QUANTITATIVE PRECIPITATION ESTIMATION (QPE) BASED ON RADAR DATA WITH Q-MATCHING CORRECTION IN EAST JAVA
Precipitation is any liquid or frozen water that forms in the atmosphere and falls back to the Earth’s surface. One of precipitation measurements is using a surface weather radar that measurement result is in the form of radar reflectivity and converted to precipitation intensity using Z-R or QPE...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/65194 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Precipitation is any liquid or frozen water that forms in the atmosphere and falls
back to the Earth’s surface. One of precipitation measurements is using a surface
weather radar that measurement result is in the form of radar reflectivity and
converted to precipitation intensity using Z-R or QPE radar relationship. The
relationship that is commonly used are Marshall-Palmer and Rosenfeld, but cannot
be applied directly due to location factors and variations in raindrop size. In
Indonesia, development of Z-R has been carried out in Surabaya where the
evalution is still not accurate and the relationship only applied to that area. In
addition, QPE radar result can be biased so that a correction method is needed,
where one of the method is Q-Matching. In this study, a new QPE radar is
developed and used Q-Matching correction with comparing the accuracy between
QPE radar result before and after correction in East Java.
This study uses C-band weather radar data and 20 observation stations in East
Java which are selected in advance by spatial, time availability, and completeness
of data. The data period is December 2018-February 2019, where December 2018-
January 2019 are training period for building linear regression model and
matching distribution functions. Meanwhile February 2019 is used as testing period
for evaluation QPE radar using correlation, RMSE, POD, FAR and comparison of
CDF. The data is averaged per hour before used.
The results showed that Z-R relationship in East Java during training period is Z
= 158,36R1,41. Then in testing period, 5 pairs of distribution functions are used and
it is found that Gamma distribution function generate the best increasing
correlation and decreasing RMSE with values of 5,29% and 85,19% respectively
and CDF of QPE radar is relatively close to the CDF of observed rainfall for
correction using Q-Matching. The prediction results for very light, light, and heavy
rain are relatively better in corrected QPE based on POD and FAR score, although
there are a decrease in POD score for very light rain event and an increase in FAR
score for heavy rain event.
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