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Climate Change and the European Water Dimension - Agri ...

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They also note that: ‘Temperature is not <strong>the</strong> only parameter of climate variation that<br />

would affect <strong>the</strong> transport processes of compounds. For instance, changes in o<strong>the</strong>r<br />

climate parameters, e.g. wind intensity, ice cover over <strong>the</strong> Great Lakes, <strong>and</strong> quantity,<br />

quality, <strong>and</strong> spatial variation of rain <strong>and</strong> snow, associated with various climate<br />

patterns would also affect scavenging <strong>and</strong> deposition of organic pollutants’.<br />

The study by Ma et al. (2004) is important, because it is <strong>the</strong> first of its kind <strong>and</strong> clearly<br />

provides evidence for <strong>the</strong> potential scope <strong>and</strong> scale of underlying climate fluctuations<br />

to impact <strong>the</strong> distribution <strong>and</strong> cycling of atmospheric POPs.<br />

VI.F.4. A brief case study of <strong>the</strong> Arctic – an illustration of potential<br />

complexities <strong>and</strong> inter-linking<br />

Macdonald <strong>and</strong> co-workers (2003) present an excellent syn<strong>the</strong>sis of <strong>the</strong> potential<br />

influences of global change on contaminant pathways to, within <strong>and</strong> from <strong>the</strong> Arctic.<br />

They state: During <strong>the</strong> 1990s, a quiet revolution took place in <strong>the</strong> perception of <strong>the</strong><br />

Arctic. Despite early evidence of cyclical change in nor<strong>the</strong>rn biological populations<br />

<strong>and</strong> ice conditions, <strong>the</strong> general view among many western physical scientists<br />

throughout <strong>the</strong> 1960s to 1980s was that <strong>the</strong> Arctic was a relatively stable place. This<br />

view has been replaced by one of an Artic where major shifts can occur in a very<br />

short time, forced primarily by natural variation in <strong>the</strong> atmospheric pressure field<br />

associated with <strong>the</strong> ‘Arctic Oscillation (AO)’.<br />

They go on to give examples, <strong>and</strong> to speculate, about <strong>the</strong> ways in which such largescale<br />

atmospheric processes can potentially influence:<br />

• Inputs of POPs/pesticides from <strong>the</strong> source regions of North America, Europe<br />

<strong>and</strong> Asia;<br />

• Gas exchange, influenced by deposition <strong>and</strong> ice cover, in <strong>the</strong> North Pacific<br />

<strong>and</strong> Bering Sea, <strong>and</strong> in <strong>the</strong> Arctic Ocean (Jantunen <strong>and</strong> Bidleman, 1995);<br />

• Inputs to <strong>the</strong> Arctic waters from Russian <strong>and</strong> Canadian riverine inputs;<br />

• Releases from glacial ice mass loss <strong>and</strong> snow melt;<br />

• Cycling of POPs within Arctic lake waters;<br />

• The chemical partitioning <strong>and</strong> degradation of POPs in <strong>the</strong> Artic;<br />

These physical <strong>and</strong> chemical changes may ultimately, in turn, be linked to key<br />

biological aspects, such as:<br />

• Altering food web structure;<br />

• Food deprivation or shifts in diet;<br />

• Altered migration pathways <strong>and</strong> invading species, <strong>and</strong> even – it is argued –<br />

• The link between organochlorine compounds, disease <strong>and</strong> epidemics in<br />

wildlife populations (Macdonald et al., 2003).<br />

214

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