The latest (version 4.3) Mars Climate Database [PDF]
Introduction: The Mars Climate Database (MCD) is a database of meteorological fields derived from General Circulation Model (GCM) numerical simulations of the Martian atmosphere and validated using available observational data.
Desjean, M.-C. +13 more
core
Noble gases as tracers of the origin and evolution of the Martian atmosphere and the degassing history of the planet [PDF]
Noble gas analysis of Martian samples can provide answers to a number of crucial questions. Some of the most obvious benefits will be in Martian chronology, using techniques that have been applied to lunar samples. However, these are by no means the only
Swindle, T. D.
core +1 more source
High-Frequency Orographically Forced Variability in a Single-Layer Model of the Martian Atmosphere [PDF]
A shallow water model with realistic topography and idealized zonal wind forcing is used to investigate orographically forced modes in the Martian atmosphere.
Ingersoll, Andrew P. +1 more
core
Atmospheric predictability of the martian atmosphere: from low-dimensional dynamics to operational forecasting? [PDF]
Not ...
Lewis, S.R. +3 more
core
We report, for the first time, the impact of interplanetary coronal mass ejections (ICME) on the recently discovered O(1S) 557.7 nm dayglow emission in the Martian atmosphere.
Aadarsh Raj Sharma +8 more
doaj +1 more source
Aeolian abrasion of rocks as a mechanism to produce methane in the Martian atmosphere. [PDF]
Safi E +12 more
europepmc +1 more source
Properties of Solar Wind Current Sheets in the Martian Space Environment
Transient current sheets (CSs) are common magnetic structures in the solar wind that can significantly disturb the planetary space environment and cause space weather phenomena.
Yangjun Chen +8 more
doaj +1 more source
Evaporation of ice in planetary atmospheres: Ice-covered rivers on Mars [PDF]
The evaporation rate of water ice on the surface of a planet with an atmosphere involves an equilibrium between solar heating and radiative and evaporative cooling of the ice layer. The thickness of the ice is governed principally by the solar flux which
Sagan, C., Wallace, D.
core +1 more source
Post-mission Viking data anaysis [PDF]
Three Mars data analysis projects from the Viking Mars program were identified initially, and three more came into being as the work proceeded. All together, these six pertained to: (1) the veritical distribution of scattering particles in the Martian ...
Baum, W. A. +3 more
core +1 more source
Millefeuille: The layering of the Martian atmosphere observed in forward scattering geometry. [PDF]
Thomas N +9 more
europepmc +1 more source

