Arctic mercury flux increased through the Last Glacial Termination with a warming climate
Delia Segato(Ca' Foscari University of Venice), Andrea Spolaor(Ca' Foscari University of Venice), Clara Turetta(Ca' Foscari University of Venice), Carlos A. Cuevas(Consejo Superior de Investigaciones Científicas), Alfonso Saiz‐Lopez(Instituto de Química Física Blas Cabrera), Helle Astrid Kjær(University of Copenhagen), Warren R. L. Cairns(Ca' Foscari University of Venice), Chantal Zeppenfeld(University of Bern), Carlo Barbante(National Research Council), Camilla Marie Jensen(University of Bern), Anoop S. Mahajan(Indian Institute of Tropical Meteorology), Tobias Erhardt(University of Bern), Fei Wang(Central South University), Juan Pablo Corella(Department of the Environment)
Cited by 25
Related Papers
Tropospheric emissions: Monitoring of pollution (TEMPO)
|Journal of Quantitative Spectroscopy and Radiative Transfer|2016|596
Global impacts of tropospheric halogens (Cl, Br, I) on oxidants and composition in GEOS-Chem
|Atmospheric chemistry and physics|2016|413
Global airborne sampling reveals a previously unobserved dimethyl sulfide oxidation mechanism in the marine atmosphere
|Proceedings of the National Academy of Sciences|2020|357
Boundary Layer Halogens in Coastal Antarctica
|Science|2007|350