Tundra near the Ny-Ålesund town in the summertime of 2019 with the Zeppelin Observatory in the background (left-hand side, engulfed in clouds). The tundra is potentially a major source of bioaerosols in the Arctic. Credit: Gabriel Freitas
An international team of researchers from Sweden, Norway, Japan, and Switzerland, has actually presented research study findings that reveal an essential role of biological particles, including pollen, spores, and germs, in the development of ice within Arctic clouds. These findings, released today in Nature Communications, have significant implications for environment science and our understanding of the rapidly altering Arctic environment.
The research, whose results have unveiled the connection between biological particles and the development of ice in Arctic clouds, was performed over several years at the Zeppelin Observatory, situated on the remote Norwegian archipelago of Svalbard, Norway, in the High Arctic.
Gabriel Freitas, lead author and PhD trainee at Stockholm University, detailed their ingenious approach: “We have actually separately recognized and counted these biological particles utilizing a delicate optical strategy reliant on light scattering and UV-induced fluorescence. This accuracy is important as we navigate through the obstacle of spotting these particles in tiny concentrations, similar to discovering a needle in a haystack.”
Sugar Alcohols and Fungal Spores
The research study delved into the seasonal dynamics of biological particles, developing correlations with variables such as snow cover, temperature, and meteorological criteria. The existence of biological particles was confirmed through numerous approaches, including electron microscopy and the detection of particular compounds, such as the sugar alcohol compounds arabitol and mannitol.
Gabriel Freitas, lead author of the research and a PhD trainee at Stockholm University. Credit: Paul Zieger
Karl Espen Yttri, senior researcher at the Climate and Environmental Research Institute NILU and a co-author of the study, highlighted that: “While arabitol and mannitol are present in various microbes, their existence in air belong to fungal spores, and may originate both from local sources or from long variety atmospheric transportation.”
Comprehending Ice Nucleation
The metrology of ice nucleating particles and comprehending their residential or commercial properties showed to be a cumbersome obstacle. Scientists used 2 unique approaches, including the collection of particles on filters over a week, followed by strenuous lab analysis.
Yutaka Tobo, Associate Professor at the National Institute of Polar Research in Japan and co-author of the research study, described their method: “Our method can quantify the ice nucleating capability of aerosol particles immersed in water beads at temperature levels varying from 0 ° C( 32 ° F) to about -30 ° C( -22 ° F), therefore exposing the concentration of ambient ice nucleating particles active in Arctic low-level clouds.”
Franz Conen, Research Fellow at the University of Basel, Switzerland, included, “By subjecting the filters to extra heating at 95 ° C (203 ° F), we could recognize the proteinaceous component of ice nucleating particles, shedding light on their possible biological origin. Our findings unquestionably establish the prevalence of biological particles contributing to ice nucleation at Zeppelin Observatory.”
Paul Zieger, Associate Professor at Stockholm University and a co-author of the research study. Credit: Stella Papadopoulou
Implications for Climate Science
Paul Zieger, Associate Professor at Stockholm University and co-author, highlighted the crucial ramification of these findings for environment science: “This research offers important insights into the origin and properties of biological and ice nucleating particles in the Arctic that could allow climate design developers to enhance the representation of aerosol-cloud interactions in designs and minimize unpredictabilities associated with anthropogenic radiative forcing quotes.”
Boosts in open ocean areas and snow-free tundra, both sources of biological particles in the Arctic, are anticipated in the coming decades. Therefore, acquiring a deeper understanding of the relationship between these particles and clouds might supply valuable insights into the ongoing and future transformations happening in the Arctic.
Recommendation: “Regionally sourced bioaerosols drive high-temperature ice nucleating particles in the Arctic” 28 September 2023, Nature Communications.DOI: 10.1038/ s41467-023-41696-7.
