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Heat --- Engineering --- Transmission --- Mathematical models. --- COMSOL Multiphysics. --- Numerical analysis --- Transmission. --- Mathematical analysis --- Heat transfer --- Thermal transfer --- Transmission of heat --- Energy transfer --- Heat-Transmission. --- Numerical analysis-Software.
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This open access textbook aims at providing detailed explanations on how to design and construct image analysis workflows to successfully conduct bioimage analysis. Addressing the main challenges in image data analysis, where acquisition by powerful imaging devices results in very large amounts of collected image data, the book discusses techniques relying on batch and GPU programming, as well as on powerful deep learning-based algorithms. In addition, downstream data processing techniques are introduced, such as Python libraries for data organization, plotting, and visualizations. Finally, by studying the way individual unique ideas are implemented in the workflows, readers are carefully guided through how the parameters driving biological systems are revealed by analyzing image data. These studies include segmentation of plant tissue epidermis, analysis of the spatial pattern of the eye development in fruit flies, and the analysis of collective cell migration dynamics. The presented content extends the Bioimage Data Analysis Workflows textbook (Miura, Sladoje, 2020), published in this same series, with new contributions and advanced material, while preserving the well-appreciated pedagogical approach adopted and promoted during the training schools for bioimage analysis organized within NEUBIAS – the Network of European Bioimage Analysts. This textbook is intended for advanced students in various fields of the life sciences and biomedicine, as well as staff scientists and faculty members who conduct regular quantitative analyses of microscopy images.
Cytology. --- Bioinformatics. --- Imaging systems in biology. --- Cell Biology. --- Computational and Systems Biology. --- Biological Imaging. --- Biological imaging systems --- Biology --- Bio-informatics --- Biological informatics --- Information science --- Computational biology --- Systems biology --- Cell biology --- Cellular biology --- Cells --- Data processing --- Analyzing Image Data in Biology --- Building a Bioimage Analysis Workflow --- Computational Analysis --- Chosing the Correct Components for Given Biological Questions --- Data Handling and Plotting --- Deep Learning --- Fast Computation --- GPU-Acceleration --- Handling Biological data --- Machine Learning --- Phyton --- Processing Language --- Understanding Bioimage Analysis Software --- Microscòpia electrònica
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Volcanoes release plumes of gas and ash to the atmosphere during episodes of passive and explosive behavior. These ejecta have important implications for the chemistry and composition of the troposphere and stratosphere, with the capacity to alter Earth's radiation budget and climate system over a range of temporal and spatial scales. Volcanogenic sulphur dioxide reacts to form sulphate aerosols, which increase global albedo, e.g., by reducing surface temperatures, in addition to perturbing the formation processes and optical properties of clouds. Released halogen species can also deplete stratospheric and tropospheric ozone. Volcanic degassing, furthermore, played a key role in the formation of Earth’s atmosphere, and volcanic plumes can affect air quality, pose hazards to aviation and human health, as well as damage ecosystems. The chemical compositions and emission rates of volcanic plumes are also monitored via a range of direct-sampling and remote-sensing instrumentation, in order to gain insights into subterranean processes, in the respect of the magmatic bodies these volatiles exsolve from. Given the significant role these gases play in driving volcanic activity, e.g., via pressurisation, the study of volcanic plumes is proving to be an increasingly fruitful means of improving our understanding of volcanic systems, potentially in concert with observations from geophysics and contributions from fluid dynamical modelling of conduit dynamics.
radioactive disequilibria 210Pb-210Bi-210Po --- volcanic geochemistry --- radiative transfer --- spherical-cap bubble --- plume --- satellite remote sensing --- portable photometry --- puffing --- Holuhraun --- interdisciplinary volcanology --- gas slug --- atmospheric remote sensing --- analysis software --- gases --- image processing --- remote sensing --- SEVIRI data --- oxygen and sulfur multi-isotopes --- nonlinear spectral unmixing --- UV cameras --- ultraviolet cameras --- cloud height --- atmospheric chemistry --- Python 2.7 --- degassing processes --- volcanic plumes --- fissure eruption --- radiative forcing --- basaltic volcanism --- volcanic plume top height --- O3 --- eruption start and duration --- Differential Absorption Lidar (DIAL) --- volcanic emissions --- volcanology --- volcanic CO2 flux --- volcanic aerosols --- 2011-2015 Etna lava fountains --- SO2 --- reactive halogen --- nonlinear PCA --- gas --- Etna volcano --- geochemical modelling --- BrO --- volcanic sulfate aerosols --- volcanic gases --- SSA --- hyperspectral remote sensing --- time averaged discharge rate --- eruption monitoring --- Bárðarbunga --- strombolian --- aerosol optical properties --- Mount Etna --- Taylor bubble --- radioactive disequilibria 210Pb-210Bi-210Po --- volcanic geochemistry --- radiative transfer --- spherical-cap bubble --- plume --- satellite remote sensing --- portable photometry --- puffing --- Holuhraun --- interdisciplinary volcanology --- gas slug --- atmospheric remote sensing --- analysis software --- gases --- image processing --- remote sensing --- SEVIRI data --- oxygen and sulfur multi-isotopes --- nonlinear spectral unmixing --- UV cameras --- ultraviolet cameras --- cloud height --- atmospheric chemistry --- Python 2.7 --- degassing processes --- volcanic plumes --- fissure eruption --- radiative forcing --- basaltic volcanism --- volcanic plume top height --- O3 --- eruption start and duration --- Differential Absorption Lidar (DIAL) --- volcanic emissions --- volcanology --- volcanic CO2 flux --- volcanic aerosols --- 2011-2015 Etna lava fountains --- SO2 --- reactive halogen --- nonlinear PCA --- gas --- Etna volcano --- geochemical modelling --- BrO --- volcanic sulfate aerosols --- volcanic gases --- SSA --- hyperspectral remote sensing --- time averaged discharge rate --- eruption monitoring --- Bárðarbunga --- strombolian --- aerosol optical properties --- Mount Etna --- Taylor bubble
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This volume comprises a carefully selected collection of articles emerging from and pertinent to the 2010 CFL-80 conference in Rio de Janeiro, celebrating the 80th anniversary of the Courant–Friedrichs–Lewy (CFL) condition. A major result in the field of numerical analysis, the CFL condition has influenced the research of many important mathematicians over the past eight decades, and this work is meant to take stock of its most important and current applications. The Courant–Friedrichs–Lewy (CFL) Condition: 80 Years After its Discovery will be of interest to practicing mathematicians, engineers, physicists, and graduate students who work with numerical methods. Contributors: U. Ascher B. Cockburn E. Deriaz M.O. Domingues S.M. Gomes R. Hersh R. Jeltsch D. Kolomenskiy H. Kumar L.C. Lax P. Lax P. LeFloch A. Marica O. Roussel K. Schneider J. Tiexeira Cal Neto C. Tomei K. van den Doel E. Zuazua .
Differential equations, Partial. --- Information theory. --- Mathematics. --- Numerical analysis -- Software. --- Numerical analysis --- Information theory --- Differential equations, Partial --- Computer science --- Engineering mathematics --- Mathematics --- Engineering & Applied Sciences --- Physical Sciences & Mathematics --- Applied Mathematics --- Mathematics - General --- Engineering --- Engineering analysis --- Informatics --- Partial differential equations --- Communication theory --- Computers. --- Partial differential equations. --- Applied mathematics. --- Engineering mathematics. --- Computer mathematics. --- Physics. --- Computational Mathematics and Numerical Analysis. --- Partial Differential Equations. --- Theory of Computation. --- Numerical and Computational Physics. --- Appl.Mathematics/Computational Methods of Engineering. --- Applications of Mathematics. --- Natural philosophy --- Philosophy, Natural --- Physical sciences --- Dynamics --- Computer mathematics --- Discrete mathematics --- Electronic data processing --- Mathematical analysis --- Automatic computers --- Automatic data processors --- Computer hardware --- Computing machines (Computers) --- Electronic brains --- Electronic calculating-machines --- Electronic computers --- Hardware, Computer --- Computer systems --- Cybernetics --- Machine theory --- Calculators --- Cyberspace --- Math --- Science --- Differential equations, partial. --- Numerical and Computational Physics, Simulation. --- Mathematical and Computational Engineering. --- Communication --- Courant, Richard, --- Lewy, Hans, --- Friedrichs, K. O. --- Friedrichs, Kurt Otto, --- Kurant, Rikhard, --- Courant, R.
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Volcanoes release plumes of gas and ash to the atmosphere during episodes of passive and explosive behavior. These ejecta have important implications for the chemistry and composition of the troposphere and stratosphere, with the capacity to alter Earth's radiation budget and climate system over a range of temporal and spatial scales. Volcanogenic sulphur dioxide reacts to form sulphate aerosols, which increase global albedo, e.g., by reducing surface temperatures, in addition to perturbing the formation processes and optical properties of clouds. Released halogen species can also deplete stratospheric and tropospheric ozone. Volcanic degassing, furthermore, played a key role in the formation of Earth’s atmosphere, and volcanic plumes can affect air quality, pose hazards to aviation and human health, as well as damage ecosystems. The chemical compositions and emission rates of volcanic plumes are also monitored via a range of direct-sampling and remote-sensing instrumentation, in order to gain insights into subterranean processes, in the respect of the magmatic bodies these volatiles exsolve from. Given the significant role these gases play in driving volcanic activity, e.g., via pressurisation, the study of volcanic plumes is proving to be an increasingly fruitful means of improving our understanding of volcanic systems, potentially in concert with observations from geophysics and contributions from fluid dynamical modelling of conduit dynamics.
n/a --- radioactive disequilibria 210Pb-210Bi-210Po --- volcanic geochemistry --- radiative transfer --- spherical-cap bubble --- plume --- satellite remote sensing --- portable photometry --- puffing --- Holuhraun --- interdisciplinary volcanology --- gas slug --- atmospheric remote sensing --- analysis software --- gases --- image processing --- remote sensing --- SEVIRI data --- oxygen and sulfur multi-isotopes --- nonlinear spectral unmixing --- UV cameras --- ultraviolet cameras --- cloud height --- atmospheric chemistry --- Python 2.7 --- degassing processes --- volcanic plumes --- fissure eruption --- radiative forcing --- basaltic volcanism --- volcanic plume top height --- O3 --- eruption start and duration --- Differential Absorption Lidar (DIAL) --- volcanic emissions --- volcanology --- volcanic CO2 flux --- volcanic aerosols --- 2011–2015 Etna lava fountains --- SO2 --- reactive halogen --- nonlinear PCA --- gas --- Etna volcano --- geochemical modelling --- BrO --- volcanic sulfate aerosols --- volcanic gases --- SSA --- hyperspectral remote sensing --- time averaged discharge rate --- eruption monitoring --- Bárðarbunga --- strombolian --- aerosol optical properties --- Mount Etna --- Taylor bubble --- 2011-2015 Etna lava fountains --- Bárðarbunga
Choose an application
Volcanoes release plumes of gas and ash to the atmosphere during episodes of passive and explosive behavior. These ejecta have important implications for the chemistry and composition of the troposphere and stratosphere, with the capacity to alter Earth's radiation budget and climate system over a range of temporal and spatial scales. Volcanogenic sulphur dioxide reacts to form sulphate aerosols, which increase global albedo, e.g., by reducing surface temperatures, in addition to perturbing the formation processes and optical properties of clouds. Released halogen species can also deplete stratospheric and tropospheric ozone. Volcanic degassing, furthermore, played a key role in the formation of Earth’s atmosphere, and volcanic plumes can affect air quality, pose hazards to aviation and human health, as well as damage ecosystems. The chemical compositions and emission rates of volcanic plumes are also monitored via a range of direct-sampling and remote-sensing instrumentation, in order to gain insights into subterranean processes, in the respect of the magmatic bodies these volatiles exsolve from. Given the significant role these gases play in driving volcanic activity, e.g., via pressurisation, the study of volcanic plumes is proving to be an increasingly fruitful means of improving our understanding of volcanic systems, potentially in concert with observations from geophysics and contributions from fluid dynamical modelling of conduit dynamics.
n/a --- radioactive disequilibria 210Pb-210Bi-210Po --- volcanic geochemistry --- radiative transfer --- spherical-cap bubble --- plume --- satellite remote sensing --- portable photometry --- puffing --- Holuhraun --- interdisciplinary volcanology --- gas slug --- atmospheric remote sensing --- analysis software --- gases --- image processing --- remote sensing --- SEVIRI data --- oxygen and sulfur multi-isotopes --- nonlinear spectral unmixing --- UV cameras --- ultraviolet cameras --- cloud height --- atmospheric chemistry --- Python 2.7 --- degassing processes --- volcanic plumes --- fissure eruption --- radiative forcing --- basaltic volcanism --- volcanic plume top height --- O3 --- eruption start and duration --- Differential Absorption Lidar (DIAL) --- volcanic emissions --- volcanology --- volcanic CO2 flux --- volcanic aerosols --- 2011–2015 Etna lava fountains --- SO2 --- reactive halogen --- nonlinear PCA --- gas --- Etna volcano --- geochemical modelling --- BrO --- volcanic sulfate aerosols --- volcanic gases --- SSA --- hyperspectral remote sensing --- time averaged discharge rate --- eruption monitoring --- Bárðarbunga --- strombolian --- aerosol optical properties --- Mount Etna --- Taylor bubble --- 2011-2015 Etna lava fountains --- Bárðarbunga
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