GeographyDrainage BasinsA-Level

Drainage Density Calculator

Length of stream channels per unit area of drainage basin.

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Drainage Density

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Overview

Drainage density is a fundamental morphometric property that quantifies the efficiency of a watershed's channel network. It is defined as the total length of all stream channels within a drainage basin divided by the basin's total surface area.

Symbols

Variables

DD = Drainage Density, L = Total Stream Length, A = Basin Area

DD
Drainage Density
km/km²
Total Stream Length
km
Basin Area
km²

Apply it well

When To Use

When to use: This equation is used in hydrology and geomorphology to compare the surface runoff characteristics of different landscapes. It is applied when analyzing soil permeability, vegetation cover, and the structural control of the underlying geology on water flow.

Why it matters: Drainage density directly influences the timing and magnitude of flood peaks; higher density often correlates with faster runoff and increased erosion potential. It helps urban planners and environmental scientists predict how land-use changes might affect local water cycles.

Avoid these traps

Common Mistakes

  • Excluding smaller tributaries from total stream length.
  • Mixing units (e.g. m and km).

One free problem

Practice Problem

A drainage basin has a total area of 50 km². The combined length of all the streams within this basin is 125 km. Calculate the drainage density.

Total Stream Length125 km
Basin Area50 km²

Solve for: DD

Hint: Divide the total stream length by the basin area.

The full worked solution stays in the interactive walkthrough.

References

Sources

  1. Wikipedia: Drainage density
  2. Fundamentals of Geomorphology by Richard J. Huggett
  3. Britannica: Drainage basin
  4. Halliday, Resnick, and Walker, Fundamentals of Physics
  5. Chow, V. T., Maidment, D. R., & Mays, L. W. (1988). Applied Hydrology. McGraw-Hill.
  6. Huggett, R. J. (2011). Fundamentals of Geomorphology (3rd ed.). Routledge.
  7. AQA A-level Geography Textbook