10 Watershed characteristics

Watershed characteristics directly influence hydrological processes, impacting runoff volume, peak flow, and timing. Understanding these characteristics is crucial for effective watershed management and predicting runoff behavior.




http://ecoursesonline.iasri.res.in/mod/page/view.php?id=2172


Source: http://ecoursesonline.iasri.res.in/mod/page/view.php?id=2172









Diagram Defining Basin Length. (Source: Zavoianu, 2011)



(Source: http://www.fgmorph.com/fg_4_8.php)


Characteristic/TermFormula/DescriptionSignificance for Hydrology & Runoff
Drainage Basin/WatershedArea draining to a pointDefines the area contributing to runoff.
Drainage DivideBoundary between basinsSeparates adjacent watersheds.
Concentration PointOutlet pointMeasurement location for stream flow.
Time of Concentration (Tc)Time for water to reach outlet from farthest pointDetermines peak flow timing.
Stream OrderHierarchy of streams (Horton-Strahler)Indicates drainage network complexity.
Stream Density (Ds)Ds = Ns/A (Ns=streams, A=area)Indicates stream frequency.
Basin Characteristics
Basin Area (A)Measured by planimeter, GIS, mapsRunoff volume, peak flow magnitude.
Basin Length (Lb)Longest flow path to outletTime of concentration, peak flow timing. Lb = 1.312 A^0.568 (small basins)
Basin Slope (S)S = h/L (h=elevation, L=distance)Runoff velocity, erosion potential, peak flow magnitude.
Basin Shape
Form Factor (Ff)Ff = A/L^2 (A=area, L=length)Basin elongation, peak flow characteristics.
Circularity Ratio (Rc)Rc = 12.57 A/Pr^2 (A=area, Pr=perimeter)Basin circularity, peak flow characteristics.
Elongation Ratio (Re)Re = 1.128A^0.5/LBasin elongation, peak flow characteristics.
Compactness Coefficient (Cc)Cc = 0.2821Pr/A^0.5Basin compactness, peak flow characteristics.
Channel Order (Nw)Nw = Rb^(W-w) (Rb=bifurcation ratio)Drainage network complexity, runoff routing.
Channel Length (Lw)Lw = L1 * RL^(w-1) (L1=1st order length, RL=length ratio)Runoff travel time within channels, peak flow timing.
Channel SlopeElevation difference / channel lengthChannel flow velocity, sediment transport.
Drainage Density (Dd)Dd = L/A (L=total channel length, A=area)Drainage network efficiency, overland flow length, infiltration capacity.
Centroid of the BasinWeighted center of watershedHydrologic modeling and analysis.
SurfaceLand cover, soil type, roughnessInfiltration, runoff volume, flow velocity.
OrientationAspect (slope direction)Solar radiation, evapotranspiration.
AltitudeElevationPrecipitation, temperature, snowmelt.
Stream Density (Ds)Ds = Ns/A (Ns = number of streams, A = area)Stream frequency, drainage texture.

 Source: http://ecoursesonline.iasri.res.in/mod/page/view.php?id=409

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