Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Taylor M. Hughlett"'
Publikováno v:
Biogeosciences. 14:781-797
Dissolved oxygen (DO) concentration in the ocean is an important component of marine biogeochemical cycles and will be greatly altered as climate change persists. In this study a global oceanic carbon cycle model (HAMOCC 2.0) is used to address how m
Differences in the Atlantic meridional overturning circulation (AMOC) from the Younger Dryas (YD) to the Holocene can be explained by, but not limited to, factors relating to atmospheric greenhouse gas concentrations, discharge of freshwater into the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a41ad0f86b82891ae56c91c7f0880580
https://doi.org/10.5194/cp-2018-23
https://doi.org/10.5194/cp-2018-23
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Christine A. Shields, Arne M.E. Winguth, Cornelia Winguth, Mikaela Brown, Mathew Rothstein, Kelin Zhuang, Taylor M. Hughlett
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.