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López-Valverde Miguel A. Gerard Jean-Claude González-Galindo Francisco Vandaele Ann-Carine Thomas Ian Korablev Oleg Ignatiev Nikolai Fedorova Anna Montmessin Franck Määttänen Anni Guilbon Sabrina Lefevre Franck Patel Manish R. Jiménez-Monferrer Sergio García-Comas Maya Cardesin Alejandro Wilson Colin F. Clancy R. T. Kleinböhl Armin McCleese Daniel J. Kass David M. Schneider Nick M. Chaffin Michael S. López-Moreno José Juan Rodríguez Julio 《Space Science Reviews》2018,214(1):1-31
Space Science Reviews - Time measured by an ideal clock crucially depends on the gravitational potential and velocity of the clock according to general relativity. Technological advances in... 相似文献
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Olivier Mousis Eric Chassefière Jérémie Lasue Vincent Chevrier Megan E. Elwood Madden Azzedine Lakhlifi Jonathan I. Lunine Franck Montmessin Sylvain Picaud Frédéric Schmidt Timothy D. Swindle 《Space Science Reviews》2013,174(1-4):213-250
Thermodynamic conditions suggest that clathrates might exist on Mars. Despite observations which show that the dominant condensed phases on the surface of Mars are solid carbon dioxide and water ice, clathrates have been repeatedly proposed to play an important role in the distribution and total inventory of the planet’s volatiles. Here we review the potential consequences of the presence of clathrates on Mars. We investigate how clathrates could be a potential source for the claimed existence of atmospheric methane. In this context, plausible clathrate formation processes, either in the close subsurface or at the base of the cryosphere, are reviewed. Mechanisms that would allow for methane release into the atmosphere from an existing clathrate layer are addressed as well. We also discuss the proposed relationship between clathrate formation/dissociation cycles and how potential seasonal variations influence the atmospheric abundances of argon, krypton and xenon. Moreover, we examine several Martian geomorphologic features that could have been generated by the dissociation of extended subsurface clathrate layers. Finally we investigate the future in situ measurements, as well as the theoretical and experimental improvements that will be needed to better understand the influence of clathrates on the evolution of Mars and its atmosphere. 相似文献
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F. Montmessin 《Space Science Reviews》2006,125(1-4):457-472
Solar variability influences the climate of a planet by radiatively forcing changes over a certain timescale; orbital variations
of a planet, which yield similar solar forcing modulations, can be studied within the same scientific context. It is known
for Earth that obliquity changes have played a critical role in pacing glacial and interglacial eras. For Mars, such orbital
changes have been far greater and have generated extreme variations in insolation. Signatures associated with the presence
of water ice reservoirs at various positions across the surface of Mars during periods of different orbital configurations
have been identified. For this reason, it has been proposed that Mars is currently evolving between ice ages. The advent of
climate tools has given a theoretical frame to the study of orbitally-induced climate changes on Mars. These models have provided
an explanation to many puzzling observations, which when put together have permitted reconstruction of almost the entire history
of Mars in the last 10 million years. This paper proposes to give an overview of the scientific work dedicated to this topic. 相似文献
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