High-resolution local gravity model of the south pole of the Moon from GRAIL extended mission data

We estimated a high-resolution local gravity field model over the south pole of the Moon using data from the Gravity Recovery and Interior Laboratory's extended mission. Our solution consists of adjustments with respect to a global model expressed in spherical harmonics. The adjustments are exp...

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Bibliographic Details
Main Authors: Goossens, Sander (Author), Sabaka, Terence J. (Author), Nicholas, Joseph B. (Author), Lemoine, Frank G. (Author), Rowlands, David D. (Author), Mazarico, Erwan Matias (Contributor), Neumann, Gregory A. (Author), Smith, David Edmund (Contributor), Zuber, Maria (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: American Geophysical Union (AGU), 2015-07-31T12:05:12Z.
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Online Access:Get fulltext
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100 1 0 |a Goossens, Sander  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences  |e contributor 
100 1 0 |a Mazarico, Erwan Matias  |e contributor 
100 1 0 |a Smith, David Edmund  |e contributor 
100 1 0 |a Zuber, Maria  |e contributor 
700 1 0 |a Sabaka, Terence J.  |e author 
700 1 0 |a Nicholas, Joseph B.  |e author 
700 1 0 |a Lemoine, Frank G.  |e author 
700 1 0 |a Rowlands, David D.  |e author 
700 1 0 |a Mazarico, Erwan Matias  |e author 
700 1 0 |a Neumann, Gregory A.  |e author 
700 1 0 |a Smith, David Edmund  |e author 
700 1 0 |a Zuber, Maria  |e author 
245 0 0 |a High-resolution local gravity model of the south pole of the Moon from GRAIL extended mission data 
260 |b American Geophysical Union (AGU),   |c 2015-07-31T12:05:12Z. 
856 |z Get fulltext  |u http://hdl.handle.net/1721.1/97926 
520 |a We estimated a high-resolution local gravity field model over the south pole of the Moon using data from the Gravity Recovery and Interior Laboratory's extended mission. Our solution consists of adjustments with respect to a global model expressed in spherical harmonics. The adjustments are expressed as gridded gravity anomalies with a resolution of 1/6° by 1/6° (equivalent to that of a degree and order 1080 model in spherical harmonics), covering a cap over the south pole with a radius of 40°. The gravity anomalies have been estimated from a short-arc analysis using only Ka-band range-rate (KBRR) data over the area of interest. We apply a neighbor-smoothing constraint to our solution. Our local model removes striping present in the global model; it reduces the misfit to the KBRR data and improves correlations with topography to higher degrees than current global models. 
546 |a en_US 
655 7 |a Article 
773 |t Geophysical Research Letters