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Quaternary EnvironmentsQuaternary EnvironmentsPaleoclimatic ReconstructionPaleoclimatic Reconstruction
Paleoclimatic ReconstructionPaleoclimatic Reconstruction
“… “…paleoclimatic data provide the basis for paleoclimatic data provide the basis for testing hypotheses about the causes of testing hypotheses about the causes of climatic change. Only when the causes of climatic change. Only when the causes of past climatic fluctuations are understood past climatic fluctuations are understood will it be possible to fully anticipate or will it be possible to fully anticipate or forecast climatic variations in the future forecast climatic variations in the future (Bradley and Eddy, 1991).” (Bradley 1999)(Bradley and Eddy, 1991).” (Bradley 1999)
ThresholdsThresholds
Nonlinear responsesNonlinear responses Critical thresholdsCritical thresholds
http://kevin.atkinson.dhs.org/fractals/
Strange AttractorsStrange Attractors
http://www.geocomplexity.com/Global_climate.htm
Lorenz attractorLorenz attractor Meteorologist, 1963Meteorologist, 1963
Signal to Noise RatioSignal to Noise Ratio
Proxy records catalog the phenomenon in Proxy records catalog the phenomenon in which we are interested. This is called which we are interested. This is called signal.signal.
At the same time they filter that signal and At the same time they filter that signal and also respond to other drivers. This we call also respond to other drivers. This we call noise.noise.
If you examine the signal to noise ratio you If you examine the signal to noise ratio you can determine the quality of the record.can determine the quality of the record.
CalibrationCalibration
Direct information on the phenomenon or Direct information on the phenomenon or other proxy materials are used to other proxy materials are used to demonstrate the relationship.demonstrate the relationship.
The principle of uniformitarianism.The principle of uniformitarianism. Never 100% accurate.Never 100% accurate.
Analog SituationsAnalog Situations
Comparable situations in the pastComparable situations in the past No-Analog situationsNo-Analog situations Multiple proxiesMultiple proxies
ExtentExtent
Spatial coverageSpatial coverage Palynology – Size of catchmentPalynology – Size of catchment Dendrochronology – Coherent climate signalsDendrochronology – Coherent climate signals Packrats – Range from midden along with Packrats – Range from midden along with
coherent ecosystemscoherent ecosystems Temporal coverageTemporal coverage
Dendrochronology – 1,000 years on averageDendrochronology – 1,000 years on average Palynology – often 10,000 yearsPalynology – often 10,000 years Marine Sediments – 100,000 yearsMarine Sediments – 100,000 years
ResolutionResolution
Sampling intervalSampling interval Dendrochronology – AnnualDendrochronology – Annual Lake Sediments – 50 - 200 yearsLake Sediments – 50 - 200 years Marine Sediments – 500 - 1000 yearsMarine Sediments – 500 - 1000 years
Sedimentation RateSedimentation Rate Non-Continuous RecordsNon-Continuous Records
Glacial AdvancesGlacial Advances
Frequency DependenceFrequency Dependence
Low Frequency SignalLow Frequency Signal High Frequency SignalHigh Frequency Signal
InertiaInertia
Response Time - LagsResponse Time - Lags Pollen Assemblages – 100 years for the Pollen Assemblages – 100 years for the
vegetation to respond to climate changevegetation to respond to climate change Insect Assemblages – Quick generation time, Insect Assemblages – Quick generation time,
so change very quickly with climateso change very quickly with climate AutocorrelationAutocorrelation
Dendrochronology - Climate responsesDendrochronology - Climate responses
Climatic Forcing FactorsClimatic Forcing Factors
Proxies record climate changeProxies record climate change Also record forcing factorsAlso record forcing factors
Volcanic aerosolsVolcanic aerosols Dust in ice coresDust in ice cores Carbon DioxideCarbon Dioxide MethaneMethane Nitrous OxideNitrous Oxide
FeedbacksFeedbacks
Positive FeedbacksPositive Feedbacks Negative FeedbacksNegative Feedbacks
http://www.geocomplexity.com/Global_climate.htm
DatingDating
Utmost importance to determine timing of Utmost importance to determine timing of eventsevents Synchronicity of timingSynchronicity of timing Forcing factorsForcing factors Lagged timingLagged timing
Levels of AnalysisLevels of Analysis
Level ILevel I Field data collection, analysis, and Field data collection, analysis, and
measurementsmeasurements Level IILevel II
Calibrated and converted to paleo recordsCalibrated and converted to paleo records Level IIILevel III
Regionalized paleo recordsRegionalized paleo records SynthesisSynthesis
ModelsModels
Simplify a system to its basic componentsSimplify a system to its basic components Types of ModelsTypes of Models
Physical ModelsPhysical Models GlobeGlobe
Computer ModelsComputer Models GCMsGCMs
Conceptual ModelsConceptual Models Flow chartFlow chart
Test HypothesesTest Hypotheses