Accumulation mode: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot No edit summary |
m (Rewrite with Template:Term and clean up) |
||
Line 1: | Line 1: | ||
{{Term | |||
|Display title=accumulation mode | |||
{{ | |Definitions={{Definition | ||
{{ | |Num=1 | ||
|Meaning= | |||
[[aerosol|Aerosol]] particles in the size [[range]] 0.5–2 μm in diameter. <br/> The name arises from the fact that [[particles]] in this size range are aerodynamically stable and do not settle out, nor do they agglomerate to form larger particles; thus they tend to accumulate in the [[atmosphere]]. <br/>''See also'' [[agglomeration]]. | |||
}} | |||
}} | |||
Latest revision as of 16:12, 7 November 2023
Aerosol particles in the size range 0.5–2 μm in diameter.
The name arises from the fact that particles in this size range are aerodynamically stable and do not settle out, nor do they agglomerate to form larger particles; thus they tend to accumulate in the atmosphere.
See also agglomeration.