Research Article

Hydrological Response of East China to the Variation of East Asian Summer Monsoon

Table 4

Calculated anomalies of hydrological variables (%) under various monsoon scenarios.

AreaEASMI (0.34~1.00)EASMI (1.00~2.00)EASMI (−2.00~−1.00)EASMI (−1.00~−0.34)
SMETSMETSMETSMET

YRB−1.0−11.5−7.1−8.23.118.66.88.6−2.3−16.8−4.8−9.3−0.41.20.20.9
YZB−0.5−5.3−2.3−3.53.17.03.53.00.21.6−0.51.6−1.2−1.0−0.9−0.6
LRB−1.7−13.4−3.0−6.74.132.110.716.7−1.2−11.0−4.3−5.3−1.1−6.9−3.0−4.8
PRB0.9−5.0−0.2−2.10.2−0.02.10.50.85.0−0.43.0−0.1−0.2−0.6−0.4
HRB−0.7−12.7−0.8−7.15.417.45.69.10.12.0−2.0−4.1−2.50.1−1.91.1
HHB−0.7−12.9−4.8−5.89.149.011.418.5−5.0−26.7−7.2−14.0−2.9−9.5−2.3−3.8
SRB−0.2−3.40.8−0.61.89.05.37.0−1.4−8.2−5.7−7.5−1.1−3.1−1.6−1.4
SEB2.710.62.09.43.14.71.3−0.4−3.4−7.2−0.7−2.3−1.42.3−0.50.9
CDP2.79.53.17.05.013.39.111.4−2.4−7.9−4.8−7.8−2.2−7.1−2.7−4.6
SJP1.19.03.05.33.319.07.311.3−1.7−13.9−4.9−10.7−2.2−8.6−3.6−4.4
NCP−1.4−14.1−3.2−7.47.032.98.213.0−2.0−13.8−4.8−10.2−2.6−4.3−2.1−0.9

Note: YRB: Yellow River Basin; YZB: Yangtze River Basin; LRB: Liaohe River Basin; PRB: Pearl River Basin; HRB: Huaihe River Basin; HHB: Haihe Basin; SRB: Songhua River Basin; SEB: Southeast Rivers Basin; CDP: Chengdu Plain; SJP: Sanjiang Plain; NCP: North China Plain.