Climate - Atmospheric system (1. Causes of global climate change) Flashcards

(21 cards)

1
Q

What is sunspot activity?

A

Sunspots are magnetic storms that, paradoxically, increase overall solar output.Sunspot activity follows an ~11-year cycle, alternating between solar maximum and solar minimum.

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2
Q

Is sunspot activity linked to a rise in global temepratures?

A

Periods of high sunspot activity correlate with higher global temperatures, but the IPCC revised solar forcing’s contribution to only ~20% of recent warming (from a previously estimated 40%).

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3
Q

How do volcanic eruptions affect global temperatures?

A

Aerosols and sulphur dioxide are ejected into the stratosphere.

Sunlight is reflected and short-term global cooling is caused

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4
Q

What is global dimming?

A

A phenomenon where where atmospheric pollution (like soot and sulphates) reduces the amount of sunlight reaching Earth — estimated to decrease by 2% per decade.

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5
Q

What is the positive feedback loop present in relation to terrestrial albedo?

A

Melting ice reduces albedo, exposing darker surfaces that absorb more energy → leads to further warming and more melting — a positive feedback loop.

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6
Q

How much lower is the area of arctic sea ice in 2024 comapred to the 1981-2010 average?

A

30% - area comparable to the size of Texas

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7
Q

How much more potent is methane compared to CO2?

A

28x

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8
Q

What are the two main sources of methane?

A
  1. Thawing permafrost in the Arctic - releases trapped methane
  2. Agriculture - cattle & rice paddies
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9
Q

Example of a feedback loop with methane

A

Rising temperatures → permafrost thaws → methane is released → more warming → more permafrost thaws.

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10
Q

What are the four main GHG released by human activity?

A

CO₂ (carbon dioxide) from fossil fuel combustion (transport, electricity, industry).

CH₄ (methane) from agriculture and landfill.

N₂O (nitrous oxide) from fertilizer use and industrial processes.

CFCs (chlorofluorocarbons) from refrigeration and aerosols (now largely banned).

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11
Q

Insolation

A

Incoming shortwave radiation from the Sun (mostly UV and visible light)

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12
Q

Shortwave vs Longwave Radiation

A

Sun emits shortwave; Earth re-emits absorbed energy as longwave (infrared) radiation

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13
Q

Back Radiation

A

Longwave radiation re-radiated downward by greenhouse gases

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14
Q

Sensible Heat

A

Heat that changes temperature but not state

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15
Q

Latent Heat

A

Heat absorbed/released during phase change

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16
Q

Sunspot Activity

A

Magnetic disturbances on the sun, create more energy output

17
Q

What type of equillibrium did the Earth used to be in?

A

The atmosphere was once in radiative equilibrium, but human activities have disrupted this by increasing greenhouse gases.

18
Q

What is an example of a negative feedback loop?

A

negative feedback - counteracts (reverses) the initial forcing process / reverses

example: increased heat → increased plant growth → absorbs CO₂

19
Q

How are carbon sinks disrupted?

A

melting permafrost, forest loss → more emissions

20
Q

What would the temperature of the Earth be without the natual greenhouse effect?

21
Q

What GHG is the most abundant in the atmosphere?

A

Water vapor: Most abundant, but not anthropogenic