Winter-to-spring transition in Europe 48-54°N: From temperature control by advection to control by insolation
As established in previous studies, and analyzed further herein for the years 1988–1998, warm advection from the North Atlantic is the predominant control of the surface‐air temperature in northern‐latitude Europe in late winter. This thesis is supported by the substantial correlation Cti between th...
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Veröffentlicht in: | Geophysical research letters 2000-02, Vol.27 (4), p.561-564 |
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