Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data

We present a method with which we determined the local lunar gravity field model over the South Pole-Aitken (SPA) basin on the farside of the Moon by estimating adjustments to a global lunar gravity field model using SELENE tracking data. Our adjustments are expressed in localized functions concentr...

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Main Authors: Matsumoto, Koji, Sasaki, Sho, Ishihara, Yoshiaki, Goossens, Sander Johannes
Format: Other/Unknown Material
Language:unknown
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/2060/20140004931
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record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20140004931 2023-05-15T18:22:03+02:00 Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data Matsumoto, Koji Sasaki, Sho Ishihara, Yoshiaki Goossens, Sander Johannes Unclassified, Unlimited, Publicly available February 2012 application/pdf http://hdl.handle.net/2060/20140004931 unknown Document ID: 20140004931 http://hdl.handle.net/2060/20140004931 Copyright, Distribution under U.S. Government purpose rights CASI Lunar and Planetary Science and Exploration GSFC-E-DAA-TN9230 E02005 Journal of Geophysical Research: Planets; 117; E2; 1-16 2012 ftnasantrs 2019-07-21T00:32:11Z We present a method with which we determined the local lunar gravity field model over the South Pole-Aitken (SPA) basin on the farside of the Moon by estimating adjustments to a global lunar gravity field model using SELENE tracking data. Our adjustments are expressed in localized functions concentrated over the SPA region in a spherical cap with a radius of 45deg centered at (191.1 deg E, 53.2 deg S), and the resolution is equivalent to a 150th degree and order spherical harmonics expansion. The new solution over SPA was used in several applications of geophysical analysis. It shows an increased correlation with high-resolution lunar topography in the frequency band l = 40-70, and admittance values are slightly different and more leveled when compared to other, global gravity field models using the same data. The adjustments expressed in free-air anomalies and differences in Bouguer anomalies between the local solution and the a priori global solution correlate with topographic surface features. The Moho structure beneath the SPA basin is slightly modified in our solution, most notably at the southern rim of the Apollo basin and around the Zeeman crater Other/Unknown Material South pole NASA Technical Reports Server (NTRS) Aitken ENVELOPE(-44.516,-44.516,-60.733,-60.733) South Pole
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Lunar and Planetary Science and Exploration
spellingShingle Lunar and Planetary Science and Exploration
Matsumoto, Koji
Sasaki, Sho
Ishihara, Yoshiaki
Goossens, Sander Johannes
Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data
topic_facet Lunar and Planetary Science and Exploration
description We present a method with which we determined the local lunar gravity field model over the South Pole-Aitken (SPA) basin on the farside of the Moon by estimating adjustments to a global lunar gravity field model using SELENE tracking data. Our adjustments are expressed in localized functions concentrated over the SPA region in a spherical cap with a radius of 45deg centered at (191.1 deg E, 53.2 deg S), and the resolution is equivalent to a 150th degree and order spherical harmonics expansion. The new solution over SPA was used in several applications of geophysical analysis. It shows an increased correlation with high-resolution lunar topography in the frequency band l = 40-70, and admittance values are slightly different and more leveled when compared to other, global gravity field models using the same data. The adjustments expressed in free-air anomalies and differences in Bouguer anomalies between the local solution and the a priori global solution correlate with topographic surface features. The Moho structure beneath the SPA basin is slightly modified in our solution, most notably at the southern rim of the Apollo basin and around the Zeeman crater
format Other/Unknown Material
author Matsumoto, Koji
Sasaki, Sho
Ishihara, Yoshiaki
Goossens, Sander Johannes
author_facet Matsumoto, Koji
Sasaki, Sho
Ishihara, Yoshiaki
Goossens, Sander Johannes
author_sort Matsumoto, Koji
title Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data
title_short Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data
title_full Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data
title_fullStr Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data
title_full_unstemmed Local Lunar Gravity Field Analysis over the South Pole-aitken Basin from SELENE Farside Tracking Data
title_sort local lunar gravity field analysis over the south pole-aitken basin from selene farside tracking data
publishDate 2012
url http://hdl.handle.net/2060/20140004931
op_coverage Unclassified, Unlimited, Publicly available
long_lat ENVELOPE(-44.516,-44.516,-60.733,-60.733)
geographic Aitken
South Pole
geographic_facet Aitken
South Pole
genre South pole
genre_facet South pole
op_source CASI
op_relation Document ID: 20140004931
http://hdl.handle.net/2060/20140004931
op_rights Copyright, Distribution under U.S. Government purpose rights
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