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ZÁVACKÁ, K. NEDĚLA, V. OLBERT, M. TIHLAŘÍKOVÁ, E. VETRÁKOVÁ, Ľ. YANG, X. HEGER, D.
Original Title
Temperature and Concentration Affect Particle Size Upon Sublimation of Saline Ice: Implications for Sea Salt Aerosol Production in Polar Regions
Type
journal article in Web of Science
Language
English
Original Abstract
Using an environmental scanning electron microscope, we quantified for the first time aerosol-sized salt particles formed during the sublimation of sea ice as a function of temperature and concentration. The sublimation temperature of the ice is a dominating physical factor to determine the size of the residua: Below -20 degrees C, micron-sized pieces of salt emerge, whereas above the temperature large chunks of salt are detected. Another such aspect influencing the distribution of sizes in salt particles is the concentration: Micron-sized particles are observed exclusively at salinities below 3.5 psu, while below 0.085 psu particles with a median smaller than 6 mu m arise from sea ices at any subzero temperature. Moreover, when a chunk of salt sublimes at less than -30 degrees C to be dried and warmed later, a large number of sub-micron crystals will appear. We relate our findings to the production of the polar atmospheric sea salt aerosols.
Keywords
sea salt aerosols; ozone depletion; sublimation; microscopy; eutectic temperature; bromine explosion
Authors
ZÁVACKÁ, K.; NEDĚLA, V.; OLBERT, M.; TIHLAŘÍKOVÁ, E.; VETRÁKOVÁ, Ľ.; YANG, X.; HEGER, D.
Released
28. 4. 2022
Publisher
AMER GEOPHYSICAL UNION
Location
WASHINGTON
ISBN
0094-8276
Periodical
GEOPHYSICAL RESEARCH LETTERS
Year of study
49
Number
8
State
United States of America
Pages from
1
Pages to
10
Pages count
URL
https://doi.org/10.1029/2021GL097098
BibTex
@article{BUT178375, author="Kamila {Závacká} and Vilém {Neděla} and Martin {Olbert} and Eva {Tihlaříková} and Ľubica {Vetráková} and Xin {Yang} and Dominik {Heger}", title="Temperature and Concentration Affect Particle Size Upon Sublimation of Saline Ice: Implications for Sea Salt Aerosol Production in Polar Regions", journal="GEOPHYSICAL RESEARCH LETTERS", year="2022", volume="49", number="8", pages="1--10", doi="10.1029/2021GL097098", issn="0094-8276", url="https://doi.org/10.1029/2021GL097098" }