Journal: Scientific Reports

Article Title: Alterations in Amygdala Connectivity in Internet Addiction Disorder

doi: 10.1038/s41598-020-59195-w

Figure Lengend Snippet: Relationship between regional rsFC of amygdala-PFC and duration of IA. ( A , B ) Regional rsFC measures between amygdala and brain regions of PFC shown in Fig. , and all the regional rsFC had statistically significant difference between IA and HC groups with p < 8.7e-03 and p < 2.5e-03 for left and right amygdala, respectively. ( C ) The negative correlation between the adjusted regional rsFC measure of left amygdala-DLPFC_R and the duration of Internet addiction (months) in the IA group( r = −0.49, p < 8.0e-03). The rsFC* is the z value of regional rsFC measure adjusted by age, sex, HAMA score and BDI-13 score using multiple linear regression. In ( A , B ), on each box, the central mark is the median, the edges of the box are the 25th and 75th percentiles, and whiskers extend from each edge of the box to the most extreme values within 1.5 times the interquartile range. Stars indicate that the difference was statistically significant, and p values were results from two-sample t-test. Abbreviations: HAMA, Hamilton Anxiety Scale; BDI-13, Beck Depression Inventory (13 items). The other abbreviations are given in Fig. and Table . The figure was drawn by using MATLAB (R2016b version 9.1.0.441655) ( https://www.mathworks.com/ ).

Article Snippet: The ( A – C ) were drawn by using MATLAB (R2016b version 9.1.0.441655) ( https://www.mathworks.com/ ), BrainNet Viewer (BrainNet Viewer 1.7) ( https://www.nitrc.org/projects/bnv/ ), and MRIcron (MRIcron version 1.0.20190902) ( https://www.nitrc.org/projects/mricron/ ), respectively.

Techniques:

Journal: Scientific Reports

Article Title: Alterations in Amygdala Connectivity in Internet Addiction Disorder

doi: 10.1038/s41598-020-59195-w

Figure Lengend Snippet: Altered structural connectivity (SC) and fractional anisotropy (FA) in subjects with IA. ( A ) SC measures of the pathway between right amygdala and ACC, and the differences in SC measures between HC and IA groups were statistically significant ( p < 2.0e-04). ( B ) 3D view of the white matter pathway traversing right amygdala and ACC (in cyan). ( C ) Brain regions (in red/yellow) with statistically significant difference in FA between IA and HC groups on the white matter pathway traversing right amygdala and ACC (in cyan). In ( A ), on each box, the central mark is the median, the edges of the box are the 25th and 75th percentiles, and whiskers extend from each edge of the box to the most extreme values within 1.5 times the interquartile range. The p values were results from two-sample t-test. The abbreviations are given in Fig. and Table . The ( A – C ) were drawn by using MATLAB (R2016b version 9.1.0.441655) ( https://www.mathworks.com/ ), BrainNet Viewer (BrainNet Viewer 1.7) ( https://www.nitrc.org/projects/bnv/ ), and MRIcron (MRIcron version 1.0.20190902) ( https://www.nitrc.org/projects/mricron/ ), respectively.

Article Snippet: The ( A – C ) were drawn by using MATLAB (R2016b version 9.1.0.441655) ( https://www.mathworks.com/ ), BrainNet Viewer (BrainNet Viewer 1.7) ( https://www.nitrc.org/projects/bnv/ ), and MRIcron (MRIcron version 1.0.20190902) ( https://www.nitrc.org/projects/mricron/ ), respectively.

Techniques:

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

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

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

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

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

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 .

Techniques: