Tracking Toxaphene in the North American Great Lakes Basin. 2. A Strong Episodic Long-Range Transport Event

In this paper we examine the modeled daily toxaphene air concentrations from September 9 to 13, 2000, during which air concentration levels were 2−3 orders of magnitude higher than those derived from in situ measurements around the Great Lakes during the same year and during the 1990s. Meteorological conditions revealed that a typical deformation flow system associated with a high-pressure system extending from the east coast of Canada to the southern United States was one of the critical elements that enabled the transport of toxaphene to the Great Lakes. Cloud bands seen on satellite imagery and the rain band predicted by an atmospheric forecast model indicate that the system also delivered warm and humid air from the Gulf of Mexico and the southern United States to the Great Lakes. This resulted in strong wet deposition of toxaphene to the lakes. Substantial increase in the air concentration of toxaphene over the Great Lakes in this short period contributed greatly to raising the annual average daily air concentration for all of 2000. The results suggest that such an episodic event could be a major pathway for atmospheric transport of toxaphene from the southern United States to the Great Lakes.