The UNAM-MARine Aerosol Tank (UNAM-MARAT): an evaluation of the ice-nucleating abilities of seawater from the Gulf of Mexico and the Mexican Pacific
Abstract. Although several studies have shown that sea spray aerosol (SSA) has the potential to act as ice-nucleating particles (INPs) impacting cloud formation, there is a lack of marine INP studies in tropical latitudes. This is partly due to the unavailability of local oceanographic cruises that perform aerosol–cloud interaction studies in the tropics, as well as the scarcity of appropriate aerosol and cloud microphysics instrumentation. The present study shows the development of the UNAM-MARine Aerosol Tank (UNAM-MARAT; Universidad Nacional Autónoma de México), a device that simulates wave breaking to generate SSA particles with the main purpose of characterizing their physicochemical properties including their ice-nucleating abilities. The UNAM-MARAT was characterized using Instant Ocean Sea Salt, and its potential to study ambient seawater was evaluated with seawater samples collected from the Port of Veracruz (PoV) in the Gulf of Mexico, the Bay of Acapulco (BoA), and the Bay of Santiago-Manzanillo (BoSM) in the Mexican Pacific Ocean. The portable and automatic UNAM-MARAT is able to generate aerosol particle concentrations as high as 2000 cm−3 covering a wide range of sizes, from 30 nm to 10 µm, similar to those found in the ambient marine boundary layer. The SSA generated from the three natural seawater samples was found to act as INPs via immersion freezing, with INP concentrations as high as 130.7 L−1. The particles generated from the BoA seawater samples were the most efficient INPs, reporting the highest ice-active site density (ns) values between −20 and −30 °C. Our results also show the direct relationship between particle size and its composition. Larger particles (> 1 µm) were found to be enriched in sodium chloride. In contrast, the fraction of Ca2+, Mg2+, and NO3- was found to increase with decreasing particle size from 10 µm to 320 nm. This suggests important differences in the presence of dissolved organic material in the submicron particles related to the sampling zone and possibly the behavior of the SSA.
Authors
- Aramis Olivos‐Ortiz (ORCID: https://orcid.org/0000-0002-9886-9817)
- Luis A. Ladino (ORCID: https://orcid.org/0000-0002-4941-7945)
- Harry Álvarez‐Ospina (ORCID: https://orcid.org/0000-0003-0577-4163)
- Graciela B. Raga (ORCID: https://orcid.org/0000-0002-4295-4991)
- Isabel Márquez (ORCID: https://orcid.org/0000-0003-2700-918X)
- Rachel Chang (ORCID: https://orcid.org/0000-0003-2337-098X)
- Guadalupe Campos
- T. Castro (ORCID: https://orcid.org/0000-0002-5998-8004)
- María F. Córdoba
- Daniel Rosas-Ramírez
Institutions
- Dalhousie University (CA)
- Federal Government of Mexico (MX)
- Universidad Nacional Autónoma de México (MX)
- Universidad de Colima (MX)
Publication Details
- Journal
- Atmospheric measurement techniques
- Published
- 2025-06-11
- DOI
- https://doi.org/10.5194/amt-18-2463-2025
- Primary Topic
- Atmospheric chemistry and aerosols
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- Fundación Marcos Moshinsky
- Consejo Nacional de Ciencia y Tecnología
- Universidad Nacional Autónoma de México
- Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México