Difference between revisions of "Weather"
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Clouds are visible as a varied stripe moving against the background that straddles world coordinates y = 123(upper) and 122(lower). | Clouds are visible as a varied stripe moving against the background that straddles world coordinates y = 123(upper) and 122(lower). | ||
| − | All rain and snow falls from these two layers, and neither falls above them. | + | All [[Rain|rain]] and [[Snow|snow]] falls from these two layers, and neither falls above them. |
===Shelter=== | ===Shelter=== | ||
Suitable blocks at the lower cloud layer or below will stop rain and snow reaching the area beneath them. | Suitable blocks at the lower cloud layer or below will stop rain and snow reaching the area beneath them. | ||
| − | Barriers include solid blocks and water. | + | Barriers include solid blocks and [[Water|water]]. |
===Contact effects=== | ===Contact effects=== | ||
| − | Puddles, snow, and moss can form as high as the upper cloud layer, while ice and snow blocks can form on the lower. | + | Puddles, snow, and [[Moss|moss]] can form as high as the upper cloud layer, while [[Ice|ice]] and [[Snow blocks|snow blocks]] can form on the lower. |
====Raindrops==== | ====Raindrops==== | ||
Revision as of 00:33, 4 December 2017
Precipitation
Clouds are visible as a varied stripe moving against the background that straddles world coordinates y = 123(upper) and 122(lower).
All rain and snow falls from these two layers, and neither falls above them.
Shelter
Suitable blocks at the lower cloud layer or below will stop rain and snow reaching the area beneath them. Barriers include solid blocks and water.
Contact effects
Puddles, snow, and moss can form as high as the upper cloud layer, while ice and snow blocks can form on the lower.
Raindrops
- Water blocks (puddles) form in 1x1 holes with a dirt floor and dirt walls.
- Moss forms on rock and cobblestone.
Snowflakes
- Ice replaces water.
- Snow forms on most surfaces.
- Snow blocks replace snow given walls, and can pile as deep as the walls allow.
