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Historic record of pasture soil water and the influence of the North Atlantic Oscillation in south-west England

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Figure

Figure 1 | Both Halstow and Hallsworth soil series at North Wyke have clay loam soil to30 cm depth (soil horizons marked A) over a dense impermeable clay subsoilwith coarse prismatic soil structure (soil horizons marked B)
Figure 2 | Map of NWFP showing the relative location of Longlands South and Wyke Moor and the weather station.
Table 1 | Key parameters for model input from field surveys
Figure 3 | Frequency distribution of (a) mean autumn minimum and (b) mean autumn maximum temperature (degrees C) and (c) mean annual minimum temperature for 1982–1992,1993–2003 and 2004–2015 periods showing shift in temperature distribution over these periods towards higher temperatures.
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