- dry season
- low flow season
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枯水季节的英文
例句与用法
- There were many rivers with abundant water in the dry season , the numerous lakes and swamps , and the innumerable mountain springs in the north china during the middle ancient age ( a period from the 3rd to the 9th centuries ) indicated that a favorable water environment was far from the situation of nowadays
摘要中古时期（约公元3 - 9世纪） ，华北地区仍然具有良好的水环境，大小河流在枯水季节亦能维持可观流量，湖泊沼泽众多，丘陵山地泉水丰富，与当代严重缺水的情况迥然有别。 - ( 3 ) dynamic state of groundwater in riverside displays : at middle and supreme areas of yeerqiang , no matter abundant water season or low water season , river water always recharge groundwater . at downsteam , in abundant water season , river water recharge groundwater ; in low water season groundwater recharge the river
( 3 )近河岸地带地下水动态分析显示叶尔羌河中上游地区，无论丰水季节还是枯水季节，河水均补给地下水：下游地区，丰水季节，河水补给地下水；枯水季节，地下水补给河水。 - Thirdly , the mathematics model of forecasting low flow was established in fengcong and fenglin regions according to these factors influencing the amount of low flow in karst drainage ( the area of drainage , lithology , the type of landforms and its special assembly and forest ) the conception of low water resources carrying capacity was first put forward according to the changing law of low water resources in space and the situation of exploitation and utilization in karst drainage ( ie , under the condition of the virtuous ecological environment and the available technology , the explorable amount of water resources in certain areas is capacity and limitation which is able to coordinate the development of population , enviroment and economy during the period of low flow seasons ) and preliminarily analyzed its connotation , characteristic and established the index system of low flow in karst drainage
三是根据影响喀斯特流域枯水径流的下垫面因素(空间尺度、岩性、地貌类型、植被) ，分别对峰丛和峰林等喀斯特地区建立枯水径流预测模型。根据喀斯特流域枯水资源的空间变化规律以及实际开发利用状况，首次提出了枯水资源承载力的概念，即在枯水季节期间，保持良性的生态环境和现有的技术条件下，某一区域内可开采的水资源量对支持该地区人口、经济与环境协调发展的能力和限度。并初步分析了枯水资源承载力的内涵、特性，从水资源的供需方面确立了喀斯特流域枯水资源承载力的指标体系。