Thiessen-Weighted Watershed Rainfall (Three Gauges)

Also known as Thiessen polygon method · Thiessen average rainfall · areal rainfall from rain gauges · watershed average rainfall depth · area weighted rainfall · rain gauge weighting by polygon area · Pw = sum of wi Pi · mean areal precipitation Thiessen · NEH 630 chapter 4 Thiessen method · weighted storm rainfall for the curve number method · Voronoi weighted rainfall

Pw=A1P1+A2P2+A3P3A1+A2+A3P_w = \frac{A_1 P_1 + A_2 P_2 + A_3 P_3}{A_1 + A_2 + A_3}
sig figs

Worked example: SI equal areas: 10, 20, 30 mm over 1 ha each → 20 mm. Press Try an example to run it live, then adjust anything.

Enter your known values, leave one input blank, and solves for the missing one. Tap a variable’s symbol to see what it means, with a typical value. Change any unit and the answer follows.

Where Thiessen-Weighted Watershed Rainfall (Three Gauges) fits

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See also

SCS Curve Number Runoff Depth: Takes the watershed rainfall depth from this page and gives the runoff depth.Rainfall Depth from Intensity and Duration: Turns a gauge's intensity and duration into the depth entered for that gauge here.Rational Method Peak Runoff: The peak flow method that uses a rainfall intensity for the same watershed.Loss-of-Natural-Storage Detention Volume: Needs runoff depths worked from the watershed rainfall found here.
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Thiessen-Weighted Watershed Rainfall (Three Gauges) explained

P1P2P3A1A2A3weightedby areaPwwholewatershed

A rain gauge measures one point, but a runoff calculation wants one rainfall depth for the whole watershed. The Thiessen method, as the Natural Resources Conservation Service describes it in the National Engineering Handbook (Part 630, chapter 4), gets there by giving each gauge its own share of the ground. Draw the perpendicular bisectors between neighbouring gauges and the watershed divides into polygons, so that every point lies in the polygon of its nearest gauge. Each gauge is then taken to represent its whole polygon. A gauge's weight is its polygon area divided by the watershed area, the weights add to 1, and the watershed depth PwP_w is the sum of each weight times its gauge's depth, which is the area-weighted mean written in the formula.

That assumption is the method's real content. The arithmetic is exact once the polygons are drawn, but how good the answer is depends on how well each gauge stands for its polygon. If a gauge is added or removed, the polygons and weights must be redrawn. For more than three gauges, combine two first: the area-weighted mean of two gauges can stand as a single gauge with the sum of their areas, and the result is the same. The handbook does not use the Thiessen method for mountainous watersheds, where elevation strongly controls the rainfall and a gauge is not typical of the ground around it; its isohyetal method is the alternative.

The handbook's Example 4-2 has polygons of 81, 31 and 87 acres in a 199 acre watershed, so weights of 0.407, 0.156 and 0.437. Gauge depths of 1.40, 1.54 and 1.94 inches give weighted depths of 0.570, 0.240 and 0.848 inches, which sum to 1.658 inches; the handbook rounds this to 1.66 inches. The page gives 1.65789, against the printed 1.658. The areas may be in any unit as long as all three match. The page's own example uses three polygons of 1 ha with 10, 20 and 30 mm: equal areas mean equal weights, so the answer is the simple mean, 20 mm.

The calculation also runs backwards. If the watershed depth is known, the page can find a missing gauge depth or polygon area. With the printed average of 1.658 inches, the third gauge comes out at 1.9403 inches, against the printed 1.94. The watershed depth is the input the curve number method wants.

Thiessen-Weighted Watershed Rainfall (Three Gauges) formula

Pw=A1P1+A2P2+A3P3A1+A2+A3P_w = \frac{A_1 P_1 + A_2 P_2 + A_3 P_3}{A_1 + A_2 + A_3}
Where
  • PwP_w= Watershed rainfall depth (mm)
  • P1P_1= Storm rainfall at gauge 1 (mm)
  • P2P_2= Storm rainfall at gauge 2 (mm)
  • P3P_3= Storm rainfall at gauge 3 (mm)
  • A1A_1= Area of the Thiessen polygon of gauge 1 (ha)
  • A2A_2= Area of the Thiessen polygon of gauge 2 (ha)
  • A3A_3= Area of the Thiessen polygon of gauge 3 (ha)
Where this comes from
  • USDA Natural Resources Conservation Service, National Engineering Handbook, Part 630 Hydrology, Chapter 4 Storm Rainfall Depth and Distribution (210-630-H, Amend. 88, August 2019), section 630.0402 Rainfall Over a Watershed, (3) Thiessen Method, Figures 4-11 to 4-14 and Example 4-2 (printed pages 630-4.14 and 630-4.15): gauge depths 1.40, 1.54 and 1.94 in, polygon areas 81, 31 and 87 ac of 199 ac, weights 0.407, 0.156 and 0.437, weighted depths 0.570, 0.240 and 0.848 in, sum 1.658 in, rounded to 1.66 in. US federal work, public domain. Read it
Revised 31 October 2026
Cite this page

formula.expert. (2026, October 31). Thiessen-Weighted Watershed Rainfall (Three Gauges) Calculator. https://formula.expert/solvers/thiessen-weighted-watershed-rainfall