lec 23: Modelling Climate Change Flashcards
predictive models
complex math-based computer programs which use past and present conditions to determine likely future conditions
predictive models are the most common models we use in climate science
rational behind all these type of models
- what has happened in the past and is currently happening
- and why/how it happened
- will probably remain true for future events
system will remain similar over the time periods covered in the predictive model
General Circulation Model (GCM)
utilizes mathematical models to simulate the circulation of energy and/or mass within and between the atmosphere and ocean
GCMs are incredibly complex and involve data collected by thousands of individuals over long time scales
(average model contains enough code for - 18 000 printed pages of text
output often in the petabytes of data (1 petabyte = 1024 TB)
requires very high computing power (this can sometime be a common limiting factor)
variables included in GCMs
air temperature
vapour pressure
solar radiation
air pressure
albedo and more
mainly physics based energy and mass fluxes
applying GCM to the terrestrial surface
land and atmosphere area is divided equally into a grid (divisions extend into the atmosphere)
The GCM will simulate climatic conditions per unit of area
why are most GCMs very broad in scale -> 100 km2 grid size
they are designed to give averages for the planet, not details on a specific area
what is the limitation to the global scale being useful for global predictions?
it misses potentially important local trends (i.e global warming trend in the oceans since 1970, but some areas have experienced a (yet unexplained) cooling trend)
downscaling
global-scale data can be converted to local-scale data (downscaling)
Regional climate models (RCMs)
mathematical models used to convert data calibrated for global regions to apply to small-scale, local topography
note that this does not mean that the local models are more accurate
(simply that the data is now calibrated over a smaller geographic area)
RCMs
RCMs are often how we make predictions about the impacts of climate change on the scale of a country or smaller
RCM-> not generating new data, changing the scale of existing data to a smaller unit area
each grid is run as a separate simulation
decreasing grid size drastically increases the number of grids which must be simulated
computing power limitation
computing power currently limits the total area that we can downscale
at one point, downscalling creates too many grids to simulate with current computing power
(downscaled maps are only of small regions, not the entire planet)
uncertainty
all predictive models include some elements of uncertainty
uncertainty:
- the parts of a model for which we have insufficient data
- uncertainly can be known or unknown
known= we know we do not have the data
unknown= we don’t even realize we are missing the data MUCH more problematic
common sources of uncertainty
frequently not possible to know all variables that should be part of a model
even if you know all the variables, can be difficult to determine how important each is
some sources of data do not stay the same over the time periods of the study (violate an assumption of predictive models)
impact of uncertainty
greater degree of uncertainty = less accurate model
uncertainty in a model is acceptable (not a flaw)
but its important to know (or at least have an idea) of where your model has greater uncertainty (often we visually display our uncertainties in our projections )
uncertainty in current GCMs
we have drastically decreased uncertainty in our GCMs over time (from the first models in the 1970 to today)
most uncertainties has been decreased by adding new global systems to our model (or better understanding known systems)