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version 9.1.0.441655 (r2016b) (MathWorks Inc)

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MathWorks Inc version 9.1.0.441655 (r2016b)
Version 9.1.0.441655 (R2016b), supplied by MathWorks Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/version+9%2E1%2E0%2E441655+(r2016b)/pmc11804811-113-6-6
Average 90 stars, based on 1 article reviews

version 9.1.0.441655 (r2016b) - by Bioz Stars, 2026-10

90/100 stars

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Article Title: Identifying and Assessing Inter-Muscular Fat at the Distal Diaphyseal Femur Measured by Peripheral Quantitative Computed Tomography (pQCT).
Article Snippet: Patrick J. Owen, Nicolas H. Hart, Christopher Latella, Ashlee M. Hendy, S everine Lamon, and Timo Rantalainen* 1 Deakin University, Institute for Physical Activity and Nutrition (IPAN), School of Exercise and Nutrition Sciences, Geelong, Victoria, Australia; 2 Exercise Medicine Research Institute, Edith Cowan University, Perth, Western Australia, Australia; 3 Institute for Health Research, University of Notre Dame Australia, Perth, Western Australia, Australia; 4 Western Australian Bone Research Collaboration, Perth, Western Australia, Australia; 5 Neurophysiology Research Laboratory, School of Medical and Health Sciences, Edith Cowan University, Perth, Wetsern Australia, Australia; and 6 Gerontology Research Center and Faculty of Sport and Health Sciences, University of Jyv€ askyl€ a, Finland

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Images showing Southwestern Atlantic Ocean and study area. (a) MUR Sea Surface Temperature (°C) with Reanalysis ERA5 Sea Level Pressure (hPa) showing the study area in a broad view. (b) Same as (a) , but in view zoom of the eddy. (c) Sea Level Anomaly (m) relative to the geoid measured by Altimetry (colors) and derived absolute geostrophic velocity current vectors (m s -1 ). (d) Chlorophyll-a concentration (Chl-a in mg m −3 ). All data are for 18th October 2019. The white circles denote the Po/V Almirante Maximiano trajectory while crossing the eddy dipole and the XBTs and radiosondes launching positions. The symbols over the continent indicate the country names of Brazil (BR), Uruguay (UY) and Argentina (AR). Grid Analysis and Display System (GrADS), Version 2.2.1.oga.1. http://opengrads.org . MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Journal: Scientific Reports

Article Title: Oceanic eddy-induced modifications to air–sea heat and CO 2 fluxes in the Brazil-Malvinas Confluence

doi: 10.1038/s41598-021-89985-9

Figure Lengend Snippet: Images showing Southwestern Atlantic Ocean and study area. (a) MUR Sea Surface Temperature (°C) with Reanalysis ERA5 Sea Level Pressure (hPa) showing the study area in a broad view. (b) Same as (a) , but in view zoom of the eddy. (c) Sea Level Anomaly (m) relative to the geoid measured by Altimetry (colors) and derived absolute geostrophic velocity current vectors (m s -1 ). (d) Chlorophyll-a concentration (Chl-a in mg m −3 ). All data are for 18th October 2019. The white circles denote the Po/V Almirante Maximiano trajectory while crossing the eddy dipole and the XBTs and radiosondes launching positions. The symbols over the continent indicate the country names of Brazil (BR), Uruguay (UY) and Argentina (AR). Grid Analysis and Display System (GrADS), Version 2.2.1.oga.1. http://opengrads.org . MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Article Snippet: MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Techniques: Derivative Assay, Concentration Assay

Synoptic, in situ measurements taken along Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H-41) route while crossing the eddy. (a) XBT temperature (°C) depth profiles. The numbers in the legend denote de XBT positions, with 1 being the westernmost position and 5 being the easternmost position. The number 2 (red) is closest to the eddy core position. (b) Salinity, measured by ship thermosalinographer. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Journal: Scientific Reports

Article Title: Oceanic eddy-induced modifications to air–sea heat and CO 2 fluxes in the Brazil-Malvinas Confluence

doi: 10.1038/s41598-021-89985-9

Figure Lengend Snippet: Synoptic, in situ measurements taken along Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H-41) route while crossing the eddy. (a) XBT temperature (°C) depth profiles. The numbers in the legend denote de XBT positions, with 1 being the westernmost position and 5 being the easternmost position. The number 2 (red) is closest to the eddy core position. (b) Salinity, measured by ship thermosalinographer. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Article Snippet: MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Techniques: In Situ

Temperature profiles (°C) of the atmosphere and ocean (colors) taken simultaneously by radiosondes and XBTs along the Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H-41) route while crossing the eddy during 18 th October 2019. The lower part of this figure also displays the oceanic sounding positions. Wind magnitude (m s -1 ) in vectors is also displayed, superimposed on the air temperature. The vector size reflects the wind magnitude. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Journal: Scientific Reports

Article Title: Oceanic eddy-induced modifications to air–sea heat and CO 2 fluxes in the Brazil-Malvinas Confluence

doi: 10.1038/s41598-021-89985-9

Figure Lengend Snippet: Temperature profiles (°C) of the atmosphere and ocean (colors) taken simultaneously by radiosondes and XBTs along the Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H-41) route while crossing the eddy during 18 th October 2019. The lower part of this figure also displays the oceanic sounding positions. Wind magnitude (m s -1 ) in vectors is also displayed, superimposed on the air temperature. The vector size reflects the wind magnitude. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Article Snippet: MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Techniques: Plasmid Preparation

$Synoptic, in situ measurements taken along Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H41) route while crossing the eddy. (a) SST bulk (°C) and salinity. (b) Stability parameters, \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\zeta$$\end{document} ζ and SST—T air (°C). (c) SST bulk (°C) and wind stress (N m -2 ). (d) SST bulk (°C) and sea level pressure (hPa). (e) Wind speed magnitude and friction velocity (u * ), both in m s -1 . (f) Components of net heat flux (Q net ), short and long wave radiation (S w and L w ), latent and sensible heat fluxes (Q l and Q s , both measured by eddy covariance) in W m -2 . The bars in (f) are the standard error oriented up for visual clarity representing 95% confidence interval. However, they must be interpreted both up and down. All information is derived from the ship-borne meteorological data. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .$

Journal: Scientific Reports

Article Title: Oceanic eddy-induced modifications to air–sea heat and CO 2 fluxes in the Brazil-Malvinas Confluence

doi: 10.1038/s41598-021-89985-9

Figure Lengend Snippet: Synoptic, in situ measurements taken along Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H41) route while crossing the eddy. (a) SST bulk (°C) and salinity. (b) Stability parameters, \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\zeta$$\end{document} ζ and SST—T air (°C). (c) SST bulk (°C) and wind stress (N m -2 ). (d) SST bulk (°C) and sea level pressure (hPa). (e) Wind speed magnitude and friction velocity (u * ), both in m s -1 . (f) Components of net heat flux (Q net ), short and long wave radiation (S w and L w ), latent and sensible heat fluxes (Q l and Q s , both measured by eddy covariance) in W m -2 . The bars in (f) are the standard error oriented up for visual clarity representing 95% confidence interval. However, they must be interpreted both up and down. All information is derived from the ship-borne meteorological data. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Article Snippet: MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Techniques: In Situ, Derivative Assay

$Atmospheric in situ CO 2 fluxes measured by Eddy Covariance method along Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H-41) route while crossing the eddy. (a) CO 2 fluxes ( \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\upmu$$\end{document} μ mol m -2 s -1 ) and stability parameter \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\zeta$$\end{document} ζ 10 2 . (b) CO 2 fluxes ( \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\upmu$$\end{document} μ mol m -2 s -1 ) and stability parameter SST—T air (°C). The error bars are the standard error and are oriented up. The bars are the standard error oriented up for visual clarity representing 95% confidence interval. However, they must be interpreted both up and down. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .$

Journal: Scientific Reports

Article Title: Oceanic eddy-induced modifications to air–sea heat and CO 2 fluxes in the Brazil-Malvinas Confluence

doi: 10.1038/s41598-021-89985-9

Figure Lengend Snippet: Atmospheric in situ CO 2 fluxes measured by Eddy Covariance method along Brazilian Navy Polar Vessel (Po/V) Almirante Maximiano (H-41) route while crossing the eddy. (a) CO 2 fluxes ( \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\upmu$$\end{document} μ mol m -2 s -1 ) and stability parameter \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\zeta$$\end{document} ζ 10 2 . (b) CO 2 fluxes ( \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\upmu$$\end{document} μ mol m -2 s -1 ) and stability parameter SST—T air (°C). The error bars are the standard error and are oriented up. The bars are the standard error oriented up for visual clarity representing 95% confidence interval. However, they must be interpreted both up and down. MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Article Snippet: MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Techniques: In Situ

Relationship between the CO 2 transfer velocity coefficient and the neutral wind speed at 10 m calculated from the data collected in this experiment. The quadratic fitted curve K = 0.34.U 10n 2 – 0.32 U 10n + 0.94 with r 2 = 0.75 is represented by the magenta line. The blue, red and green curves represent the CO 2 transfer coefficient obtained in the literature , , . MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Journal: Scientific Reports

Article Title: Oceanic eddy-induced modifications to air–sea heat and CO 2 fluxes in the Brazil-Malvinas Confluence

doi: 10.1038/s41598-021-89985-9

Figure Lengend Snippet: Relationship between the CO 2 transfer velocity coefficient and the neutral wind speed at 10 m calculated from the data collected in this experiment. The quadratic fitted curve K = 0.34.U 10n 2 – 0.32 U 10n + 0.94 with r 2 = 0.75 is represented by the magenta line. The blue, red and green curves represent the CO 2 transfer coefficient obtained in the literature , , . MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

Article Snippet: MATLAB, Version 9.1.0.441655 (R2016b). https://www.mathworks.com .

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