Article ID Journal Published Year Pages File Type
6348413 Global and Planetary Change 2012 13 Pages PDF
Abstract
► It is possible to constrain a climate model to follow proxy-based reconstructions using data assimilation. ► MCA in Europe displays a rich structure that cannot be characterized as uniformly warm in space and time. ► In winter, warm MCA conditions are associated with a circulation similar to the positive phase of the NAO.► In summer, warm MCA conditions are associated with reduced westerlies and an anomalous advection from North Africa.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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The medieval climate anomaly in Europe: Comparison of the summer and annual mean signals in two reconstructions and in simulations with data assimilation
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