North Atlantic-Fennoscandian Holocene climate trends and mechanisms

Hans Petter Sejrup, Heikki Seppä, Nicholas P. McKay, Darrell S Kaufman, Áslaug Geirsdóttir, Anne de Vernal, Hans Renssen, Katrine Husum, Anne Jennings, John T. Andrews

Research output: Contribution to journalArticle

22 Citations (Scopus)

Abstract

To investigate the mechanisms behind Holocene regional climate trends from north of 58°N in the North Atlantic-Fennoscandian region Principal Component Analysis (PCA) was performed and a temperature anomaly stack produced from 81 proxy derived summer temperature time series from 74 sites. The PC results show distinctly different trends for near-surface versus surface temperatures, demonstrating the importance of handling these separately. The first PC of weighted sea surface summer temperature time series and continental time series explains 45 ± 8% of the variance, where the uncertainty is the standard deviation of the distribution of variance explained across the 1000 age-uncertain ensemble members. PC1 has a relatively uniform expression over the whole region, closely following the summer insolation at 65°N. The second PC explains 22 ± 4% of the variance and shows a non-uniform expression, with loadings in opposite directions in the northern and southeastern parts of the region. Comparing the PC time series with model runs and with the timing of the demise of the Laurentide Ice Sheet (LIS), suggest that this pattern reflects both topographic and albedo effects of the LIS as well as release of meltwater into the North Atlantic and Arctic Oceans. Comparing the stack of gridded records with published global stacks reveals an unusual Holocene temperature development in the North Atlantic-Fennoscandian region most likely resulting from the location relative to the decaying LIS.

Original languageEnglish (US)
Pages (from-to)365-378
Number of pages14
JournalQuaternary Science Reviews
Volume147
DOIs
StatePublished - Sep 1 2016

Fingerprint

PC
Laurentide Ice Sheet
time series
time series analysis
Holocene
climate
ice
trend
summer
temperature
snowmelt
Arctic
insolation
meltwater
Atlantic Ocean
regional climate
temperature anomaly
surface temperature
albedo
Arctic region

Keywords

  • climate
  • Fennoscandia
  • Holocene
  • North Atlantic

ASJC Scopus subject areas

  • Global and Planetary Change
  • Archaeology
  • Ecology, Evolution, Behavior and Systematics
  • Archaeology
  • Geology

Cite this

Sejrup, H. P., Seppä, H., McKay, N. P., Kaufman, D. S., Geirsdóttir, Á., de Vernal, A., ... Andrews, J. T. (2016). North Atlantic-Fennoscandian Holocene climate trends and mechanisms. Quaternary Science Reviews, 147, 365-378. https://doi.org/10.1016/j.quascirev.2016.06.005

North Atlantic-Fennoscandian Holocene climate trends and mechanisms. / Sejrup, Hans Petter; Seppä, Heikki; McKay, Nicholas P.; Kaufman, Darrell S; Geirsdóttir, Áslaug; de Vernal, Anne; Renssen, Hans; Husum, Katrine; Jennings, Anne; Andrews, John T.

In: Quaternary Science Reviews, Vol. 147, 01.09.2016, p. 365-378.

Research output: Contribution to journalArticle

Sejrup, HP, Seppä, H, McKay, NP, Kaufman, DS, Geirsdóttir, Á, de Vernal, A, Renssen, H, Husum, K, Jennings, A & Andrews, JT 2016, 'North Atlantic-Fennoscandian Holocene climate trends and mechanisms', Quaternary Science Reviews, vol. 147, pp. 365-378. https://doi.org/10.1016/j.quascirev.2016.06.005
Sejrup, Hans Petter ; Seppä, Heikki ; McKay, Nicholas P. ; Kaufman, Darrell S ; Geirsdóttir, Áslaug ; de Vernal, Anne ; Renssen, Hans ; Husum, Katrine ; Jennings, Anne ; Andrews, John T. / North Atlantic-Fennoscandian Holocene climate trends and mechanisms. In: Quaternary Science Reviews. 2016 ; Vol. 147. pp. 365-378.
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