Black Carbon in a City of the Atacama Desert before and after the Start of the COVID-19 Lockdown: Ground Measurements and MERRA-2 Reanalysis

Author:

Liñán-Abanto Rafael N.1ORCID,Arnott William Patrick2,Paredes-Miranda Guadalupe2,Ramos-Pérez Omar3,Salcedo Dara4ORCID,Torres-Muro Hugo1,Liñán-Abanto Rosa M.5,Carabali Giovanni6ORCID

Affiliation:

1. Departamento de Física, Facultad de Ciencias, Universidad Nacional Jorge Basadre Grohmann, Av. Miraflores s/n, Tacna 230003, Peru

2. Department of Physics, University of Nevada, 1664 N. Virginia Street, Reno, NV 89557, USA

3. Instituto de Ciencias de la Atmósfera y Cambio Climático, Universidad Nacional Autónoma de México (UNAM), Circuito Exterior s/n, Ciudad Universitaria, Ciudad de Mexico 04510, Mexico

4. Unidad Multidisciplinaria de Docencia e Investigación Juriquilla, Facultad de Ciencias, Universidad Nacional Autónoma de México, Boulevard Juriquilla 3001, Col. Juriquilla, Querétaro 76230, Mexico

5. Departamento de Biología, Facultad de Ciencias, Universidad Nacional Jorge Basadre Grohmann, Av. Miraflores s/n, Tacna 230003, Peru

6. Instituto de Geofísica, Universidad Nacional Autónoma de México (UNAM), Circuito Exterior s/n, Ciudad Universitaria, Ciudad de Mexico 04510, Mexico

Abstract

In this study, the temporal variations of black carbon (BC) were analyzed from November 2019 to September 2021, in Tacna, Peru. Ground measurements obtained with a photoacoustic extinctiometer (PAX BC) and NASA’s MERRA-2 reanalysis data (MERRA-2 BC) were used. The seasonal concentrations of PAX BC (mean ± standard deviation) were as follows: 0.70 ± 0.35, 0.73 ± 0.46, 0.70 ± 0.39, and 0.85 ± 0.46 µg m−3, for spring, summer, autumn, and winter, respectively; while MERRA-2 BC values were 0.12 ± 0.11, 0.06 ± 0.02, 0.06 ± 0.02, and 0.11 ± 0.06 µg m−3, for the same seasons. We found a large discrepancy between these two techniques, as the PAX BC measurements were an order of magnitude higher than the MERRA-2 BC values. In addition, MERRA-2 did not record urban pollution events and did not present the BC weekend effect. The most frequent wind direction (81%) was from the southwest and the sources of greatest contamination were located to the northeast and southeast. The Mann–Kendall test confirmed a downward trend in PAX BC one week (37%) and two weeks (30%) after the start of the COVID-19 lockdown, and no trend in MERRA-2 BC. These results suggest that MERRA-2 underestimates the BC emissions from local sources.

Funder

Jorge Basadre Grohmann National University

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

Reference79 articles.

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3. Bounding the role of black carbon in the climate system: A scientific assessment;Bond;J. Geophys. Res. Atmos.,2013

4. Aerosol light absorption and its measurement: A review;Chakrabarty;J. Quant. Spectrosc. Radiat. Transf.,2009

5. How sensitive is the world’s climate?;Hansen;Natl. Geog. Res. Explor.,1993

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