1.1 Climate Flashcards

1
Q

Global atmospheric circulation model

Which part of the earth receives more sunlight?

A
  • the earth receives unequal heating
  • the equator receives more sunlight, and more heat
  • the poles receives less sunlight, and less heat.
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2
Q

Global atmospheric circulation model

Where are each cells?

A

Hadley cells: at the equator
Ferrel cells: besides the Hadley cells
Polar cells: at the North and South poles.

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3
Q

Global atmospheric circulation model

What happens at the Hadley cells?

A
  • warm, moist air at the equator rises (because of sunlight/heat)
  • as it rises, it cools and condenses, creating heavy rainfall at the equator
  • rainforests on the equator
  • as air moves towards the pole, it cools and sinks at the tropics. brings warm, dry air to the tropics - creating deserts.
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4
Q

Global atmospheric circulation model

What happens at Ferrel cells?

A
  • as it moves towards higher latitudes, it meets cool air (returning back to the equator)
  • forces the air up at 60 degrees, creating an area of high rainfall
  • air carries on towards the poles
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5
Q

Global atmospheric circulation model

What happens at the Polar cell?

A
  • air sinks
  • moves back to the equator
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6
Q

Global atmospheric circulation model

Global atmospheric circulation model summary

A
  • warm, moist air rises (low pressure)
  • air cools & condenses, creates heavy rainfall and high pressure (rainforests)
  • sinks at tropics. brings warm dry air = deserts at tropics
  • air meets cool air. air is forces up - creating an area of high rainfall
  • sinks at the poles. air moves back to equator.
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7
Q

Which direction does ocean currents work in?

A
  • warm waters from the equator travel towards the poles, near the surface of the oceans.
  • cooler water (which carry nutrients) travel from poles to the equator
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8
Q

Natural causes of climate change

Volcanic eruptions

A

When a large volcano erupts, it launches ash and dust into the atmosphere. This blocks the sunlight reaching the surface, so the Earth’s temperature drops, leading to an ice age.

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9
Q

Natural causes of climate change

Sunspot theory

A
  • dark spots on the sun which means that the sun is working harder to produce more energy
  • generates slightly more heat which increases the temperature
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10
Q

Natural causes of climate change

Orbital theory

A
  • Circular orbit: temperature increases because the Earth is closer to the sun
  • Elliptical orbit: temperature decreases because Earth is further away from the sun
  • Tilts: equator gets more sunlight, poles become cooler (less sun)
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11
Q

Natural causes of climate change

Albedo effect

A
  • Lighter colours reflect more light/sun than darker colours (absorbs heat)
  • a lot of ice coverage reflects light and heat, creating a cooling effect.
  • when the ice melts, it exposes the darker ocean water underneath, which absorbs the heat and increases temperature.
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12
Q

Evidence of natural climate change

Ice cores

A
  • when snow falls, it traps air into the ice
  • when scientists take a core of ice, it reveals the gas concentrations of when the snow fell
  • used to calculate temperatures of that time
  • rapid increase in temperature in the past decades.
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13
Q

Evidence of natural climate causes

Tree rings

A
  • every year, a new ring forms in the trunks of trees.
  • tree rings are thicker in warm, wet conditions.
  • they are a reliable source of evidence for the past 10,000 year
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14
Q

Evidence for natural climate causes

Historical sources

A
  • Temps were measured and recorded globally using thermometers since 1850s.
  • The record is highly reliable but very short term.
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15
Q

Human causes to climate change

Greenhouse effect and the enhanced greenhouse effect.

A
  • atmosphere naturally traps radiation from the sun, allowing Earth to be habitably warm.
  • humans have enhanced the natural effect and more heat is being allowed in, but less is able to escape the atmosphere, **creating a warming effect. **
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16
Q

Human causes to climate change

What human activities lead to the enhanced greenhouse effect?

A
  • Burning fossil fuels - releases carbon dioxide into the atmosphere.
  • Deforestation - trees absorb carbon dioxide during photosynthesis. If they are cut down, there will be higher amounts of carbon dioxide in the atmosphere.
  • Dumping waste in landfill - when the waste decomposes it produces methane.
  • Agriculture - agricultural practices lead to the release of nitrogen oxides into the atmosphere.
17
Q

Human causes of climate change

Why are projections uncertain?

A

what we do now will depend on the future, including the amount of emissions we release and the resulting impacts.