Mars Climatology from Viking 1 After 20 Sols
- 1 October 1976
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 194 (4260) , 78-81
- https://doi.org/10.1126/science.194.4260.78
Abstract
The results from the meteorology instruments on the Viking 1 lander are presented for the first 20 sols of operation. The daily patterns of temperature, wind, and pressure have been highly consistent during the period. Hence, these have been assembled into 20-sol composites and analyzed harmonically. Maximum temperature was 241.8 degrees K and minimum 187.2 degrees K. The composite wind vector has a mean diurnal magnitude of 2.4 meters per second with prevailing wind from the south and counterclockwise diurnal rotation. Pressure exhibits diurnal and semidiurnal oscillations. The diurnal is ascribed to a combination of effects, and the semidiurnal appears to be the solar semidiurnal tide. Similarities to Earth are discussed. A major finding is a continual secular decrease in diurnal mean pressure. This is ascribed to carbon dioxide deposition at the south polar cap.Keywords
This publication has 9 references indexed in Scilit:
- Preliminary Meteorological Results on Mars from the Viking 1 LanderScience, 1976
- Viking: Mars Atmospheric Water Vapor Mapping Experiment—Preliminary Report of ResultsScience, 1976
- Winds on Mars during the Viking season: Predictions based on a general circulation model with topographyGeophysical Research Letters, 1976
- Diurnal Tide in the Martian AtmosphereJournal of the Atmospheric Sciences, 1976
- Seasonal buffering of atmospheric pressure on MarsIcarus, 1975
- The nature of the residual Martian polar capsIcarus, 1974
- DIURNAL WIND VARIATIONS, SURFACE TO 30 KILOMETERSMonthly Weather Review, 1969
- Atmospheric TidesPublished by Springer Nature ,1969
- DIURNAL VARIATIONS IN THE SUMMER WIND FIELD OVER THE CENTRAL UNITED STATESJournal of the Atmospheric Sciences, 1962