yangtze river source region
基本解釋
- [地球科學(xué)]長(zhǎng)江源區(qū)
英漢例句
- The main drainage system in the source region of Yangtze River formed and developed by riverhead erosion along the N-S-trending grabens and normal faults.
長(zhǎng)江源區(qū)主要水系是沿南北走曏的地塹搆造和正斷層侵蝕發(fā)育而成的。 - Infiltration is an important process in hydrologic cycle, in the source region of Yangtze River, infiltration of soil moisture has impact in runoff and plateau ecology.
入滲是水文循環(huán)過(guò)程中一個(gè)重要環(huán)節(jié),在長(zhǎng)江源區(qū),土壤水分入滲對(duì)逕流的影響很大,也是高原生態(tài)系統(tǒng)重要的影響因素。
雙語(yǔ)例句
專(zhuān)業(yè)釋義
- 長(zhǎng)江源區(qū)
The Yangtze River Source Region is the type region of the high-cold ecosystem in China. Where have Unique and fragile ecosystem and especial hydrological characteristics.
長(zhǎng)江源區(qū)是我國(guó)高寒生態(tài)系統(tǒng)典型區(qū)域,獨(dú)特而脆弱的生態(tài)系統(tǒng)和特殊的水文特征,在寒區(qū)生態(tài)環(huán)境、水文循環(huán)及氣候變化中起著極其重要的作用。