NW European winter climate - colder in the coming 2-3 decades?
A 2000 years marine geological perspective of North Atlantic SST anomalies and NW European winter climate - colder in the coming 2-3 decades ?
Antoon Kuijpers 1 , Marit-Solveig Seidenkrantz 2 , Mads F. Knudsen 2 , Bo H. Jakobsen 2 and Bjørn A. Malmgren 3
1) Geological Survey of Denmark and Greenland (GEUS), firstname.lastname@example.org
2) Department of Earth Sciences, Aarhus University, email@example.com / firstname.lastname@example.org / email@example.com
3) Norrtälje, Sweden, firstname.lastname@example.org
It is well-known that since the late 19th century major regional climatic variations have occurred at multi-annual to multi-decadal time scales. Part of these variations can be linked to multi-decadal changes in Atlantic Sea Surface Temperature (SST) anomaly patterns ('Atlantic Multidecadal Oscillation', AMO) observed in the 20th century, a feature which probably persisted during most of the Holocene.
Marine sediment core records from the NE Caribbean and West Greenland Current region covering the past 1500-2000 years show centennial-scale SST fluctuations with warming anomalies marking here the termination of the Medieval Climate Anomaly about AD1200 that persisted during the early Little Ice Age. Ensemble simulations with an atmospheric GCM forced with reconstructed SST data for the period 1871-1999* confirm linkage between a warm North Atlantic subpolar gyre (Fig. 1) and weakening of both the westerly windsaround 60°N and subtropical NE trade winds. Weaker North Atlantic trade winds and associated tropical North Atlantic positive SST anomalies are likewise typical features of a negative North Atlantic Oscillation index. Considering the actual AMO status characterised by North Atlantic SST warming since 1997, we may infersimilar climate development as after the 1930's (positive AMO started late 1920's), with more common cold winters in the coming 2-3 decades. Presumed AMO development in the mid 21th century, possibly enhanced by a global warming trend, may lead to fast and significant (winter) warming.
*) Sutton, R.T., Hodson, P.L.R. 2003. Influence of the ocean on North Atlantic climate variability 1871-1999. Journal of Climate 16, 3296-3313
Fig. 1 North Atlantic SST anomaly pattern, June 2010, showing positive anomalies (dark grey) in the subpolar gyre and (sub)tropical region, a persistent pattern since the late 1990's.