ArmaDB
Workshop mod

AWM - Southeast Asia

by EO · all their mods

An Atmospheric Weather Mod for Southeast Asian terrains.

Players now

11

Servers

33

Rating

94%

18 votes

Subscribers

-

8,404 downloads

Get it on the Workshop reforger.armaplatform.com/workshop/688F3A64E85ECB53

Busiest servers running it 33 in total

All servers

Players on servers with it

daily, last 30 days

0 10 20 30 40 17 Sep 24 Sep 1 Oct 8 Oct 15 Oct peak 37
Average players Low to peak in each bucket

Details

Author
EO
Version
1.0.18
Size
10.4 MB
Licence
APL-ND
Game version
1.7.0.41
Likes
0 / 0 dislikes
Published
7 Feb 2026
Updated
4 months ago
Workshop ID
688F3A64E85ECB53

Recent adoption

30 days: +75 −68 ↑0

Version history

10
  1. v1.0.18 10.4 MB 31 May 2026

    Updated to latest game version.

  2. v1.0.17 10.4 MB 7 Mar 2026
  3. v1.0.16 10.4 MB 26 Feb 2026
  4. v1.0.15 10.4 MB 26 Feb 2026
  5. v1.0.14 10.4 MB 20 Feb 2026
  6. v1.0.13 10.4 MB 20 Feb 2026
Description from the Workshop

As the author I highly recommend using the EO HDR 10 mod as it's specifically designed for AWM. This version of AWM will hopefully reproduce a slice of tropical weather specific to that region, ranging from hot and humid through to heavy monsoons. - Clear Light Fog - Damp Fog - Damp Fog (Thunder) - Monsoon Rain - Monsoon Thunder Increased the weather state transition and duration times, resulting in a faster more dynamic weather system without the need for the time progression multiplier. - Transition time from one weather state to another: 20-30 minutes. - Duration time once forecasted weather state has been reached: 20-30 minutes Weather forecast transition path... - Clear Light Fog > - Damp Fog > - Damp Fog (Thunder) > - Monsoon Rain > - Monsoon Thunder, then back to Clear Light Fog. As monsoons begin and end it is common to observe rainfall from what seems like a cloudless sky, this is to be expected and can occur naturally in this region... Wind Transportation: Strong high-altitude winds can carry rain droplets several miles away from the storm clouds that created them. By the time the rain reaches the ground, the clouds are no longer directly overhead.