Heavy rain in the upper reaches of Yangtze river
the upper reaches in Shule river
Subalpine forest in the upper reaches of the Yangtze River
hilly red soil regions in the south of China
mountainous regions in the south of Anhui
cause of formation in the river pattern
cold in the upper and heat in the lower
deficiency in the upper and excess in the lower
Diexi in the upper Minjiang River
Divergence in the upper and lower troposphere
excess in the upper and deficiency in the lower
gas extraction in the upper corner
heat in the upper and cold in the lower
In the upper reach of Changjiang river
In the upper reach of Yellow River
Jinping Dahewan in Yalong river
river channel of the Longchuan River in the urban district of Chuxiong