Attabad-no substantial changes in the lake level.
阿塔·阿瓦德湖——湖泊水位没有明显变化。
Starting about 8, 000 years ago, however, the lake level dropped dramatically, falling from 570 meters (1, 870 feet) to about 320 meters (1, 050 feet) above sea level.
然而，从8000年前开始，湖水急剧地下降，从海拔570米(1870英尺)到320米(1050英尺)。
The reliable paleo-lake level data supply the valuable and useful information for quantitative reconstruction of hydrological and climatic parameters of past relative periods.
可靠的古湖水位重建为定量恢复过去相关时段的水文和气候参数提供了十分宝贵和有用的资料。
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。
Fluctuations in the lake level have impacted fish breeding sites.
湖泊水位的波动对该种鱼类的繁殖地造成影响。
Huangqihai lake is an inland closed lake. Climatic change is a major factor to control the lake level fluctuations.
黄旗海是一封闭湖泊，气候是控制其湖面变化的主要因素。
Taking the Upper Sha-4 turbidite fan in Wang-58 block as an example, we explain how lake level fluctuations control the development of turbidite fan.
以东营凹陷南斜坡王58地区沙四上浊积扇为例，分析了湖平面变化对浊积扇发育的控制作用。
The coupling between basement nonlinear subsidence and lake level elevation and subsidence has strong control over fluviation manner and the deposit distribution.
基底的非线性沉降和湖平面升降的藕合关系对河流的作用方式以及河流沉积的展布特征有很强的控制作用。
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。
The former research results indicated that the lake level and water balance changing of this closed large water body sensitively record the paleoclimatic variations on different time scales.
前人的研究结果表明，这个封闭型大湖的水位及水量平衡的变化敏感地记录了发生在过去不同时间尺度上的气候变化幅度。
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。
The formation of entrenched valley is the mutual effect of tectonic movement and sea (lake) level.
下切谷的形成是构造运动和海(或湖)平面共同作用的结果。
The lacustrine regression caused by the falling of the relative lake-level in rift basin is called Forced lacustrine regression (FLR).
断陷湖盆中相对湖平面下降引起的湖退作用称之为强制湖退作用。
The lacustrine regression caused by the falling of the relative lake-level in rift basin is called Forced lacustrine regression (FLR).
断陷湖盆中相对湖平面下降引起的湖退作用称之为强制湖退作用。
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