Zobrazeno 1 - 10
of 98
pro vyhledávání: '"Toby Tyrrell"'
Autor:
Yingxu Wu, Dorothee C. E. Bakker, Eric P. Achterberg, Amavi N. Silva, Daisy D. Pickup, Xiang Li, Sue Hartman, David Stappard, Di Qi, Toby Tyrrell
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-11 (2022)
Comparison of carbon dioxide and oxygen concentrations in ocean surface waters relative to saturation can be used to identify erroneous data collected by autonomous ocean platforms, suggests an analysis of data from multiple global datasets
Externí odkaz:
https://doaj.org/article/a552693798a641368cbff3d18620aa2a
Autor:
Richard E. Zeebe, Toby Tyrrell
Publikováno v:
Geochimica et Cosmochimica Acta. 257:373-392
In an earlier contribution to this journal, we provided a reconstruction of seawater carbonate ion concentration over the last 100 million years (Tyrrell, T. and Zeebe, R.E., Geochim. Cosmoch. Acta, 68, 3521-3530, 2004; TZ04 hereafter). Since then, m
What drives the latitudinal gradient in open-ocean surface dissolved inorganic carbon concentration?
Publikováno v:
Biogeosciences, Vol 16, Pp 2661-2681 (2019)
Biogeosciences (1726-4170) (Copernicus Gesellschaft Mbh), 2019-07, Vol. 16, N. 13, P. 2661-2681
Biogeosciences (1726-4170) (Copernicus Gesellschaft Mbh), 2019-07, Vol. 16, N. 13, P. 2661-2681
Previous work has not led to a clear understanding of the causes of spatial pattern in global surface ocean dissolved inorganic carbon (DIC), which generally increases polewards. Here, we revisit this question by investigating the drivers of observed
Autor:
Toby Tyrrell
Earth’s climate has remained continuously habitable throughout 3 or 4 billion years. This presents a puzzle (the ‘habitability problem’) because loss of habitability appears to have been more likely. Solar luminosity has increased by 30% over t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9cc360a24641ba5631fe5255e4c58f2
https://eprints.soton.ac.uk/445510/
https://eprints.soton.ac.uk/445510/
Autor:
Toby Tyrrell, Daisy Pickup
Understanding of controls on the spatial distributions of chemical elements in the surface ocean has improved over time. Macronutrients were understood first, followed by dissolved inorganic carbon and alkalinity. Utilising data collected in the Atla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f86ce0071d93f191ea435d910fcc5cf4
https://doi.org/10.5194/bg-2020-371
https://doi.org/10.5194/bg-2020-371
Autor:
Toby Tyrrell, Mark Christopher Moore, Adrian Martin, Alberto C. Naveira Garabato, Pieter Demuynck
Publikováno v:
Biogeosciences (1726-4170) (Copernicus Gesellschaft Mbh), 2020-04, Vol. 17, N. 8, P. 2289-2314
Biogeosciences, Vol 17, Pp 2289-2314 (2020)
Biogeosciences, Vol 17, Pp 2289-2314 (2020)
The nutrient composition (high in nitrate but low in silicate) of Subantarctic Mode Water (SAMW) forces diatom scarcity across much of the global surface ocean. This is because diatoms cannot grow without silicate. After formation and downwelling at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9138aef94ebbcb7ab8a8121803485915
https://archimer.ifremer.fr/doc/00676/78840/
https://archimer.ifremer.fr/doc/00676/78840/
Autor:
Toby Tyrrell, Richard E. Zeebe
Publikováno v:
Global Biogeochemical Cycles. 32:895-897
The nutrient composition (high in nitrate but low in silicate) of Subantarctic Mode Water (SAMW) forces diatom scarcity across much of the global surface ocean. This is because diatoms cannot grow without silicate. After formation and downwelling at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0421f575a56fc1294a4fdbcb37f5a83
https://doi.org/10.5194/bg-2019-120
https://doi.org/10.5194/bg-2019-120
Publikováno v:
Global Biogeochemical Cycles. 30:1493-1508
The causes of natural variation in alkalinity in the North Pacific surface ocean need to be investigated to understand the carbon cycle and to improve predictive algorithms. We used GLODAPv2 to test hypotheses on the causes of three longitudinal phen
Autor:
Eric P. Achterberg, Toby Tyrrell
Publikováno v:
Biogeosciences (BG), 11 (24). pp. 7269-7274.
Biogeosciences, Vol 11, Iss 24, Pp 7269-7274 (2014)
Biogeosciences, Vol 11, Iss 24, Pp 7269-7274 (2014)
The pH of the ocean is being lowered by its uptake of anthropogenic atmospheric carbon dioxide (CO2), produced as a result of combustion of fossil fuels and land use changes. This acidification is especially pronounced in the surface ocean, where the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::993fa92cb56d9369a64bafad15e543bb
https://www.biogeosciences.net/11/7269/2014/bg-11-7269-2014.pdf
https://www.biogeosciences.net/11/7269/2014/bg-11-7269-2014.pdf