用户名: 密码: 验证码:
平原河网区暴雨致洪的水文气象预报模型研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
本文建立了平原河网区暴雨致洪的水文预报模型,并利用苏北里下河平原河网区的水文气象资料进行模拟验证;再结合气象模式,实现了平原河网区暴雨致洪的水文预报模型与气象模式的耦合;在此基础上进行了业务平台的开发。本文得出以下几点结论:
     (1)全面系统地考虑了单元划分,产汇流的模拟,边界、河道、堰闸等处理,以及入河水量与水位变化的关系,建立了适合平原河网区暴雨致洪的水文预报模型。
     (2)根据苏北里下河地区的区域特点,设置了水文模型各类参数。经过苏北里下河地区1980—1988年间共8场暴雨来进行率定,再选取苏北里下河地区1980—1988年间4次致洪暴雨(全局性暴雨、局地性暴雨、连续性暴雨和大暴雨)来进行模拟验证。结果表明:率定是水文预报模型模拟不可缺少的一部分。模型能够模拟实际洪水,具有很高的精度和很强的实用性。
     (3)基于新一代中尺度天气预报模式WRF和所建的平原河网区暴雨致洪的水文预报模型,利用计算水面蒸发的彭曼公式,实现WRF与水文预报模型耦合,建立起平原河网区暴雨致洪的水文气象预报模型。在苏北里下河地区对其进行了验证,结果表明:模型预报过程与实测过程非常吻合,具有很高的精度和很强的实用性,这标志着平原河网区暴雨致洪的水文气象预报模型最终成功实现。
     (4)对平原河网区暴雨致洪的水文气象预报模型进行业务平台开发,充分发挥了Fortran在数学与工程计算方面的优点,同时集合VB具有图形处理能力强和人机交互界面的特点,实现混合编程。再利用VB接口方便的优点,集成GIS组件MapObjects和VB自身的控件,开发出所需的直观和具体的可视化图表。该平台的开发大大增强了水文气象预报模型的实用性,降低了预报员的工作强度,提高了劳动效率。
This paper establishes the hydro-meteorological forecasting model of flood caused by torrential rain in the plain river network region,and simulation verification is done on it with hydro-meteorological data of Lixiahe region in Northern Jiangsu; Combined with meteorological models,it is realized that the hydro-meteorological forecasting model is coupled;Based on this,this paper develops operational platform. This paper draws the following conclusions:
     1) Through the comprehensive and systematic consideration from the unit,the simulated runoff,borders,watercourse,weir gates,and the relationship between the water quantity and water level changes,this paper establishes the hydro-meteorological forecasting model of flood caused by torrential rain in the plain river network region.
     2) According to regional characteristics of Lixiahe region in Northern Jiangsu, this paper sets up various parameters of hydrological forecasting model.By using 8 torrential rains of Lixiahe region for 1980-88,hydrological forecasting model is calibrated.Then,this paper selects 4 flood-causing torrential rains(overall rain,local rain,continuous rain and heavy rain) to verify hydrological forecasting model.The results show that:the model calibration is an indispensable part.Model for simulating the practical flood has high precision and strong practicability.
     3) Based on the new generation mesoscale weather prediction model(WRF) and hydrological forecasting model,and using Penman equation for the calculation of water surface evaporation,this paper realizes the coupling between WRF and the-hydrological forecasting model.The hydro-meteorological forecasting model of flood caused by torrential rain in the plain river network region is established.Then,it is verified in Lixiahe region.The results show that:forecast value and measured value of water level is consistent.The model has high precision and strong practicability, which shows the ultimate achievement of the hydro-meteorological forecasting model.
     4) This paper develops operational platform of the hydro-meteorological forecasting model of flood caused by torrential rain in the plain river network region. In the development process,hybrid programming gives fully the advantages of Fortran in the calculation of math and engineering and the characteristics of VB in graphics processing capability and human-computer interaction.According to the advantages of VB interface,operational platform integrates GIS component (MapObjects) and VB own ActiveX control to develop the intuitive and concrete visual graph.The platform development greatly enhances the practicality of the hydro-meteorological forecasting model,to reduce the work intensity of forecasters, and to improve labor efficiency.
引文
[1]Darcy,H.Les fontaines publiques de la ville de Dijon(The Public Fountains of the City of Dijon).Paris:Dalmont,1856.
    [2]Sherman L.K.Streamflow from rainfall by the unit-graph method.Eng.News Record,1932,108:501-505.
    [3]Horton,R.E.The role of infiltration in hydrologic cycle.Trans.A.G..U.,1931,12:189-202.
    [4]Horton,R.E.Surface runoff phenomena.1935,Mchigan:Horton Hydrology Laboratory Publication 101,Ann Arbor.1-73.
    [5]陆建华,刘金清.流域产、汇流研究的进展及展望.北京水利,1995,(4):3-6.
    [6]Dunne,T.,L.B.Leopold.Water in Environmental Planning.W.H.Freeman.New York, 1978.
    [7]黄新会,王占礼,牛振华.水文过程及模型研究主要进展.水土保持研究,2004,11(4):105-105.
    [8]Clark,C.O.Storage and the Unit Hydrograph.Trans.Am.Soc.Civ.Eng.,ASCE,1945,110:1419-1488.
    [9]Nash J.E.The form of instantaneous unit hydrobmaph.Hydrol.Sci.Bull.,1957,3::114-121.
    [10]DoogeJ.C.Ageneral theory of the unit hydrograph.J.GeophysicalRes.,1959,64(1):241.
    [11]Rodriguez-Iturbe,I.,J.B.Valdes.The geomorphologic structure of hydrologic response.Water Resources Res.,1979,15(6):1409-1420.
    [12]Gupta,V.K.,E.Waymire,C.T.Wang.A representation of an instantaneous unit hydrograph from geomorphology.Water Resour.Res.,1980,16(5):855-862.
    [13]McCarthy,G.T.The Unit Hydrograph and Flood Routing.the Conference of the North Atlantic Division of U.S.Corps of Engineers,1938,6.
    [14]Cunge,J.A.On the subject of a flood propagation method(Muskingum method)J.Hydro.Res.,1969,7(2):205-230.
    [15]Saint-Vincent,B.d.Theory of unsteady water flow with application to river floods and propagation of tides in river channels.Acad.Sci.(Pans) Comptes Rendus,1871,73:237-240.
    [16]Linsley,R.K.,N.H.Crawford.Computation of a synthetic stream-flow record on a digital computer.Hydrol.Sci.Bull.,1960,51:526-538.
    [17]Johanson,R.C.,lmhoff J C,Davis H H.Users manual for the Hydrological Simulation Program-Fortran(HSPF).Environmental Protection Agency Report FPA-600,1980:9-80.
    [18]Sugawara,M.An analysis of runoff structure about several Japanese rivers.Japanese J.Geophys,1961,2:10-17.
    [19]陈仁升,康尔泅,杨建平,等.水文模型研究综述.中国沙漠,2003,23(3):221-229.
    [20]赵人俊.流域水文模拟.北京:水利电力出版社,1984.
    [21]Franchini,M.,M.Paceiani.Comparative analysis of several conceptual rainfall-runoff models J.Hydrol.,1991,122:161-219.
    [22]Freeze,R.A.,R.L.Harlan.Blue Print for aphysically-based digital simulated Hydrologic response model.J.Hydrol.,1969,(9):237-258.
    [23]Beven,K.J.,M.J.Kirky.A physieally-based variable contributing area model of basin hydrology.Hydro.Sci.Bull.,1979,24(1):43-69.
    [24]Kutehnlent,L.S.A two-dimensional rainfall-runoff model:identification of parameters and possible use for hydrological forecasts.Hydrological Forecasting.1980:ISHS Publication 129.215-219.
    [25]Jonch-Clausen,T.Système Hydrologique Européen,A Short Description.Danish Hydraulics Institute.SHE Report I.1979,Horsholm,Denmark.
    [26]Beven,K.J.,R.Warren,J.Zaoui.SHE:towards a methodology for Physieally-based distributed forecasting in hydrology.Hydrological Forecasting.1980:IAHS Publication 129.133-137.
    [27]DeCoursey,D.G.ARS small watershed model.Am.Soc.A-grie.Eng.Paper.,1982: 2094.
    [28]Morris,E.M.Forecasting flood flows in grassy and forested basins using a deterministic distributed mathematical model.Hydrological Forecasting.1980:IAHS Publication 129.247-255.
    [29]张超.地理信息系统.2002,北京:高等教育出版社.
    [30]刘凤莲,陈植华.流域水文模型发展展望.地质灾害与环境保护,2005,16(1):71-74.
    [31]Zhang,W.,O.Katsuro,B.Ye.A monthly stream flow model for estimating the potential changes of river runoff on the projected global warming.Hydrological Processes,2000,(14):1851-1868.
    [32]Marks,S.W.,W.V.Lance.Dennis P L.A distributed hydrology vegetation model for complex terrain.Water Resources Res.,1994,30(6):1665-1679.
    [33]Jean-Pierre,V.,H.Sylvain,I.Denis.A distributed hydrological model Adapted to the automatic calibration of parameters.J.of Hydrology,1986,87:1-8.
    [34]Putty,M.R.Y.,R.Prasad.Understanding runoff processes using a watershed model -a case study in the Western 6hats in South India.J.of Hydrology,2000,228:215-227.
    [35]沈晓东,腊春,谢顺平.基于栅格数据的流域降雨径流模型.地理学报,1995,50(3):264-269.
    [36]黄平,毛朵生.湖泊三维风生流隐式差分模型的研究.湖泊科学,1997,9(1):15-21.
    [37]郭生练.基于DEM的分布式流域水文模型.武汉水利电力大学学报,2000,33(6):1-5.
    [38]任立良,刘新仁.基于DEM的水文物理过程模拟.19,2000,4(369-376).
    [39]张成才,马双梅,孙喜梅.基于DIEM模型的流域参数识别方法研究.灌溉排水,2002,21(1):33-40.
    [40]赵人俊,王佩兰.新安江模型参数的分析.水文,1988,6.
    [41]李致家,孔祥光,张初旺.对新安江模型的改进.水文,1998,4:19-23.
    [42]瞿思敏.新安江模型与垂直混合产流模型的比较.河海大学学报,2003,31(4):372-377.
    [43]朱求安,张万昌.新安江模型在汉江口流域的应用及适应性分析.水资源与水工程学报,2004,15(3):19-23.
    [44]陈洋波,朱德华.小流域洪水预报新安江模型参数优选法及其应用.中山大学学报(自然科学版),2005,44(3):93-96。
    [45]黄国如,陈永勤.基于新安江水文模型的东江流域枯水径流模拟.华南理工大学学报(自然科学版),2006,34(11):93-98.
    [46]肖珊珊,古钟壁,周新志.利用自由水畜水库对新安江模型产流模型的改进.水资源与水工程学报,2006,17(6):76-78.
    [47]杨小辉,郭菲菲.率定新安江模型(三水源)产流参数.贵州水力发电,2000,14(1):7-10.
    [48]田向荣,赵英林.遗传算法和Rosenbrock法在水文预报汇流参数优选中的比较研究.水电能源科学,2002,20(1):23-25.
    [49]陆桂华,郦建强,杨晓华.水文模型参数优选遗传算法的应用。水利学报,2004,(2):50-56.
    [50]武新宇.基于并行遗传算法的新安江模型参数优化率定方法.水利学报,2004,(11): 85-90.
    [51]江燕.粒子群算法在新安江模型参数优选中的应用.武汉大学学报,2006,39(4):14-24.
    [52]陈沂.对平原地区降雨径流模型问题的探讨.海河水利,1987,(5):6-12.
    [53]刘新仁,王玉太,朱国仁.淮北平原汾泉河流域水文模型.水文,1989,(01):12-18.
    [54]梁瑞驹,程文辉,蔡文祥,等.太湖流域水文数学模型.湖泊科学,1993,5(2):99-106.
    [55]沈言贤,钱毅,徐小林.平原水网区产汇流模式探讨.水文,1996,(3):16-21.
    [56]王腊春,彭鹏,周寅康,等.湿润地区平原圩区产流机制研究.南京大学学报,1997,33(1):156-160.
    [57]赵永军,杨压,程文辉.太湖流域产汇流模拟.河海大学学报,1998,(2):110-113.
    [58]邓孺孺,陈晓翔,胡细凤,等.遥感和GIS支持下的平原河网区暴雨产流模型研究.水文,1999,(3):19-24.
    [59]程文辉,王船海,朱琐.太湖流域模型.2006,南京:河海大学出版社.
    [60]杨文峰,周辉,李明,等.水文气象预报研究述评.陕西气象,2007,(5):14-17.
    [61]Pietroniro,A.A framework for coupling atmospheric and hydrological models.Soil-vegetation-atmosphere Transfer Schemes and Large-scale Hydrological Models.The Netberlands:IAHS Publishing,2001:27-34.
    [62]Miller,J.,Russell G,Caliri G.Continental-scale river flow in climate models.Journal of Climate,1994,(7):914-928.
    [63]Arnell,N.The effect of climate change on hydrological regimes in Europe:A continental perspective.Global Environmental Change,1999,(9):5-23.
    [64]Nijssen,B.,O D'onnell G,Lettenmaier D.Predicting the discharge of global rivers.Journal of Climate,2001,(14):3307-3323.
    [65]Van Rheenen,N.,Wood W,Palmer N.Potential implications of PCM climate change scenarios for Sacramento-San Joaquin River basin hydrology and water resources.Climate Change,2004,62:257-281.
    [66]Warner,T.T.,D.F.Kibler,R.L.Steinhart.Separate and coupled testing of meteorological and hydrological forecast models for the Susquehanna River basin in Pennsylvania.J.Appl.Meteor.,1991,30:1521-1533.
    [67]Kenneth,J.W.,Clifford F.Mass.An Evaluation of a High-Resolution Hydrometeorological Modeling System for Prediction of a Cool-Season Flood Event in a Coastal Mountainous Watershed.Journal of Hydrometeorology,2001,(02):161-179.
    [68]Evans,J.Improving the characteristics of stream flow modeled by regional climate models.Journal of Hydrology,2003,284:211-222.
    [69]雍斌,张万吕,赵登忠,等.HEC-HMS水文模型系统在汉江褒河流域的应用研究.水土保持通报,2006,26(3):86-90.
    [70]Benoit,R.,Pellerin P,Kouwen N.Toward the use of coupled atmospheric and hydrologicalmodels at regional scale.MonthlyWeatherReview,2000,128:1681-1706.
    [71]Jasper,K.,Gurtz J,Lang H.Advanced flood forecasting in Alpine watersheds by coupling meteorological observations and forecasts with a distributed hydrological model.Journal of Hydrology,2002,267:40-52.
    [72]Mǒlders,N.,Raabe A.Testing the effect of a two-way-coupling of a meteorological and a hydrologic model on the predicted local weather.Atmospheric Research,1997,45:81-107.
    [73]Seuffert.,G.,Gross P,Simmer C.The influence of hydrologic modeling on the predicted local weather:Two-way coupling of a mesoscale weather prediction model and a]and surface hydrologic model.Journal of Hydrometeorology,2002,(3):505-522.
    [74]Yu,Z.,Pollard D,Cheng L.On continental-scale hydrologic simulations with a coupled hydrologic model..lournal of Hydrology,2006,331:110-124.
    [75]王守荣.水文模式DHSVM与区域气候模式RegCM2/China嵌套模拟试验.气象学报,2002,60(4):421-427.
    [76]陆桂华,吴志勇,LeiWen.陆气耦合技术应用研究进展.中国水文科学与技术研究进展.南京:河海大学出版社,2004.
    [77]Zeng,X.,Zhao Ming,Su B.jngka.Simulations of a hydrologicalmodel as coupled to a regional climate model.Advances in Atmospheric Sciences,2003,20(2):227-236.
    [78]高艳红.黑河流域水-土-气-生相互作用的数值研究.中国科学院寒区旱区环境与工程研究所,2003.
    [79]高艳红,程国栋,崔文瑞,等.陆面水文过程与大气模式的耦合及其在黑河流域的应用.地球科学进展,2006,21(12):1283-1291.
    [80]杨文发,段红.三峡水库中期水文气象耦合预报应用试验及探讨.水资源研究,2006,27(1):31-33.
    [81]雍斌,张万昌,刘传胜.水文模型与陆面模式耦合研究进展.冰川冻土,2006,28(6):961-970.
    [82]杨传国,林朝晖,郝振纯,等.大气水文模式耦合研究综述.地球科学进展,2007,.22(8):810-817.
    [83]钱乐祥.GIS分析与设计.中国环境科学出版社,2002:1.
    [84]黄杏元.地理信息系统概论.高等教育出版社,2001:5.
    [85]吴元芳.GIS支持下的枣庄市羊庄盆地地下水资源动态分析.山东师范大学,2000.
    [86]林文福.GIS支持下的小流域综合治理效益分析.福建农林大学,2001.
    [87]黄文典.GIS技术在成都水系水质模拟中的应用.四川大学,2002.
    [88]李昌志.基于GIS的流域产沙及水土保持决策支持系统研究.四川大学,2002.
    [89]龚健雅.地理信息系统基础。北京:科学出版社,2001.
    [90]缪海洋.基于GIS的圩区水系规划计算机辅助设计系统开发.扬州大学硕士学位论文,2006.
    [91]李德仁,关泽群.空间信息系统的集成与实现.武汉:武汉测绘科技大学出版社,2000.
    [92]陆汝钤,金芝,陈刚.面向本体的需求分析.软件学报,2000,11(8):1009-017.
    [93]王伟长.地理信息系统控件(ACtiveX)-MapObjects培训教程.北京:科学出版社,2000.
    [94]侯国祥,张开华,李可芳,等.基于MapObjects的汉江水污染控制决策支持系统.环境科学与技术,2004,(5):35-36.
    [95]侯国祥,郑文波,康玲,等.基于Mo技术的流域水文水情信息系统.水文,2004,32(5):90-92.
    [96]洪金益,谢琨磊,曾详坤.基于VB和Arcobjects的组件式地理信息系统开发.地理空间信息,2006,(4):6-7.
    [97]张轶辉.基于MaDOb iects下的GIS二次开发.中南大学,2005.
    [1]薛明.桥涵水文.上海同济大学出版社,2002.
    [2]张春宁.平原河网地区公路桥涵水文的探讨.公路,1997,(8):10-12.
    [3]刘芹.平原河网水力汁算及闸群防洪体系优化调度研究.河海大学硕士研究生毕业论文,2006,3.
    [4]高冬光。桥位勘测设计.北京:人民交通出版社,2001.
    [5]林芸.平原河网地区水文计算及洪水影响评价方法的探讨.河海大学硕士研究生毕业论文,2005,2.
    [6]盐城水文水资源勘测局.盐城地区水资源评价报告.2004:15-23.
    [7]冯锦明,赵天保,张英娟.基于台站降水资料对不同空间内插方法的比较.气候与环境研究,2004,9(2):261-277.
    [1]韩龙喜,张书农,金忠青.复杂河网非恒定流计算模型-单元划分法.水利学报,1994,(2):52-56.
    [2]陈春.泰森多边形的建立及其在计算机制图中的应用.测绘学报,1987,16(3):223-231.
    [3]赵永军,杨压,程文辉.太湖流域产汇流模拟.河海大学学报,1998,(2):110-113.
    [4]张磊.平原感潮河网区城市防洪规划中的水文计算方法研究.河海大学,2005.
    [5]程文辉,王船海,朱琐.太湖流域模型.2006,南京:河海大学出版社.
    [6]赵人俊.流域水文模拟.北京:水利电力出版社,1984.
    [7]齐清兰.水力学.北京:中国铁道出版社,2008.
    [8]冯锦明,赵天保,张英娟.基于台站降水资料对不同空间内插方法的比较.气候与环境研究,2004,9(2):261-277.
    [9]胡娅敏,丁一汇,廖菲.江淮地区梅雨的新定义及其气候特征.大气科学,2008,32(1):200-211.
    [10]何红艳,郭志华,肖文发.降水空间插值技术的研究进展.生态学杂志,2005,24(10):1187-1191.
    [11]方正杰.感潮河口城市防洪计算方法研究.南京:河海大学硕士学位论文,2005,5.
    [12]Ambrose,R.B.,T.A.Wool,J.Martin.A Hydrodynamic and Water Quality Model -Model Theory.Environmental Laboratory,1986" 35-36.
    [13]朱琐.太湖流域实时洪水预报调度系统研究.河海大学博士研究生毕业论文,2003.
    [14]陈方.数值模拟技术在太湖流域防洪控制与规划中的应用.河海大学硕士研究生毕业论文,2003.
    [15]侯玉.太湖流域水文模型.河海大学博士研究生毕业论文,1992.
    [1]汤国安,杨昕.ArcGIS地理信息系统空间分析实验教程.北京:科学山版社,2006:202-211.
    [2]毛锐,高俊峰.太湖地区湖泊水面蒸发.北京:科学技术文献山版社,1993.
    [3]张磊.平原感潮河网区城市防洪规划中的水文计算方法研究.河海大学,2005.
    [4]赵人俊.流域水文模型--新安江模型与陕北模型.北京:水利电力出版社,1984.
    [5]程文辉,王船海,朱琐.太湖流域模型.2006,南京:河海大学出版社.
    [1]董长宝.渭河流域致洪暴雨的天气学诊断分析与数俏模拟研究.兰州大学硕士研究生毕业论文,2008.
    [2]陈少平等.长江上游致洪暴雨天文天气耦合预报方法研究及应用.北京:气象出版社,2001.
    [3]中华人民共和国水利部.水文情报预报规范.北京:中国水利水电出版社 2000.
    [4]朱星明,卢长娜,王如云,等.基于人工神经网络的洪水水位预报模型.水利学报,2005,36(7):806-811.
    [5]余钟波.流域分布式水文学原理及应用.北京:科学山版社,2008:56-66.
    [6]赵求东.WRF+DHSVM融雪径流预报模式研究.新疆大学硕士研究生毕业论文,2008.
    [7]樊明兰.基于DEM的分布式水文模型在中尺度径流模拟中的应用研究.四川大学硕士学位论文,2004.
    [1]http://www.mmm.ucar.edu/wrf/users/model.html.
    [2]http://www.mmm.ucar.edu/wrf/users/supports/tutorial.html.
    [3]陈致颖.桃芝台风(2001)数值仿真研究:台风路径与结构之仿真与分析.台湾:国立中央大学大气物理研究所,2006.
    [4]Laprise,R.The Eu]er Equations of Motion wtih Hydrostatic PressUre as Independent Variable.Monthly Weather Review,1992,120:197-207.
    [5]Lin,Y.-L.,R.D.Farley,H.D.Orville.Bulk parameterization of the snow field in a cloud model.J.Climate Appl.Meteor.,1983,22:1065-1092.
    [6]Hong,S.Y.,H.-M.H.Juang,Q.Zhao.Implementation of prognostic cloud scheme for a regional spectral model.Mon.Wea.Rev.,1998,126:2621-2639.
    [7]Kain,J.S.,J.M.Fritsch.A one-dimensional entraining/detraining plume modei and its application in convective parameterization.J.Atmos.Sci.,1990,47:2784-2802.
    [8]Kain,J.S.,J.M.Fritsch.Convective parameterization for mesoscalemodels:The Kain-Fritcsh scheme.The representation of cumulus convection in numerical models,K.A.Emanuel and D.J.Raymond,Eds.Amer.Meteor.Soc.,Boston,MA,,1993:246pp.
    [9]Betts,A.K.A new convective adjustment scheme.Part Ⅰ:Observational and theoretical basis.Quart.J.Roy.Meteor.Soc.,1986,112:677-691.
    [10]Betts,A.K.,M.J.Miller.A new convective adjustment scheme.Part Ⅱ:Single column tests using GATE wave,BOMEX,and arctic air-mass data sets.Quart.J.Roy.Meteor.Soc.,1986,112:693-709.
    [11]Mlawer,E.J.,S.J.Taubman,P.D.Brown,等.Radiative transfer for inhomogeneous atmospheres:RRTM,a validated correlated-k model for the longwave.J.Geophys.Res.,1997,102(D14):16663-16682.
    [12]Dudia,J.Numerical study of.convection observed during the winter monsoon experiment using amesoscale two-dimensional model.J.Atmos.Sci.,1989,46:3077-3107.
    [13]Chou,M.D.,M.J.Suarez.An efficient thermal infrared radiation parameterization for use in general circuiation models.NASA Tech.Memo.,1994, 104606(3):85pp.
    [14]Lacis,A.A.,J.E.Hansen.A parameterization for the absorption of solar radiation in the earth's atmosphere.J.Atmos.Sci.,1974,31:118-133.
    [15]Hong,S.-Y.,H.-L.Pan.Nonlocal boundary layer vertical diffusion in a medium-range forecast model.Mon.Wea.Rev.,1996,124:2322-2339.
    [16]Janjic,Z.I.The step-mountain coordinate:physical package.Mon.Wea.Rev.,1990,118:1429-1443.
    [17]Janjic,Z.I.The step-mountain eta coordinate model:further developments of the convection,viscous sublayer and turbulence closure schemes.Mon.Wea.Rev.,1994,122:927-945.
    [18]Paulson,C.A.The mathematical representation of wind speed and temperature profiles in the unstable atmospheric surface layer.J.Appl.Meteor.,1970,9:857-861.
    [19]Dyer,A.J.,B.B.Hicks.Flux-gradient relationships in the constant flux layer.Quart.J.Roy.Meteor.Soc.,1970,96:715-721.
    [20]Janjic,Z.I.The surface layer in the NCEP EtaModel.Eleventh Conference on Numerical Weather Prediction,Norfolk,VA,19-23 August 1996.Amer.Meteor.Soc.,Boston,MA,,1996a:354-355.
    [21]Janjic,Z.I.Comments on "Development and Evaluation of a Convection Scheme for Use in Climate Models." J.Atmos.Sci.,2000,57:3686.
    [22]Chen,S.-H.,J.Dudhia.Annual report:WRF physics.Air Force Weather Agency,2000:38pp.
    [23]吴绍洪,尹云鹤,郑度,等.近30年中国陆地表层干湿状况研究.中国科学(D辑),2005,35(3):276-283.
    [24]潘守文.现代气候学原理.北京:气象出版社,1994:128-137.
    [25]Penman,H.L..Natural evaporation from open water,bare soil,and grass.Proceedings,Royal Society,London 193,1948:120-146.
    [26]王守荣.水文模式DHSVM与区域气候模式RegCM2/China嵌套模拟试验.气象学报,2002,60(4):421-427.
    [27]刘春蓁.气候变化对我国水文水资源的可能影响.水科学进展,1997,8(3):220-225.
    [1]仆维俊.visual Basic 6.0完全自学手册.北京:机械工业出版社.2007.
    [2]缪海洋.基于GIS的圩区水系规划计算机辅助设计系统开发.扬州大学硕士学位论文,2006.
    [3]彭国伦.Fortran 95程序设计.北京:中国电力出版社,2005.
    [4]薛伟.MapObjects:地理信息系统程序设计.北京:国防工业山版社,2004.
    [5]张轶辉.基于MapObjeCtS下的GIS二次开发.中南大学,2005.
    [6]朱从旭,邓宏贵.用VB利Fortran混合编程开发科学计算与作图软件.计算机应用,2000,4(20):65-67.
    [7]封基良,林灿星.Visual Fortran与Visual Basic混合编程.交通与计算机,2002,20(107):62-64.
    [8]黄瑞,徐学军.基于MapObjeCtS的流域6IS系统开发及应用.计算机工程,2003,13:186-187

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700