Difference between revisions of "Eur 002.temperature"
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( InferredVariable (L) )
(WTLiPD: New page Eur_002.temperature with Category: InferredVariable_(L)) |
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| − | [[Category:InferredVariable_(L)]] | + | [[Category:InferredVariable_(L)]]{{#set:| |
| + | ArchiveType=lake sediment| | ||
| + | CalibratedVia (L)=Eur_002.temperature.Calibration| | ||
| + | FoundInTable (L)=Eur-LakeSilvaplana.Trachsel.2010.paleo2measurement1| | ||
| + | HasColumnNumber (L)=1| | ||
| + | HasMaxValue (L)=0.585587997| | ||
| + | HasMeanValue (L)=0.0031690267922581| | ||
| + | HasMedianValue (L)=0.009957594| | ||
| + | HasMinValue (L)=-0.519523345| | ||
| + | HasResolution (L)=Eur_002.temperature.Resolution| | ||
| + | HasUnits (L)=degC| | ||
| + | HasVariableID (L)=Eur_002| | ||
| + | InferredVariableType (L)=Temperature| | ||
| + | Name (L)=temperature| | ||
| + | Pages2kID=Eur_015| | ||
| + | QCCertification=JPW| | ||
| + | QCnotes=We used multiple linear regression (MLR) to establish a calibration model that explains 84% of the variance of summer (JJAS) temperature during the calibration period 1864_1950. We then applied the calibration model downcore to develop a quantitative summer temperature reconstruction extending back to AD 1177.| | ||
| + | UseInPAGES2kGlobalTemperatureAnalysis=t}} | ||
