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The effect of solar magnetic activity on the yearly mean average temperatureis extracted from the historical record for much of North America. The level ofsolar activity is derived from the international sunspot number by therenormalized continuous wavelet transform using the Morlet basis to provide arunning estimate of the power associated with the magnetic cycle. The solaractivity gives the abscissa for a scatter plot of temperature for each station,from which the solar dependence and mean temperature are extracted. Theseparameters are then plotted against the latitude, longitude, and elevation foreach station, revealing a dependence of their values on geophysical location. Amechanism to explain the latitudinal variation of the solar dependence issuggested.

Influence of solar magnetic activity on the North American temperature record