| Composition and mixing state of atmospheric aerosols determined by electron microscopy: method development and application to aged Saharan dust deposition in the Caribbean … K Kandler, K Schneiders, M Ebert, M Hartmann, S Weinbruch, M Prass, ... Atmospheric Chemistry and Physics 18 (18), 13429-13455, 2018 | 46 | 2018 |
| Field comparison of dry deposition samplers for collection of atmospheric mineral dust: results from single-particle characterization A Waza, K Schneiders, J May, S Rodríguez, B Epple, K Kandler Atmospheric Measurement Techniques 12 (12), 6647-6665, 2019 | 24 | 2019 |
| Differences and similarities of central Asian, African, and arctic dust composition from a single particle perspective K Kandler, K Schneiders, J Heuser, A Waza, S Aryasree, D Althausen, ... Atmosphere 11 (3), 269, 2020 | 16 | 2020 |
| Geochemistry and source contribution of fugitive phosphogypsum particles in Huelva,(SW Spain) R Torres-Sánchez, D Sánchez-Rodas, AMS de la Campa, K Kandler, ... Atmospheric research 230, 104650, 2019 | 15 | 2019 |
| XMED-dry–a cross-Mediterranean dry deposition measurement network: first results K Kandler, J De La Rosa, R Torres-Sanchez, M Aviles, ... Digilabs, 2018 | 1 | 2018 |
| Analysis of Size Distribution, Chemical Composition, and Optical Properties of Mineral Dust Particles from Dry Deposition Measurement in Tenerife: Determined by Single-Particle … A Waza, K Schneiders, J Heuser, K Kandler Atmosphere 14 (4), 700, 2023 | | 2023 |
| Einfluss räumlich inhomogener Verschmutzungen auf den PV-Wirkungsgrad K Schneiders Influence of spatially inhomogeneous soiling on PV-efficiency, 2021 | | 2021 |
| Methodological aspects of mineral dust deposition measurement in a dust transport region (Tenerife): results from single-particle characterization. A Waza, K Schneiders, JF May, S Rodríguez, K Kandler Geophysical Research Abstracts 21, 2019 | | 2019 |
| XMed-Dry network: results of the first year of sampling in Lecce K Kandler, P Ielpo, K Schneiders, M Eknayan, CL Ciricugno, F De Tomasi, ... www. pm2020. it, 26, 0 | | |
