Martin Gysel‐Beer
Biographic Data
| ID | 7998803 |
|---|---|
| NAME | Martin Gysel‐Beer |
| GIVEN NAMES | Martin |
| FAMILY NAME | Gysel‐Beer |
| SIGNATURE | BEER M G |
| AFFILIATIONS | Paul Scherrer Institute |
| ORCID | 0000-0002-7453-1264 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2011 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
The Arctic is sensitive to cloud radiative forcing. Due to the limited number of aerosols present throughout much of the year, cloud formation is susceptible to the presence of cloud condensation nuclei and ice nucleating particles (INPs). Primary biological aerosol particles (PBAP) contribute to INPs and can impact cloud phase, lifetime, and radiative properties. We present yearlong observations of hyperfluorescent aerosols (HFA), tracers for PB…
Changes of hygroscopicity and morphology during ageing of diesel soot
Soot particles are an important component of atmospheric aerosol and their interaction with water is important for their climate effects.The hygroscopicity of fresh and photochemically aged soot and secondary organic aerosol (SOA) from diesel passenger car emissions was studied under atmospherically relevant conditions in a smog chamber at sub-and supersaturation of water vapor.Fresh soot particles show no significant hygroscopic growth nor cloud…
No prominent works on this page.
Changes of hygroscopicity and morphology during ageing of diesel soot
Soot particles are an important component of atmospheric aerosol and their interaction with water is important for their climate effects.The hygroscopicity of fresh and photochemically aged soot and secondary organic aerosol (SOA) from diesel passenger car emissions was studied under atmospherically relevant conditions in a smog chamber at sub-and supersaturation of water vapor.Fresh soot particles show no significant hygroscopic growth nor cloud…
Characteristics and sources of fluorescent aerosols in the central Arctic Ocean
The Arctic is sensitive to cloud radiative forcing. Due to the limited number of aerosols present throughout much of the year, cloud formation is susceptible to the presence of cloud condensation nuclei and ice nucleating particles (INPs). Primary biological aerosol particles (PBAP) contribute to INPs and can impact cloud phase, lifetime, and radiative properties. We present yearlong observations of hyperfluorescent aerosols (HFA), tracers for PB…
Atmospheric chemistry and aerosols (2 works) · Chemistry (2 works) · Environmental Science (2 works) · Geology (2 works) · Aerosol (1 work) · Ageing (1 work) · Air Quality and Health Impacts (1 work) · Arctic (1 work) · Atmospheric and Environmental Gas Dynamics (1 work) · Atmospheric Ozone and Climate (1 work)