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by
M.D. Morecroft, W.A. Scott, M.E. Taylor, T.W. Parr, S.M. Smart & R.G.H.
Bunce
Contact: Mike Morecroft (mdm@ceh.ac.uk).
CEH Merlewood, c/o University Field Laboratory, Wytham, Oxford, OX2 8QJ, UK
Contents
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Executive Summary
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Module
10 of the Countryside Survey 2000 research programme addressed the issue of
year-to-year variability in vegetation: whether it was likely to influence
Countryside Survey results and how it might relate to weather patterns.
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The
vegetation of plots at Environmental Change Network (ECN) sites throughout
the UK was recorded in 1998 and 1999. ECN is a collaborative, long-term
monitoring programme, with the aim of detecting change in a wide range of
environmental variables, using a series of intensively studied sites. For
many of these plots, data were also available from 1997, 1996 and in some
cases 1994. The data were analysed by testing for year-to-year differences
in numbers of species and the ecological characteristics of those species
(using the systems of Grime and Ellenberg); these variables have also been
used in the analysis of the main CS2000 vegetation results. The Countryside
Vegetation System (CVS) was used for classifying the vegetation and
stratifying the sampling and analysis.
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Year-to-year
changes in CVS aggregate vegetation classes were found: 23% of the studied
plots changed classification at some point. Between 1998 and 1999, the two
years with the most data, 12% of plots changed. This compares with a change
of 30% between 1990 and 1998 in CS2000 data.
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Arable
Crop/ Weed communities showed the largest year-to-year variability in
species number and ecological characteristics; fertile grasslands and
woodlands were also relatively variable.
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The
number of species per plot decreased significantly between 1997 and 1999,
taking all vegetation classes together. The difference was also
statistically significant in fertile grassland, lowland woodland and heath /
bog classes when analysed separately. In the fertile grasslands, which
showed the largest significant decrease, the decline in numbers of species
was largely due to decreases in ruderal species ('weeds' able to grow
quickly in temporary gaps in the grass sward). This may relate to the
differences in weather between the dry conditions of 1995-7 and the
substantially wetter period between 1997 and 1999.
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In
infertile grassland there were significant differences in some vegetation
characteristics, but not species richness, between 1999 and earlier years;
the tendency was away from stress tolerant plants and towards more
fast-growing competitive ones. An increase in the mean Ellenberg fertility
score in this vegetation class, indicated a higher proportion of species
adapted to high nutrient conditions. This may reflect an ongoing change in
response to nutrient enrichment (e.g. from atmospheric pollution and spray
drift), detected in both CS1990 and CS2000 data.
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Although
there were significant differences between years, and climate may well have
been an important factor causing these, very few significant correlations
between vegetation and weather variables were found. This is probably
because of the short length of the time series. Many climatic effects may be
subject to a time-lag and interactions between variables.
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An
understanding of year-to-year changes in vegetation can help to inform the
results of Countryside Surveys. Year to year variability can be large enough
to obscure or distort long-term changes and should be accounted for in the
interpretation of CS2000 and similar monitoring exercises. In the case of
the CS2000 survey it is likely that changes of a similar nature would have
been detected if the main field survey were carried out in 1997 or 1999
rather than 1998; the size of the changes could however have been quite
different.
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We
recommend that annual vegetation monitoring be continued at ECN sites with
further developments to improve the coverage of vegetation types and sites.
More detailed analysis, using other data from ECN sites should be carried
out to improve understanding of the underlying mechanisms. Ultimately it
should be possible to develop models of vegetation response to climate to
help interpret results of wider, intermittent monitoring programmes.
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