Match each river basin morphometric parameter with its corresponding quantitative definition and hydrological significance.
- Bifurcation Ratio ()The ratio of the number of stream segments of a given order () to the number of segments of the next higher order (), reflecting structural disturbance.
- Drainage Density ()The ratio of the total length of all stream channels in a basin to the total basin area, indicating surface runoff efficiency and bedrock permeability.
- Stream Frequency ()The total number of stream channel segments of all orders per unit area of the drainage basin, reflecting surface texture and infiltration capacity.
- Form Factor ()The ratio of basin area () to the square of maximum basin length (), describing the outline shape of the basin and flood peak behavior.
Answer
Bifurcation Ratio () pairs with the ratio of stream numbers between successive orders (). Drainage Density () pairs with the total stream length divided by basin area. Stream Frequency () pairs with the total number of stream segments per unit basin area. Form Factor () pairs with the ratio of basin area to the square of basin length.
Each morphometric parameter correctly maps to its distinct mathematical definition and hydrological role: Bifurcation Ratio relates channel counts across orders (); Drainage Density measures stream length per area (); Stream Frequency measures individual stream counts per area (); and Form Factor evaluates areal shape ().
Step-by-Step Solution
Key Concept
Morphometric Analysis of River Basins