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| § |
a
/ sin b
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l |
(Beven
and Kirkby 1979)
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l |
a
represents a grid cell’s upslope contributing area per
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contour
length
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l |
sin b is the
local slope of the grid cell
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| § |
The
index calculates drainage area and the ability
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of
the landscape to accommodate hydrologic flow
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l |
The
index defines potential areas of high saturation and
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runoff
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l |
The
topographic index serves as the basis for many
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hydrologic
models
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