Figures & data
Fig. 1 Location of the YRB and the meteorological stations used in this study (▴). The two straight lines show the division of the basin into upper, middle and lower regions.
![Fig. 1 Location of the YRB and the meteorological stations used in this study (▴). The two straight lines show the division of the basin into upper, middle and lower regions.](/cms/asset/105ae250-159b-467c-80df-d0f06553bc59/thsj_a_590810_o_f0001g.gif)
Fig. 2 Mean monthly variations of the key meteorological variables for: the upper, middle and lower regions (see ) and whole YRB in the period 1961–2006: (a) air temperature; (b) relative humidity; (c) wind speed; and (d) sunshine hours.
![Fig. 2 Mean monthly variations of the key meteorological variables for: the upper, middle and lower regions (see Fig. 1) and whole YRB in the period 1961–2006: (a) air temperature; (b) relative humidity; (c) wind speed; and (d) sunshine hours.](/cms/asset/f8a9256e-c70d-40b5-9647-7bdc8372d6f0/thsj_a_590810_o_f0002g.gif)
Fig. 4 The abrupt change tested by the Mann-Kendall method for annual ETref series of Yangcheng station for 1961–2006. Here, as the line C1 is over the confidence line (P = 0.05), the cross-over point of C1 and C2 is the start point of abrupt change in this series.
![Fig. 4 The abrupt change tested by the Mann-Kendall method for annual ETref series of Yangcheng station for 1961–2006. Here, as the line C1 is over the confidence line (P = 0.05), the cross-over point of C1 and C2 is the start point of abrupt change in this series.](/cms/asset/7ac74965-9ab2-49bc-9d3d-6136b6b3e298/thsj_a_590810_o_f0004g.gif)
Fig. 5 The upward trends (▴), downward trends (▪), and no trends (○) in annual ETref in the YRB, China in the 1961–2006 period, detected by the Mann-Kendall method.
![Fig. 5 The upward trends (▴), downward trends (▪), and no trends (○) in annual ETref in the YRB, China in the 1961–2006 period, detected by the Mann-Kendall method.](/cms/asset/db311870-3e16-4a57-914b-511a967c0f09/thsj_a_590810_o_f0005g.gif)
Fig. 6 The time and frequency of the abrupt changes in ETref detected by the M-K method in the YRB in the 1961–2006 period, with the years when abrupt changes occurred (where two abrupt changes were detected at one station, the years are in brackets).
![Fig. 6 The time and frequency of the abrupt changes in ETref detected by the M-K method in the YRB in the 1961–2006 period, with the years when abrupt changes occurred (where two abrupt changes were detected at one station, the years are in brackets).](/cms/asset/1a92a855-18ef-484e-976b-9cac0f0703be/thsj_a_590810_o_f0006g.gif)