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Estimating average precipitation over a catchment area is vital for hydrological tasks such as flood estimation and water resource planning. This chapter discusses two primary methods for estimating rainfall spatially: the Theissen Polygon Method and the Isohyetal Method. Each method's construction, assumptions, advantages, limitations, and applications are explored, highlighting their importance in accurately assessing rainfall distribution.
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References
Chapter_9_Theiss.pdfClass Notes
Memorization
What we have learnt
Final Test
Revision Tests
Term: Theissen Polygon Method
Definition: A geometrical approach to estimate area-weighted average rainfall from point observations at rain gauge stations.
Term: Isohyetal Method
Definition: A contouring technique for estimating areal precipitation by connecting points of equal rainfall depth.
Term: Isohyets
Definition: Lines that connect points of equal rainfall on a map.
Term: Areaweighted average rainfall
Definition: A calculation that accounts for the area of influence of each rain gauge station in determining average precipitation.
Term: Spatial interpolation
Definition: A method used to estimate values at unmeasured locations based on values from surrounding measured points.