Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars

Radio occultation measurements with Mariners 6 and 7 provided refractivity data in the atmosphere of Mars at four points above its surface. For an atmosphere consisting predominantly of carbon dioxide, surface pressures between 6 and 7 millibars are obtained at three of the points of measurement, an...

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Published in:Science
Main Authors: Kliore, Arvydas, Fjeldbo, Gunnar, Seidel, Boris L., Rasool, S. I.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1969
Subjects:
Online Access:http://dx.doi.org/10.1126/science.166.3911.1393
https://www.science.org/doi/pdf/10.1126/science.166.3911.1393
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author Kliore, Arvydas
Fjeldbo, Gunnar
Seidel, Boris L.
Rasool, S. I.
author_facet Kliore, Arvydas
Fjeldbo, Gunnar
Seidel, Boris L.
Rasool, S. I.
author_sort Kliore, Arvydas
collection AAAS Resource Center (American Association for the Advancement of Science)
container_issue 3911
container_start_page 1393
container_title Science
container_volume 166
description Radio occultation measurements with Mariners 6 and 7 provided refractivity data in the atmosphere of Mars at four points above its surface. For an atmosphere consisting predominantly of carbon dioxide, surface pressures between 6 and 7 millibars are obtained at three of the points of measurement, and 3.8 at the fourth, indicating an elevation of 5 to 6 kilometers. The temperature profile measured by Mariner 6 near the equator in the daytime indicates temperatures in the stratosphere about 100°K warmer than those predicted by theory. The measurements of Mariner 6 taken at 79°N at the beginning of polar night indicate that conditions are favorable for the condensation of carbon dioxide at almost all altitudes. Mariner 7 measurements taken at 58°S in daytime and 38°N at night also show that carbon dioxide condensation is possible at altitudes above about 25 kilometers. Measurements of the electron density in the ionosphere show that the upper atmosphere is substantially warmer than it was in 1965, possibly because of increased solar activity and closer proximity to the sun.
format Article in Journal/Newspaper
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op_doi https://doi.org/10.1126/science.166.3911.1393
op_source Science
volume 166, issue 3911, page 1393-1397
ISSN 0036-8075 1095-9203
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spelling craaas:10.1126/science.166.3911.1393 2025-01-17T00:23:00+00:00 Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars Kliore, Arvydas Fjeldbo, Gunnar Seidel, Boris L. Rasool, S. I. 1969 http://dx.doi.org/10.1126/science.166.3911.1393 https://www.science.org/doi/pdf/10.1126/science.166.3911.1393 en eng American Association for the Advancement of Science (AAAS) Science volume 166, issue 3911, page 1393-1397 ISSN 0036-8075 1095-9203 journal-article 1969 craaas https://doi.org/10.1126/science.166.3911.1393 2024-05-16T12:54:30Z Radio occultation measurements with Mariners 6 and 7 provided refractivity data in the atmosphere of Mars at four points above its surface. For an atmosphere consisting predominantly of carbon dioxide, surface pressures between 6 and 7 millibars are obtained at three of the points of measurement, and 3.8 at the fourth, indicating an elevation of 5 to 6 kilometers. The temperature profile measured by Mariner 6 near the equator in the daytime indicates temperatures in the stratosphere about 100°K warmer than those predicted by theory. The measurements of Mariner 6 taken at 79°N at the beginning of polar night indicate that conditions are favorable for the condensation of carbon dioxide at almost all altitudes. Mariner 7 measurements taken at 58°S in daytime and 38°N at night also show that carbon dioxide condensation is possible at altitudes above about 25 kilometers. Measurements of the electron density in the ionosphere show that the upper atmosphere is substantially warmer than it was in 1965, possibly because of increased solar activity and closer proximity to the sun. Article in Journal/Newspaper polar night AAAS Resource Center (American Association for the Advancement of Science) Science 166 3911 1393 1397
spellingShingle Kliore, Arvydas
Fjeldbo, Gunnar
Seidel, Boris L.
Rasool, S. I.
Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars
title Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars
title_full Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars
title_fullStr Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars
title_full_unstemmed Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars
title_short Mariners 6 and 7: Radio Occultation Measurements of the Atmosphere of Mars
title_sort mariners 6 and 7: radio occultation measurements of the atmosphere of mars
url http://dx.doi.org/10.1126/science.166.3911.1393
https://www.science.org/doi/pdf/10.1126/science.166.3911.1393