Fig. 6: Dynamical processes associated with SCEII.
From: A dynamic link between spring Arctic sea ice and the Tibetan Plateau snow increment indicator
Anomalous FMA a 850-hPa wind (purple vectors; unit: m s−1), b wind stress (unit: N m−2), c Ekman transport (unit: m2 s−1), c sea ice drift (unit: cm s−1), e sea ice thickness (unit: cm) and f SIC (unit: 5 × 10−2 %) derived from regression onto SCEII. Green vectors in a show the climatological FMA wind (unit: m s−1) at 850 hPa. The stippled regions and purple vectors indicate the statistical significance of the regression coefficients at the 5% level. The signs “AC” and “C” in a and b refer to the anticyclone and cyclone anomalies, respectively.
