Suchergebnisse

The paper makes a convincing case that the Brewer network is capable of detecting enhanced SO2 columns, as observed, e.g., after volcanic eruptions. For this reason, large volcanic eruptions of the past decade have been used to detect and forecast SO2 plumes of volcanic origin using the Brewer and other ground-based networks, aided by satellite, trajectory analysis calculations and modelling. ; This project has received funding from the European Union's Horizon 2020 research and innovation programme under grant agreement no. 654109.

The paper makes a convincing case that the Brewer network is capable of detecting enhanced SO2 columns, as observed, e.g., after volcanic eruptions. For this reason, large volcanic eruptions of the past decade have been used to detect and forecast SO2 plumes of volcanic origin using the Brewer and other ground-based networks, aided by satellite, trajectory analysis calculations and modelling. ; This project has received funding from the European Union's Horizon 2020 research and innovation programme under grant agreement no. 654109.

Póster presentado en: 9th International Workshop on Sand/Duststorms and Associated Dustfall, celebrado en Tenerife del 22 al 24 de mayo de 2018. ; This work has been performed within the framework of COST Action ES1207 "The European Brewer Network" (EUBREWNET), supported by COST (European Cooperation in Science and Technology). Part of this work has been developed within the IDEAS+ project of the European Space Agency, in collaboration with LuftBlick Earth Observation Technologies. This work has been supported by the European Metrology Research Programme (EMRP) within the joint research project ENV59 "Traceability for atmospheric total column ozone" (ATMOZ). The EMRP is jointly funded by the EMRP participating countries within EURAMET and the European Union. These activities have been partially developed in the WMO-CIMO Testbed for Aerosols and Water Vapor Remote Sensing Instruments (Izaña, Spain). We also acknowledge the support of the Ministry of Economy and Competitiveness of Spain and the European Regional Development Fund (ERDF) under the POLARMOON (CTM2015-66742-R) and AEROATLAN (CGL2015-66299-P) projects. Stratospheric ozone and spectral UV baseline monitoring in the United Kingdom is supported by DEFRA, The Department for the Environment, Food, and Rural Affairs, since 2003. Some of the AERONET sun photometers used in this work have been calibrated within the AERONET Europe TNA, supported by the European Community-Research Infrastructure Action under the Horizon 2020 research and innovation program, ACTRIS-2 grant agreement No. 654109. We gratefully the acknowledge the PIs of the Madrid, Izaña, and Tamanrasset AERONET stations.