Wintertime aerosol measurements during the Chilean Coastal Orographic Precipitation Experiment

被引:2
|
作者
Fults, Sara Lynn [1 ]
Massmann, Adam K. [2 ]
Montecinos, Aldo [3 ]
Andrews, Elisabeth [4 ,5 ]
Kingsmill, David E. [5 ]
Minder, Justin R. [2 ]
Garreaud, Rene D. [6 ]
Snider, Jefferson R. [1 ]
机构
[1] Univ Wyoming, Laramie, WY 82071 USA
[2] SUNY Albany, Albany, NY 12222 USA
[3] Univ Concepcion, Concepcion, Chile
[4] NOAA ESRL Global Monitoring Div, Boulder, CO USA
[5] Univ Colorado, Boulder, CO 80309 USA
[6] Univ Chile, Santiago, Chile
基金
美国国家科学基金会;
关键词
CLOUD CONDENSATION NUCLEI; MARINE BOUNDARY-LAYER; HYGROSCOPIC GROWTH; SIZE DISTRIBUTIONS; PARTICLE-SIZE; AIR MASSES; NUMBER; SPECTROMETER; ATLANTIC; CCN;
D O I
10.5194/acp-19-12377-2019
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Chilean Coastal Orographic Precipitation Experiment (CCOPE) was a 3-month field campaign (June, July and August 2015) that investigated wintertime coastal rain events. Reported here are analyses of aerosol measurements made at a coastal site during CCOPE. The aerosol monitoring site was located near Arauco, Chile. Aerosol number concentrations and aerosol size distributions were acquired with a condensation particle counter (CPC) and an ultra high sensitivity aerosol spectrometer (UHSAS). Arauco CPC data were compared to values measured at the NOAA observatory Trinidad Head (THD) on the northern Pacific coast of California. The winter-averaged CPC concentration at Arauco is 2971 +/- 1802 cm(-3); at THD the average is 1059 +/- 855 cm(-3). Despite the typically more pristine South Pacific region, the Arauco average is larger than at THD (p < 0.01). Aerosol size distributions acquired during episodes of onshore flow were analyzed with Kohler theory and used to parameterize cloud condensation nuclei activation spectra. In addition, sea salt aerosol (SSA) concentration was parameterized as a function of sea surface wind speed. It is anticipated these parameterizations will be applied in modeling of wintertime Chilean coastal precipitation.
引用
收藏
页码:12377 / 12396
页数:20
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