Zobrazeno 1 - 10
of 620
pro vyhledávání: '"Katavouta, A."'
Autor:
Rulent, Julia, James, Molly K., Rameshwaran, Ponnambalam, Jardine, Jennifer E., Katavouta, Anna, Wakelin, Sarah, Jayathilaka, Ruchira, Arulananthan, Kanapathipillai, Holt, Jason, Sutton, Mark A., Artioli, Yuri
Publikováno v:
In Marine Pollution Bulletin December 2024 209 Part A
Publikováno v:
Biogeosciences, Vol 20, Pp 1671-1690 (2023)
The ocean carbon store plays a vital role in setting the carbon response to emissions and variability in the carbon cycle. However, due to the ocean's strong regional and temporal variability, sparse carbon observations limit our understanding of his
Externí odkaz:
https://doaj.org/article/ea2b5f66953b4e19afb441a380fcfdf3
Autor:
J. Polton, J. Harle, J. Holt, A. Katavouta, D. Partridge, J. Jardine, S. Wakelin, J. Rulent, A. Wise, K. Hutchinson, D. Byrne, D. Bruciaferri, E. O'Dea, M. De Dominicis, P. Mathiot, A. Coward, A. Yool, J. Palmiéri, G. Lessin, C. G. Mayorga-Adame, V. Le Guennec, A. Arnold, C. Rousset
Publikováno v:
Geoscientific Model Development, Vol 16, Pp 1481-1510 (2023)
In response to an increasing demand for bespoke or tailored regional ocean modelling configurations, we outline fundamental principles and practices that can expedite the process to generate new configurations. The paper develops the principle of rep
Externí odkaz:
https://doaj.org/article/8c6899a9059d42b7b462ebe30e4e28f1
Akademický článek
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Publikováno v:
Journal of Climate, 2021 May . 34(10), 3907-3925.
Externí odkaz:
https://www.jstor.org/stable/27076832
Autor:
A. Katavouta, R. G. Williams
Publikováno v:
Biogeosciences, Vol 18, Pp 3189-3218 (2021)
The ocean response to carbon emissions involves the combined effect of an increase in atmospheric CO2, acting to enhance the ocean carbon storage, and climate change, acting to decrease the ocean carbon storage. This ocean response can be characteris
Externí odkaz:
https://doaj.org/article/419ad4d692524adc96d1ad2322186d00
Publikováno v:
Journal of Climate, 2019 Aug . 32(16), 5085-5105.
Externí odkaz:
https://www.jstor.org/stable/26754331
Autor:
V. K. Arora, A. Katavouta, R. G. Williams, C. D. Jones, V. Brovkin, P. Friedlingstein, J. Schwinger, L. Bopp, O. Boucher, P. Cadule, M. A. Chamberlain, J. R. Christian, C. Delire, R. A. Fisher, T. Hajima, T. Ilyina, E. Joetzjer, M. Kawamiya, C. D. Koven, J. P. Krasting, R. M. Law, D. M. Lawrence, A. Lenton, K. Lindsay, J. Pongratz, T. Raddatz, R. Séférian, K. Tachiiri, J. F. Tjiputra, A. Wiltshire, T. Wu, T. Ziehn
Publikováno v:
Biogeosciences, Vol 17, Pp 4173-4222 (2020)
Results from the fully and biogeochemically coupled simulations in which CO2 increases at a rate of 1 % yr−1 (1pctCO2) from its preindustrial value are analyzed to quantify the magnitude of carbon–concentration and carbon–climate feedback p
Externí odkaz:
https://doaj.org/article/94990c91dee946e5b96eace492047b42
Publikováno v:
Environmental Research Letters, Vol 15, Iss 9, p 0940c1 (2020)
The surface warming response to carbon emissions is diagnosed using a suite of Earth system models, 9 CMIP6 and 7 CMIP5, following an annual 1% rise in atmospheric CO _2 over 140 years. This surface warming response defines a climate metric, the Tran
Externí odkaz:
https://doaj.org/article/1de803d5118d4c62ac60889108c2e2fb