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Deposition of sulfur and nitrogen oxide (NOx)-nitrogen to the Great Lakes estimated with a regional deposition model

Atmospheric loading of anthropogenic S and NO x N to the Great Lakes is estimated with a regional deposition model. Dry deposition calculations include the effects of the wet surface and the predominant seasonal atmospheric boundary-layer structure over the lakes, i.e., strong stability in spring and summer and strong instability in autumn and winter. Modeling results are generally consistent with objective analyses of observed deposition. Best agreement is shown for the lower lakes; the model appears to underestimate deposition to Lake Superior, particularly for S