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Search indexed NASA NTRS and DOE OSTI research on propulsion, heat transfer, battery materials and energy systems. Follow report and document links to the original sources.

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182 records · Page 11
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Evaluation of the KOKEE12M/ONSA13NE Baseline as a KOKEE12M/WETTZ13S Backup

USNO's IERS Rapid Service/Prediction Center (RS/PC) uses the KOKEE12M/WETTZ13S (K2/Ws) baseline for its combination solutions. It would be useful for the RS/PC to be able to use backup baselines in case K2 or Ws is not available. While Ws was undergoing repair in late 2022 through early 2023, ONSA13NE (Oe) replaced Ws to provide immediate UT1 for IVS Analysis Center products but also to begin building a data set for the RS/PC to eventually use to ``characterize'' (assess and approve) the K2/Oe baseline for use in its solutions. The RS/PC needs 60 sessions to be able to characterize a baseline, and the data from the repair period provided 58 sessions, with three additional sessions being observed later. Here we evaluate the K2/Oe baseline to see if it is a viable candidate for submission to the RS/PC for characterization. We evaluate the K2/Oe baseline itself and also compare the K2/Oe baseline to the K2/Ws baseline.

VLBI↗
NASA NTRS1996

Venusian k(sub 2) Tidal Love Number from Magellan and PVO Tracking Data

The k(sub 2) potential ove number which scales the tidal deformation of Venus by the Sun has been estimated from Doppler tracking of Magellan and Pioneer Venus Orbiter (PVO) spacecraft data. The nominal range for k(sub 2) from theoretical models is 0.23(less than or equal to)k(sub 2)(less than or equal to)0.29 for a liquid iron core and about 0.17 if the iron core has solidified. Our best estimate of this parameter is k(sub 2) = 0.295 +/- 0.662 (2X formal {delta}) and supports the hypothesis that Venus core is solid.

orbiter pvo↗