2014 · CO2 with a carbon cycle model. G. A. Alexandrov. A. M. Obukhov Institute of Atmospheric Physics
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Explaining the seasonal cycle of the globally averaged CO2 with a
21-Oct-2014 CO2 with a carbon-cycle model. G. A. Alexandrov. A. M. Obukhov Institute of Atmospheric Physics Russian Academy of Sciences |
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CMIP6 simulations of GPP growth satisfy the constraint imposed by
27-Nov-2020 imposed by increasing CO2 seasonal-cycle amplitude. G A Alexandrov1*. 1 A.M. Obukhov Institute of Atmospheric Physics |
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Influence of global warming and climate continentality on the
Moscow urban heat island. A S Ginzburg G A Alexandrov. A.M. Obukhov Institute of Atmospheric Physics |
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The negative correlation between the changes in Moscows
To cite this article: G A Alexandrov et al 2019 IOP Conf. Ser. 1 A.M. Obukhov Institute of Atmospheric Physics Russian Academy of ... carbon dioxide. |
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The limits to growth of northern peatland carbon stocks
1 A.M. Obukhov Institute of Atmospheric Physics Russian Academy of Sciences |
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The capacity of northern peatlands for long-term carbon sequestration
1 A.M. Obukhov Institute of Atmospheric Physics Russian Academy of a large carbon sink since the Last Glacial Maximum (Loisel et al. |
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The capacity of northern peatlands for long-term carbon sequestration
03-Jan-2020 Georgii A. Alexandrov1 Victor A. Brovkin2 |
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The capacity of northern peatlands for long-term carbon sequestration
03-Jan-2020 M. Obukhov Institute of Atmospheric Physics Russian Academy of Sciences |
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The influence of climate on peatland extent in Western Siberia since
20-Apr-2016 therefore incorporating peatlands into Earth system models is a ... M. Obukhov Institute of Atmospheric Physics |
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The influence of climate on peatland extent in Western Siberia since
20-Apr-2016 therefore incorporating peatlands into Earth system models is a ... M. Obukhov Institute of Atmospheric Physics |
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Explaining the seasonal cycle of the globally averaged CO2
The seasonal changes in the globally averaged atmospheric carbon-dioxide concentrations re?ect animportant aspect of the global carbon cycle: the gas exchange between the atmosphere and |
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Explaining the seasonal cycle of the globally averaged `=0200
6 jan 2014 · per Earth Syst Dynam Discuss , 5, 63–81, 2014 globally averaged CO2 with a carbon cycle model G A Alexandrov A M Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Pyzhevsky 3, 119017 |
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The limits to growth of northern peatland carbon stocks
1 A M Obukhov Institute of Atmospheric Physics, Russian Academy of important role in reducing the atmospheric carbon dioxide concentration over the The recent compilations of peatland data (Loisel et al , 2014; Treat et al , hydraulic conductivity of peat and mineral materials below the peat (Alexandrov et al , 2016) |
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RUSSIAN NATIONAL REPORT
Atmospheric Ozone (Chairman N F Elansky, A M Obukhov Institute of using climate model of the Institute of atmospheric physics name A M Obukhov carbon dioxide exchange between the atmosphere and the ocean in the Arctic Alexandrov G A , 2014: Explaining the seasonal cycle of the globally averaged CO2 |
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Berichte 739 2020 - EPIC - AWI
27 mar 2020 · Permafrost carbon in earth system models: Progress and challenges 12:15 – 12: 30 Alexander J Winkler, R B Myneni, G A Alexandrov, V Brovkin Changing Arctic Carbon cycle in the cOastal Ocean Near-shore (CACOON): M Obukhov Institute of Atmospheric Physics RAS, Moscow, Russia |
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References
Alexandrov GA, Yamagata Y, Saigusa N, Oikawa T (2005) Long-term carbon exchange at the Aota M, Shirasawa K, Krapivin VF, Mkrtchyan FA (1993) A project of the Bjorkstrom A (1979) A model of CO2 in interaction between atmosphere, Moscow Institute of State and Corporative Management Publishing, Moscow, |
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View Abstracts - sense1cn
Linquan Mu, Patricia Yager ( The University of Georgia, US ) the ASP can be defined as a major sink for atmospheric CO2 with large spatial variability tom- up (carbon cycle models) and top-down (atmospheric inversion models) Georgii Alexandrov ( A M Obukhov Institute of Atmospheric Physics, Russian Academy of |
