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of 46
pro vyhledávání: '"Baird ME"'
© 2020 Elsevier B.V. Ocean colour data are commonly used to quantify primary production, study phytoplankton dynamics and calibrate marine models, thus understanding the origin of errors in the retrieved chlorophyll-a (Chl-a) product is critical. On
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::2e1895d2acc9fa364771058a98da4fee
https://hdl.handle.net/10453/144628
https://hdl.handle.net/10453/144628
Autor:
Soja-Woźniak M, Laiolo L, Baird ME, Matear R, Clementson L, Schroeder T, Doblin MA, Suthers IM
© 2020 Elsevier B.V. Remotely-sensed ocean colour is the main tool for estimating chlorophyll a (Chl-a) concentration and primary productivity on the global scale. In order to investigate the source of errors in remotely-sensed Chl-a concentration w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::25db104e3d06489b91a6fec835dd56e8
https://hdl.handle.net/10453/144177
https://hdl.handle.net/10453/144177
Autor:
Messer, LF, Ostrowski, M, Doblin, MA, Petrou, K, Baird, ME, Ingleton, T, Bissett, A, Van de Kamp, J, Nelson, T, Paulsen, I, Bodrossy, L, Fuhrman, JA, Seymour, JR, Brown, MV
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::d85bb60aabd47f31d71642289a091171
https://hdl.handle.net/10453/141875
https://hdl.handle.net/10453/141875
© 2018 Chlorophyll-a measurements in the form of in situ observations and satellite ocean colour products are commonly used in data assimilation to calibrate marine biogeochemical models. Here, a two size-class phytoplankton biogeochemical model, wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::cfe1f17d0354cddc7573f54859a37458
https://hdl.handle.net/10453/127486
https://hdl.handle.net/10453/127486
Autor:
Robson, BJ, Arhonditsis, GB, Baird, ME, Brebion, J, Edwards, KF, Geoffroy, L, Hébert, MP, van Dongen-Vogels, V, Jones, EM, Kruk, C, Mongin, M, Shimoda, Y, Skerratt, JH, Trevathan-Tackett, SM, Wild-Allen, K, Kong, X, Steven, A
© 2017 Elsevier Ltd Mechanistic models rely on specification of parameters representing biophysical traits and process rates such as phytoplankton, zooplankton and seagrass growth and respiration rates, organism sizes, stoichiometry, light, temperat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::b58547bc8e2f1c6c503d5c18495d3182
https://hdl.handle.net/10453/131123
https://hdl.handle.net/10453/131123
© 2016 Elsevier B.V. Remote sensing observations show optical signatures to conform to the physical oceanographic patterns in the Tasman Sea. To test the link between physical oceanographic processes and bio-optical properties we investigated an in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::4723961d3446d6efea59be8b18610eff
https://hdl.handle.net/10453/127490
https://hdl.handle.net/10453/127490
© Australian Mathematical Society 2015. Because of its central role in the global carbon cycle, quantifying the biomass of photosynthetic microalgae in the oceans is crucial to our ability to estimate the oceans' carbon drawdown. Many traditional me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::bf71580d1251be0857870d1b2eb7748e
https://hdl.handle.net/10453/36379
https://hdl.handle.net/10453/36379
© 2015. American Geophysical Union. All Rights Reserved. The volume transport of nutrient-rich continental shelf water into a cyclonic frontal eddy (entrainment) was examined from satellite observations, a Slocum glider and numerical simulation outp
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https://explore.openaire.eu/search/publication?articleId=od_______363::1f2ec1e4f56a7701f3ddecf5251d74fa
https://hdl.handle.net/10453/33141
https://hdl.handle.net/10453/33141
Strengthening Western Boundary Currents (WBCs) advect warm, low nutrient waters into temperate latitudes, displacing more productive waters. WBCs also influence phytoplankton distribution and growth through current-induced upwelling, mesoscale eddy i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::52cade8cb743da5f543888d1684ac7cb
https://hdl.handle.net/10453/33188
https://hdl.handle.net/10453/33188
[1] Warm-core eddies (WCEs) often form in the meanders of Western Boundary Currents (WBCs). WCEs are frequently overwashed with less dense waters sourced from the WBC. We use the Regional Ocean Modelling System to investigate the ocean state during t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______363::6decccb585d3fb52bf8f50f81e1f155b
https://hdl.handle.net/10453/27475
https://hdl.handle.net/10453/27475