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。
Main controlling factors of sequence development in lacustrine basins are tectonic uplift and subsidence, lake-level changes, and changes of sediment supply rates.
湖相盆地层序发育的主要控制因素为构造升降、湖平面变化和沉积物供应速率的变化。
Cyclical changes in climate conditions could cause the changes of lake level, sediment supply and sedimentation types, then impact the lake basin deposit and the lake level fluctuation.
气候条件的周期性变化可引起湖平面、沉积物供给和沉积物类型的变化，从而控制湖盆沉积充填和湖平面的变化。
Changes in lake level must be due to the net difference [between a and b].
湖水含量的变化一定是由于A和B之间的净差值。
Changes in lake level must be due to the net difference [between a and b].
湖水含量的变化一定是由于A和B之间的净差值。
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