Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
Item
Title (Dublin Core)
Precipitation susceptibility in marine stratocumulus and shallow cumulus
from airborne measurements
from airborne measurements
Description (Dublin Core)
Precipitation tends to decrease as aerosol concentration increases in warm marine boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this relationship is captured using the precipitation susceptibility (<i>S</i><sub><i>o</i></sub>) metric. Previously published works disagree on the qualitative behavior of <i>S</i><sub><i>o</i></sub> in marine low clouds: <i>S</i><sub><i>o</i></sub> decreases monotonically with increasing LWP or cloud depth (<i>H</i>) in stratocumulus clouds (Sc), while it increases and then decreases in shallow cumulus clouds (Cu). This study uses airborne measurements from four field campaigns on Cu and Sc with similar instrument packages and flight maneuvers to examine if and why <i>S</i><sub><i>o</i></sub> behavior varies as a function of cloud type. The findings show that <i>S</i><sub><i>o</i></sub> increases with <i>H</i> and then decreases in both Sc and Cu. Possible reasons for why these results differ from those in previous studies of Sc are discussed.
Creator (Dublin Core)
Jung, Eunsil
Albrecht, Bruce A.
Sorooshian, Armin
Zuidema, Paquita
Jonsson, Haflidi H.
Date (Dublin Core)
2018-09-09
Type (Dublin Core)
Text
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
10.5194/acp-16-11395-2016
https://acp.copernicus.org/articles/16/11395/2016/
Source (Dublin Core)
eISSN: 1680-7324
Language (Dublin Core)
eng
