal conditions

A

Easterly trades cause thermocline to deepen in the west, shoal in the east

18
Q

Why is there a Cold Tongue?

A

Divergence: causes “upwelling” at the equator

Upwelling brings COLD water to surface in the eastern Pacific

19
Q

Tropical Pacific normal conditions

A

Eastelry trades cause thermocline to deepend in the west, shoal in the east

Winds also cause upwelling along the equator, bringing cooler subsurface water to the surface

Cooling from upwelling is most pronounced in the east, where the thermocline is close to the surface

20
Q

El niño

A

anomalous warming of the ocean surface in the central and eastern equatorial Pacific

21
Q

Southern Oscilation

A

Oscillation in mass (pressure) between the eastern Pacific, and the western Pacific and Indian oceans

22
Q

El Niño history

A

Señor Dr. Luiz carranza

23
Q

sourthern oscilation history

A

Sir Gilber Walker

Atmospheric component

24
Q

El Niño / Southern Oscilation

A

Jacob Bjerknes ENSO: connects el niño with the southern oscilation => it’s a coupled phenomenom

25
Q

“Proxy Data”

A

Indirect information that tells us about climatic conditions in the past

26
Q

Proxy data examples

A

Ocean Sediments - achieve past climatic info (shells, chemical composition of sediment, thickness of layers)

Ice cores - tell us about climate over last 500 ka

Tree rings (tell us about temperature and precipitation variations)Fossil corals and Speleothems: annual accumulation => temperature, precipitation

27
Q

Forcing

A

A process external to Earth’s climate that affects the climate

Volcanoes, orbital changes, changes in the sun’s strength, antropogenic processes

28
Q

Volcanic activity

A

aerosols from volcanoes reduce the amount of solar radiation reaching the surface

29
Q

Obliquity

A

the amount of “tilt” of Earth’s axis

30
Q

Eccentricity

A

How “eliptical” earth’s orbit is

More eliptical => more solar radiation at perihelion

31
Q

Some dominant forcing mechanisms

A

Aerosols

Changes in Earth’s orbit

Solar variations

Anthropogenic Greenhouse Gasses

32
Q

Anthropogenic Forcing

A

Emissions: rate at which a particular gas is being added to the atmosphere

Concentration: how much of that gas is actually in our atmosphere

33
Q

Change in Concentration =

A

Natural Emissions + Anthropogenic Emissions - Natural Sink

34
Q

Negative forcing

A

Causes cooling of the planet (aerosols)

35
Q

Feedback

A

A process that alters climate changes that are already underway

Positive feedback: amplifies change

Negative feedback:supresses change

36
Q

Snow and Ice Albedo Feedback

A

Warmer temperatures => snow melts quicker => more solar radiation absorbed => warmer temperatures

37
Q

Stefan-Boltzman Feedback

A

Warmer climate => more emitted radiation => climate doesn’t warm as much

38
Q

Water Vapor Feedback

A

Warmer temp and little change in RH => higher mixing ratio => enhanced greenhouse effect => warmer temperature

39
Q

Global temperature will rise by about

A

1-5 degrees Celsius (2 degrees Farenheight)

40
Q
A