On North Atlantic lntedecadal Variability: A Stochastic View
167
Fig. 9.14 Maps oflagged regression coefficients ofselected anomaly fields (lag -10 years,
i.e. the fields show the conditions 10 years prior to the maximum overtuming). a) SLP (hPa!
Sv), b) SST (K/Sv), c) fresh water flux (mmld/Sv), d) SSS (psulSv). e) surface currents
«cmls)/Sv), and t) loss of potential energy by convection [(mW/m 2 )/Sv]. The shading
denotes regions in which the results are statistically significant at the 95% level. From
Timmermann et al. (1998).
167
Fig. 9.14 Maps oflagged regression coefficients ofselected anomaly fields (lag -10 years,
i.e. the fields show the conditions 10 years prior to the maximum overtuming). a) SLP (hPa!
Sv), b) SST (K/Sv), c) fresh water flux (mmld/Sv), d) SSS (psulSv). e) surface currents
«cmls)/Sv), and t) loss of potential energy by convection [(mW/m 2 )/Sv]. The shading
denotes regions in which the results are statistically significant at the 95% level. From
Timmermann et al. (1998).