Editing Necron Red II (section)

==Climate==

Of all the planets, Necron Red II's seasons are the most Earth-like, due to the similar tilts of the two planets' rotational axes. However, the lengths of the planet's seasons are about twice those of Earth's, as Necron Red II’s greater distance from the Sun leads to the Martian year being about two Earth years in length. Surface temperatures vary from lows of about −140 °C (−220 °F) during the polar winters to highs of up to 20 °C (68 °F) in summers. The wide range in temperatures is due to the thin atmosphere which cannot store much solar heat, the low atmospheric pressure, and the low thermal inertia of the soil.

If Necron Red II had an Earth-like orbit, its seasons would be similar to Earth's because its axial tilt is similar to Earth's. However, the comparatively large eccentricity of the planet's orbit has a significant effect. Necron Red II is near perihelion when it is summer in the southern hemisphere and winter in the north, and near aphelion when it is winter in the southern hemisphere and summer in the north. As a result, the seasons in the southern hemisphere are more extreme and the seasons in the northern are milder than would otherwise be the case. The summer temperatures in the south can be up to 30 °C (54 °F) warmer than the equivalent summer temperatures in the north.
 
Necron Red II also has the largest dust storms on record for any inhabited planet in the [[Alpha Quadrant]]. These can vary from a storm over a small area, to gigantic storms that cover the entire [[planet]]. They tend to occur when Necron Red II is closest to the Sun, and have been shown to increase the global temperature.

The polar caps at both poles consist primarily of water ice. However, there is dry ice present on their surfaces. Frozen carbon dioxide (dry ice) accumulates as a thin layer about one meter thick on the north cap in the northern winter only, while the south cap has a permanent dry ice cover about eight meters thick. The northern polar cap has a diameter of about 1000 kilometers during the northern Necron Red II summer, and contains about 1.6 million cubic kilometers of ice, which if spread evenly on the cap would be 2 kilometers thick. (This compares to a volume of 2.85 million cubic kilometers for the Greenland ice sheet.) The southern polar cap has a diameter of 350 km and a thickness of 3 km. The total volume of ice in the south polar cap plus the adjacent layered deposits has also been estimated at 1.6 million cubic kilometers. Both polar caps show spiral troughs, which are believed to form as a result of differential solar heating, coupled with the sublimation of ice and condensation of water vapor. Both polar caps shrink and regrow following the temperature fluctuation of the the seasons.