High-dimensional experiments for the downward continuation using the LRFMP algorithm
Naomi Schneider, Volker Michel, Nico Sneeuw

TL;DR
This paper advances the application of (Learning) Inverse Problem Matching Pursuits (L)IPMPs) to high-dimensional satellite gravity data for Earth's gravitational potential downward continuation, demonstrating feasibility with over 500,000 data points.
Contribution
It extends (L)IPMPs methods to large-scale, high-dimensional datasets, adapting algorithms for practical use in satellite gravity inverse problems.
Findings
Successfully applied to datasets with over 500,000 points
Achieved a resolution of approximately 20 km
Provided updated code for big data applications
Abstract
Time-dependent gravity data from satellite missions like GRACE-FO reveal mass redistribution in the system Earth at various time scales: long-term climate change signals, inter-annual phenomena like El Nino, seasonal mass transports and transients, e. g. due to earthquakes. For this contemporary issue, a classical inverse problem has to be considered: the gravitational potential has to be modelled on the Earth's surface from measurements in space. This is also known as the downward continuation problem. Thus, it is important to further develop current mathematical methods for such inverse problems. For this, the (Learning) Inverse Problem Matching Pursuits ((L)IPMPs) have been developed within the last decade. Their unique feature is the combination of local as well as global trial functions in the approximative solution of an inverse problem such as the downward continuation of the…
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Taxonomy
TopicsGeophysics and Gravity Measurements · Statistical and numerical algorithms · Reservoir Engineering and Simulation Methods
