With the development of computer technology and intercross subjects, the methods of hydrology simulation have great advances. The remarkable trends of watershed hydrological models are the research of physically distributed based models and the use of Geography Information System (GIS) and Remote Sensing (RS) technology. The hydrological model integrated with GIS has many advantages, but it does not mean that the model itself is with high quality. The data arrived from RS is difficult to use in hydrological model directly. Study on mechanism of runoff and streamflow has great foreground to build hydrological model coupled with GIS and RS, and hydrological scale problems should always be paid attention to.
WU Xian feng, LIU Chang ming,
. Progress in Watershed Hydrological Models[J]. PROGRESS IN GEOGRAPHY, 2002
, 21(4)
: 341
-357
.
DOI: 10.11820/dlkxjz.2002.04.007
[1] 赵人俊.流域水文模拟——新安江模型与陕北模型[M].水利电力出版社,北京,1984.
[2] Singh V P.水文系统流域模拟[M].赵卫民等译.郑州:黄河水利出版社,2000.
[3] 袁作新.流域水文模型[M].北京:水利电力出版社,1990.
[4] F reeze R A,H arlan R L.B luep rin t of a p hysically2based d ig itally2sim u lated hyd ro log ical respon se m odel[J].J ou rna l of H y d rology,1969,9:237-258.
[5] A bbo tt M B,Bathu rst J C et al.A n in troduction to the Eu rop ean H yd ro log ical System-System e H yd ro log ique Europ ean,“SH E.”1:h isto ry and p h ilo sop hy of a p hysically based d istribu ted m odeling system[J].J ou rna l of H y d rology,1986a,87:45-59.A n in troduction to the Eu rop ean H yd ro log ical System-System e H yd ro log ique Eu rop ean,“SH E.”2:structu re of ap hysically based d istribu ted m odeling system[J].J ou rna l of H y d rology,1986b,87:61-77.
[6] Sto rm B,J en sen K H.Exp eriences w ith field testing s of SH E on research catchm en ts[J].N ord ic H y d rology,1984,15:283-294.
[7] Charbonneau R,Fo rtin J P,M o rin G.T he CEQU EAU m odel:descrip tion and exam p les of its u se in p rob lem s re-lated to w ater resou rce m anagem en t[J].H y d rolog ica l S cience B u lletin,1977,22(1 3):193-202.
[8] R efsgard J C,H an sen E.A d istribu ted g roundw ater su rface w ater m odel fo r the Su sa2catchm en t,Part)——m odeldescrip tion[J].N ord ic H y d rology,1982,13:299-310.
[9] Benven K J.A d iscu ssion of d istribu ted m odeling[A].In:A bbo tt M B,R efsgard J 2C ed s.D istribu ted H yd ro log ical M odelling[C].K luw er,Do rd rech t,1996.255-278.
[10] 李兰等.流域水文数学物理耦合模型[A].见:朱尔明编.中国水利学会优秀论文集[C].北京:中国三峡出版社,2000.322-329.
[11] 李兰等.流域水文分布动态参数反问题模型[A].见:朱尔明编.中国水利学会优秀论文集[C].北京:中国三峡出版社,2000.48-54.
[12] 郭生练等.分布式流域水文物理模型的研究现状与进展[A].见:刘昌明等编.黄河流域水资源演化规律与可再生性维持机理研究和进展[C].郑州:黄河水利出版社,2001.51-57.
[13] 张建云等.气候异常对我国水资源及水分循环影响的评估模型研究[D].国家“九五”重中之重科技攻关项目,2000.
[14] 郭生练等.基于D EM的分布式流域水文物理模型[J].武汉水利电力大学学报,2000,33(6).
[15] 郭生练等.分布式流域水文物理模型的应用和检验[J].武汉大学学报(工学版),2001,34(1).
[16] 周成虎.地理信息系统概要[M].北京:中国科学技术出版社,1992.
[17] 魏文秋,于建营.地理信息系统在水文学和水资源管理中的应用[J].水科学进展,1997(9):296-300.
[18] M artz W,Garb rech t J.N um erical defin ition of d rainage netw o rk and subcatchm en t areas from d ig ital elevationm odels[J].Com p u ters&Geosciences,1992,18(6):747-761.
[19] Beven K J.D istribu ted H yd ro log icalM odelling A pp lication s of the TO PM OD EL Concep t[M].W IL EY,1997.
[20] 郭方等.以地形为基础的流域水文模型——TO PM OD EL及其拓宽应用[J].水科学进展,2000(9):296-301.
[21] 任立良,刘新仁.数字高程模型在流域水系拓扑结构计算中的应用[J].水科学进展,1999(6):129-134.
[22] 任立良.流域数字水文模型研究[J].河海大学学报,2000(7):127.
[23] M artz W,Garb rech t J.N um erical defin ition of d rainage netw o rk and subcatchm en t areas from d ig ital elevationm odels[J].Com p u ters&Geosciences,1992,18(6):747-761.
[24] 胡著智等.遥感技术与地学应用[M].南京:南京大学出版社,1999.
[25] 刘昌明等.水文循环过程理论与方法的研究进展[A].见:刘昌明等.黄河流域水资源演化规律与可再生性维持机理研究和进展[C].郑州:黄河水利出版社,2001.22-33.
[26] 王燕生.遥感水文模型及其应用[J].水文,1989(5):20-24.
[27] 魏文秋,谢淑琴.遥感资料在SCS模型产流计算中的应用[J].环境遥感,1992(4):243-250.
[28] 徐雨清等.遥感和地理信息系统在半干旱地区降雨——径流关系模拟中的应用[J].遥感技术与应用,2000.
[29] 王腊春,熊江波.用遥感资料建立分块产流模型[J].地理科学,1997(2):76-80.
[30] 夏军.水文学科发展与思考[A].见:21世纪中国水文科学研究的新问题新技术和新方法.北京:科学出版社,2001.18-27.
[31] 陈喜,陈永勤.水文过程中的尺度问题[A].见:21世纪中国水文科学研究的新问题新技术和新方法.北京:科学出版社,2001.28-37.
