attribution of changes
DESCRIPTION
Attribution of Changes. Primary Source: IPCC WG-I Chapter 9 - Understanding and Attributing Climate Change. What is climate?. - PowerPoint PPT PresentationTRANSCRIPT
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Attribution of ChangesAttribution of Changes
Primary Source: Primary Source:
IPCC WG-I Chapter 9 - Understanding and Attributing Climate ChangeIPCC WG-I Chapter 9 - Understanding and Attributing Climate Change
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
What is climate?What is climate?
ClimateClimate is usually defined as the average weather, is usually defined as the average weather, or more rigorously, as the statistical description in or more rigorously, as the statistical description in terms of the mean and variability of relevant terms of the mean and variability of relevant quantities over a period of time ranging from quantities over a period of time ranging from months to thousands or millions of years. months to thousands or millions of years.
WMO period: 30 yearsWMO period: 30 years
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
What is climate change and variability?What is climate change and variability?Climate changeClimate change refers to a change in the state of the refers to a change in the state of the climate that can be identified (e.g., by using statistical climate that can be identified (e.g., by using statistical tests) by changes in the mean or variability of its tests) by changes in the mean or variability of its properties, and that persists for an extended period, properties, and that persists for an extended period, typically decades or longer.typically decades or longer.
Climate variabilityClimate variability refers to variations beyond refers to variations beyond individual weather events in the mean state and other individual weather events in the mean state and other statistics of the climate (such as standard deviations, the statistics of the climate (such as standard deviations, the occurrence of extremes, etc.) on all spatial and temporal occurrence of extremes, etc.) on all spatial and temporal scales. scales.
This includes “internal variability”.This includes “internal variability”.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
What is detection and attribution?What is detection and attribution?
Detection Detection of climate changeof climate change is the process of is the process of demonstrating that climate has changed in some defined demonstrating that climate has changed in some defined statistical sense, without providing a reason for that statistical sense, without providing a reason for that change. change.
AttributionAttribution of causes of climate change is the process of of causes of climate change is the process of establishing the most likely causes for the detected establishing the most likely causes for the detected change with some defined level of confidence.change with some defined level of confidence.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Net RF: Net RF: 1750 to 20051750 to 2005(from Chapter 2)(from Chapter 2)
Note uncertaintiesNote uncertainties
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Atmospheric Temperature Changes - PCM Modelsolar only volcanic only
GHGs only O3 only
direct sulphate aerosol
all
1890 to
1999 (˚C/100Y)
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Reflected Solar RadiationReflected Solar Radiation
SatellitesModels
Deceasing Cloud Cover?
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
NH NH T: T: Reconstructions Reconstructions
vs. EBMvs. EBM
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
GCM Simulations: Natural ForcingsGCM Simulations: Natural Forcings
19 Simulations 5 Models
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
GCM Simulations: All ForcingsGCM Simulations: All Forcings58 Simulations
14 Models
Solar, volcanic effects?
Internal variability?
Aerosols?
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Latitudinal Distribution of TrendsLatitudinal Distribution of Trends
Red:Red: All forcings, middle 90% of GCM range All forcings, middle 90% of GCM range
(58 simulations by 14 GCMs)(58 simulations by 14 GCMs)
Blue:Blue: Natural forcings only, middle 90% of GCM rangeNatural forcings only, middle 90% of GCM range
(19 simulations by 5 GCMs)(19 simulations by 5 GCMs)
Land & Ocean ChangesLand & Ocean Changes
IPCC:IPCC: Most global warming Most global warming very likelyvery likely due to increase in due to increase in anthropogenic GHG concentrationsanthropogenic GHG concentrations
Likely anthropogenic warming on continental scaleLikely anthropogenic warming on continental scale
IPCC Statement
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Spatial Distribution of TrendsSpatial Distribution of Trends
58 Sim. 14
GCMs
19 Sim.
5 GCMs
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Changes in Tropopause HeightChanges in Tropopause Height
ERA40: Observation-based analysisERA40: Observation-based analysis
Model results (each 4 simulations by PCM):Model results (each 4 simulations by PCM):
Red - All forcingsRed - All forcings Blue - Natural forcings onlyBlue - Natural forcings only
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Ocean-Change Signal StrengthOcean-Change Signal Strength
Observed Signal: Red dotsObserved Signal: Red dots
Model results (individual basins from PCM):Model results (individual basins from PCM):
Green - All forcingsGreen - All forcings Blue - Natural forcings onlyBlue - Natural forcings only
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Methods of Detection - Optimal FingerprintingMethods of Detection - Optimal Fingerprinting
Response patterns Response patterns to forcings - from a to forcings - from a GCMGCM
Observed climate Observed climate patternspatterns
Scale factorsScale factorsInternal variability Internal variability (“noise”)(“noise”)
Earlier slideEarlier slide
solar volcanic
GHGs O3
Aerosol All
Linear Linear RegressionRegression
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Methods of Detection - Inferring ChangeMethods of Detection - Inferring Change
Are at least some of the scale factors Are at least some of the scale factors significantly different from zero?significantly different from zero? DETECTIONDETECTION
Is a forcing distinguishable from others? Is a forcing distinguishable from others? Can it (or some combination) explain Can it (or some combination) explain the observed pattern?the observed pattern?
ATTRIBUTIONATTRIBUTION
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Scale Factors - 4 GCMsScale Factors - 4 GCMs
Bars: 5-95% uncertainty rangeBars: 5-95% uncertainty range
Red: GHGsRed: GHGs Green: Other human factorsGreen: Other human factors Blue: NaturalBlue: Natural
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Inferred Climate Change - 4 GCMsInferred Climate Change - 4 GCMs
1990s minus 1900s1990s minus 1900s
(decades)(decades)
Trend: 1950 - 1999Trend: 1950 - 1999
Observed: Black lineObserved: Black line
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Can Greenhouse Warming Cause Can Greenhouse Warming Cause a Climatic Extreme? a Climatic Extreme?
Summer temperatures in SwitzerlandSummer temperatures in Switzerland
A single event cannot be attributed to a forcing factor, A single event cannot be attributed to a forcing factor, butbut … …
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
Probability of extreme European summer temperatures(using the Hadley Centre GCM)
… … the the probabilityprobability (risk) of an occurrence can change due to (risk) of an occurrence can change due to external influences. external influences.
No anthropogenic change
With anthropogenic change
(Mt/Ag/EnSc/EnSt 404/504 - Global Change)(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 9)Climate Models (from IPCC WG-I, Chapter 9)
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Attribution of ChangesAttribution of Changes