融雪洪水预警DSS,DSS for snowmelt flood early warning
1)DSS for snowmelt flood early warning融雪洪水预警DSS
英文短句/例句

1.Key Technologies and Realization of Early Warning DSS for Snowmelt Flood in Xinjiang;新疆融雪洪水预警DSS关键技术及实现方式研究
2.The Prediction, Early-warning for Snowmelt Flood and Decision Support Based on '3S' Technologies in Xinjiang基于“3S”技术的新疆融雪洪水预测预警及决策支持研究
3.Establishment and validation of early-warning model for snowmelt flood in North Xinjiang新疆北疆地区融雪洪水灾害预警模型的建立与验证
4.A sudden overflow of a stream resulting from a heavy rain or a thaw.洪水由于大雨或融雪引起的河水泛滥
5.melting snows that Betoken spring floods;雪化了,融成了春天的洪水;
6.Information Publication & Management System for Snowmelt Flood Based on WebGIS;基于WebGIS的融雪洪水信息发布管理系统
7.Study on Design of ArcGIS Server-based Flood Forecasting and Warning System基于ArcGIS Server的洪水预报与预警系统设计研究
8.Web-Based Reservoir Forecasting Regulation System Research in Snowmelt Area;基于Web的融雪地区水库预报调度研究
9.Research on Methods of PMF with Thaw Military Supplies Calculationin in Western of Tianshan Mountains;天山西部山区含融雪补给的可能最大洪水计算方法的研究
10.STUDY ON THE SPRING FLOODS CAUSED BY SNOW MELT WATER IN LOW-MOUNTAIN AND HILL REGIONS OF NORTHERN PIEDMONT OF THE TIANSHAN MOUNTAINS-A Case Study in the Paleochannels of Sangong River;天山北麓低山丘陵地区春季融雪洪水的研究——以三工河古河道为例
11.Research on the Ice-Snow Melting Runoff Forecasting Model in Xinjiang Xiabandi Reservoir;新疆下坂地水库冰雪融水径流预报模型研究
12.Construction of flood and water logging early warning system for Hongzehu Lake Basin洪泽湖流域洪涝灾害预警系统的构建
13.When the snow melted, the mountain stream became a deluge .雪融化时,山间溪流变成山洪暴发
14.When the snow melts, the mountain stream becomes a deluge.雪融化时, 山间溪流变成山洪暴发.
15.When the snow melt, the mountain stream become a deluge.雪融化时,山间溪流变成山洪暴发。
16.And with warm rains melting snow or drenching already saturated ground, the risk of extreme floods will rise dramatically.并且随着暖雨融化冰雪或者下到水量已饱和的地面,大洪水泛滥的危险将急剧增长。
17.The Key Technique Research of Forecasting and Early-warning System on Flood-induced Heavy Rain;致洪暴雨预报预警系统关键技术研究
18.The river was swollen with melted snow.河水因融雪而上涨。
相关短句/例句

snowmelt flood融雪洪水
1.Key problem research and implementation of snowmelt flood precaution model base system based on B/S structure;B/S结构融雪洪水预警模型库系统关键问题研究与实现
2.Establishment and validation of early-warning model for snowmelt flood in North Xinjiang新疆北疆地区融雪洪水灾害预警模型的建立与验证
3.The decision support system(DSS) of snowmelt flood prediction in Xinjiang based on "3S" is realized by the mode which integrates warehouses,method base,model base and knowledge base,and is put forward by the author as a new method.提出以数据仓库、方法库、模型库、知识库一体化模式实现基于“3S”的新疆融雪洪水预警决策支持系统的研究思路。
3)snow melting flood融雪型洪水
1.The research analysis indicates that its achievement is reasonable ,and this article supply a new idea and research method of snow melting flood.研究分析表明,结果比较合理,这为融雪型洪水预报提供了一种新的思路和研究方法。
4)flood warning and forecasting洪水预警报
1.In this article, Fujian provincial flood warning and forecasting system construction situation is described.洪水预警报系统是防汛指挥决策支持系统的重要组成部分,介绍了福建省洪水预警报系统的建设情况,结合工作实际,分析了系统建设、运行管理中存在的问题,以及系统建设的经验和体会,并针对目前系统存在的问题,提出了改进对策。
5)storm-snowmelt flood暴雨融雪型洪水
6)flood of melting glacier冰雪消融洪水
延伸阅读

融雪洪水融雪洪水snow-melt flood  rorlgxue hongshul融雪洪水(snow一rnelt flood)由积雪融化形成的洪水,简称雪洪。融雪洪水在春、夏两季常发生在中高纬地沉和高山地区一影响雪洪大小和过程的仁要因素是:积雪的面积、雪深、雪密度、持水能力和雪面冻深,融雪的热量(其中一大半为太阳辐射热).积雪场的地形、地貌、方位、气候和土地使用情况这些因素彼此之间有交叉影响就一定积雪场而言.关键因素是融雪率和雪深。一般融雪率小于降雨强度,而融雪历时大于降雨历时,同时雪盖对融水有滞蓄作用,因此洪水总量与雨洪洪水总量相等的雪洪,其洪峰流量较雨洪洪峰流量低,而洪水历时较雨洪洪水历时长‘雪洪过程线,由逐日融雪径流过程线迭加而成,因此有明显的日变化而呈锯齿状雪洪可分为两大类:①积雪融水洪水。在一些中高纬地区和高山地区,如中国东北、西北地区和苏联、北欧、北美北部南美西南部等地区,冬季漫长而严寒,积雪较深,来年春、夏季气温升高超过零摄氏度,积雪融化形成雪洪它有平原型和山区型。有些高山(如天山、喜马拉雅山等,地区,当夏季气温较高且持续时间较长时,永久积雪和冰川也发生融化形成夏汛,它与冬季积雪融水洪水相比,涨落较缓,洪水总量则受控于消融范围有些地区,如帕米尔和昆仑山北坡,还有永久积雪和冰川融水与夏季降雪融水的混合洪水。②积雪融水与降雨混合洪水。融雪同时降雨所形成的洪水,情况比较复杂如果降雨情况相同,若积雪场较干、微冻则部分雨水将滞留在冰粒间和冻结在雪盖内,加之冰层促使雨水侧渗构成栖留水体,而雪盖内和雪盖下面又缺渗径、沟槽,于是融水和雨水汇流较漫,洪峰流量较低而洪水历时较长。若积雪场比较暖湿,则汇流较快,洪峰流量较高而洪水历时较短。如果降雨的强度和热恰都较大,则降雨除直接增大洪水外,又促使积雪急剧融化并破坏其滞蓄作用,结果形成的洪水可比积雪融水洪水大的多,如1948年哥伦比亚河洪水(见洪水儿寒冷地区的大河,多系自山地流向平原.要流经几个不同洪水成因的垂直地带,因此,它们的下游河段洪水大多是两种甚至多种洪水叠加的结果;如果洪峰叠加,则可能发生较大或特大洪水。雪洪的年际变化和年内变化一般都较雨洪为小,这是因为流域中的融雪期及融雪范围内热量变化一般是小于降雨变化。人类活动的影响:山坡劈为梯田后,地面储蓄加大,会使洪峰流量减小;地区城市化后,融雪热量增多而地面储蓄和下渗率减小,于是洪水总量和洪峰流量都增大。雪洪在中国西北等干旱地区,可用于灌溉。雪洪的产汇流过程比雨洪复杂,融雪资料的收集更比降雨资料困难得多.因此今后需要深入研究积雪场物理学,并不断改进雪冰遥感测验技术。