Jonas Gliß

ORCID: 0000-0003-1147-4482
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About
Contact & Profiles
Research Areas
  • Atmospheric chemistry and aerosols
  • Atmospheric aerosols and clouds
  • Atmospheric Ozone and Climate
  • Atmospheric and Environmental Gas Dynamics
  • Air Quality Monitoring and Forecasting
  • Ocean Acidification Effects and Responses
  • Spectroscopy and Laser Applications
  • Urban Heat Island Mitigation
  • Photoacoustic and Ultrasonic Imaging
  • Geochemistry and Geologic Mapping
  • Particle Dynamics in Fluid Flows
  • Health, Environment, Cognitive Aging
  • High-pressure geophysics and materials
  • earthquake and tectonic studies
  • Air Quality and Health Impacts
  • Calibration and Measurement Techniques
  • Nutrition, Genetics, and Disease
  • Image Enhancement Techniques
  • Geological and Geochemical Analysis
  • Vehicle emissions and performance
  • Hydrocarbon exploration and reservoir analysis
  • Marine and coastal ecosystems
  • Geological and Geophysical Studies
  • Remote Sensing and Land Use
  • Advanced Chemical Sensor Technologies

Norwegian Meteorological Institute
2020-2024

University of Oslo
2015-2018

University Graduate Center
2017-2018

NILU
2015-2018

Heidelberg University
2015

Institut für Energie- und Umweltforschung Heidelberg
2015

Abstract. Within the framework of AeroCom (Aerosol Comparisons between Observations and Models) initiative, state-of-the-art modelling aerosol optical properties is assessed from 14 global models participating in phase III control experiment (AP3). The are similar to CMIP6/AerChemMIP Earth System Models (ESMs) provide a robust multi-model ensemble. Inter-model spread species lifetimes emissions appears be that mass extinction coefficients (MECs), suggesting depth (AOD) uncertainties...

10.5194/acp-21-87-2021 article EN cc-by Atmospheric chemistry and physics 2021-01-06
Paolo Laj Alessandro Bigi Clémence Rose Elisabeth Andrews Cathrine Lund Myhre and 95 more Martine Collaud Coen Yong Lin Alfred Wiedensohler Michael Schulz J. A. Ogren Markus Fiebig Jonas Gliß Augustin Mortier Marco Pandolfi Tuukka Petäjä Sang‐Woo Kim Wenche Aas Jean‐Philippe Putaud O. L. Mayol‐Bracero Melita Keywood Lorenzo Labrador Tuula Aalto Erik Ahlberg Lucas Alados‐Arboledas Andrés Alástuey Marcos Andrade Begoña Artı́ñano Stina Ausmeel Todor Arsov Eija Asmi John Backman Urs Baltensperger Susanne Bastian Olaf Bath Johan P. Beukes Benjamin T. Brem Nicolas Bukowiecki Sébastien Conil Cédric Couret Derek E. Day Wan Dayantolis Anna Degórska Konstantinos Eleftheriadis Prodromos Fetfatzis Olivier Favez H. Flentje Maria Gini Asta Gregorič Martin Gysel‐Beer A. Gannet Hallar J. L. Hand András Hoffer Christoph Hueglin Rakesh K. Hooda Antti Hyvärinen Ivo Kalapov Nikos Kalivitis Anne Kasper‐Giebl Jeong Eun Kim Giorgos Kouvarakis Irena Kranjc Radovan Krejčí Markku Kulmala Casper Labuschagne Haejung Lee Heikki Lihavainen Neng‐Huei Lin G. Löschau Krista Luoma Angela Marinoni Sebastiao Martins Dos Santos Frank Meinhardt Maik Merkel Jean‐Marc Metzger N. Mihalopoulos Nhat Anh Nguyen Jakub Ondráček Noemí Pérez M. R. Perrone Jean‐Eudes Petit David Picard Jean‐Marc Pichon Véronique Pont Natalia Prats A. J. Prenni Fabienne Reisen Salvatore Romano Karine Sellegri Sangeeta Sharma Gerhard Schauer Patrick J. Sheridan James P. Sherman Maik Schütze Andreas Schwerin Ralf Sohmer M. Sorribas Martin Steinbacher Junying Sun Gloria Titos Barbara Toczko

Abstract. Aerosol particles are essential constituents of the Earth's atmosphere, impacting earth radiation balance directly by scattering and absorbing solar radiation, indirectly acting as cloud condensation nuclei. In contrast to most greenhouse gases, aerosol have short atmospheric residence times, resulting in a highly heterogeneous distribution space time. There is clear need document this variability at regional scale through observations involving, particular, situ near-surface...

10.5194/amt-13-4353-2020 article EN cc-by Atmospheric measurement techniques 2020-08-17

Abstract. This study presents a multiparameter analysis of aerosol trends over the last 2 decades at regional and global scales. Regional time series have been computed for set nine optical, chemical-composition mass properties by using observations from several ground-based networks. From these derived different regions world. Most related to loading exhibit negative trends, both surface in total atmospheric column. Significant decreases optical depth (AOD) are found Europe, North America,...

10.5194/acp-20-13355-2020 article EN cc-by Atmospheric chemistry and physics 2020-11-11

Abstract. Aerosol-induced absorption of shortwave radiation can modify the climate through local atmospheric heating, which affects lapse rates, precipitation, and cloud formation. Presently, total amount aerosol is poorly constrained, main absorbing species (black carbon (BC), organic aerosols (OA), mineral dust) are diversely quantified in global models. As part third phase Aerosol Comparisons between Observations Models (AeroCom) intercomparison initiative (AeroCom III), we here document...

10.5194/acp-21-15929-2021 article EN cc-by Atmospheric chemistry and physics 2021-10-26

This paper encompasses an assessment of air pollution trends in rural environments Europe over the 2000–2019 period, benefiting from extensive long-term observational data EMEP monitoring network and MSC-W model computations. The pollutant concentrations align with decreasing emission patterns observed throughout Europe. Annual average sulfur dioxide, particulate sulfate, wet deposition have shown consistent declines 3-4% annually since 2000. Similarly, oxidized nitrogen species markedly...

10.4209/aaqr.230237 article EN cc-by Aerosol and Air Quality Research 2024-01-01

Abstract. Spatial and temporal profiles of chlorine dioxide (OClO), bromine monoxide (BrO) sulfur (SO2) the volcanic plume at Mt. Etna, Italy, were investigated in September 2012 using Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS). OClO was detected 119 individual measurements covering ages up to 6 min. BrO could be 452 spectra 23 min downwind. The retrieved slant column densities (SCDs) reached maximum values 2.0 × 1014 molecules cm-2 (OClO) 1.1 1015 (BrO). Mean mixing...

10.5194/acp-15-5659-2015 article EN cc-by Atmospheric chemistry and physics 2015-05-26

Abstract. Accurate gas velocity measurements in emission plumes are highly desirable for various atmospheric remote sensing applications. The imaging technique of UV SO2 cameras is commonly used to monitor emissions from volcanoes and anthropogenic sources (e.g. power plants, ships). camera systems capture the at high spatial temporal resolution. This allows velocities plume be retrieved directly images. latter can measured a pixel level using optical flow (OF) algorithms. particularly...

10.5194/amt-11-781-2018 article EN cc-by Atmospheric measurement techniques 2018-02-08

Abstract Mount Cleveland is one of Alaska's most active volcanoes, yet little known about the magmatic system driving persistent and dynamic volcanic activity. Volcanic gas melt inclusion (MI) data from 2016 were combined to investigate shallow processes. SO 2 emission rates between 166 324 t/day H O/SO was 600 ± 53, whereas CO S below detection. Olivine‐, clinopyroxene‐, plagioclase‐hosted MIs have up 3.8 wt.% O, 514 ppm , 2,320 S. Equilibration depths, based on MI O contents, suggest that...

10.1029/2019gc008882 article EN publisher-specific-oa Geochemistry Geophysics Geosystems 2020-05-21

Ultraviolet (UV) SO2 cameras have become a common tool to measure and monitor emission rates, mostly from volcanoes but also anthropogenic sources (e.g., power plants or ships). Over the past decade, analysis of UV camera data has seen many improvements. As result, for required steps, several alternatives exist today cell vs. DOAS based calibration; optical flow cross-correlation gas-velocity retrieval). This inspired development Pyplis (Python plume imaging software), an open-source...

10.3390/geosciences7040134 article EN cc-by Geosciences 2017-12-15

Abstract. Within the framework of AeroCom (Aerosol Comparisons between Observations and Models) initiative, present day modelling aerosol optical properties has been assessed using simulated data representative for year 2010, from 14 global models participating in Phase III Control experiment. The model versions are close or equal to those used CMIP6 AerChemMIP inform also on bias state art ESMs. Modelled column depths (total, fine coarse mode AOD) Angstrom Exponents (AE) were compared both...

10.5194/acp-2019-1214 article EN cc-by 2020-03-18

Abstract. This study presents a multi-parameter analysis of aerosol trends over the last two decades at regional and global scales. Regional time series have been computed for set nine optical, chemical composition mass properties by using observations several ground-based networks. From these derived different regions world. Most related to loading exhibit negative trends, both surface in total atmospheric column. Significant decreases optical depth (AOD) are found Europe, North America,...

10.5194/acp-2019-1203 preprint EN cc-by 2020-01-13
Paolo Laj Alessandro Bigi Clémence Rose Elisabeth Andrews Cathrine Lund Myhre and 95 more Martine Collaud Coen Alfred Wiedensohler Michael Schultz J. A. Ogren Markus Fiebig Jonas Gliß Augustin Mortier Marco Pandolfi Tuukka Petäjä Sang‐Woo Kim Wenche Aas Jean-Phillipe Putaud O. L. Mayol‐Bracero Melita Keywood Lorenzo Labrador Pasi Aalto Erik Ahlberg Lucas Alados‐Arboledas Andrés Alástuey Marcos Andrade Begoña Artı́ñano Stina Ausmeel Todor Arsov Eija Asmi John Backman Urs Baltensperger Susanne Bastian Olaf Bath Johan P. Beukes Benjamin T. Brem Nicolas Bukowiecki Sébastien Conil Cédric Couret Derek E. Day Wan Dayantolis Anna Degórska Sebastiao Martins Dos Santos Konstantinos Eleftheriadis Prodromos Fetfatzis Olivier Favez H. Flentje Maria Gini Asta Gregorič Martin Gysel‐Beer G. Hallar J. L. Hand András Hoffer Christoph Hueglin Rakesh K. Hooda Antti Hyvärinen Ivo Kalapov Nikos Kalivitis Anne Kasper‐Giebl Jeong Eun Kim Giorgos Kouvarakis Irena Kranjc Radovan Krejčí Markku Kulmala Casper Labuschagne Haejung Lee Heikki Lihavainen Neng‐Huei Lin G. Löschau Krista Luoma Angela Marinoni Frank Meinhardt Maik Merkel Jean‐Marc Metzger N. Mihalopoulos Nhat Anh Nguyen Jakub Ondráček Noemí Pérez M. R. Perrone Jean‐Eudes Petit David Picard Jean‐Marc Pichon Véronique Pont Natalia Prats A. J. Prenni Fabienne Reisen Salvatore Romano Karine Sellegri Sangeeta Sharma Gerhard Schauer Patrick J. Sheridan James P. Sherman Maik Schütze Andreas Schwerin Ralf Sohmer M. Sorribas Martin Steinbacher Junying Sun Gloria Titos Barbara Tokzko Thomas Tuch

Abstract. Aerosol particles are essential constituents of the Earth’s atmosphere, impacting earth radiation balance directly by scattering and absorbing solar radiation, indirectly acting as cloud condensation nuclei. In contrast to most greenhouse gases, aerosol have short atmospheric residence time resulting in a highly heterogeneous distribution space time. There is clear need document this variability at regional scale through observations involving, particular, in-situ near-surface...

10.5194/amt-2019-499 article EN cc-by 2020-02-11

Abstract. Accurate gas velocity measurements in emission plumes are highly desirable for various atmospheric remote sensing applications. The imaging technique of UV SO2 cameras is commonly used monitoring emissions from volcanoes and anthropogenic sources (e.g. power plants, ships). camera systems capture the at high spatial temporal resolution. This allows to retrieve velocities plume directly images. latter can be measured a pixel level using optical flow (OF) algorithms. particularly...

10.5194/amt-2017-185 article EN cc-by 2017-08-14

Abstract. Spatial and temporal profiles of chlorine dioxide (OClO), bromine monoxide (BrO) sulphur (SO2) were measured in the plume Mt. Etna, Italy, September 2012 using Multi-Axis-Differential-Optical-Absorption-Spectroscopy (MAX-DOAS). OClO was detected 119 (452) individual measurements covering ages up to 6 (23) minutes. The retrieved slant column densities (SCDs) reached values 2.0 × 1014 molecules cm−2 (OClO) 1.1 1015 (BrO). In addition, spectra analysed for signatures IO, OIO OBrO,...

10.5194/acpd-14-25213-2014 preprint EN cc-by 2014-10-01

Abstract. Aerosol induced absorption of shortwave radiation can modify the climate through local atmospheric heating, which affects lapse rates, precipitation, and cloud formation. Presently, total amount such is poorly constrained, main absorbing aerosol species (black carbon (BC), organic aerosols (OA) mineral dust are diversely quantified in global models. As part third phase AeroCom model intercomparison initiative (AeroCom Phase III) we here document distribution magnitude current...

10.5194/acp-2021-51 preprint EN cc-by 2021-02-03

UV SO2 cameras have become a common tool to measure and monitor SO2-emission-rates, mostly from volcanoes but also anthropogenic sources (e.g. power plants or ships). In the past years, analysis of camera data has seen many improvements. As result, for required steps, several alternatives exist today. This inspired development Pyplis, an open-source software toolbox written in Python 2.7, which aims unify most prevalent methods literature within single, cross-platform framework. Pyplis...

10.20944/preprints201710.0085.v1 preprint EN 2017-10-13

<p>Within the framework of AeroCom (Aerosol Comparisons between Observations and Models) initiative, present day modelling aerosol optical properties has been assessed using simulated data representative for year 2010, from 14 global models participating in Phase III Control experiment. The model versions are close or equal to those used CMIP6 AerChemMIP inform also on bias state art Earth-System-Models (ESMs).<br>Modelled column depths (total, fine coarse mode...

10.5194/egusphere-egu2020-18390 article EN 2020-03-10

<p>Aerosol particles are essential constituents of the Earth’s atmosphere, impacting earth radiation balance directly by scattering and absorbing solar radiation, indirectly acting as cloud condensation nuclei. In contrast to most greenhouse gases, aerosol have short atmospheric residence time resulting in a highly heterogeneous distribution space time. There is clear need document this variability at regional scale through observations involving, particular,...

10.5194/egusphere-egu2020-2147 article EN 2020-03-09
Paolo Laj Alessandro Bigi Clémence Rose Elisabeth Andrews Cathrine Lund Myhre and 95 more Martine Collaud Coen Alfred Wiedensohler Michael Schultz J. A. Ogren Markus Fiebig Jonas Gliß Augustin Mortier Marco Pandolfi Tuukka Petäjä Sang‐Woo Kim Wenche Aas Jean-Phillipe Putaud O. L. Mayol‐Bracero Melita Keywood Lorenzo Labrador Tuula Aalto Erik Ahlberg Lucas Alados‐Arboledas Andrés Alástuey Marcos Andrade Begoña Artı́ñano Stina Ausmeel Todor Arsov Eija Asmi John Backman Urs Baltensperger Susanne Bastian Olaf Bath Johan P. Beukes Benjamin T. Brem Nicolas Bukowiecki Sébastien Conil Cédric Couret Derek E. Day Wan Dayantolis Anna Degórska Sebastiao Martins Dos Santos Konstantinos Eleftheriadis Prodromos Fetfatzis Olivier Favez H. Flentje Maria Gini Asta Gregorič Martin Gysel‐Beer G. Hallar J. L. Hand András Hoffer Christoph Hueglin Rakesh K. Hooda Antti Hyvärinen Ivo Kalapov Nikos Kalivitis Anne Kasper‐Giebl Jeong Eun Kim Giorgos Kouvarakis Irena Kranjc Radovan Krejčí Markku Kulmala Casper Labuschagne Haejung Lee Heikki Lihavainen Neng‐Huei Lin G. Löschau Krista Luoma Angela Marinoni Frank Meinhardt Maik Merkel Jean‐Marc Metzger N. Mihalopoulos Nhat Anh Nguyen Jakub Ondráček Noemí Pérez M. R. Perrone Jean‐Eudes Petit David Picard Jean‐Marc Pichon Véronique Pont Natalia Prats A. J. Prenni Fabienne Reisen Salvatore Romano Karine Sellegri Sangeeta Sharma Gerhard Schauer Patrick J. Sheridan James P. Sherman Maik Schütze Andreas Schwerin Ralf Sohmer M. Sorribas Martin Steinbacher Junying Sun Gloria Titos Barbara Tokzko Thomas Tuch

Table SM1: Overview of Aerosol Absorption Coefficient measurements.For each site, the instrument used for data collection and corresponding availability are indicated.The statistics, i.e. median, 10th 90th quantiles σ ap only reported when is above 75% over period interest (year or season).For MLO BRW, where screening provenance from clean air sectors, summary statistics regardless coverage.

10.5194/amt-2019-499-supplement preprint EN 2020-02-11
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