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Are PCBs in the Canadian Arctic atmosphere declining? : evidence from 5 years of monitoring.

Research output: Contribution to journal › Journal article


<mark>Journal publication date</mark>1/04/2001
<mark>Journal</mark>Environmental Science and Technology
Issue number7
Number of pages9
Pages (from-to)1303-1311
<mark>Original language</mark>English


A long-term database of weekly air concentrations was examined to establish temporal trends of PCBs in the Arctic atmosphere. Several methods were employed to reduce the intra-annual variability allowing the elucidation of long-term trends for a selection of congeners at Alert located in the Canadian Arctic. These methods included temperature normalization (TN), multiple linear regression (MLR), and digital filtration (DF). Estimation of the slope (m) resulting from the linear regression between the natural logarithm of the partial pressure in air versus reciprocal temperature (ln P = m/T + b), required for TN and MLR, proved difficult due to the poor correlation with temperature experienced for the majority of congeners. Values of m were considerably lower than those obtained from temperate studies, implying that regional air−surface exchange plays a minor role in supporting the observed air concentrations in the Arctic. The lighter congeners generally showed very low slopes, and some even showed positive correlation with 1/T. This might be a result of their relatively fast reaction rates with OH radicals following the onset of 24-h sunlight in spring. Use of DF (in combination with TN and MLR) revealed declining trends for several of the lower chlorinated congeners in the high Arctic atmosphere, with estimated first-order half-lives, t1/2, ranging from 3 to 20 yr. Declining trends of the lower congeners probably reflect falling levels in source regions, as a result of long-range transport to this Arctic site. There were no apparent trends for the higher chlorinated congeners (penta-substituted and above), except for PCB 180, in marked contrast to temperate studies, indicating a lag time for decline between the Arctic and source regions.