When the humid and warm vapors (
) rise (
or
) and reach the colder regions, they condense and form clouds :.
Loading the clouds (
) with rain (
).
The simplified version relieves the clouds (
) of their load, reverting the character to its original form :
.
) rise (
or
) and reach the colder regions, they condense and form clouds :
.
Loading the clouds (
).
The simplified version relieves the clouds (
) of their load, reverting the character to its original form :
