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2
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0028667033
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M. T. Zuber et al., Science 266, 1839 (1994).
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(1994)
Science
, vol.266
, pp. 1839
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Zuber, M.T.1
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4
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60149105749
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B. A. Archinal et al, The Unified Lunar Control Network 2005 Open-File Report 2006-1367 ver. 1.0, U.S. Geological Survey, 2006
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B. A. Archinal et al., "The Unified Lunar Control Network 2005" (Open-File Report 2006-1367 ver. 1.0, U.S. Geological Survey, 2006).
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7
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0038414822
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June
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T. Tsubokawa et al., Proc. of the 23rd International Symposium on Space Technology and Science (ISTS), Matsue Shimane, Japan, 26 May to 2 June 2002 (2002), pp. 1986-1991.
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(2002)
Proc. of the 23rd International Symposium on Space Technology and Science (ISTS), Matsue Shimane, Japan, 26 May to 2
, pp. 1986-1991
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Tsubokawa, T.1
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9
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60149103081
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One remaining concern is about systematic errors in measurements of pulse arrivals due to distortion of the return pulse caused by the sloped and/or rough target terrain in combination with unknown albedo effects. This error (range shift) may result in underestimates of ranges by 12 m in the very worst case of 30° slope and 30% surface reflectance before the pulse spreading correction. For moderately flat surfaces, systematic range errors are expected to be 2.5 m 8
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One remaining concern is about systematic errors in measurements of pulse arrivals due to distortion of the return pulse caused by the sloped and/or rough target terrain in combination with unknown albedo effects. This error (range shift) may result in underestimates of ranges by 12 m in the very worst case of 30° slope and 30% surface reflectance before the pulse spreading correction. For moderately flat surfaces, systematic range errors are expected to be 2.5 m (8).
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10
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0042799896
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GEODYN II system description
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vols, SGT Inc
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D. E. Pavlis et al., "GEODYN II system description, vols. 1-5," Contractor Report, SGT Inc. (2006).
-
(2006)
Contractor Report
, vol.1-5
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Pavlis, D.E.1
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12
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60149103305
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N. Namiki et al., Science 323, 900 (2009).
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(2009)
Science
, vol.323
, pp. 900
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Namiki, N.1
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13
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60149102864
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Orbits are determined by full-scale precision force and measurement modeling. For each data arc, estimated parameters include the state vector at epoch, a solar radiation pressure coefficient, empirical accelerations with a once per orbital revolution signature in the along-track and cross-track direction, and measurement biases to absorb systematic effects and mismodeling. Orbit precision has been evaluated by computing orbit overlap differences. Overlap analysis showed a radial consistency of 1 m in general, with outliers (that were excluded from topography data processing) up to 4 m.
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Orbits are determined by full-scale precision force and measurement modeling. For each data arc, estimated parameters include the state vector at epoch, a solar radiation pressure coefficient, empirical accelerations with a once per orbital revolution signature in the along-track and cross-track direction, and measurement biases to absorb systematic effects and mismodeling. Orbit precision has been evaluated by computing orbit overlap differences. Overlap analysis showed a radial consistency of 1 m in general, with outliers (that were excluded from topography data processing) up to 4 m.
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14
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60149093827
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The pointing error is considered to be <0.1° (175 m for 100-km altitude), based on the thermal and other deformation analysis of the main orbiter. Time-tag error is <1 msec (1.5 m along-track for 100-km altitude) through the correction that takes into account the propagation time from the main orbiter to each station and the processing delay on each tracking station. These values (175 m and 1.5 m) are incorporated into the final budget as 3 SD errors.
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The pointing error is considered to be <0.1° (175 m for 100-km altitude), based on the thermal and other deformation analysis of the main orbiter. Time-tag error is <1 msec (1.5 m along-track for 100-km altitude) through the correction that takes into account the propagation time from the main orbiter to each station and the processing delay on each tracking station. These values (175 m and 1.5 m) are incorporated into the final budget as 3 SD errors.
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15
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60149112020
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The laser power has decreased since the middle of April 2008 for yet unexplained reasons, disrupting our data analysis schedule.
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The laser power has decreased since the middle of April 2008 for yet unexplained reasons, disrupting our data analysis schedule.
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18
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84882907026
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M. A. Wieczorek, in Treatise on Geophysics, G. Schubert, Ed. in Chief (Elsevier, Amsterdam, 2007), 10, pp. 165-206.
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M. A. Wieczorek, in Treatise on Geophysics, G. Schubert, Ed. in Chief (Elsevier, Amsterdam, 2007), vol. 10, pp. 165-206.
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22
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60149085314
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We would like to express our great appreciation for the contributions of all staff engineers of NEC Co. Ltd. and the entire staff of the Kaguya (SELENE) project at JAXA in their development and operational support of LALT. We would also express our special thanks to M. Wieczorek for SHTOOLS on his Web site (www.ipgp.jussieu.fr/~wieczor) used for the spherical harmonic analysis and F. Lemoine and his colleagues at NASA Goddard Space Flight Center for invaluable discussions on the orbit accuracy of the Kaguya main orbiter. Finally, we are grateful to the reviewers for their helpful review and comments and to editors for their careful checking of our manuscript. All of the science data obtained by the Kaguya mission will be made available to the public in a PDS-like format (not PDS itself) via the Internet and/or some other method on 1 November 2009. LALT data sets are summarized in table S1
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We would like to express our great appreciation for the contributions of all staff engineers of NEC Co. Ltd. and the entire staff of the Kaguya (SELENE) project at JAXA in their development and operational support of LALT. We would also express our special thanks to M. Wieczorek for SHTOOLS on his Web site (www.ipgp.jussieu.fr/~wieczor) used for the spherical harmonic analysis and F. Lemoine and his colleagues at NASA Goddard Space Flight Center for invaluable discussions on the orbit accuracy of the Kaguya main orbiter. Finally, we are grateful to the reviewers for their helpful review and comments and to editors for their careful checking of our manuscript. All of the science data obtained by the Kaguya mission will be made available to the public in a PDS-like format (not PDS itself) via the Internet and/or some other method on 1 November 2009. LALT data sets are summarized in table S1.
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