“…For North Atlantic SST variations, we use average SST in the subpolar gyre (SPG), defined as a weighted area average in 80-0 • W, 50-70 • N (gray box in Figures 1c and 1d). We examine extremely warm summers in central Europe (EU: 0-35 • E, 45-52 • N; as in Duchez et al, 2016a), northern Europe and Scandinavia (SCAN: 10-50 • E, 50-65 • N), and NEA (90-130 • E, 40-50 • N, as in black, red, and cyan boxes in Figures 1c and 1d, respectively; Monerie et al, 2017). These regions were constructed to cover mostly land surface to minimize direct influence of the underlying ocean on the results.…”