Fluvial geomorphology

被引：15
作者：
Hardy, Richard J. [1 ]
机构：
[1] Univ Durham, Dept Geog, Durham DH1 3LE, England
来源：
PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT | 2006年 / 30卷 / 04期
基金：
英国自然环境研究理事会;
关键词：
D O I：
10.1191/0309133306pp498pr
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
[No abstract available]
引用
收藏
页码：553 / 567
页数：15
相关论文
共 71 条
[31]  
Hu TS, 2005, HYDROLOG SCI J, V50, P299, DOI 10.1623/hysj.50.2.299.61794
[32]   Implications of bank failures and fluvial erosion for gully development: Field observations and modeling [J].
Istanbulluoglu, E ;
Bras, RL ;
Flores-Cervantes, H ;
Tucker, GE .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2005, 110 (F1)
[33]   Effect of submerged flexible vegetation on flow structure and resistance [J].
Järvelä, J .
JOURNAL OF HYDROLOGY, 2005, 307 (1-4) :233-241
[34]  
Kies A, 2005, ANN GEOPHYS-ITALY, V48, P101
[35]   Large woody debris characteristics and contributions to pool formation in forest streams of the Boreal Shield [J].
Kreutzweiser, DP ;
Good, KP ;
Sutton, TM .
CANADIAN JOURNAL OF FOREST RESEARCH, 2005, 35 (05) :1213-1223
[36]   The importance of high-resolution monitoring in erosion and deposition dynamics studies: examples from estuarine and fluvial systems [J].
Lawler, DM .
GEOMORPHOLOGY, 2005, 64 (1-2) :1-23
[37]   Sediment sorting and transport by flash floods [J].
Malmon, DV ;
Reneau, SL ;
Dunne, T .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2004, 109 (F2)
[38]   Two dimensional modelling of flood flows and suspended sediment transport: the case of the Brenta River, Veneto (Italy) [J].
Martini, P ;
Carniello, L ;
Avanzi, C .
NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2004, 4 (01) :165-181
[39]   Theoretical regime equations for mobile gravel-bed rivers with stable banks [J].
Millar, RG .
GEOMORPHOLOGY, 2005, 64 (3-4) :207-220
[40]   Practical aspects of ADCP data use for quantification of mean river flow characteristics; Part 1: moving-vessel measurements [J].
Muste, M ;
Yu, K ;
Spasojevic, M .
FLOW MEASUREMENT AND INSTRUMENTATION, 2004, 15 (01) :1-16
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