气象
氣象
기상
METEOROLOGICAL MONTHLY
2014年
8期
1013-1018
,共6页
姜智怀%章毅之%蔡哲%李嫦
薑智懷%章毅之%蔡哲%李嫦
강지부%장의지%채철%리항
山洪灾害%淹没模型%嵌入河道栅格
山洪災害%淹沒模型%嵌入河道柵格
산홍재해%엄몰모형%감입하도책격
flood disasters%FloodArea model%embedded river raster
文章以江西省曹水作为山洪灾害淹没模拟的研究区域,通过嵌入河道栅格修订数字地形,采用 FloodArea 水文淹没模型对数字高程模型(Digital Elevation Model,DEM)对修订前后的同一降水过程进行模拟,结合实地考察流域内淹没痕迹和水文站水位资料对比分析两者的模拟结果,并利用确定性系数和 Nash-Sutcliffe 效率系数对2000-2010年间出现的强降水过程的模拟结果进行验证。结论表明:基于嵌入河道栅格的山洪灾害淹没模拟能较好地反映曹水流域内的因降水导致的山洪推进路线、淹没范围及淹没水深,该方法可作为推算曹水流域的山洪灾害致灾临界面雨量的基础。
文章以江西省曹水作為山洪災害淹沒模擬的研究區域,通過嵌入河道柵格脩訂數字地形,採用 FloodArea 水文淹沒模型對數字高程模型(Digital Elevation Model,DEM)對脩訂前後的同一降水過程進行模擬,結閤實地攷察流域內淹沒痕跡和水文站水位資料對比分析兩者的模擬結果,併利用確定性繫數和 Nash-Sutcliffe 效率繫數對2000-2010年間齣現的彊降水過程的模擬結果進行驗證。結論錶明:基于嵌入河道柵格的山洪災害淹沒模擬能較好地反映曹水流域內的因降水導緻的山洪推進路線、淹沒範圍及淹沒水深,該方法可作為推算曹水流域的山洪災害緻災臨界麵雨量的基礎。
문장이강서성조수작위산홍재해엄몰모의적연구구역,통과감입하도책격수정수자지형,채용 FloodArea 수문엄몰모형대수자고정모형(Digital Elevation Model,DEM)대수정전후적동일강수과정진행모의,결합실지고찰류역내엄몰흔적화수문참수위자료대비분석량자적모의결과,병이용학정성계수화 Nash-Sutcliffe 효솔계수대2000-2010년간출현적강강수과정적모의결과진행험증。결론표명:기우감입하도책격적산홍재해엄몰모의능교호지반영조수류역내적인강수도치적산홍추진로선、엄몰범위급엄몰수심,해방법가작위추산조수류역적산홍재해치재림계면우량적기출。
Flood disaster was simulated in Cao-Shui Basin in Jiangxi Province.By revising the Digital Ele-vation Model (DEM)with river raster layer in,flooding simulation results carried out by FloodArea hydrological model was compared by deterministic coefficient and Nash-Sutcliffe efficiency coefficient with the actual flooded traces and hydrological data from hydrological observatories during 2000-2010.The re-sults showed that based on the embedded river raster DEM,flood disasters simulation process is signifi-cantly associated with the moving route,submerged area and depths of floods are caused by severe precipi-tation.The method can be used as a basic way to simulate the flood disaster caused by critical areal precipi-tation.