Modelling Climate Change - C Flashcards
Predictive models + rationale
most common models we use in climate science
complex math-based computer
rationale:
what happned in the past and currently will proabbly remain true for future events
General Circulation Model
uses math models to simulate circulation of energy and mass within and between the atmosphere and ocean
includes air temp, vapor pressure, solar radiation, albedo, air pressure (fluxes)
simulate climatic conditions by unit of area
Scale of GCMs
100km^2 grid size, very broad but varies by model
useful for global predictions but misses local trends
have been able to reduce scale of our GCMs over time with greater computing power and more data
downscaling and regional climate modal
global-scale data can be converted to local-scale data (Regional climate model)
to apply to small-scale, local topography
not necessarily more accurate, just data is calibrated over smaller geographic area
Uncertainty + sources
all predictive models include some uncertainty, insufficient
known or unknown (don’t even realize you’re missing data)
some sources do not stay the same over time periods in study, difficult to determine how important each is, not possible to know all variable
Earth System Models
new class of GCMs that incorporate biogeochemical cycles like carbon and nitrogen cycles and life
Integrated Assessment Models
integration of predictions based on human activities into GCMs
Representative concentration pathway
type of global temperature projections published by IPCC (made using IAMs)
represent different projections based on future CO2 emissions
RCP 1.9
limits global warming to below 1.5C
RCP 2.6
1.5-2C by 2100
CO2 emissions goes to 0 by 2100
RCP 4.5
2.5-3C at 2100
CO2 emissions peak in 2045 with peak oil
RCP 8.5
5C by 2100
CO2 emissions do not peak before 2100
Hindcasting
use past environmental conditions to calibrate a model
then use it see if it can predict current conditions
then it should be able to predict future
Uncertainty with clouds
formation and breakdown are frequently fast and local events
no proxy data on clouds
cannot be captured at scale of most GCMs or RCMs (15km long)
Parameterize
average a variable over a large area as accurately as possible
use that as best estimate for a small area
(split cloud into quadrants and calculate average coverage)