ISSN: 2572-3103
+44 1300 500008
Darius Ceburnis, Jurgita Ovadnevaite and Colin D O Dowd
National University of Ireland Galway, Ireland
Scientific Tracks Abstracts: J Oceanogr Mar Res
The marine aerosol produces haze and cloud layers overlying an immense ocean covering >70% of the Earth�??s surface. Small changes even in low-albedo layers superimposing this relatively dark surface can have profound effects on the global radiation budget and climate change. Bursting bubbles at the ocean-surface produce airborne salt-water spray-droplets, in turn, forming climate-cooling marine haze and cloud layers. The reflectance and ultimate cooling effect of these layers can be determined, but the sprays water-uptake properties are modified through entrainment of ocean-surface organic matter into the airborne droplets. Particulate carbonaceous matter (PCM) is a significant contributor to ambient particulate matter originating from intervening sources which contribution is difficult to quantify due to source diversity, chemical complexity of PCM and processes during atmospheric transport. Carbon isotope analysis of stable and radioactive carbon spun out several techniques for identifying the sources and elucidating processes along atmospheric transport due to the unique isotopic signatures. Three principal sources have been quantified in marine North Atlantic air masses using dual carbon isotope analysis. A hypothetical model conceived to describe the sea-to-air transfer of oceanic OM was capable of reproducing stable carbon measurements at Amsterdam Island in the Southern Indian Ocean and subsequently linked ocean biological processes to the primary marine aerosol. The hypothetical model suggested that fresh organic matter readily resulted in organic matter enrichment in sea spray particles and likely contained fresh colloidal and nanogel particulate matter. Our experimental evidence suggested that virus attack on plankton blooms, triggering their demise, releases the organic matter and this organic matter, through aggregation processes, leads to enrichment in sea spray, thus demonstrating an important coupling between virus-driven plankton dynamics, marine productivity and sea spray modification with potentially significant climate impacts.
Darius Ceburnis received PhD degree in Natural Sciences in 1997 from the Institute of Physics, Lithuania and has been working at the National University of Ireland Galway since 2001. Our most significant work on marine aerosols has been recognized by three Nature publications. Another novel idea was developed around carbon isotopes for an unambiguous determination of organic matter origin in atmospheric aerosols which later helped to elucidate organic matter cycling in the marine environment with the recent publication in Nature Scientific Reports. He published around 100 peer-review papers to-date and being among the top 1% of cited authors in the geosciences discipline (Clarivate Analytics) with nearly 2000 total citations in the last decade and have provided critical technical and research support for Mace Head Atmospheric Research Station which has significantly contributed towards the establishing Mace Head infrastructure as the top atmospheric research infrastructure in the world.
E-mail: darius.ceburnis@nuigalway.ie