Spatial Patterns of Climate change Flashcards

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1
Q

What is a temperature anomaly?

A

A temperature anomaly refers to a depature from a reference value/long term baseline (1961-1980)

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2
Q

Why can we say the rise in CO₂ in recent years is entierly anthropogenic?

A

Because if caused by natural forcings, there would have been an increase in solar radiaition
(e.g. positive solar forcing causing more CO₂ to be released from the ocean)
But there hasn’t

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3
Q

What is the difference in land vs oceanic regions in terms of warming?

A

Land (terrestrial) regions have warmed faster than oceans

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4
Q

What are the 3 reasons behind why the terrestrial surface is warming more than oceans?

A
  • Heat capacity - land has a lower heat capacity than water
  • Suface energy balance - this is the energy exchange between the Earth’s surface and atmosphere, oceans have practically unlimited potential for evaporation driving cooling, continents do not
  • Atmospheric dynamics - the lapse rates (rate of temp decrease with height) decreases more strongly over oceans than lands
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5
Q

When is the greatest warming in the N.Hemipshere?

A

Greatest warming in the spring and winter in the N.Hemisphere

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6
Q

There has been a larger change in surface temperature near the pole than global average (polar amplification)
Why?

A
  • Melting of ice (13% per decade)
  • Ice is more reflective (albedo)
  • Less ice = less reflection and increased absorption = associated warming
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7
Q

Why is the intensified warming of the poles, not as strong in Antarctica?

A
  • Arctic is an ocean covered by sea ice
  • Antarctica is an elevated continent covered in more permanent ice and snow
  • (however not the case for the Antarctic peninsula)
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8
Q

Define Permafrost

A

Soil, rock or sediment that continously remains below 0°C for 2yrs

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9
Q

What are the core lays which exist around the permafrost?

A
  • Active layer (living biomass + carbon exchange)
  • Permafrost with low ice content (more affected by changes in temperature
  • Ice rich (ground ice) permafrost (thicker layer trapping GHGs)
  • Mud despoits from thawing
  • Permafrost
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10
Q

What are some issues associated with the thawing of permafrost?

A
  • Harder than concrete - thawing can destroy infrastructure which is built upon it
  • Microbes begin to decompose trapped organic carbon, releasing GHGs (started to decreas however due to stored carbon being used up)
  • Bacteria + viruses in ice and soil could be released, which have been trapped for >400K
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11
Q

How can the warming of the poles affect atmospheric circulation?

A
  • Warming of the poles results in weaker atmospheric pressure gradient (warm air rises = low pressure)
  • Results in lower wind speeds
  • In the north, leads to weakening of the west-to-east jet streams in the northern hemisphere - climate instability
  • Could lead to wavey polar vortex (cotroversial)
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12
Q

Are CO₂ concentrations the same globally?

A

More or less

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13
Q

What is the link between surface temperature and precipitation?

A

Areas that have become wetter have not warmed as much as other land areas

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14
Q

What is Latent heat?

A

Latent heat is energy released/absorbed, by a thermodynamic system, during a constant-temperature process
E.g. condensatio or evaporation (phase change)

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15
Q

What is sensible heat?

A

Release/absorption of heat by a thermodynamic system without a change in phase

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16
Q

There is enhanced …….. from wetter surfaces

A

There is enhanced latent vs sensible heat fluxes from wetter surfaces (evaporation)

17
Q

What is the issues with predicting future precipitation?

A

There is lots of uncertainity within the models
(however generally good enough to try to understand what is happening)

18
Q

Where are we likely to see an increase in precipitation trends?

A

North of 30°N

19
Q

Where are we likely to see a decrease in precipitation trends?

A

South and Sub-Saharan Africa
e.g. decrease in the South Asian monsoon due to decrease pressure gradient between warming see and land)

20
Q

If there is predicted tropospheric water vapour increases due to rising temperature, what affect will this have?

A

Cloud cover changes

21
Q

How does solar radiation change from different latitudes?
How does this affect circulation?

A
  • The angle of incoming solar raidation depends on latitudes (less curve = higher concentration of light
  • Will also influence seasonal temperature of locations
  • Results in average surface temperatures being warmer at lower latitudes
  • Atmospheric and oceanic circulation allow the distribution of this heat
22
Q

Between 40°N and 40°S, how is incoming heat radiation relative to outgoing heat radiation

A

Incoming heat radiation from the sun exceeds the outgoing heat radiation from the Earth

23
Q

North and South of 40°, how is outgoing heat radiation relative to incoming heat radiation?

A

Outgoing heat radiation from Earth exceeds the incoming heat radiation from the sun

24
Q

What are the 3 atmospheric circulation cells called?

A
  • Hadley
  • Ferrel
  • Polar
25
Q

The Hadely cell in the largest cell, cloest to the equator
How does it operate?

A
  • Warmer less dense air rises and moves out towards the poles
  • It then cools and sinks towards the surface, where it moves back towards the equator
26
Q

The polar cell is the smallest cell
Describe how it operates

A
  • Cool dense air descends on the polar regions between 60-70° N/S
  • The air moves towards the warmer equators, where it starts to warm and rise, returning to the poles at high levels
27
Q

Describe some key features of the ferrel cell

A
  • Not driven by temperature
  • Cells flow in the opposite direction to other cells
  • Transport heat from equator to poles, resulting in semi-permanenet areas of high + low pressures
28
Q

The atmospheric cells create distinct climate zones, what climate do they produce in these areas of low pressure

A
  • The rising air creates low pressures, resulting in increased rainfall
  • Rainforests or UK wet climate
29
Q

The atmospheric cells create distinct climate zones, what climate do they produce in these areas of high pressure

A
  • Air decends and creates high pressure
  • Produces little rainfall and clear skies
  • Relatively dry areas and deserts
30
Q

How does climate change affect the atmospheric cells?

A

Climates changes: changes in temperature and precipitation causes the cells to change
Causes the cells to move towards the poles

31
Q

If climate change affects the atmospheric cells, how does this affect the Atlantic and southern polar jet winds?

A

Intensification and a polewards shift of Atlantic and S.Polar jet

32
Q

If climate change affects the atmospheric cells, how does this affect the NH winter storm-track and extra-tropical storm activity?

A
  • Increased intensity and poleward shift in N.Hemisphere storm-track activity
  • Increased storm activity in the extra-tropical Hadely cells
33
Q

Apart from winds, what else can changes in global circulation affect

A

Changes in global circulation also affect wave height (happened since the 1950s)

34
Q

If climate change is affecting atmospheric circulation, how has this affected the Hadley cell and the S.Asian Monsoon?

A
  • Indication of stronger Hadley Circulation (equatorial cell)
  • Intensification of the Monsoon
35
Q

Due to global warming there has been an increase in the global mean temperature, where is this seen most?

A

In the N.Hemisphere

36
Q

Due to global warming, there is a prediction of a global increase in mean precipitation, where will this be highest?

A

Increased precipitation at higher latitudes - less in the tropics