modelling future climate Flashcards

1
Q

variables and scenarios that affect future emissions

A
  • global economy
  • human lifestyle
  • political climate
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2
Q

CMIP6

A
  • coupled model intercomparison models
  • used in AR6 report, the latest IPCC report
  • multiple runs of >100 models and 49 modelling groups
  • allowed the comparison and calibration of a range of different climate models under different emission scenarios
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3
Q

RCP and SSP coupled scenarios

A
  • socioeconomic outcomes affect RCPs
  • some coupled scenarios highly unlikely
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4
Q

SSP1 = sustainability

A
  • Gradual and continuous move to sustainability
  • Rapid move to renewables
  • Equitable distribution of wealth
  • Curb on population growth
  • Stable cooperative governance
  • Consumption directed to lower material growth and lower resource/energy intensity
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5
Q

SSP2 = middle of the road

A
  • Social, technological and economic trends don’t change notably
  • Development of income growth inequitable but patchy
  • International cooperation but slow progress
  • Still environmental degradation
  • Some improvements and a decline in energy intensity
  • Income inequalities only slowly improve
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6
Q

SSP3 = regional rivalry

A
  • Resurgence of nationalism
  • Regional conflict
  • Policy shift to national and regional interests
  • Regions concentrate on on food security, no wider concern for mitigation
  • Investments in education and technology decline
  • Consumption is materially orientated and energy intensive
  • Population growth, slowly in developed countries and quickly in developing countries
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7
Q

SSP4 =inequality

A
  • Large difference in investment in human capital
  • Widening differences in economic and political opportunity
  • Fragmentation of society between educated knowledge driven and labour intensive low paid work
  • Diversification of energy sector to include carbon and renewables
  • Environmental issues focused on localised issues in middle and high income areas
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8
Q

SSP5 = fossil-fueled development

A
  • Rapid development of technology
  • Fueled by fossil fuels
  • Strong investment in healthcare and education
  • Resource and energy intensive economy
  • Global population peaks and declines
  • Faith in ability to manage ecological and social systems
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9
Q

representative concentration pathways (RCPs)

A
  • represent radiative forcing (w/m²) by the end of the century
  • based on future emission scenario predictions taking into account population, land use, energy intensity, energy use
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10
Q

problems with predicting climate change

A
  • depends on future emissions
  • can’t rely on past records as it is much more rapid than past climate warming
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11
Q

improvements in climate models

A
  • better knowledge of systems
  • increased computational power
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12
Q

most recent IPCC models

A
  • 50-100 layers in ocean and atmosphere
  • horizontal resolution of 50-200km²
  • updateable every 30 minutes
  • contains regional models with much higher resolution
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13
Q

radiative forcing, global energy balance

A
  • the changing of energy stores within a system
  • solar energy is received (incidence), reflected, stored or used then reemitted
  • global temperature depends on the amount of this energy that is emitted into space
  • cooling + incidence < emitted
  • warming = incidence > emitted
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14
Q

global climate models (GCMs)

A
  • comprehensive 3D models based on physical laws represented by mathematical equations
  • uses a 3D grid across the globe
  • used to model future climate change
  • uses sub-models of all major parts of the climate system: ocean, atmosphere, topography, biosphere, cryosphere
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15
Q

parameterisation

A
  • some factors happen over a smaller scale than the grids used in CGMs such as atmospheric chemistry, production and movement of aerosols, cloud formation and ocean convection
  • smaller scale models within a grid check for accuracy and then an average is taken
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16
Q

GCMs in the 1960s, two box model

A
  • tracks a variable in a set geographic zone
  • start of simple computational models
  • describes the flux of energy between two geographic zones e.g. the tropics and the poles
  • equations determine the energy entering and leaving the system and the transfer of energy
17
Q

general circulation models (GCMs)

A
  • grid system over earth forms cells in ocean and atmosphere
  • factors in exchange of energy and fluid motion between these cells
  • often low resolution due to data gathering and computational power limitations
18
Q

atmospheric GCMs

A
  • includes equations for radiation, atmospheric pressure and temperature
  • takes into account albedo, convection and hydrology
19
Q

oceanic GCMs

A
  • includes equations for temperature, surface pressure, moisture and winds
  • takes into account conservation of heat, mass, linear movement and salinity
20
Q

AOGCMs

A
  • atmospheric oceanic GCMs
  • combines atmosphere and ocean GCMs into a singular model