Climate Change and the European Water Dimension - Agri ...
Climate Change and the European Water Dimension - Agri ...
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view has been replaced by one of an Artic where major shifts can occur in a very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 />
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