This paper describes the procedure we have used to produce multi-annual dust scenarios for Martian years 24 to 30 from a multi-instrument dataset of total dust opacity observations. This procedure includes gridding the observations on a pre-defined longitude-latitude grid with 1 sol resolution in time, and spatially interpolating the results to obtain complete daily maps of total dust opacity. We used weighted binning as gridding technique, and spatial kriging as method of interpolation. The new dust scenarios are available as NetCDF files, easy to interface to any model including global circulation and mesoscale models for the Martian atmosphere. 1
This document compares the MCD with such observational data as is available concerning the atmospher...
We present spatial and temporal distributions of dust on Mars from Ls = 331° in MY 26 until Ls = 80...
This is a dataset of meteorological variables for the atmosphere of Mars, obtained by assimilating m...
We have produced a multiannual climatology of airborne dust from martian year 24–31 using multiple d...
We have reconstructed the climatology of airborne dust from Martian years (MY) 24 to 31 using multip...
International audienceWe have reconstructed longitude‐latitude maps of column dust optical depth (CD...
A new dust data assimilation scheme has been developed for the UK version of the Laboratoire de M&ea...
Airborne dust is the main driver of Martian atmospheric temperature, and accurately accounting for i...
Our Global Circulation Model (GCM) simulates the atmospheric environment of Mars. It is developped a...
We study the interannual variability of dust storms on Mars in an assimilation of thermal profiles a...
We used thermal-infrared spectra returned by the Mars Express Planetary Fourier Spectrometer (PFS/ME...
The redistribution of a finite amount of martian surface dust during global dust storms and in the i...
The dust cycle is critically important for Mars' current climate system. Suspended atmospheric dust ...
This document compares the MCD with such observational data as is available concerning the atmospher...
We present spatial and temporal distributions of dust on Mars from Ls = 331° in MY 26 until Ls = 80...
This is a dataset of meteorological variables for the atmosphere of Mars, obtained by assimilating m...
We have produced a multiannual climatology of airborne dust from martian year 24–31 using multiple d...
We have reconstructed the climatology of airborne dust from Martian years (MY) 24 to 31 using multip...
International audienceWe have reconstructed longitude‐latitude maps of column dust optical depth (CD...
A new dust data assimilation scheme has been developed for the UK version of the Laboratoire de M&ea...
Airborne dust is the main driver of Martian atmospheric temperature, and accurately accounting for i...
Our Global Circulation Model (GCM) simulates the atmospheric environment of Mars. It is developped a...
We study the interannual variability of dust storms on Mars in an assimilation of thermal profiles a...
We used thermal-infrared spectra returned by the Mars Express Planetary Fourier Spectrometer (PFS/ME...
The redistribution of a finite amount of martian surface dust during global dust storms and in the i...
The dust cycle is critically important for Mars' current climate system. Suspended atmospheric dust ...
This document compares the MCD with such observational data as is available concerning the atmospher...
We present spatial and temporal distributions of dust on Mars from Ls = 331° in MY 26 until Ls = 80...
This is a dataset of meteorological variables for the atmosphere of Mars, obtained by assimilating m...