Research Article

Spatiotemporal Variability and Trends in Extreme Temperature Events in Finland over the Recent Decades: Influence of Northern Hemisphere Teleconnection Patterns

Table 2

Summary of the Northern Hemisphere teleconnection patterns (NHPs) affecting climate variability in Finland considered in this study.

NHTPCentre(s) of circulationNatural signature over Finland in positive phaseReference

North Atlantic Oscillation (NAO)Ponta Delagada (Azores) and Stykkisholmur (Iceland)Strong westerly circulation bringing warmer and wetter weather than normalBarnston and Livezey [38], Irannezhad et al. [35, 39]
Arctic Oscillation (AO)A dipole between the polar cap area and the adjacent zonal ring centred along 45°NLow pressure in the Arctic and high pressure at midlatitudes, leading to warmer and wetter weather than normalThompson and Wallace [40], CPC [11], Irannezhad et al. [35, 39]
East Atlantic (EA)North-south dipoles across the North AtlanticIntensive westerly circulation, causing the weather to be warmer and wetter than normalBarnston and Livezey [38], CPC [41], Irannezhad et al. [35, 39]
West Pacific (WP)Kamchatka (Russia) and a centre between the western, North Pacific, and South Asia and East AsiaNorth-south dipole anomalies causing the weather to be wetter than normal in February and colder than normal in spring and summerIrannezhad et al. [35, 39]
East Atlantic/West Russia (EA/WR)Western Europe, northwest Europe, and Portugal in spring and autumn; Caspian Sea in winter and RussiaNortherly and northwesterly circulation across the Baltic Sea, resulting in milder and drier weather than normalBarnston and Livezey [38], Lim and Kim [42], Irannezhad et al. [35, 39]
Scandinavia (SCA)West of Europe, Mongolia, and ScandinaviaHigh pressure over Scandinavia, bringing milder and drier weather than normalBarnston and Livezey [38], Bueh and Nakamura [43], Irannezhad et al. [35, 39]
Polar/Eurasia (POL)North Pole, Europe, and northeastern China,Strong polar vortex resulting in milder and drier weather than normalCPC [41], Irannezhad et al. [35, 39]