🏠 🔎 © 🔁 ？

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 km to 160 km)
-
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)
Get data ⛃

You may be interested in...

Dust number density (given) on Mars dependence from Time in Ls 0-10° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Height 10 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 0-10° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Height 10 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Pressure on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 130°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Pressure on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 130°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water vapor mix. ratio on Mars dependence from Longitude -180-180° and Latitude -10-90° in North polar stereographic projection with Diurnally averaged, Ls 76°, Alt 0 km. In version 1.089: Water cycle WITH molecular diffusion, CO2 cycle, dust bimodal distribution and GW.
Water vapor mix. ratio on Mars dependence from Longitude -180-180° and Latitude -10-90° in North polar stereographic projection with Diurnally averaged, Ls 76°, Alt 0 km. In version 1.089: Water cycle WITH molecular diffusion, CO2 cycle, dust bimodal distribution and GW.
Water vapor on Mars dependence from Time in Ls 160-360° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Lat -55°, Summing Height 0-100 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water vapor on Mars dependence from Time in Ls 160-360° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Lat -55°, Summing Height 0-100 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water ice number density on Mars dependence from Time in Ls 50-200° in Equirectangular (default) projection with Diurnally averaged, Lon -107°, Lat -3°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Water ice number density on Mars dependence from Time in Ls 50-200° in Equirectangular (default) projection with Diurnally averaged, Lon -107°, Lat -3°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Temperature on Mars dependence from Longitude -180-180° and Latitude -30-90° in North polar stereographic projection with Diurnally averaged, Ls 76°, Height 15 km. In version 1.089: Water cycle WITH molecular diffusion, CO2 cycle, dust bimodal distribution and GW.
Temperature on Mars dependence from Longitude -180-180° and Latitude -30-90° in North polar stereographic projection with Diurnally averaged, Ls 76°, Height 15 km. In version 1.089: Water cycle WITH molecular diffusion, CO2 cycle, dust bimodal distribution and GW.