Journal: eLife

Article Title: Myelination synchronizes cortical oscillations by consolidating parvalbumin-mediated phasic inhibition

doi: 10.7554/eLife.73827

Figure Lengend Snippet:

Article Snippet: Software, algorithm , Neurolucida 360Neurolucida Explorer , MBF Bioscience , V2018.02;RRID: SCR_001775 , .

Techniques: Transfection, Construct, Recombinant, Software, Patch Clamp, In Vivo

Journal: Scientific Data

Article Title: A dataset of direct observations of sea ice drift and waves in ice

doi: 10.1038/s41597-023-02160-9

Figure Lengend Snippet: Overview of the deployments, their locations and time spans, the sea ice conditions, and the kind and number of instruments deployed.

Article Snippet: 2021-02 , Arctic, Barents Sea, east Svalbard, 77 N 30E , MIZ: 5/10 to 10/10 , v2018: 6 + v2021: 11 (6 with waves).

Techniques:

Journal: Scientific Data

Article Title: A dataset of direct observations of sea ice drift and waves in ice

doi: 10.1038/s41597-023-02160-9

Figure Lengend Snippet: Validation of the instrument v2018 IMU measurement and processing (IMU curves) against co-located pressure-sensor-based measurements of waves using a Seabird pressure sensor (SBE curves), reproduced from . The measurements were obtained during a test campaign of the IMU measurement methodology performed on landfast ice in Tempelfjorden, Svalbard, in 2016. Shaded areas indicate the 5-sigma confidence intervals, computed from the Chi-squared uncertainty distribution estimate for stochastic Gaussian wave spectrum following the methodology discussed in , . Agreement within the confidence intervals is observed.

Article Snippet: 2021-02 , Arctic, Barents Sea, east Svalbard, 77 N 30E , MIZ: 5/10 to 10/10 , v2018: 6 + v2021: 11 (6 with waves).

Techniques: Biomarker Discovery

Journal: Scientific Data

Article Title: A dataset of direct observations of sea ice drift and waves in ice

doi: 10.1038/s41597-023-02160-9

Figure Lengend Snippet: Validation of the instrument v2018 (I810) against the Sofar Spotter instrument (W0173), reproduced from . The instruments were deployed close to each other, but drifted slightly with time. Still, agreement within 5% is obtained for the significant wave height estimate (Hs, top), and the location and height of the wave spectrum peak (bottom). Slight differences are observed regarding the high frequency tail of the spectra. This is due to the increased noise of the GPS-based measurement methodology of the Sofar Spotter in quiet conditions corresponding to waves in ice, compared with the accelerometer-based measurement methodology of the v2018 in the same conditions.

Article Snippet: 2021-02 , Arctic, Barents Sea, east Svalbard, 77 N 30E , MIZ: 5/10 to 10/10 , v2018: 6 + v2021: 11 (6 with waves).

Techniques: Biomarker Discovery

Journal: Scientific Data

Article Title: A dataset of direct observations of sea ice drift and waves in ice

doi: 10.1038/s41597-023-02160-9

Figure Lengend Snippet: Illustration of the noise threshold at rest for the instrument v2018, reproduced from . This characterizes the typical noise level of the combination of the VN100 IMU and the wave processing algorithm used to generate the spectra transmitted over Iridium.

Article Snippet: 2021-02 , Arctic, Barents Sea, east Svalbard, 77 N 30E , MIZ: 5/10 to 10/10 , v2018: 6 + v2021: 11 (6 with waves).

Techniques: