PMID- 12829779 OWN - NLM STAT- MEDLINE DCOM- 20030711 LR - 20131121 IS - 1095-9203 (Electronic) IS - 0036-8075 (Linking) VI - 300 IP - 5628 DP - 2003 Jun 27 TI - CO2 snow depth and subsurface water-ice abundance in the northern hemisphere of Mars. PG - 2081-4 AB - Observations of seasonal variations of neutron flux from the high-energy neutron detector (HEND) on Mars Odyssey combined with direct measurements of the thickness of condensed carbon dioxide by the Mars Orbiter Laser Altimeter (MOLA) on Mars Global Surveyor show a latitudinal dependence of northern winter deposition of carbon dioxide. The observations are also consistent with a shallow substrate consisting of a layer with water ice overlain by a layer of drier soil. The lower ice-rich layer contains between 50 and 75 weight % water, indicating that the shallow subsurface at northern polar latitudes on Mars is even more water rich than that in the south. FAU - Mitrofanov, I G AU - Mitrofanov IG AD - Space Research Institute, Russian Academy of Sciences, Moscow, 117997, Russia. imitrofa@space.ru FAU - Zuber, M T AU - Zuber MT FAU - Litvak, M L AU - Litvak ML FAU - Boynton, W V AU - Boynton WV FAU - Smith, D E AU - Smith DE FAU - Drake, D AU - Drake D FAU - Hamara, D AU - Hamara D FAU - Kozyrev, A S AU - Kozyrev AS FAU - Sanin, A B AU - Sanin AB FAU - Shinohara, C AU - Shinohara C FAU - Saunders, R S AU - Saunders RS FAU - Tretyakov, V AU - Tretyakov V LA - eng PT - Journal Article PT - Research Support, Non-U.S. Gov't PT - Research Support, U.S. Gov't, Non-P.H.S. PL - United States TA - Science JT - Science (New York, N.Y.) JID - 0404511 RN - 0 (Dry Ice) RN - 059QF0KO0R (Water) SB - IM MH - Atmosphere MH - *Dry Ice MH - Extraterrestrial Environment MH - *Mars MH - Seasons MH - Water/*analysis EDAT- 2003/06/28 05:00 MHDA- 2003/07/12 05:00 CRDT- 2003/06/28 05:00 PHST- 2003/06/28 05:00 [pubmed] PHST- 2003/07/12 05:00 [medline] PHST- 2003/06/28 05:00 [entrez] AID - 300/5628/2081 [pii] AID - 10.1126/science.1084350 [doi] PST - ppublish SO - Science. 2003 Jun 27;300(5628):2081-4. doi: 10.1126/science.1084350.