Projected changes in droughts and extreme droughts in Great Britain are strongly influenced by the choice of drought index: UKCP18-based bias adjusted potential evapotranspiration
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Potential evapotranspiration calculated from the UKCP18 RCM ensemble using the Penman-Monteith method as implemented by Robinson et al. (2017), bias adjusted using Lange et al. (2019), used for Reyniers et al. (2022). See paper for further details.
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Reyniers, N., Osborn, T.J., Addor, N., Darch. G. (2022). Projected changes in droughts and extreme droughts in Great
Britain strongly influenced by the choice of drought index. in prep for HESS.
Robinson, E. L., Blyth, E. M., Clark, D. B., Finch, J., Rudd, A. C. (2017). Trends in atmospheric evaporative demand in Great Britain using high-resolution meteorological data. HESS, 21(2), 1189-1224.
Lange, S. (2019). Trend-preserving bias adjustment and statistical downscaling with ISIMIP3BASD (v1. 0). GMD, 12(7), 3055-3070.
创建时间:
2022-03-03



