Zobrazeno 1 - 5
of 5
pro vyhledávání: '"K. R. Ramsley"'
Autor:
Jatan Mehta, Joel Alexander Wilner, E. Nathan, James W. Head, A. Kothandhapani, Alexandrea G. Pimentel, K. R. Ramsley, Yuan Chen, B. D. Boatwright, C. Adeene Denton, Leif Tokle, Vishesh Vatsal, Hari Prasad Gokul, Udit Shah, J. D. Tarnas, Ariel N. Deutsch, A. M. Palumbo, B. A. Anzures, L. Lark, M. S. Bramble, Grant Casey
Publikováno v:
New Space. 7:137-150
OrbitBeyond, Inc. is a new U.S.-based lunar transportation company. In 2020, it plans to land its Z-01 lander and Ek Choti si Asha (ECA) rover in Mare Imbrium on the Moon. The landing site...
Autor:
K. R. Ramsley, Hannah Kaplan, A. C. Pascuzzo, Ariel N. Deutsch, Erica Jawin, Connor F. Lynch, Le Qiao, A. M. Palumbo, Ross W. K. Potter, James P. Cassanelli, M. S. Bramble, James W. Head, D. K. Weiss, Carle M. Pieters, Lauren Jozwiak
Publikováno v:
Advances in Space Research. 62:2174-2186
Phobos and Deimos are the only natural satellites of the terrestrial planets, other than our Moon. Despite decades of revolutionary Mars exploration and plans to send humans to the surface of Mars in the 2030’s, there are many strategic knowledge g
Autor:
James W. Head, K. R. Ramsley
Publikováno v:
Planetary and Space Science. 138:7-24
A global and uniformly distributed spike of secondary impact craters on Phobos with diameters (D) effective impulse by incorporating the energy conversion inefficiencies of the crater formation process. We also calculate the pre- and post-impact Phob
Autor:
Alexander T. Basilevsky, T.V. Shingareva, A. E. Zubarev, James W. Head, K. R. Ramsley, C.A. Lorenz
Publikováno v:
Planetary and Space Science. 102:95-118
The martian moon Phobos is 26 km×22.8 km×18.2 km in size, and the major landforms on its surface are craters and grooves. We analyzed the visible craters on the surface of Phobos where ~1300 craters≥200 m in diameter, ~70 craters≥1 km, and ~30
Autor:
K. R. Ramsley, James W. Head
Publikováno v:
Planetary and Space Science. 87:115-129
The gravity of Mars and the observation of a thick Phobos regolith suggest that nearly all Phobos ejecta returns to Phobos and re-impacts on Phobos. Primary ejecta from Mars typically impacts Phobos at velocities of ~2–3 km/s and due to the low esc