Publication
An approach to evaluate aerosol optical depth at marine boundary layer : the Pico-Graciosa measurement platform
dc.contributor.author | Henriques, Diamantino | |
dc.contributor.author | Carvalho, Fernanda | |
dc.contributor.author | Fialho, Paulo | |
dc.date.accessioned | 2018-01-22T13:18:45Z | |
dc.date.available | 2018-01-22T13:18:45Z | |
dc.date.issued | 2015 | |
dc.date.updated | 2015-09-02T11:49:43Z | |
dc.description | Workshop: An opportunity for international cooperation on atmospheric sciences, Lisboa, 2015 (Comunicação). | pt_PT |
dc.description.abstract | Aerosols are an important constituent of the atmospheric boundary layer. Aerosol particles provide surfaces for heterogeneous chemical processes, they also act as a condensation sink for atmospheric trace species. In the marineatmosphere originate from a variety of production and transformation processes that includes sea spray aerosol produced at the sea surface through the interactions between wind and surface waves (Liss and Johnson, 2013). | en |
dc.description.version | N/A | pt_PT |
dc.identifier.citation | Henriques, Diamantino; Carvalho, Fernanda; Fialho, Paulo (2015). An approach to evaluate aerosol optical depth at marine boundary layer: the Pico-Graciosa measurement platform. Workshop "An opportunity for international cooperation on atmospheric sciences", Lisboa (Comunicação). | pt_PT |
dc.identifier.uri | http://hdl.handle.net/10400.3/4558 | |
dc.language.iso | eng | pt_PT |
dc.subject | Aerosol Optical | en |
dc.subject | Pico Mountain Observatory | en |
dc.subject | Azores Archipelago | en |
dc.title | An approach to evaluate aerosol optical depth at marine boundary layer : the Pico-Graciosa measurement platform | en |
dc.type | conference object | |
dspace.entity.type | Publication | |
oaire.citation.conferencePlace | Lisboa, Portugal | pt_PT |
oaire.citation.title | Workshop an opportunity for international cooperation on atmospheric sciences | pt_PT |
rcaap.rights | openAccess | pt_PT |
rcaap.type | conferenceObject | pt_PT |