HR: 1340h
AN: A23D-1574 [Abstracts]
TI: Cloud water and aerosol studies in a background marine environment
AU: * Gioda, A
EM: adriana@adam.uprr.pr
AF: University of Puerto Rico, ITES and Department of Chemistry, San Juan, PR 00931,
AU: Mayol-Bracero, O L
EM: omayol@adam.uprr.pr
AF: University of Puerto Rico, ITES and Department of Chemistry, San Juan, PR 00931,
AU: Reyes-Rodriguez, G
EM: gabillo2000@hotmail.com
AF: University of Puerto Rico, ITES and Department of Chemistry, San Juan, PR 00931,
AU: Santos-Figueroa, G
EM: gilmarie17@hotmail.com
AF: University of Puerto Rico, ITES and Department of Chemistry, San Juan, PR 00931,
AU: Morales-de Jesus, R
EM: rjmorales@uprrp.edu
AF: University of Puerto Rico, Physical Sciences Department, San Juan, 00931,
AU: Collett, J
EM: collett@lamar.colostate.edu
AF: Colorado State University, Department of Atmospheric Science, Fort Collins, CO 80525,
AU: Decesari, S
EM: s.decesari@isac.cnr.it
AF: Institute of Atmospheric Science and Climate, CNR, Bologna, 40100, Italy
AU: de Aquino Neto, F R
EM: radler@iq.ufrj.br
AF: Federal University of Rio de Janeiro, LADETEC, Rio de Janeiro, BRA 21941-909,
AU: Klaus, C
EM: cklaus@iq.ufrj.br
AF: Federal University of Rio de Janeiro, LADETEC, Rio de Janeiro, BRA 21941-909,
AU: Bezerra, H
EM: agioda@hotmail.com
AF: Federal University of Rio de Janeiro, LADETEC, Rio de Janeiro, BRA 21941-909,
AB:
The study of aerosol and cloud water chemical composition is essential to understand cloud processing of
different compounds, determining which species are more efficiently removed and which ones stay longer in the
atmosphere and, therefore, are more important for aerosol climate forcing. As part of the Rain In Cumulus over
the Ocean Experiment (RICO), cloud water and aerosol samples were collected in Puerto Rico. We present
concentrations of water-soluble ions, total and dissolved organic carbon (TOC and DOC), total nitrogen (TN), and
the speciation of nitrogen compounds (amino acids) for water and aerosol samples collected at East Peak and
Cape San Juan, Puerto Rico. Mass and elemental/organic carbon (EC, OC) concentrations were also determined
for the aerosol samples. The results show average concentrations of TOC and TN in cloud water of about 1.1
mg/L and for DOC about 0.9 mg/L. The DOC/TOC ratio averaged 0.78, indicating that most of the organic
compounds present are dissolved in the cloud water. TOC was composed mainly of organic acids (47 percent)
and TN of inorganic species (80 percent). With respect to the aerosol samples, the average mass concentration
of fine particles (Dp < 1.7 um) was 2.4 ug/m3. EC was found at low-to-non detectable levels (< 0.5 ng/m3). The
concentrations of OC, DOC, TOC, and TN ranged from 30 to 100 ng/m3. The size distributions showed that OC
and TN were mainly present in the fine particle fractions (Dp < 1 um). The predominant ions for both cloud and
aerosol samples were Cl- and Na+, the primary components of sea salt. However, when air masses arrived from
Northwest Africa or from islands upwind of Puerto Rico there was a decrease in Na+ and Cl- concentrations and
an increase in SO42-, NH3+ and Ca2+ concentrations, likely reflecting anthropogenic and crustal sources of
these species. Overall, the average concentrations of all species are similar to those typically found in
background (remote) environments; however, these concentrations showed a significant increase when aged
pollution from Northwest Africa and/or fresh pollution from neighboring Caribbean islands reached Puerto Rico.
Speciation of nitrogen compounds and details about the size distributions results will also be presented at the
conference.
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 0320 Cloud physics and chemistry
DE: 0345 Pollution: urban and regional (0305, 0478, 4251)
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting