ANALYSIS OF BATHYMETRIC DATA INFLUENCE ON TERRAIN CORRECTION IN GRAVITY DATA PROCESSING: CASE STUDY IN BANDA NEIRA AND KUR ISLAND REGIONS
Terrain correction is one of the crucial stages in gravitational data processing. Previous research at Mount Pandan showed that terrain correction using topographic data resulted in a maximum correction of 14,74 mGal, while in a study in Taiwan Island, the inclusion of bathymetric data led to cor...
Saved in:
Main Author: | |
---|---|
Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/75594 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Terrain correction is one of the crucial stages in gravitational data processing.
Previous research at Mount Pandan showed that terrain correction using
topographic data resulted in a maximum correction of 14,74 mGal, while in a study
in Taiwan Island, the inclusion of bathymetric data led to corrections up to 29,1
mGal. To accommodate terrain correction calculations in research areas in
Indonesia, we utilized both DEMNAS topographic data and BATNAS bathymetric
data in conjunction with gravitational data. DEMNAS topographic data has been
widely used by researchers in gravity methods for terrestrial research areas in
general, while the utilization of BATNAS bathymetric data is still rare, especially
in terrestrial research areas near the sea. In this study, both data sets were
employed in computational terrain correction using a combination of the sloped
triangle method for the near zone, flat-topped square prism for the intermediate
zone, and annular ring for the far zone. The research was conducted in the Banda
Neira and Kur Island regions because between these two regions lies the complex
undulation of the Weber Trench, making it suitable for demonstrating the
contribution of bathymetric data to the total terrain correction.The results indicated
that terrain correction calculations involving bathymetric data significantly
contributed to the maximum total terrain correction values. The difference reached
approximately 81,5 mGal in Banda Neira region and 69,8 mGal in Kur Island
region. However, concerning correction patterns, the contribution of bathymetric
data was inversely related to the contribution of topographic data when correlated
with the topographic conditions. In regions further away from the Weber Trench,
like Banda Neira, the inclusion of bathymetric data showed a terrain correction
pattern similar to using only topographic data. However, in the case of Kur Island,
which is closer to the Weber Trench, the inclusion of bathymetric data has a more
significant impact and is capable of reversing the terrain correction pattern when
using only topographic data. This makes bathymetric data worthy of consideration
for high-resolution gravitational data processing, particularly in areas with
extensive and deep trenches or seas nearby |
---|