Double MASS Analysis - Lecture notes 1 PDF

Title Double MASS Analysis - Lecture notes 1
Author Lors Mercedes
Course Hydrology
Institution Cornell University
Pages 2
File Size 74.7 KB
File Type PDF
Total Views 145

Summary

Sir Mark...


Description

Topic: DOUBLE MASS ANALYSIS Common Causes of Inconsistency 1. Shifting for rain gauge station to a new location. 2. The Neighborhood of the station undergoing a marked change. 3. Change in the ecosystem due to a calamity such as forest fires, landslides, and 4. Occurrence of an observational error from a certain date.

USE OF DOUBLE MASS ANALYSIS •

This technique is based on the principle that when each recorded data comes form same parent population, they are consistent.



Used to detect if data at a site have been subjected to a significant change in magnitude due to external factors such as problems with instrumentation, observation and practices, or recording conditions.



The checking for inconsistency of a record is done by DOUBLE MASS – CURVE TECHNIQUE.

LIMITATIONS OF DOUBLE MASS ANALYSIS •

Base station should be relatively close to station being tested.



Method should not be used in mountainous areas where precipitation can deviate significantly for hereby stations.



Method should only use for long-term adjustment of precipitation data but not for adjusting daily or storm precipitation.

The Corrected Precipitation Formula

Pcx=P x

Mc Ma

Where;

Pcx - corrected precipitation at any time period Px - original recorded precipitation at time period M c - corrected slope of the mass double curve. M � a - original slope of the mass double curve.

t1 at station X. t 1 at station X.

1st Step The data is sorted in descending order of the year, starting from the latest year 1979. Cumulative values of station M rainfall and the ten station average rainfall values ( ∑ P Ave ) are calculated. 2nd Step Plot the given data then analyze the breakpoint. 3rd Step Solve for

M c using the data from the breakpoint to the latest year.

4th Step Solve for

M a using the data from year 1968 – 1950.

5th Step Apply the corrected precipitation from year 1968 – 1950 using the formula

Pcorrected M =P M

Mc Ma...


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