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Estimation of missing rainfall data is crucial in hydrology for designing effective water resources projects. The chapter outlines various estimation methods, criteria for selecting appropriate techniques, and emphasizes the importance of consistency checks using tools like the Double Mass Curve. Additionally, it highlights the role of the Indian Meteorological Department in providing normals for effective data estimation.
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References
Chapter_10_Missi.pdfClass Notes
Memorization
What we have learnt
Final Test
Revision Tests
Term: Arithmetic Mean Method
Definition: A simple method where the average of surrounding stations' rainfall is calculated, applicable when rainfall is uniform.
Term: Normal Ratio Method
Definition: Used when normal rainfall varies more than 10% from those of missing data stations; adjusts for climatic variability.
Term: Inverse Distance Weighting (IDW)
Definition: Estimation based on geographic proximity, where nearby stations' readings influence the missing value.
Term: Double Mass Curve
Definition: A tool for checking the consistency of rainfall data by plotting cumulative readings against neighboring stations.
Term: IMD Normals
Definition: 30-year averages provided by the Indian Meteorological Department, used for consistency checks and as a reference for estimation.