Zobrazeno 1 - 10
of 16
pro vyhledávání: '"P E Land"'
Publikováno v:
PLoS ONE, Vol 11, Iss 9, p e0161105 (2016)
The global oceans are considered a major sink of atmospheric carbon dioxide (CO2). Rain is known to alter the physical and chemical conditions at the sea surface, and thus influence the transfer of CO2 between the ocean and atmosphere. It can influen
Externí odkaz:
https://doaj.org/article/7df9a5a01c2a4fef82b01ad0ef36256e
Publikováno v:
Earth System Science Data, Vol 15, Pp 2499-2516 (2023)
Large rivers play an important role in transferring water and all of its constituents, including carbon in its various forms, from the land to the ocean, but the seasonal and inter-annual variations in these riverine flows remain unclear. Satellite E
Externí odkaz:
https://doaj.org/article/b7dee4d4efff496ab5cbc1782d7b3489
Autor:
Hannah L. Green, Helen S. Findlay, Jamie D. Shutler, Richard Sims, Richard Bellerby, Peter E. Land
Publikováno v:
Earth and Space Science, Vol 10, Iss 12, Pp n/a-n/a (2023)
Abstract The long‐term absorption by the oceans of atmospheric carbon dioxide is leading to the slow decline of ocean pH, a process termed ocean acidification (OA). The Arctic is a challenging region to gather enough data to examine the changes in
Externí odkaz:
https://doaj.org/article/9490ee7d54874b8f9c24a4a581654b33
OceanSODA-MDB: a standardised surface ocean carbonate system dataset for model–data intercomparisons
Autor:
P. E. Land, H. S. Findlay, J. D. Shutler, J.-F. Piolle, R. Sims, H. Green, V. Kitidis, A. Polukhin, I. I. Pipko
Publikováno v:
Earth System Science Data, Vol 15, Pp 921-947 (2023)
In recent years, large datasets of in situ marine carbonate system parameters (partial pressure of CO2 (pCO2), total alkalinity, dissolved inorganic carbon and pH) have been collated, quality-controlled and made publicly available. These carbonate sy
Externí odkaz:
https://doaj.org/article/b3f09421812f4a4d8e0619fc7d006a92
Autor:
T. Holding, I. G. Ashton, J. D. Shutler, P. E. Land, P. D. Nightingale, A. P. Rees, I. Brown, J.-F. Piolle, A. Kock, H. W. Bange, D. K. Woolf, L. Goddijn-Murphy, R. Pereira, F. Paul, F. Girard-Ardhuin, B. Chapron, G. Rehder, F. Ardhuin, C. J. Donlon
Publikováno v:
Ocean Science, Vol 15, Pp 1707-1728 (2019)
The flow (flux) of climate-critical gases, such as carbon dioxide (CO2), between the ocean and the atmosphere is a fundamental component of our climate and an important driver of the biogeochemical systems within the oceans. Therefore, the accurate c
Externí odkaz:
https://doaj.org/article/6cfcb06ea1004170acce92d3a4054bf2
Publikováno v:
Frontiers in Marine Science, Vol 8 (2021)
It is widely projected that under future climate scenarios the economic importance of Arctic Ocean fish stocks will increase. The Arctic Ocean is especially vulnerable to ocean acidification and already experiences low pH levels not projected to occu
Externí odkaz:
https://doaj.org/article/afc9aed6d582463c9c929499d7780705
Publikováno v:
Remote Sensing, Vol 12, Iss 15, p 2476 (2020)
Oceanic internal waves occur within stratified water along the boundary between water layers of different density and are generated when strong tidal currents flow over seabed topography. Their amplitude can exceed 50 m and they transport energy over
Externí odkaz:
https://doaj.org/article/0bc07d5f5d3344159d6c03e36b57120f
Autor:
Peter E. Land, Trevor C. Bailey, Malcolm Taberner, Silvia Pardo, Shubha Sathyendranath, Kayvan Nejabati Zenouz, Vicki Brammall, Jamie D. Shutler, Graham D. Quartly
Publikováno v:
Remote Sensing, Vol 10, Iss 5, p 695 (2018)
Uncertainty estimation is crucial to establishing confidence in any data analysis, and this is especially true for Essential Climate Variables, including ocean colour. Methods for deriving uncertainty vary greatly across data types, so a generic stat
Externí odkaz:
https://doaj.org/article/debcdd9356a9414dbaa2722a801925af
Autor:
J. D. Shutler, P. E. Land, C. W. Brown, H. S. Findlay, C. J. Donlon, M. Medland, R. Snooke, J. C. Blackford
Publikováno v:
Biogeosciences, Vol 10, Iss 4, Pp 2699-2709 (2013)
Coccolithophores are the primary oceanic phytoplankton responsible for the production of calcium carbonate (CaCO3). These climatically important plankton play a key role in the oceanic carbon cycle as a major contributor of carbon to the open ocean c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::98183e202c2649a14d041017b8c07100
https://www.biogeosciences.net/10/2699/2013/
https://www.biogeosciences.net/10/2699/2013/
Autor:
P. E. Land, J. D. Shutler, R. D. Cowling, D. K. Woolf, P. Walker, H. S. Findlay, R. C. Upstill-Goddard, C. J. Donlon
Publikováno v:
Biogeosciences, Vol 10, Iss 12, Pp 8109-8128 (2013)
We applied coincident Earth observation data collected during 2008 and 2009 from multiple sensors (RA2, AATSR and MERIS, mounted on the European Space Agency satellite Envisat) to characterise environmental conditions and integrated sea–air fluxes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a80ef737cf7dc0548b292dc50df5eb63
https://www.biogeosciences.net/10/8109/2013/
https://www.biogeosciences.net/10/8109/2013/