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Record #116861:
- #116861
Main publication details
MARC recordVertical transport of water ice at low latitudes in the Martian atmosphere / E. Chassefière, J.E. Blamont.
| Title: | Vertical transport of water ice at low latitudes in the Martian atmosphere / E. Chassefière, J.E. Blamont. |
| Author(s): | Chassefière, E. Blamont, J. E. |
| Date: | 1992. |
| In: | Geophysical Research Letters. (1992.), Vol. 19(9) (1992) |
| Abstract: | Based on solar occultation measurements made from Phobos 2 spacecraft, which show that two condensation levels for H₂O are generally present at 15 and 50 km altitude at low latitudes. Suggests that sublimation level (boundary between saturated region and non-saturated layer below clouds) is close to 35 km altitude. Existence of sublimation level is consequence of two condensation levels. |
| Notes: | Geophysical Research Letters. Vol. 19(9) :945-948 (1992). |
| Keywords: | 551.32 -- Glaciology. 523.43 -- Mars. E13 -- Glaciology: glacioastronomy. |
| SPRI record no.: | 116861 |
LDR 01138naa#a2200000#a#4500 001 SPRI-116861 005 20240416205752.0 007 ta 008 240416s1992####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-116861 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aChassefière, E. 245 10 ‡aVertical transport of water ice at low latitudes in the Martian atmosphere /‡cE. Chassefière, J.E. Blamont. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 945-948 :‡bdiags., table. 500 ## ‡aGeophysical Research Letters. Vol. 19(9) :945-948 (1992). 520 3# ‡aBased on solar occultation measurements made from Phobos 2 spacecraft, which show that two condensation levels for H₂O are generally present at 15 and 50 km altitude at low latitudes. Suggests that sublimation level (boundary between saturated region and non-saturated layer below clouds) is close to 35 km altitude. Existence of sublimation level is consequence of two condensation levels. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a523.43 -- Mars.‡2udc 650 07 ‡aE13 -- Glaciology: glacioastronomy.‡2local 700 1# ‡aBlamont, J. E. 773 0# ‡7nnas ‡tGeophysical Research Letters. ‡gVol. 19(9) (1992) ‡wSPRI-1033 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416