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Atmospheric turbulence. --- Large eddy simulation. --- Time dependence. --- Three dimensional models. --- Mesoscale phenomena. --- Civil aviation.
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Doppler radar. --- Mesoscale phenomena. --- Prediction analysis techniques. --- Weather forecasting. --- Wind (meteorology)
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Mountainous regions occupy a significant fraction of the Earth’s continents and are characterized by specific meteorological phenomena operating on a wide range of scales. Being a home to large human populations, the impact of mountains on weather and hydrology has significant practical consequences. Mountains modulate the climate and create micro-climates, induce different types of thermally and dynamically driven circulations, generate atmospheric waves of various scales (known as mountain waves), and affect the boundary layer characteristics and the dispersion of pollutants. At the local scale, strong downslope winds linked with mountain waves (such as the Foehn and Bora) can cause severe damage. Mountain wave breaking in the high atmosphere is a source of Clear Air Turbulence, and lee wave rotors are a major near-surface aviation hazard. Mountains also act to block strongly-stratified air layers, leading to the formation of valley cold-air pools (with implications for road safety, pollution, crop damage, etc.) and gap flows. Presently, neither the fine-scale structure of orographic precipitation nor the initiation of deep convection by mountainous terrain can be resolved adequately by regional-to global-scale models, requiring appropriate downscaling or parameterization. Additionally, the shortest mountain waves need to be parameterized in global weather and climate prediction models, because they exert a drag on the atmosphere. This drag not only decelerates the global atmospheric circulation, but also affects temperatures in the polar stratosphere, which control ozone depletion. It is likely that both mountain wave drag and orographic precipitation lead to non-trivial feedbacks in climate change scenarios. Measurement campaigns such as MAP, T-REX, Materhorn, COLPEX and i-Box provided a wealth of mountain meteorology field data, which is only starting to be explored. Recent advances in computing power allow numerical simulations of unprecedented resolution, e.g. LES modelling of rotors, mountain wave turbulence, and boundary layers in mountainous regions. This will lead to important advances in understanding these phenomena, as well as mixing and pollutant dispersion over complex terrain, or the onset and breakdown of cold-air pools. On the other hand, recent analyses of global circulation biases point towards missing drag, especially in the southern hemisphere, which may be due to processes currently neglected in parameterizations. A better understanding of flow over orography is also crucial for a better management of wind power and a more effective use of data assimilation over complex terrain. This Research Topic includes contributions that aim to shed light on a number of these issues, using theory, numerical modelling, field measurements, and laboratory experiments.
Turbulent fluxes --- Downslope winds --- Large eddy simulation --- Sub-mesoscale circulations --- orographic precipitation --- Thermally-driven flows --- Horizontal inhomogeneity --- Cold air pools --- Hydraulic jumps --- mountain waves
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Mountainous regions occupy a significant fraction of the Earth’s continents and are characterized by specific meteorological phenomena operating on a wide range of scales. Being a home to large human populations, the impact of mountains on weather and hydrology has significant practical consequences. Mountains modulate the climate and create micro-climates, induce different types of thermally and dynamically driven circulations, generate atmospheric waves of various scales (known as mountain waves), and affect the boundary layer characteristics and the dispersion of pollutants. At the local scale, strong downslope winds linked with mountain waves (such as the Foehn and Bora) can cause severe damage. Mountain wave breaking in the high atmosphere is a source of Clear Air Turbulence, and lee wave rotors are a major near-surface aviation hazard. Mountains also act to block strongly-stratified air layers, leading to the formation of valley cold-air pools (with implications for road safety, pollution, crop damage, etc.) and gap flows. Presently, neither the fine-scale structure of orographic precipitation nor the initiation of deep convection by mountainous terrain can be resolved adequately by regional-to global-scale models, requiring appropriate downscaling or parameterization. Additionally, the shortest mountain waves need to be parameterized in global weather and climate prediction models, because they exert a drag on the atmosphere. This drag not only decelerates the global atmospheric circulation, but also affects temperatures in the polar stratosphere, which control ozone depletion. It is likely that both mountain wave drag and orographic precipitation lead to non-trivial feedbacks in climate change scenarios. Measurement campaigns such as MAP, T-REX, Materhorn, COLPEX and i-Box provided a wealth of mountain meteorology field data, which is only starting to be explored. Recent advances in computing power allow numerical simulations of unprecedented resolution, e.g. LES modelling of rotors, mountain wave turbulence, and boundary layers in mountainous regions. This will lead to important advances in understanding these phenomena, as well as mixing and pollutant dispersion over complex terrain, or the onset and breakdown of cold-air pools. On the other hand, recent analyses of global circulation biases point towards missing drag, especially in the southern hemisphere, which may be due to processes currently neglected in parameterizations. A better understanding of flow over orography is also crucial for a better management of wind power and a more effective use of data assimilation over complex terrain. This Research Topic includes contributions that aim to shed light on a number of these issues, using theory, numerical modelling, field measurements, and laboratory experiments.
Turbulent fluxes --- Downslope winds --- Large eddy simulation --- Sub-mesoscale circulations --- orographic precipitation --- Thermally-driven flows --- Horizontal inhomogeneity --- Cold air pools --- Hydraulic jumps --- mountain waves
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Classifications. --- Data systems. --- Wind velocity. --- Wind shear. --- Wind direction. --- Temperature inversions. --- Static stability. --- Probability theory. --- Meteorological parameters. --- Mesoscale phenomena. --- Interpolation. --- Forecasting.
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Mountainous regions occupy a significant fraction of the Earth’s continents and are characterized by specific meteorological phenomena operating on a wide range of scales. Being a home to large human populations, the impact of mountains on weather and hydrology has significant practical consequences. Mountains modulate the climate and create micro-climates, induce different types of thermally and dynamically driven circulations, generate atmospheric waves of various scales (known as mountain waves), and affect the boundary layer characteristics and the dispersion of pollutants. At the local scale, strong downslope winds linked with mountain waves (such as the Foehn and Bora) can cause severe damage. Mountain wave breaking in the high atmosphere is a source of Clear Air Turbulence, and lee wave rotors are a major near-surface aviation hazard. Mountains also act to block strongly-stratified air layers, leading to the formation of valley cold-air pools (with implications for road safety, pollution, crop damage, etc.) and gap flows. Presently, neither the fine-scale structure of orographic precipitation nor the initiation of deep convection by mountainous terrain can be resolved adequately by regional-to global-scale models, requiring appropriate downscaling or parameterization. Additionally, the shortest mountain waves need to be parameterized in global weather and climate prediction models, because they exert a drag on the atmosphere. This drag not only decelerates the global atmospheric circulation, but also affects temperatures in the polar stratosphere, which control ozone depletion. It is likely that both mountain wave drag and orographic precipitation lead to non-trivial feedbacks in climate change scenarios. Measurement campaigns such as MAP, T-REX, Materhorn, COLPEX and i-Box provided a wealth of mountain meteorology field data, which is only starting to be explored. Recent advances in computing power allow numerical simulations of unprecedented resolution, e.g. LES modelling of rotors, mountain wave turbulence, and boundary layers in mountainous regions. This will lead to important advances in understanding these phenomena, as well as mixing and pollutant dispersion over complex terrain, or the onset and breakdown of cold-air pools. On the other hand, recent analyses of global circulation biases point towards missing drag, especially in the southern hemisphere, which may be due to processes currently neglected in parameterizations. A better understanding of flow over orography is also crucial for a better management of wind power and a more effective use of data assimilation over complex terrain. This Research Topic includes contributions that aim to shed light on a number of these issues, using theory, numerical modelling, field measurements, and laboratory experiments.
Turbulent fluxes --- Downslope winds --- Large eddy simulation --- Sub-mesoscale circulations --- orographic precipitation --- Thermally-driven flows --- Horizontal inhomogeneity --- Cold air pools --- Hydraulic jumps --- mountain waves --- Turbulent fluxes --- Downslope winds --- Large eddy simulation --- Sub-mesoscale circulations --- orographic precipitation --- Thermally-driven flows --- Horizontal inhomogeneity --- Cold air pools --- Hydraulic jumps --- mountain waves
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This thematic issue presents 11 scientific articles that are extremely useful for understanding the processes and phenomena of the interacting geospheres of the Earth. These processes have an important impact on the biosphere and many human activities. The results of scientific research presented in this book are fully united by the common theme "investigation of the fundamental foundations of the emergence, development, transformation, and interaction of hydroacoustic, hydrophysical and geophysical fields in the World Ocean." The book is recommended to a wide range of readers, as well as to specialists in the field of hydroacoustics, oceanology, and geophysics.
gravitational waves --- pressure variations --- period variation --- laser meter of hydrosphere pressure variations --- infragravity waves --- gravity wind waves --- laser strainmeter --- typhoon --- mesoscale eddy --- parabolic equation --- normal mode --- mesoscale vortex --- acoustic propagation --- AIPOcean --- OW method --- COMSOL software --- sea surface --- wave spectra --- satellite imagery processing --- aerospace monitoring --- sea waves --- retrieving operator --- Scholte wave --- theoretical dispersion curve --- stiffness matrices --- layered media --- wind waves --- progressive waves --- standing waves --- primary microseisms --- secondary microseisms --- wave dynamics --- wave transformation --- swell --- tides --- seiches --- remote probing --- space monitoring --- nonlinearity --- modulation --- oceanic front --- ray theory --- horizontal refraction --- coastal video monitoring --- streaming video --- image and video processing --- real-time mode --- subpixel resolution --- underwater currents --- microseisms --- coastal water areas --- red tide --- harmful algal bloom --- sea surface height --- sea surface temperature --- chlorophyll-a --- biogenic slicks --- river runoff --- Kamchatka --- earthquake --- tsunami --- deformation jump --- sine-Gordon equation --- kink --- anti-kink --- underwater landslide --- n/a
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The development of porous materials has attracted the attention of the research community for years. Porosity characteristics have specific impacts on the material properties and materials that are applied in many areas, such as pollutant removal, CO2 capture, energy storage, catalytic oxidation and reduction processes, the conversion of biomass to biofuels, and drug delivery. Examples of porous materials are activated carbons, clays, and zeolites. The aim of this book is to collect the recent advances and progress regarding porous materials and their applications in the environmental area.
spherical seeds --- spherical activated carbons --- activation --- microporosity --- mechanical properties --- diatomite --- zeolite X --- hydrothermal method --- calcium ion exchange capacity --- clay minerals particles --- orientational anisotropy --- granular systems --- disk packing --- X-Ray microtomography --- mesoscale simulation --- water produced --- adsorbent materials --- composite --- AlFe-pillared clay --- CrCeOx --- chlorobenzene --- catalytic combustion --- temperature-programmed reaction --- lignite --- porous structure --- carbon dioxide --- pressure --- CuCl/AC adsorbent --- CO adsorption --- monolayer dispersion --- isosteric heat --- adsorption isotherms --- Fischer–Tropsch --- supported iron oxide --- supported cobalt oxide --- reducibility --- dispersion --- biosorption --- weed --- methylene blue dye --- natural biosorbents --- adsorption kinetics
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This thematic issue presents 11 scientific articles that are extremely useful for understanding the processes and phenomena of the interacting geospheres of the Earth. These processes have an important impact on the biosphere and many human activities. The results of scientific research presented in this book are fully united by the common theme "investigation of the fundamental foundations of the emergence, development, transformation, and interaction of hydroacoustic, hydrophysical and geophysical fields in the World Ocean." The book is recommended to a wide range of readers, as well as to specialists in the field of hydroacoustics, oceanology, and geophysics.
Technology: general issues --- History of engineering & technology --- gravitational waves --- pressure variations --- period variation --- laser meter of hydrosphere pressure variations --- infragravity waves --- gravity wind waves --- laser strainmeter --- typhoon --- mesoscale eddy --- parabolic equation --- normal mode --- mesoscale vortex --- acoustic propagation --- AIPOcean --- OW method --- COMSOL software --- sea surface --- wave spectra --- satellite imagery processing --- aerospace monitoring --- sea waves --- retrieving operator --- Scholte wave --- theoretical dispersion curve --- stiffness matrices --- layered media --- wind waves --- progressive waves --- standing waves --- primary microseisms --- secondary microseisms --- wave dynamics --- wave transformation --- swell --- tides --- seiches --- remote probing --- space monitoring --- nonlinearity --- modulation --- oceanic front --- ray theory --- horizontal refraction --- coastal video monitoring --- streaming video --- image and video processing --- real-time mode --- subpixel resolution --- underwater currents --- microseisms --- coastal water areas --- red tide --- harmful algal bloom --- sea surface height --- sea surface temperature --- chlorophyll-a --- biogenic slicks --- river runoff --- Kamchatka --- earthquake --- tsunami --- deformation jump --- sine-Gordon equation --- kink --- anti-kink --- underwater landslide --- gravitational waves --- pressure variations --- period variation --- laser meter of hydrosphere pressure variations --- infragravity waves --- gravity wind waves --- laser strainmeter --- typhoon --- mesoscale eddy --- parabolic equation --- normal mode --- mesoscale vortex --- acoustic propagation --- AIPOcean --- OW method --- COMSOL software --- sea surface --- wave spectra --- satellite imagery processing --- aerospace monitoring --- sea waves --- retrieving operator --- Scholte wave --- theoretical dispersion curve --- stiffness matrices --- layered media --- wind waves --- progressive waves --- standing waves --- primary microseisms --- secondary microseisms --- wave dynamics --- wave transformation --- swell --- tides --- seiches --- remote probing --- space monitoring --- nonlinearity --- modulation --- oceanic front --- ray theory --- horizontal refraction --- coastal video monitoring --- streaming video --- image and video processing --- real-time mode --- subpixel resolution --- underwater currents --- microseisms --- coastal water areas --- red tide --- harmful algal bloom --- sea surface height --- sea surface temperature --- chlorophyll-a --- biogenic slicks --- river runoff --- Kamchatka --- earthquake --- tsunami --- deformation jump --- sine-Gordon equation --- kink --- anti-kink --- underwater landslide
Choose an application
The development of porous materials has attracted the attention of the research community for years. Porosity characteristics have specific impacts on the material properties and materials that are applied in many areas, such as pollutant removal, CO2 capture, energy storage, catalytic oxidation and reduction processes, the conversion of biomass to biofuels, and drug delivery. Examples of porous materials are activated carbons, clays, and zeolites. The aim of this book is to collect the recent advances and progress regarding porous materials and their applications in the environmental area.
Technology: general issues --- spherical seeds --- spherical activated carbons --- activation --- microporosity --- mechanical properties --- diatomite --- zeolite X --- hydrothermal method --- calcium ion exchange capacity --- clay minerals particles --- orientational anisotropy --- granular systems --- disk packing --- X-Ray microtomography --- mesoscale simulation --- water produced --- adsorbent materials --- composite --- AlFe-pillared clay --- CrCeOx --- chlorobenzene --- catalytic combustion --- temperature-programmed reaction --- lignite --- porous structure --- carbon dioxide --- pressure --- CuCl/AC adsorbent --- CO adsorption --- monolayer dispersion --- isosteric heat --- adsorption isotherms --- Fischer–Tropsch --- supported iron oxide --- supported cobalt oxide --- reducibility --- dispersion --- biosorption --- weed --- methylene blue dye --- natural biosorbents --- adsorption kinetics