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G. P. Weedon, S. Gomes, P. Viterbo, W. J. Shuttleworth, E. Blyth, H. Österle, J. C. Adam, N. Bellouin, O. Boucher, and M. Best

. Quantities are: Net rad = net radiation, VPD = vapor pressure deficit, Wind = 10-m wind speed, Tair = 2-m temperature, Neff = Effective number of data points (allowing for lag-1 autocorrelation), and adjusted slope P = probability of zero slope adjusted for lag-1 autocorrelation. Note that the units for snowfall are in water equivalent mm yr −1 . Throughout this paper linear trend significance is assessed using a Student’s t test in which the lag-1 autocorrelation is used to estimate the (lower

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