Publication Notice: Chemical properties of insoluble precipitation residue particles

CW3E Publication Notice

Chemical properties of insoluble precipitation residue particles

Jessie Creamean posing for a photo while clearing snow from the top of the NOAA trailer at Sugar Pine Dam after the storm on 2/25/11.

This article provides an in-depth analysis of resuspended residues from precipitation samples collected at a remote site in the Sierra Nevada Mountains in California during the 2009-2011 winter seasons. These residues may be used as a benchmark for classification of insoluble precipitation. Knowledge of the precipitation chemistry of insoluble residues coupled with meteorological and cloud microphysical measurements will ultimately improve our understanding of the link between aerosols, clouds, and precipitation.

This paper represents a significant milestone from the CalWater experiment, which is led by members of UCSD/Scripps’ new Centers on aerosols (CAICE) and extreme events (CW3E), as well as NOAA, DOE, NASA, USGS. It also highlights the multi-disciplinary research stimulated by CalWater, and the partnerships between key researchers across organizations. The lead author, Jessie Creamean, received her PhD in atmospheric chemistry from UCSD under Kim Prather using CalWater data, and is now bringing that expertise to a primarily meteorological group in NOAA as she pursues emerging topics in aerosol-precipitation interactions in collaboration with CW3E scientists.

A personal use copy of the article is available here.

Dust storms: enhancing California’s precipitation

Dust Storms: enhancing California’s precipitation

Dust, as shown by orange colors, in a storm approaching California on 24 February 2014. (NASA Earth Observing System Data and Information System)

As CW3E continues to investigate rainfall over California from Atmospheric River storms, other researchers examine the same storms to evaluate the role of dust in enhancing precipitation amounts. A recent KQED story examines the work of Dr. Kim Prather (UCSD; atmospheric chemist). Dr. Prather evaluates the role of dust from storms over Africa and Asia that reach the California coast in 7-10 days. The high altitude particles have been found to increase the amount of rain and snowfall when they coincide with approaching coastal storms. See more on the story (including an audio piece) at: