🏠 🔎 © 🔁 ？

MAOAM: Martian Atmosphere Observation and Modeling. v1.058

Data Request

Variable (diurnally averaged)
Time in Ls (from 0° to 360°)
-
Hour at 0 lon. (from 0 h to 23 h)
-
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 ⛃

Results

Download as
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude 50-90° in North polar stereographic projection with Diurnally averaged, Ls 120°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.

Description

Surface Water ice on Mars dependence from Longitude -180-180° and Latitude 50-90° in North polar stereographic projection with Diurnally averaged, Ls 120°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.

 

Extensions

© How to cite us?

🔁 Need more power? Use our API

？ Frequently asked questions

Key Words

Mars, MGCM, global circulation, MAOAM, graph, picture, Martian climate, weather, atmosphere, Diurnally averaged, Ls 120°, Height 0 km, Longitude, °, Latitude, °.

 

Disclaimer

The information contained in this website is for general information purposes only. The information is provided by MPS and MIPT and while we endeavour to keep the information up to date and correct, we make no representations or warranties of any kind, express or implied, about the completeness, accuracy, reliability, suitability or availability with respect to the website or the information, products, services, or related graphics contained on the website for any purpose. Any reliance you place on such information is therefore strictly at your own risk. In no event will we be liable for any loss or damage including without limitation, indirect or consequential loss or damage, or any loss or damage whatsoever arising from loss of data or profits arising out of, or in connection with, the use of this website. Through this website you are able to link to other websites which are not under the control of MPS and MIPT. We have no control over the nature, content and availability of those sites. The inclusion of any links does not necessarily imply a recommendation or endorse the views expressed within them. Every effort is made to keep the website up and running smoothly. However, MPS and MIPT take no responsibility for, and will not be liable for, the website being temporarily unavailable due to technical issues beyond our control.

Other similar graphs

Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 100°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 100°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Time in Ls 100-110° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Time in Ls 100-110° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude 60-90° in North polar stereographic projection with Diurnally averaged, Average Ls 0-360°, Height 0 km. In version 1.074: Water cycle, CO2 cycle, dust bimodal distribution and GW.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude 60-90° in North polar stereographic projection with Diurnally averaged, Average Ls 0-360°, Height 0 km. In version 1.074: Water cycle, CO2 cycle, dust bimodal distribution and GW.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Spherical stereographic projection with Diurnally averaged, Ls 120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Spherical stereographic projection with Diurnally averaged, Ls 120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude -90-90° in Equirectangular (default) projection with Diurnally averaged, Ls 120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Time in Ls 100-110° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Average Lat -90-90°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Time in Ls 100-110° in Equirectangular (default) projection with Diurnally averaged, Average Lon -180-180°, Average Lat -90-90°, Height 0 km. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude 50-90° in North polar stereographic projection with Diurnally averaged, Average Ls 90-120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.
Surface Water ice on Mars dependence from Longitude -180-180° and Latitude 50-90° in North polar stereographic projection with Diurnally averaged, Average Ls 90-120°, Height 607 Pa. In version 1.058: Limited height with water cycle, weak diffusion and dust bimodal distribution.