North Atlantic Oscillation in winter is largely insensitive to autumn Barents-Kara sea ice variability
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Abstract A two-and-a-half-dimensional interactive stratospheric model(i.e., a zonally averaged dynamical-chemical model combined with a truncated spectral dynamical model),
Figure 5 shows an ice area anomaly for the Barents Sea. The variability in the
This study uses the Causal Effect Networks (CEN) frame- work to quantify the robustness of the stratospheric pathway between late autumn Barents–Kara sea ice and the Febru- ary