Zobrazeno 1 - 10
of 24
pro vyhledávání: '"Miho Ishizu"'
Linear and nonlinear response functions (RF) are extracted for the climate system and the carbon cycle represented by the MPI-ESM and cGENIE models, respectively. Appropriately designed simulations are run for this purpose. Joining these RFs, we have
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9c869fef22211ec8415991277d2d1cd
https://doi.org/10.5194/egusphere-egu23-10813
https://doi.org/10.5194/egusphere-egu23-10813
To gain a deeper understanding of why atmospheric CO2 varied on Milanković timescales, we conducted a 3 million-year transient carbon cycle simulation with the intermediate-complexity Grid Enabled Integrated Earth System (cGENIE). To this end we nud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a48813592d1bc814ffbd915bd0867e0
https://doi.org/10.5194/egusphere-egu23-10022
https://doi.org/10.5194/egusphere-egu23-10022
Publikováno v:
Environmental sciencetechnology. 56(17)
Calculating accurate air-sea fluxes for polychlorinated biphenyls (PCBs) is an essential condition for evaluating their transport in the atmosphere. A three-dimensional hydrodynamic-ecosystem-PCB coupled model was developed for the northwestern Pacif
Publikováno v:
Climatic Change. 162:877-902
Here, we investigate the seasonal variability in the dissolved inorganic carbon (DIC) cycle in the Northwest Pacific using a high-resolution biogeochemical and carbon model coupled with an operational ocean model. Results show that the contribution t
Publikováno v:
Climatic Change. 168
Long-term variations in ocean acidification indices in the Northwest Pacific were examined using observational data and a biogeochemical model with an operational ocean model product for the period 1993–2018. The model and observational data for th
Publikováno v:
Biogeosciences, Vol 16, Pp 4747-4763 (2019)
In recent decades, acidification of the open ocean has shown a consistent increase. However, analysis of long-term data in coastal seawater shows that the pH is highly variable because of coastal processes and anthropogenic carbon inputs. It is there
The multi-decadal variation in ocean acidification indices in the Northwest Pacific was examined using a biogeochemical model with an operational ocean model product for the period 1993–2018. We found that ocean acidification varied regionally in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e575bc6a2af37a5e9603e4c231665b0f
https://doi.org/10.21203/rs.3.rs-165133/v1
https://doi.org/10.21203/rs.3.rs-165133/v1
In recent decades, acidification of the open ocean has shown consistent increases. However, analysis of long-term data in coastal waters shows that the pH is highly variable because of coastal processes and anthropogenic carbon inputs. It is therefor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::860d89865805da06478f5cfbb001cded
https://www.biogeosciences-discuss.net/bg-2019-150/
https://www.biogeosciences-discuss.net/bg-2019-150/