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Climate change between the mid and late Holocene in the northern high latitudes: Part I: Survey of temperature and precipitation proxy data
Stockholm University, Faculty of Science, Department of Physical Geography and Quaternary Geology.
Stockholm University, Faculty of Science, Department of Meteorology .
Stockholm University, Faculty of Science, Department of Physical Geography and Quaternary Geology.
Stockholm University, Faculty of Science, Department of Physical Geography and Quaternary Geology.
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2010 (English)In: Climate of the Past, ISSN 1814-9324, Vol. 6, 591-608 p.Article in journal (Refereed) Published
Abstract [en]

We undertake a study in two parts, where theoverall aim is to quantitatively compare results from climateproxy data with results from several climate model simulationsfrom the Paleoclimate Modelling IntercomparisonProject for the mid-Holocene period and the pre-industrial,conditions for the pan-arctic region, north of 60 N. In thisfirst paper, we survey the available published local temperatureand precipitation proxy records. We also discuss andquantifiy some uncertainties in the estimated difference inclimate between the two periods as recorded in the availabledata. The spatial distribution of available published localproxies has a marked geographical bias towards land areassurrounding the North Atlantic sector, especially Fennoscandia.The majority of the reconstructions are terrestrial, andthere is a large over-representation towards summer temperaturerecords. The available reconstructions indicate that thenorthern high latitudes were warmer in both summer, winterand the in annual mean temperature at the mid-Holocene(6000 BP±500 yrs) compared to the pre-industrial period(1500AD±500 yrs). For usage in the model-data comparisons(in Part 1), we estimate the calibration uncertainty andalso the internal variability in the proxy records, to derive acombined minimum uncertainty in the reconstructed temperaturechange between the two periods. Often, the calibrationuncertainty alone, at a certain site, exceeds the actual reconstructedclimate change at the site level. In high-density regions,however, neighbouring records can be merged into aCorrespondence to: H. S. Sundqvist( record to increase the signal-to-noise ratio. Thechallenge of producing reliable inferred climate reconstructionsfor the Holocene cannot be underestimated, consideringthe fact that the estimated temperature and precipitationfluctuations during this period are in magnitude similar to, orlower than, the uncertainties the reconstructions. We advocatea more widespread practice of archiving proxy recordsas most of the potentially available reconstructions are notpublished in digital form.

Place, publisher, year, edition, pages
2010. Vol. 6, 591-608 p.
Keyword [en]
climate change, Holocene, proxy data, northern high latitudes
National Category
Climate Research
Research subject
Physical Geography
URN: urn:nbn:se:su:diva-43497DOI: 10.5194/cp-6-739-2010ISI: 000283667900004OAI: diva2:357348
Holocene Climate Variability over Scandinavia
Available from: 2010-10-19 Created: 2010-10-18 Last updated: 2011-12-06Bibliographically approved

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Sundqvist, Hanna S.Zhang, QiongMoberg, AndersHolmgren, KarinKörnich, HeinerNilsson, JohanBrattström, Gudrun
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Department of Physical Geography and Quaternary GeologyDepartment of Meteorology Department of Mathematics
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