1) Plain dry land
平川旱地
2) Hanpingchuan fault basin
旱平川断陷盆地
1.
The Hanpingchuan fault basin is controlled by two regional major faults on both north and south,and formed a SE-NW strike,dip NE striped hydrogeological unit.
旱平川断陷盆地受南北两区域大断裂控制,形成走向南东—北西向、倾向东北的条带状水文地质单元。
3) Non irrigated flatland
旱作平地
4) Irrigated field in flat land
平川水地
5) the mid-summer drought in east Sichuan
川东伏旱
1.
This paper analyzes the relationship between the mid-summer drought in east Sichuan Province,and the atmospheric diabatic heat flow (ADHF).
本文分析了川东伏旱与大气非绝热热流量的关系,结果表明:与四川“西涝东旱”气候特征相关的川东伏旱与北半球大范围非绝热热流量异常相联系。
6) Zhaoyuan-taipingchuan area
肇源-太平川地区
补充资料:平川
广阔的平地:平川广野|有时惊叠嶂,何处觅平川?
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