Original Research ARTICLE
Aerosol concentrations in relationship to local atmospheric conditions on James Ross Island, Antarctica
- 1Faculty of Science, Masaryk University, Czechia
- 2Agricultural University of Iceland, Iceland
- 3UMR7328 Laboratoire de physique et chimie de l'environnement et de l'Espace (LPC2E), France
Several important ice-free areas (e.g. Seymour Island, Cape Lamb on Vega Island, Terrapin Hill) are located in the region of Eastern Antarctic Peninsula. The largest deglaciated region can be found on the Ulu Peninsula, James Ross Island, where the study was carried out. This area of 312 km2 has been found important active High Latitude Dust source. Aerosol concentrations and local wind properties are described together with their linkages and typical synoptic situations. The highest aerosol concentrations of 57 µgm−3 for PM10 were detected during the high wind speed events exceeding 10 m s-1, which is also a threshold level for activating local mineral material sources. Apart the local dust sources, influence of long range aerosol transport out of Antarctica (especially Patagonia) is discussed too.
Keywords: aerosol, wind speed, wind direction, Antarctica, high latitude dust sources, Atmospheric conditions, Antartic Peninsula
Received: 30 Jul 2018;
Accepted: 30 Oct 2018.
Edited by:Gert-Jan Steeneveld, Wageningen University & Research, Netherlands
Reviewed by:Yoav Y. Yair, Interdisciplinary Center Herzliya, Israel
Lucas Alados-Arboledas, University of Granada, Spain
Copyright: © 2018 Kavan, Dagsson-Waldhauserova, Renard, Laska and Ambrozova. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence: Mr. Jan Kavan, Faculty of Science, Masaryk University, Brno, 611 37, South Moravia, Czechia, email@example.com