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piv software pivlab  (MathWorks Inc)


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    MathWorks Inc piv software pivlab
    Piv Software Pivlab, 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/result/piv software pivlab/product/MathWorks Inc
    Average 90 stars, based on 1 article reviews
    piv software pivlab - by Bioz Stars, 2026-03
    90/100 stars

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    Flow <t>PIV</t> fluid <t>measurement</t> <t>software</t> tracking the movement of the ISP ( yellow dot square ) during internal rotation. The muscle belly of the ISP is indicated by the yellow square. The direction of the arrows (green and orange) inside the region of interest ( blue dot square ) indicates the direction in which the particle moves. PIV , particle image velocimetry; ISP , infraspinatus.
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    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    MathWorks Inc piv software pivlab for
    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    Image Search Results


    Flow PIV fluid measurement software tracking the movement of the ISP ( yellow dot square ) during internal rotation. The muscle belly of the ISP is indicated by the yellow square. The direction of the arrows (green and orange) inside the region of interest ( blue dot square ) indicates the direction in which the particle moves. PIV , particle image velocimetry; ISP , infraspinatus.

    Journal: JSES International

    Article Title: Investigation of the limiting factors of shoulder joint complex motion in college baseball players: motion analysis of the humeral head and rotator cuff using ultrasound

    doi: 10.1016/j.jseint.2023.12.012

    Figure Lengend Snippet: Flow PIV fluid measurement software tracking the movement of the ISP ( yellow dot square ) during internal rotation. The muscle belly of the ISP is indicated by the yellow square. The direction of the arrows (green and orange) inside the region of interest ( blue dot square ) indicates the direction in which the particle moves. PIV , particle image velocimetry; ISP , infraspinatus.

    Article Snippet: We then used PIV fluid measurement software (PIVlab, Version 2.36, an add-in software from MATLAB 2021, MathWorks, Natick, MA, USA) to analyze the velocity of ISP motion., To facilitate analysis, we divided all the ultrasound movies into 30 static images per second.

    Techniques: Software

    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).

    Journal: Scientific Reports

    Article Title: Anatomy of the Bezymianny volcano merely before an explosive eruption on 20.12.2017

    doi: 10.1038/s41598-021-81498-9

    Figure Lengend Snippet: TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).

    Article Snippet: Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python.

    Techniques: Generated, Software