太湖水位达到了历史最高值。
魔鬼湖水位的上升客观上给周围的社区带来威胁。
Devils Lake’s rising waters have caused considerable grief to the nearby community.
相比之下，原本较低的洪泽湖水位又比以前增高了。
In contrast, water level of the Hongze Lake in the lower reaches has been rising.
用环太湖地区的当月降水量建立下个月太湖水位的预报方程。
The next month forecast equation for Taihu water level was established by this month precipitation around Taihu.
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。
These climatic changes had great impacts on Qinghai Lake level and runoffs in this watershed.
古代村落的遗迹因水电站建设而被淹没，而当湖水位下降时又重新露出水面。
The ruins of an ancient village submerged by the construction of a hydroelectric dam resurface when lake levels are low.
近年来，由于气候条件的变化，青海湖水位呈下降趋势，水域面积逐年缩小。
The water level of Qinghai Lake descends and its water area reduces in recent years owing to the climate changing.
受持续暴雨影响，18日南京固城湖水位从7米多的水位上升到8.71米。
The continuous rain influence, 18, nanjing city a solid lake from seven metres more rising water to 8.71 m.
北川县城附近的唐家山堰塞湖水位不断上涨，抢险人员准备实施爆破、分流排水。
Rescuers are preparing to blast the barrier of the swelling dammed lake at Tangjiashan near Beichuan County with dynamite.
根据航天飞机雷达地形测绘数据，上图中山谷周围的白线近似于苏加塔湖水位最高时的湖岸线。
Derived from Shuttle Radar Topography Mission (SRTM) data, the white line around the valley in the top image approximates the Lake Suguta shoreline when water levels were at their highest.
造成湖岸形态变化的主要原因是气候暖干化、湖水位下降、土地沙漠化和人类活动的共同影响。
Warm and dry climate, water level declined, desert land and human activity are the primary reasons of this evolution.
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。
The reliable paleo-lake level data supply the valuable and useful information for quantitative reconstruction of hydrological and climatic parameters of past relative periods.
本文利用环太湖地区站点的月降水资料，用曲面拟合方法作客观分析，与太湖水位进行相关性研究。
The monthly rainfall data of the stations around Taihu were objectively analysed by a method of curved surface fitting in this paper and the correlation with the Taihu water level was studied.
建立了青藏高原热力作用和气候变化的关系及其对青海湖水位下降趋缓(年际差增大)的概念模型。
So a concept model has been get up by above research, this model explain that how the thermal in the Qinghai-Xizang Plateau effects on the water level in Qinghai Lake through basin climate change.
正是由于湖区夏季风降雨增大，湖水位迅速升高到4米以上，沉水植物川蔓藻从此未能在湖中央生长。
The lake level thereafter became deeper than 4 m so that Ruppia L. plants were no longer growing in the middle of the lake.
本文在调查鄱阳湖区湿地生态环境特征的基础上，分析两种控湖水位运行方案对湖区湿地生态环境的影响。
After analysised the characteristic of wetland ecosystem in Poyang Lake, we state the impact of two water lever operation scheme to the wetland ecosystem in Poyang Lake.
这幅2010年4月份的图来自最近更新的“地球观察”的专题变化的世界：鲍威尔湖水位，（此系列图文）记录了自1999年以来每年春季该湖水位的变化。
This image from April 2010 is the latest update in the Earth Observatory’s feature World of Change: Water Levels in Lake Powell, which documents changes in lake levels each spring since 1999.
当湖水的水位在湖的支流为洛杉矶供水改道而急剧下降后，这些石灰华就显露了出来。
They were exposed when lake levels dropped dramatically after tributary rivers were diverted to provide water for nearby Los Angeles.
最终旱灾平息了下来，持续的降雨使湖水在达到更危险水位前回升了上来。
The drought eventually subsided and consistent rain returned the lake to less dangerous levels.
当水位达到海拔1447英尺(441米)时，魔鬼湖的湖水可以流到临近的斯顿普湖。
At a water level of 1,447 feet (441 meters) above sea level, Devils Lake spills into neighboring Stump Lake.
当水位达到海拔1447英尺(441米)时，魔鬼湖的湖水可以流到临近的斯顿普湖。
At a water level of 1, 447 feet (441 meters) above sea level, Devils Lake spills into neighboring Stump Lake.
当水位达到海拔1459英尺(445米)时，两个湖泊的湖水可以流入红河的支流雪耶里河。
At a height of 1, 459 feet (445 meters) above sea level, both lakes spill into a Red River tributary, the Sheyenne River.
到20世纪90年代末，魔鬼湖湖面水位上升，湖水开始溢出，流向斯顿普湖。
By the late 1990s, Devils Lake rose high enough to begin flowing into Stump Lake.
世界自然基金会的一份报告表明，青海高原的湿地湖水水位已开始下降。
A report by the World Natural Fund says that the water level of wetlands in Qinhai Plateau is subsiding.
利用这一方法建立的太湖水网区区域水位模型，与实际情况相比，获得了较好的效果。
The model in Tat Lake Area has been developed with the method and the results are reasonable.
根据蚌湖和鄱阳湖修水站的水位同步观测资料，结合湖区地形，分析蚌湖与鄱阳湖的水量交换关系，并利用三峡工程对鄱阳湖修水、星子、都昌站水位影响的预测结果，讨论三峡工程对蚌湖水情的影响。
According to observed data at Banghu and Xiushui hydrologie stations, this paper in combination with topography of the lake region analyzes water exchange between Banghu Lake and Poyang Lake.
莫诺湖之所以会出现如此独特的景致，是因为分洪使得湖水水位降低，从而露出了更多的石柱。
Mono lake's tufa are particularly dramatic because water diversions have significantly lowered the lake's level, exposing more of the columns.
莫诺湖之所以会出现如此独特的景致，是因为分洪使得湖水水位降低，从而露出了更多的石柱。
Mono lake's tufa are particularly dramatic because water diversions have significantly lowered the lake's level, exposing more of the columns.
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