Difference between revisions of "Eur 026.temperature"

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( InferredVariable (L) )
(WTLiPD: New page Eur_026.temperature with Category: InferredVariable_(L))
 
(WTLiPD: Edit Page)
 
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[[Category:InferredVariable_(L)]]
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[[Category:InferredVariable_(L)]]{{#set:|
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ArchiveType=documents|
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CalibratedVia (L)=Eur_026.temperature.Calibration|
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DataType=N|
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FoundInTable (L)=Eur-Tallinn.Tarand.2001.paleo1measurement1|
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HasColumnNumber (L)=1|
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HasMaxValue (L)=0.5|
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HasMeanValue (L)=-4.628716904277|
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HasMedianValue (L)=-4.8|
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HasMinValue (L)=-11.3|
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HasResolution (L)=Eur_026.temperature.Resolution|
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HasUncertainty (L)=Eur_026.temperature.Uncertainty|
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HasUnits (L)=degC|
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HasVariableID (L)=Eur_026|
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InferredVariableType (L)=Temperature|
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MeasurementMaterial=ice break-up and rye harvest chronicles|
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Method (L)=application of transfer function|
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Name (L)=temperature|
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Pages2kID=Eur_020|
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QCCertification=JPW|
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QCnotes=In order to extend the Tallinn temperature series backward in time three different climate proxies were used. These were: the first day of ice break-up in Tallinn port a proxy for the mean winter air temperature (December to March); the first day of ice break-up on the rivers in northern Estonia a proxy for the beginning of spring; and the first day of the rye harvest a proxy for the mean air temperature in spring and summer (April to July). On the basis of these proxies the mean winter temperature could be extended back to the year AD 1500 and the spring and summer temperature back to 1731.|
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UseInPAGES2kGlobalTemperatureAnalysis=t}}

Latest revision as of 00:12, 8 May 2017