Articles | Volume 18, issue 10
https://doi.org/10.5194/acp-18-7001-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-7001-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
18 May 2018
Research article |
| 18 May 2018
| 18 May 2018
Hygroscopic growth study in the framework of EARLINET during the SLOPE I campaign: synergy of remote sensing and in situ instrumentation
Andrés Esteban Bedoya-Velásquez
CORRESPONDING AUTHOR
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Sciences Faculty, Department of Physics, Universidad Nacional de Colombia, Medellín, Colombia
Francisco Navas-Guzmán
Federal Office of Meteorology and Climatology MeteoSwiss, Payerne, Switzerland
María José Granados-Muñoz
Remote Sensing Laboratory/CommSensLab, Universitat Politècnica de Catalunya, Barcelona, 08034, Spain
Gloria Titos
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Institute of Environmental Assessment and Water Research (IDAEA), CSIC, Barcelona, 08034, Spain
Roberto Román
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Grupo de Óptica Atmosférica (GOA), Universidad de Valladolid, Paseo Belén, 7, 47011, Valladolid, Spain
Juan Andrés Casquero-Vera
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Pablo Ortiz-Amezcua
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Jose Antonio Benavent-Oltra
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Gregori de Arruda Moreira
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Institute of Research and Nuclear Energy, IPEN, São Paulo, Brazil
Elena Montilla-Rosero
Physical Sciences Department, School of Science, EAFIT University, Medellín, Colombia
Carlos David Hoyos
Minas Faculty, Department of Geosciences and Environment, Universidad Nacional de Colombia, Medellín, Colombia
Begoña Artiñano
CIEMAT, Environment Department, Associated Unit to CSIC on Atmospheric Pollution, Avenida Complutense 40, Madrid, Spain
Esther Coz
CIEMAT, Environment Department, Associated Unit to CSIC on Atmospheric Pollution, Avenida Complutense 40, Madrid, Spain
Francisco José Olmo-Reyes
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Lucas Alados-Arboledas
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
Juan Luis Guerrero-Rascado
Andalusian Institute for Earth System Research (IISTA-CEAMA),
University of Granada, Autonomous Government of Andalusia, 18006, Granada, Spain
Departament of Applied Physics, University of Granada, Granada, Spain
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Short summary
This study focuses on the analysis of aerosol hygroscopic growth during the SLOPE I campaign combining active and passive remote sensors at ACTRIS Granada station and in situ instrumentation at a mountain station (Sierra Nevada station, SNS). The results showed good agreement on gamma parameters by using remote sensing with respect to those calculated using Mie theory at SNS, with relative differences lower than 9 % at 532 nm and 11 % at 355 nm.
This study focuses on the analysis of aerosol hygroscopic growth during the SLOPE I campaign...
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