Research Article

Spatiotemporal Characteristics of Evapotranspiration Paradox and Impact Factors in China in the Period of 1960–2013

Table 1

Change trends of temperature and potential evapotranspiration (ET0) in China.

ET0Temperature
1960–20131960–19992000–20131960–20131960–19992000–2013
(%) (%) (%)

China−3.9*59.1−14.78**75.110.0843.70.24**97.80.21**90−0.0841.4
YaRB−2.5158.7−17.64**8652.2716.80.18**96.50.0774.30.1662.2
SERB3.6160.7−20.93**89.319.3721.40.21**1000.192.9−0.1446.4
HaRB−9.21**75.8−18.08**84.8−17.0572.70.28**970.3**97−0.4139.4
HuRB−5.9560.5−8.1665.8−17.2460.50.2**97.40.17*97.4−0.139.5
YeRB1.0261.2−5.9455.2−6.2253.70.27**970.23**98.5−0.113.4
LRB−10.68*52.8−12.6780.6−78.286.10.23**1000.31**100−0.512.7
SRB−4.0470.9−3.7758.2−74.2690.90.33**1000.44**98.2−0.3627.3
NWRB−11.13**69.1−27.65**81.426.6939.20.34**990.31**94.8045.4
SWRB3.8948.6−3.2660102.45.70.28**1000.22**88.60.497.1
PRB−1.0144.8−14.65**76.15.7443.30.14**98.50.11**88.1−0.2825.4

slope of ET0 (mm per decade); percent of downward (%); slope of temperature (°C per decade); percent of upward; * = 0.05, ** = 0.01, the significance in 2000–2013 was not calculated because of the short time.