MAOAM: Martian Atmosphere Observation and Modeling. v1.058

Data Request

Variable (diurnally averaged)
Time in Ls (from 0° to 360°)
-
Longitude (from -180° to 180°)
-
Latitude (from -90° to 90°)
-
(from 0.0000036 Pa to 607 Pa)
-
Scenario
Setting sets
Logarithm format
Value range (only for 2D)
-
Design



The vertical velocities multiplied by 100
Map projection (only for 2D)
Center point (only for sphere)
Lon: Lat:
Colormap (only for 2D)

You may be interested in...

Zonal velocities on Mars dependence from Latitude -90-90° and Height above surface 0-160 km in Equirectangular (default) projection with Diurnally averaged, Ls 68°, Average Lon -180-180°. In version 1.029: Extended height and CO2 cycle with weak solar acivity.
Zonal velocities on Mars dependence from Latitude -90-90° and Height above surface 0-160 km in Equirectangular (default) projection with Diurnally averaged, Ls 68°, Average Lon -180-180°. In version 1.029: Extended height and CO2 cycle with weak solar acivity.
Surface CO2 ice on Mars dependence from Time in Ls 0-360° and Latitude -90-90° in Equirectangular (default) projection with Time 0 h, Average Lon -180-180°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface CO2 ice on Mars dependence from Time in Ls 0-360° and Latitude -90-90° in Equirectangular (default) projection with Time 0 h, Average Lon -180-180°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water vapor on Mars dependence from Longitude -180-180° and Latitude 0-90° in North polar stereographic projection with Diurnally averaged, Ls 110°, Summing Height 0-120 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water vapor on Mars dependence from Longitude -180-180° and Latitude 0-90° in North polar stereographic projection with Diurnally averaged, Ls 110°, Summing Height 0-120 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Vertical velocities on Mars dependence from Latitude -90-90° and Height above surface 0-160 km in Equirectangular (default) projection with Diurnally averaged, Ls 90°, Average Lon -180-180°. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Vertical velocities on Mars dependence from Latitude -90-90° and Height above surface 0-160 km in Equirectangular (default) projection with Diurnally averaged, Ls 90°, Average Lon -180-180°. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Dust number density (given) on Mars dependence from Time in Ls 0-360° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Lon 0°, Height 1 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Dust number density (given) on Mars dependence from Time in Ls 0-360° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Lon 0°, Height 1 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water vapor on Mars dependence from Longitude -180-180° and Latitude 0-90° in North polar stereographic projection with Diurnally averaged, Ls 100°, Height 0.0000036 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water vapor on Mars dependence from Longitude -180-180° and Latitude 0-90° in North polar stereographic projection with Diurnally averaged, Ls 100°, Height 0.0000036 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.