Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/353133
COMPARTIR / EXPORTAR:
logo share SHARE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Invitar a revisión por pares abierta
Título

Climatological assessment of the vertically resolved optical and microphysical aerosol properties by lidar measurements, sun photometer, and in situ observations over 17 years at Universitat Politècnica de Catalunya (UPC) Barcelona

AutorLolli, Simone; Sicard, Michaël; Amato, Francesco; Comeron, Adolfo; Gil-Díaz, Cristina; Landi, Tony C.; Munoz-Porcar, Constantino; Oliveira, Daniel; Dios Otin, Federico; Rocadenbosch, Francesc; Rodriguez-Gomez, Alejandro; Alastuey, Andrés CSIC ORCID ; Querol, Xavier CSIC ORCID
Palabras claveAerosols
Fecha de publicación2023
EditorEuropean Geosciences Union
CitaciónEGU General Assembly 2023
ResumenAerosols are one of the most important pollutants in the atmosphere and have been monitored for the past few decades by remote sensing and in situ observation platforms to assess the effectiveness of government-managed reduction emission policies and assess their impact on the radiative budget of the Earth's atmosphere. In fact, aerosols can directly modulate incoming short-wave solar radiation and outgoing long-wave radiation and indirectly influence cloud formation, lifetime, and precipitation. In this study, we quantitatively evaluated long-term temporal trends and seasonal variability from a climatological point of view of the optical and microphysical properties of atmospheric particulate matter at the Universitat Politècnica de Catalunya (UPC), Barcelona, Spain, over the past 17 years, through a synergy of lidar, sun photometer, and in situ concentration measurements. Interannual temporal changes in aerosol optical and microphysical properties are evaluated through the seasonal Mann–Kendall test. Long-term trends in the optical depth of the recovered aerosol; the Ångström exponent (AE); and the concentrations of PM10, PM2.5, and PM1 reveal that emission reduction policies implemented in the past decades were effective in improving air quality, with consistent drops in PM concentrations and optical depth of aerosols. The seasonal analysis of the 17-year average vertically resolved aerosol profiles obtained from lidar observations shows that during summer the aerosol layer can be found up to an altitude of 5 km, after a sharp decay in the first kilometer. In contrast, during the other seasons, the backscatter profiles fit a pronounced exponential decay well with a well-defined scale height. Long-range transport, especially dust outbreaks from the Sahara, is likely to occur throughout the year. During winter, the dust aerosol layers are floating above the boundary layer, while during the other seasons they can penetrate the layer. The analysis also revealed that intense, short-duration pollution events during winter, associated with dust outbreaks, have become more frequent and intense since 2016. This study sheds some light on the meteorological processes and conditions that can lead to the formation of haze and helps decision makers adopt mitigation strategies to preserve large metropolitan areas in the Mediterranean basin.
URIhttp://hdl.handle.net/10261/353133
Aparece en las colecciones: (IDAEA) Comunicaciones congresos




Ficheros en este ítem:
Fichero Descripción Tamaño Formato
acp-23-12887-2023.pdfComunicación de congreso3,08 MBAdobe PDFVisualizar/Abrir
Mostrar el registro completo

CORE Recommender
sdgo:Goal

Page view(s)

7
checked on 05-may-2024

Download(s)

3
checked on 05-may-2024

Google ScholarTM

Check


NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.