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  • An evaluation of methods for estimating Manning's n in small mountain streams
  • Alaska ; Discharge ; Flow ; Hydrodynamics ; Mountain ; Roughness ; Stream ; Torrent
  • None of the 11 techniques used for estimating Manning's roughness coefficient in a small mountain stream in Alaska proved suitable. More accurate methods are needed for estimating flow velocities in steep mountain streams with large-scale roughness
  • 1992
  • Secondary flow in anabranch confluences of a braided, graveled-bed stream
  • Alberta ; Canada ; Confluent ; Discharge ; Flow ; Fluvial dynamics ; Fluvial hydrology ; Ground survey ; Hydrodynamics ; Low water ; Stream
  • This paper reports the results of field measurements made with the objective of documenting the primary (downstream) and secondary (cross-stream) flow fields. Measurements of the velocity components were made in two, active, braided river anabranch
  • 1992
  • Relationship between discharge, velocity and flow area for rills eroding loose, non-layered materials
  • A relationship betwen discharge, flow velocity and flow area in rills is established using data from four field and laboratory studies. The proposed relationship may be used to improve performance of deterministic flow routing models when applied
  • to rilled catchments. Furthermore, it allows the calculation of unit stream power, which has been shown to be related to the transporting capacity of overland fow, in terms of slope and discharge.
  • 1992
  • Ungauged catchment modelling. I. Assessment of flood plain flow model enhancements
  • Catchment area;Watershed ; Flood ; Floodplain ; Forecast;Prediction ; Germany ; Hydrology ; Model ; Simulation ; Stream
  • There is major interest in the development of ungauged flood forecasting models. This paper examines possible methods for improving the floodplain flow computation procedures. Specifically, the concepts of momentum exchange and multiple routing
  • 1992
  • Flow competence : a criticism of a classic concept
  • Concept ; Fluvial dynamics ; Fluvial processes ; Grain size distribution;Granulometry ; Hydrodynamics ; Methodology ; Sediment load ; Sedimentary ; Stream
  • 1992
  • Atmospheric circulation ; Climatic variation ; Eastern Europe ; Europe ; Hydrometeorology ; Hydrosphere ; Model ; Plain ; Precipitation ; Stream ; Stream flow
  • 1992
  • Differential bedload transport rates in a gravel-bed stream : a grain-size distribution approach. Discussion and reply
  • on the changing grain-size distributions as the flow discharge and mean bottom stress increase.
  • 1992
  • Travel distance in gravel-bed rivers of tagged particles of various sizes are related to excess stream power estimated for peak discharge. Mean distance of movement, irrespective of grain size, is weakly correlated with stream power, especially near
  • by the data, which are derived from a wide range of flow regime types.
  • 1992
  • Fluvial hydrology ; Linear regression ; Model ; Multivariate analysis ; Regression analysis ; Runoff ; Slovak Republic ; Statistics ; Stream ; Stream flow
  • 1992
  • Catchment area;Watershed ; Drought ; Flood ; Flow ; Flow regime ; Fluvial hydrology ; France ; Hydraulic works ; Loire ; Stream ; Water quality ; Water resources
  • 1992
  • Bibliography ; Carrying capacity ; Channel geometry ; Drainage network ; Floodplain ; Fluvial processes ; Fluvial terrace ; Human impact ; Hydraulic works ; Model ; Sediment budget ; Sediment transport ; Stream flow ; Suspended load
  • 1992
  • Catalonia ; Catchment area;Watershed ; Discharge ; Drainage ; Flood ; Flow ; Infiltration ; Precipitation ; Spain ; Stream ; Urban environment ; Urbanization ; Water parting;Watershed
  • 1992
  • Frequency and importance of major debris-flows in Arctic and other mountains
  • Arctic Ocean;Arctic Region ; Cold area ; Debris flow ; Earth surface processes ; Mass movement ; Mountain ; Norway ; Permafrost ; Precipitation ; Rill wash;Runoff ; Slope dynamics ; Soil erosion ; Sweden ; United States ; Vegetation
  • Etude des coulées de blocs dans les montagnes scandinaves, des précipitations et des mouvements de masse dans l'est des Etats-Unis, des téléconnexions atmosphériques et de leurs conséquences dans les zones sous influence du Gulf Stream.
  • 1992
  • Former USSR ; Hydrometeorology ; Multivariate analysis ; Principal components analysis ; Stream ; Stream flow
  • 1992
  • Fluvial dynamics ; Fluvial processes ; Former USSR ; Human impact ; River bed ; Stream ; Stream flow
  • 1992
  • Amudarya ; Arid area ; Evaporation ; Runoff ; Stream ; Stream flow ; Uzbekistan ; Water cycle ; Water resources
  • 1992
  • Alluvium ; Hydrodynamics ; Ob ; River bed ; Russia ; Sediment load ; Stream ; Stream flow ; Turbidity ; West Siberia
  • 1992
  • . The results suggest three general mechanisms by which bedrock channels erode: 1) vertical wearing of the channel bed due to stream flow; 2) scour by periodic debris flows; and 3) knickpoint propagation. Consequently, application of a single erosion law
  • 1992
  • Czechoslovakia ; Danube ; Flow ; Ground water;Underground water ; Groundwater hydrology ; Human impact ; Slovakia ; Stream flow ; Water economics ; Water resources
  • 1992
  • Climate ; Climate oscillation ; Discharge ; Drought ; El Niño ; Holocene ; South America ; Stream flow
  • 1992