Palaeotemperature reconstructions of the European permafrost zone during marine oxygen isotope Stage 3 compared with climate model results

A palaeotemperature reconstruction based on periglacial phenomena in Europe north of approximately 51 °N, is compared with high‐resolution regional climate model simulations of the marine oxygen isotope Stage 3 (Stage 3) palaeoclimate. The experiments represent Stage 3 warm (interstadial), Stage 3 c...

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Veröffentlicht in:Journal of quaternary science 2003-07, Vol.18 (5), p.453-464
Hauptverfasser: van Huissteden, Ko, Vandenberghe, Jef, Pollard, David
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Sprache:eng
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