attribution of changes

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t/Ag/EnSc/EnSt 404/504 - Global Change) t/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter Climate Models (from IPCC WG-I, Chapter Attribution of Changes Attribution of Changes Primary Source: Primary Source: IPCC WG-I Chapter 9 - Understanding and Attributing Climate Change IPCC WG-I Chapter 9 - Understanding and Attributing Climate Change

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Attribution of Changes. Primary Source: IPCC WG-I Chapter 9 - Understanding and Attributing Climate Change. What is climate?. - PowerPoint PPT Presentation

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Page 1: Attribution of Changes

(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

Page 2: Attribution of Changes

(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

Page 3: Attribution of Changes

(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”.

Page 4: Attribution of Changes

(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.

Page 5: Attribution of Changes

(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

Page 6: Attribution of Changes

(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)

Page 7: Attribution of Changes

(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?

Page 8: Attribution of Changes

(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

Page 9: Attribution of Changes

(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

Page 10: Attribution of Changes

(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?

Page 11: Attribution of Changes

(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)

Page 12: Attribution of Changes

Land & Ocean ChangesLand & Ocean Changes

Page 13: Attribution of 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

Page 14: Attribution of Changes

(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

Page 15: Attribution of Changes

(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

Page 16: Attribution of Changes

(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

Page 17: Attribution of Changes

(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

Page 18: Attribution of Changes

(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

Page 19: Attribution of Changes

(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

Page 20: Attribution of Changes

(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

Page 21: Attribution of Changes

(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 … …

Page 22: Attribution of Changes

(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

Page 23: Attribution of Changes

(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)

ENDEND

Attribution of ChangesAttribution of Changes