Tudung es kutub Mars
(Dialihkan dari Tudung es Mars)
Tudung kutub Utara pada 1999
Tudung kutub Selatan pada 2000
Planet Mars memiliki dua tudung es kutub permanen. Pada musim dingin di kutub tersebut, wilayah tersebut mengalami kegelapan dan menyebabkan deposisi 25–30% atmosfer dalam kandungan es CO2 (es kering).[1]
Pranala luar[sunting | sunting sumber]
- http://seg.org/podcast/Post/4604/Episode-10-Remote-sensing-on-Mars Podcast describing the use of SHARAD radar data to explore the ice caps
- https://sharad.psi.edu/3D/movies/SHARAD_PB3D_depth_20161223.mp4 Diarsipkan 2018-04-17 di Wayback Machine. High-resolution movie showing the interior of the north polar ice cap in 3D, as determined with SHARAD radar data
- https://sharad.psi.edu/3D/movies/SHARAD_PA3D_depth_20170105.mp4 Diarsipkan 2018-04-17 di Wayback Machine. High-resolution movie showing the interior of the south polar ice cap in 3D, as determined with SHARAD radar data
Referensi[sunting | sunting sumber]
- ^ Mellon, J. T.; Feldman, W. C.; Prettyman, T. H. (2003). "The presence and stability of ground ice in the southern hemisphere of Mars". Icarus. 169 (2): 324–340. Bibcode:2004Icar..169..324M. doi:10.1016/j.icarus.2003.10.022.
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