Gotowa bibliografia na temat „Terrigenous dissolved carbon”
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Artykuły w czasopismach na temat "Terrigenous dissolved carbon"
Hansell, D. A. "Degradation of Terrigenous Dissolved Organic Carbon in the Western Arctic Ocean". Science 304, nr 5672 (7.05.2004): 858–61. http://dx.doi.org/10.1126/science.1096175.
Pełny tekst źródłaAarnos, Hanna, Yves Gélinas, Ville Kasurinen, Yufei Gu, Veli-Mikko Puupponen i Anssi V. Vähätalo. "Photochemical Mineralization of Terrigenous DOC to Dissolved Inorganic Carbon in Ocean". Global Biogeochemical Cycles 32, nr 2 (luty 2018): 250–66. http://dx.doi.org/10.1002/2017gb005698.
Pełny tekst źródłaOpsahl, Stephen P., i Richard G. Zepp. "Photochemically-induced alteration of stable carbon isotope ratios (δ13C) in terrigenous dissolved organic carbon". Geophysical Research Letters 28, nr 12 (15.06.2001): 2417–20. http://dx.doi.org/10.1029/2000gl012686.
Pełny tekst źródłaBenner, Ronald, Bryan Benitez-Nelson, Karl Kaiser i Rainer M. W. Amon. "Export of young terrigenous dissolved organic carbon from rivers to the Arctic Ocean". Geophysical Research Letters 31, nr 5 (10.03.2004): n/a. http://dx.doi.org/10.1029/2003gl019251.
Pełny tekst źródłaFichot, Cédric G., i Ronald Benner. "The fate of terrigenous dissolved organic carbon in a river-influenced ocean margin". Global Biogeochemical Cycles 28, nr 3 (marzec 2014): 300–318. http://dx.doi.org/10.1002/2013gb004670.
Pełny tekst źródłaMartin, P., N. Sanwlani, TWQ Lee, JMC Wong, KYW Chang, EWS Wong i SC Liew. "Dissolved organic matter from tropical peatlands reduces shelf sea light availability in the Singapore Strait, Southeast Asia". Marine Ecology Progress Series 672 (19.08.2021): 89–109. http://dx.doi.org/10.3354/meps13776.
Pełny tekst źródłaZhang, Zheyue, Jihong Qin, Hui Sun, Jiyuan Yang i Yanyang Liu. "Spatiotemporal Dynamics of Dissolved Organic Carbon and Freshwater Browning in the Zoige Alpine Wetland, Northeastern Qinghai-Tibetan Plateau". Water 12, nr 9 (31.08.2020): 2453. http://dx.doi.org/10.3390/w12092453.
Pełny tekst źródłaMartin, Patrick, Nagur Cherukuru, Ashleen S. Y. Tan, Nivedita Sanwlani, Aazani Mujahid i Moritz Müller. "Distribution and cycling of terrigenous dissolved organic carbon in peatland-draining rivers and coastal waters of Sarawak, Borneo". Biogeosciences 15, nr 22 (16.11.2018): 6847–65. http://dx.doi.org/10.5194/bg-15-6847-2018.
Pełny tekst źródłaFichot, Cédric G., Steven E. Lohrenz i Ronald Benner. "Pulsed, cross-shelf export of terrigenous dissolved organic carbon to the Gulf of Mexico". Journal of Geophysical Research: Oceans 119, nr 2 (luty 2014): 1176–94. http://dx.doi.org/10.1002/2013jc009424.
Pełny tekst źródłaLeushina, Evgeniya, Timur Bulatov, Elena Kozlova, Ivan Panchenko, Andrey Voropaev, Tagir Karamov, Yakov Yermakov, Natalia Bogdanovich i Mikhail Spasennykh. "Upper Jurassic–Lower Cretaceous Source Rocks in the North of Western Siberia: Comprehensive Geochemical Characterization and Reconstruction of Paleo-Sedimentation Conditions". Geosciences 11, nr 8 (30.07.2021): 320. http://dx.doi.org/10.3390/geosciences11080320.
Pełny tekst źródłaRozprawy doktorskie na temat "Terrigenous dissolved carbon"
Bertin, Clément. "The role of the Mackenzie River in the carbon biogeochemistry of the Beaufort Sea coastal waters (Arctic Ocean)". Electronic Thesis or Diss., La Rochelle, 2023. http://www.theses.fr/2023LAROS007.
Pełny tekst źródłaAbout 10 % of atmospheric carbon dioxide is sequestered in the ocean above 60°N, half of which is in coastal seas where 10 % of the global riverine freshwater volume flows in. Five of the world’s largest rivers convey in the Arctic Ocean (AO) huge quantities of dissolved carbon in the organic (DOC) and inorganic (DIC) form. The response of the coastal ocean to this supply is still highly uncertain, which makes the assessment of air-sea CO2fluxes challenging in this remote region. It is thus timely to gain a better understanding of the impact of terrestrial carbon released by watersheds on air-sea CO2 fluxes in Arctic rivers plumes, especially in a context of global warming. In the present PhD thesis, the ECCO-Darwin ocean-sea ice-biogeochemical model is used to investigate the synoptic to interannual response of the South eastern Beaufort Sea (Western AO) to the Mackenzie River’s carbon exports. The model includes the very first daily terrestrial DOC (tDOC) runoff forcing estimated through merging riverine in situ measurements and coastal remotely sensed data at three major delta outlets, over the last two decades (2000-2019). We find that interannual variability in river discharge modulates localized air-sea CO2flux in the coastal plume with riverine DIC contributing twice as much as riverine DOC to CO2 outgassing. As current knowledge on tDOC remineralization in Arctic plume regions is still uncertain, the range of air-sea CO2 flux variability due to microbial remineralization is estimated to ±0.39 TgC yr−1 in 2009. Other biophysical processes also contribute to the high CO2 flux variability, such as tDOC flocculation (+0.14 TgC yr−1 in gassing) and enhanced plume stratification (+0.35 TgC yr−1 outgassing). To conclude, the work presented here intends to pave the way toward a better representation of the land-to-ocean continuum (LOAC) in regional Arctic models with the aim to improve the simulated carbon cycle in rapidly changing Arctic watersheds and coastal seas