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CivilWater Resources Management
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If area and rainfall in respective rainguage station are given which method is usefull..

A

aerithmetic average method

B

Theissen polygon method

C

Iso-Hyetal Method

D

all of the above

Correct Answer

тЪЩя╕П TE тАв Technical Concept & PrincipleCivilWater Resources Management
Option B

Theissen polygon method

Quick Summary:

The Thiessen polygon method calculates the average rainfall over a catchment area by assigning weights to each rain gauge station based on the area of the polygon surrounding it. The area is determined by drawing perpendicular bisectors between adjacent gauges to form unique influence zones.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

The Thiessen polygon method calculates the average rainfall over a catchment area by assigning weights to each rain gauge station based on the area of the polygon surrounding it. The area is determined by drawing perpendicular bisectors between adjacent gauges to form unique influence zones.

ЁЯФв Key Formulas

Pavg=тИСPiAiтИСAiP_{avg} = \frac{\sum P_i A_i}{\sum A_i}PavgтАЛ=тИСAiтАЛтИСPiтАЛAiтАЛтАЛ тАФ Average areal rainfall

тЪЩя╕П Working Principle

The catchment is divided into polygons such that any point within a polygon is closer to the rain gauge located inside it than to any other gauge. The average rainfall is then computed as the weighted average of the rainfall at each station, where weights are the proportions of the total area covered by each polygon.

ЁЯУМ Key Points
  • тЦ╕

    Accounts for non-uniform distribution of rain gauges.

  • тЦ╕

    More accurate than the arithmetic mean method.

  • тЦ╕

    Does not account for orographic effects (unlike Iso-Hyetal method).

  • тЦ╕

    Once the network is established, the polygons remain fixed.

тЬЕ Advantages
  • тЦ╕

    Superior to arithmetic average in handling non-uniform spatial distribution.

  • тЦ╕

    Mathematically objective and repeatable process.

тЭМ Disadvantages / Limitations
  • тЦ╕

    Does not consider elevation or topographical changes.

  • тЦ╕

    Rigid structure; requires re-calculation if a rain gauge is added or removed.

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Catchment areas with flat topography.

  • тЦ╕

    Hydrological modeling where gauge spatial weight is required.

ЁЯФД Comparison Table
FeatureArithmetic MethodThiessen Method

Requirement

Simple Mean

Thiessen Polygon

Spatial Bias

Ignores Area

Weights by Area

ЁЯУД Additional Information
  • тЦ╕

    The Thiessen polygon method is essentially a weighted average method where the weights are the Thiessen coefficients.

  • тЦ╕

    Option A (Arithmetic average) assumes uniform distribution; Option C (Iso-Hyetal) uses lines of equal rainfall and is generally considered the most accurate but complex.

ЁЯУК Diagram / Illustration
Average Rainfall Formula
Pavg=тИСPiAiAtotalP_{avg} = \frac{\sum P_i A_i}{A_{total}}PavgтАЛ=AtotalтАЛтИСPiтАЛAiтАЛтАЛ
Where Pс╡в is rainfall and Aс╡в is polygonarea
тЬЕ

B is correct тАФ The Thiessen polygon method determines the areal average rainfall by weighting individual gauge readings based on their surrounding polygonal influence area.

Core Concepts Used
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Areal Precipitation Weighted Average Perpendicular Bisectors
ЁЯТб EXAM TIP

If the problem mentions 'topographical influence' or 'elevation', the Iso-Hyetal method is usually the preferred choice over the Thiessen method.

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