Airborne observations over the North Atlantic Ocean reveal the importance of gas-phase urea in the atmosphere.
Airborne observations over the North Atlantic Ocean reveal the importance of gas-phase urea in the atmosphere.
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DOI:
10.1073/pnas.2218127120
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发表时间:
2023-06-20
影响因子:
11.1
通讯作者:
Coe, Hugh
中科院分区:
文献类型:
--
作者:
Matthews, Emily;Bannan, Thomas J.;Khan, M. Anwar H.;Shallcross, Dudley E.;Stark, Harald;Browne, Eleanor C.;Archibald, Alexander T.;Mehra, Archit;Bauguittei, Stephane J. -B.;Reed, Chris;Thamban, Navaneeth M.;Wu, Huihui;Barker, Patrick;Lee, James;Carpenter, Lucy J.;Yang, Mingxi;Bell, Thomas G.;Allen, Grant;Jayne, John T.;Percival, Carl J.;McFiggansa, Gordon;Gallaghera, Martin;Coe, Hugh
Reduced nitrogen (N) plays a fundamental role in ocean biogeochemistry, yet marine-reduced organic nitrogen (ON) species are poorly characterized as is their role in the global N cycle. Our observations suggest that biologically rich ocean environments are a significant source of urea to the atmosphere and that the atmosphere is likely to provide a fast transport route for the redistribution of reduced N across the seawater surface and as such have implications for marine productivity. Our findings show that the global marine burden of urea is significant which necessitates a revision of the atmospheric N cycle. Reduced nitrogen (N) is central to global biogeochemistry, yet there are large uncertainties surrounding its sources and rate of cycling. Here, we present observations of gas-phase urea (CO(NH2)2) in the atmosphere from airborne high-resolution mass spectrometer measurements over the North Atlantic Ocean. We show that urea is ubiquitous in the lower troposphere in the summer, autumn, and winter but was not detected in the spring. The observations suggest that the ocean is the primary emission source, but further studies are required to understand the responsible mechanisms. Urea is also observed aloft due to long-range transport of biomass-burning plumes. These observations alongside global model simulations point to urea being an important, and currently unaccounted for, component of reduced-N to the remote marine atmosphere. Airborne transfer of urea between nutrient-rich and -poor parts of the ocean can occur readily and could impact ecosystems and oceanic uptake of carbon dioxide, with potentially important climate implications.
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DOI:
10.1073/pnas.1516847113
发表时间:
2016-01-26
影响因子:
11.1
作者:
Altieri, Katye E.;Fawcett, Sarah E.;Hastings, Meredith G.
通讯作者:
Hastings, Meredith G.
影响因子:
4.4
作者:
Mace, KA;Artaxo, P;Duce, RA
通讯作者:
Duce, RA
影响因子:
1.4
作者:
Bratbak, G;Jacobsen, A;Heldal, M
通讯作者:
Heldal, M
影响因子:
5
作者:
Khan, M. A. H.;Gillespie, S. M. P.;Shallcross, D. E.
通讯作者:
Shallcross, D. E.
影响因子:
5.5
作者:
Khan, M. A. H.;Lowe, D.;Shallcross, D. E.
通讯作者:
Shallcross, D. E.