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Original Articles

Spatial distribution and temporal variation of reference evapotranspiration during 1961–2006 in the Yellow River Basin, China

Distribution spatiale et variation temporelle de l'évapotranspiration de référence pendant la période 1961–2006 dans le bassin du Fleuve Jaune, en Chine

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Pages 1015-1026 | Received 05 Oct 2010, Accepted 18 Feb 2011, Published online: 09 Sep 2011

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.

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.

Fig. 3 Spatial distributions of mean seasonal and annual ETref during 1961–2006 in the YRB, China.

Fig. 3 Spatial distributions of mean seasonal and annual ETref during 1961–2006 in the YRB, China.

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.

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.

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).

Fig. 7 Trends (mm year-2) for the annual ETref from 1961 to 2006 in the YRB, China. Circles placed around the dots denote significant trend (0.05 level).

Fig. 7 Trends (mm year-2) for the annual ETref from 1961 to 2006 in the YRB, China. Circles placed around the dots denote significant trend (0.05 level).

Fig. 8 The relative change in ETref due to changes in air temperature, wind speed, relative humidity and sunshine hours, respectively.

Fig. 8 The relative change in ETref due to changes in air temperature, wind speed, relative humidity and sunshine hours, respectively.

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