lake-level changes 湖平面变化
Attabad-no substantial changes in the lake level.
阿塔·阿瓦德湖——湖泊水位没有明显变化。
Lake basin sequence is formed through and sedimentation, showing the changes of the sedimentary systems or system tracts in time and space with the lake level variation.
湖盆层序是指在湖盆地内由沉积作用形成的一类层序，表现为随湖水面的升降变化沉积体系或体系域在时空上的变化。
These climatic changes had great impacts on Qinghai Lake level and runoffs in this watershed.
这种气候变化特征对流域内的青海湖水位和河川径流有重要影响。
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