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SMILE Workshop, Aug. 2, 2021
Climate
Models
Andreas Schmittner
Oregon State University
Textbook
https://open.oregonstate.education/climatechange/
Hierarchy of Climate Models
• 0D Energy Balance Model (EBM)

• 1D EBM

• 1D Radiative-Convective Models

• Intermediate Complexity Models (e.g. 2D EBMs)

• 3D General Circulation Models (GCMs)
Increasing
Complexity
Climate Models Equations based
on conservation of

• mass

• momentum

• energy

• water

• carbon

• ...
Equations are solved in each of the grid boxes of the model.
Typically global climate models have
about 20-30 layers in the atmosphere
and about the same amount in the
ocean. The horizontal grid box size
varies from about 5 degrees (500 km) to
about 1 degree (100 km) or less.
Models with smaller grid box sizes
r e s o l v e m o r e d e t a i l s ( h i g h e r
resolution), but they are also more
computationally expensive to run.
Interactive Components Included
• Atmosphere

• Ocean

• Sea Ice

• Land Surface (sometimes with interactive vegetation)

• Ocean Biology and Chemistry (e.g. Carbon, Nutrient,
and Oxygen Cycles)

• (Ice Sheets, usually prescribed)
Models that include biogeochemistry are also often 

called Earth System Models
Parameterizations
• Processes that cannot be resolved (smaller than
grid box size need to be expressed in terms of
resolved quantities; often empirical formulas)

• Examples are clouds, convection (atmosphere),
and mixing (ocean)
Forcings
• Models are driven by boundary conditions, e.g. incident
solar radiation at the top-of-the-atmosphere, surface
properties (albedo), changes in atmospheric CO2

• Interior is solved without the use of observations
Model Evaluation
Models are tested by comparing results to observations.
What are climate models used for?
• Paleoclimate Studies

How did climate change in the past and why?

• Detection and Attribution 

Is climate changing signi
fi
cantly and if so why?

• Projections

How may climate change in the future?
http://www.image.ucar.edu/~nychka/Animations/BTSCAMT340.mp4

http://www.image.ucar.edu/~nychka/talks.html

http://vets.ucar.edu/vg/T341/
High-Resolution Climate Model
1024x512 grid points (30 km)
Water vapor
Global Climate Model Grid Box Size ~ 1 degree NS x 1 degree EW
Sheehan et al. 2015
Vegetation Type 4 km grid vegetation &
fi
re model
Fire Frequency
West of the Cascades
fi
re frequency increases from ~80 yr recurrence times in 20th century to ~27 yr in 21st century
Coast Range forests shift from
conifer to more
fi
re resistant mixed
forests.
No
fi
re suppression
Thank You!

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Climate Models

  • 1. SMILE Workshop, Aug. 2, 2021 Climate Models Andreas Schmittner Oregon State University
  • 3.
  • 4. Hierarchy of Climate Models • 0D Energy Balance Model (EBM) • 1D EBM • 1D Radiative-Convective Models • Intermediate Complexity Models (e.g. 2D EBMs) • 3D General Circulation Models (GCMs) Increasing Complexity
  • 5. Climate Models Equations based on conservation of • mass • momentum • energy • water • carbon • ... Equations are solved in each of the grid boxes of the model. Typically global climate models have about 20-30 layers in the atmosphere and about the same amount in the ocean. The horizontal grid box size varies from about 5 degrees (500 km) to about 1 degree (100 km) or less. Models with smaller grid box sizes r e s o l v e m o r e d e t a i l s ( h i g h e r resolution), but they are also more computationally expensive to run.
  • 6. Interactive Components Included • Atmosphere • Ocean • Sea Ice • Land Surface (sometimes with interactive vegetation) • Ocean Biology and Chemistry (e.g. Carbon, Nutrient, and Oxygen Cycles) • (Ice Sheets, usually prescribed) Models that include biogeochemistry are also often called Earth System Models
  • 7. Parameterizations • Processes that cannot be resolved (smaller than grid box size need to be expressed in terms of resolved quantities; often empirical formulas) • Examples are clouds, convection (atmosphere), and mixing (ocean)
  • 8. Forcings • Models are driven by boundary conditions, e.g. incident solar radiation at the top-of-the-atmosphere, surface properties (albedo), changes in atmospheric CO2 • Interior is solved without the use of observations
  • 9. Model Evaluation Models are tested by comparing results to observations.
  • 10. What are climate models used for? • Paleoclimate Studies How did climate change in the past and why? • Detection and Attribution Is climate changing signi fi cantly and if so why? • Projections How may climate change in the future?
  • 12. Global Climate Model Grid Box Size ~ 1 degree NS x 1 degree EW
  • 13.
  • 14. Sheehan et al. 2015 Vegetation Type 4 km grid vegetation & fi re model Fire Frequency West of the Cascades fi re frequency increases from ~80 yr recurrence times in 20th century to ~27 yr in 21st century Coast Range forests shift from conifer to more fi re resistant mixed forests. No fi re suppression