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Changes in atmospheric variability in a glacial climate and the impacts on proxy data: a model intercomparison

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Academic year: 2017

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Table 1. Spatial resolution of PMIP2 model components.
Fig. 1. The mean (contours: 4 hPa interval from 1000 to 1040 hPa; higher values omitted for clarity; bold contour denotes 1016 hPa) and standard deviation (colored shading: hPa) of monthly SLP averaged over all months in simulations of PI (left) and LGM (c
Fig. 2. Leading EOF of monthly SLP anomalies (colored shading: hPa/standard deviation of PC) and SLP climatology (contours: 4 hPa interval from 1000 to 1040 hPa; higher values omitted for clarity; bold contour denotes 1016 hPa) in the North Atlantic sector
Fig. 4. The seasonality of NAO-like variability in LGM and PI simulations. For each month, the shading in each 0.5 standard deviation bin (y-axis) represents the occurrence frequency of the NAOlike PC1 within that interval
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