Worrall, F. and Harriman, R. and Evans, C. D. and Watts, C. and Adamson, J. and Neal, C. and Tipping, E. and Burt, T. P. and Grieve, I. and Montieth, D. and Naden, P. S. and Nisbet, T. and Reynolds, B. and Stevens, P. (2004) 'Trends in dissolved organic carbon in UK rivers and lakes.', Biogeochemistry., 70 (3). pp. 369-402.
Several studies have highlighted an increase in DOC concentration in streams and lakes of UK upland catchments though the causal mechanisms controlling the increase have yet to be fully explained. This study, compiles a comprehensive data set of DOC concentration records for UK catchments to evaluate trends and test whether observed increases are ubiquitous over time and space. The study analysed monthly DOC time series from 198 sites, including 29 lakes, 8 water supply reservoirs and 161 rivers. The records vary in length from 8 to 42 years going back as far as 1961. Of the 198 sites, 153 (77%) show an upward trend in DOC concentration significant at the 95% level, the remaining 45 (23%) show no significant trend and no sites show a significant decrease in DOC concentration. The average annual increase in DOC concentration was 0.17 mg C/l/year. The dataset shows: (i) a spatial consistent upward trend in the DOC concentration independent of regional effects of rainfall, acid and nitrogen deposition, and local effects of land-use change; (ii) a temporally consistent increase in DOC concentration for period back as far as the 1960s; (iii) the increase in DOC concentration means an estimated DOC flux from the UK as 0.86 Mt C for the year 2002 and is increasing at 0.02 Mt C/year. Possible reasons for the increasing DOC concentration are discussed.
|Keywords:||Climate change, DOC, Lakes, Rivers, Trends.|
|Full text:||Full text not available from this repository.|
|Publisher Web site:||http://dx.doi.org/10.1007/s10533-004-8131-7|
|Date accepted:||No date available|
|Date deposited:||No date available|
|Date of first online publication:||September 2004|
|Date first made open access:||No date available|
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