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Investigating Shock Wave—Boundary Layer Interaction Caused By
... detonation travels from the point of ignition to the tube end at the Chapman-Jouget (CJ) speed, UCJ, as derived in detonation textbooks (e.g., Lee, 2008). Trailing the detonation is the Taylor expansion that terminates on the characteristic moving at sound speed c3, the sound speed in the constant p ...
... detonation travels from the point of ignition to the tube end at the Chapman-Jouget (CJ) speed, UCJ, as derived in detonation textbooks (e.g., Lee, 2008). Trailing the detonation is the Taylor expansion that terminates on the characteristic moving at sound speed c3, the sound speed in the constant p ...
Variability of currents in front of the Venice Lagoon, Northern Adriatic
... From a physical point of view, the limited depth of the investigated area means that the Ekman boundary layers potentially interact, with a partial or total overlap. In other words, this implies that two opposing phenomena may occur, the direct transfer of momentum from surface to bottom, while the ...
... From a physical point of view, the limited depth of the investigated area means that the Ekman boundary layers potentially interact, with a partial or total overlap. In other words, this implies that two opposing phenomena may occur, the direct transfer of momentum from surface to bottom, while the ...
coherence property estimation for various ocean depths
... V.G.Sivakumar et.al / Indian Journal of Computer Science and Engineering (IJCSE) ...
... V.G.Sivakumar et.al / Indian Journal of Computer Science and Engineering (IJCSE) ...
A mission concept for simultaneous measurements of marine winds
... Addressing the user needs set out in the previous section, requires repeated measurements of ocean currents at temporal and spatial scales compatible with the remote sensing mission. The envisaged remote sensing component is a C-band dual polarimetric Doppler Scatterometer mission, named DopSCAT. Th ...
... Addressing the user needs set out in the previous section, requires repeated measurements of ocean currents at temporal and spatial scales compatible with the remote sensing mission. The envisaged remote sensing component is a C-band dual polarimetric Doppler Scatterometer mission, named DopSCAT. Th ...
Coastal Erosion Studies—A Review
... Fitzgerald 2010), which is a short time in terms of human occupation of the coast. This phenomenon has the tendency to expose a significant proportion of vulnerable coastal areas to flooding and destruction of habitats for migratory birds and other endangered species. Occurring in synchrony with the ...
... Fitzgerald 2010), which is a short time in terms of human occupation of the coast. This phenomenon has the tendency to expose a significant proportion of vulnerable coastal areas to flooding and destruction of habitats for migratory birds and other endangered species. Occurring in synchrony with the ...
Bathymetry: Assessing Methods - COLORS
... time and effort to cover relatively small portions of the sea bed. In general, acoustic methods can be used throughout all oceanic depths from shallow estuaries to the deepest trenches. However, ship time is costly even in deep water, and because of increasing time and effort to operate in shallow w ...
... time and effort to cover relatively small portions of the sea bed. In general, acoustic methods can be used throughout all oceanic depths from shallow estuaries to the deepest trenches. However, ship time is costly even in deep water, and because of increasing time and effort to operate in shallow w ...
Tsunami - Pacific Disaster Net
... washing away entire villages. The inundation can also cause severe coastal erosion and affect areas upstream from the coast since tsunami waves can travel up rivers and streams from the ocean. Wave speed/force. Tsunami waves travel at 36-54 km/h in shallow water, faster than most people can run. Thi ...
... washing away entire villages. The inundation can also cause severe coastal erosion and affect areas upstream from the coast since tsunami waves can travel up rivers and streams from the ocean. Wave speed/force. Tsunami waves travel at 36-54 km/h in shallow water, faster than most people can run. Thi ...
Coupled Marine Boundary Layers and Air-Sea Interaction Initiative:
... these forecasts are also used to provide much needed information about the visibility of the fleet and their ability to peer through the atmosphere and ocean. Increasingly, these forecasts are required to provide ever more detailed information without losing their generality, i.e., they must be appl ...
... these forecasts are also used to provide much needed information about the visibility of the fleet and their ability to peer through the atmosphere and ocean. Increasingly, these forecasts are required to provide ever more detailed information without losing their generality, i.e., they must be appl ...
AMSR-E Ocean Algorithms - Remote Sensing Systems
... method of retrieval algorithms. The retrievals are done by a set of two-stage regression algorithms. The first-first stage is a set of regressions trained with global data. The first-stage retrievals provide reasonably good estimates of SST, wind, vapor, and cloud. However, because of the non-linear ...
... method of retrieval algorithms. The retrievals are done by a set of two-stage regression algorithms. The first-first stage is a set of regressions trained with global data. The first-stage retrievals provide reasonably good estimates of SST, wind, vapor, and cloud. However, because of the non-linear ...
Seismic Anisotropy: Tracing Plate Dynamics in the Mantle
... Media with hexagonal symmetry can be described by three anisotropic parameters (18), but only two find common usage in global seismology, one each for VP and VS anisotropy. The symmetry axis can be fast, as for strained olivine-rich rock (6), or slow, as for anisotropy induced by cracks and/or finel ...
... Media with hexagonal symmetry can be described by three anisotropic parameters (18), but only two find common usage in global seismology, one each for VP and VS anisotropy. The symmetry axis can be fast, as for strained olivine-rich rock (6), or slow, as for anisotropy induced by cracks and/or finel ...
Volcanoes and Earthquakes
... b. molten rock blowing into the air c. calm lava flows d. violent explosions 10. Lava with a high viscosity a. is runny, almost like water. c. smells like sulphur. b. is thick, like pudding. d. dries smooth and glassy. 11. A large depression that forms when the magma chamber partially empties is a a ...
... b. molten rock blowing into the air c. calm lava flows d. violent explosions 10. Lava with a high viscosity a. is runny, almost like water. c. smells like sulphur. b. is thick, like pudding. d. dries smooth and glassy. 11. A large depression that forms when the magma chamber partially empties is a a ...
Design of a Piezoelectric Energy Harvesting Syste+
... Waves form in water when it is excited by external forces, such as wind, vibrations, displacement, etc. The primary reason why ocean waves are a good choice for energy extraction is that an ocean wave is an efficient carrier of energy. “The global power potential represented by waves that hit all co ...
... Waves form in water when it is excited by external forces, such as wind, vibrations, displacement, etc. The primary reason why ocean waves are a good choice for energy extraction is that an ocean wave is an efficient carrier of energy. “The global power potential represented by waves that hit all co ...
Exchange processes between the Gulf of Finland and
... Especially, WAM was not able to reproduce the observed fetch-limited. The energy of the longer waves is clearly overestimated by WAM (Fig. 1). This behaviour might be caused by two reasons. The shape of the wind input source term might be too broad, in which case it would feed too much energy to the ...
... Especially, WAM was not able to reproduce the observed fetch-limited. The energy of the longer waves is clearly overestimated by WAM (Fig. 1). This behaviour might be caused by two reasons. The shape of the wind input source term might be too broad, in which case it would feed too much energy to the ...
Secondary wave lift degradation
... the fluid tests in Ref 7 (20 different tests) open up some new aspects. The behavior of all fluid tests followed evidently a clear pattern as seen in Fig 6. The initial lift loss mean value of 6 % decreases down to 4 % within 10 first seconds after the rotation. The next 1.5 percentage point decreas ...
... the fluid tests in Ref 7 (20 different tests) open up some new aspects. The behavior of all fluid tests followed evidently a clear pattern as seen in Fig 6. The initial lift loss mean value of 6 % decreases down to 4 % within 10 first seconds after the rotation. The next 1.5 percentage point decreas ...
Chapter 16: The Marine Environment
... Waves move faster in deep water than in shallow water. This difference in wave speed causes initially straight wave crests to bend when part of the crest moves into shallow water, a process known as wave refraction, illustrated in Figure 16-1. Along an irregular coast with headlands and bays, the wa ...
... Waves move faster in deep water than in shallow water. This difference in wave speed causes initially straight wave crests to bend when part of the crest moves into shallow water, a process known as wave refraction, illustrated in Figure 16-1. Along an irregular coast with headlands and bays, the wa ...
Earthquakes
... Origin of Seismic Waves You learned earlier that rocks move past each other along faults, creating stress at points where the rocks’ irregular surfaces catch each other. The stress continues to build up until the elastic limit is exceeded and energy is released in the form of seismic waves. The poin ...
... Origin of Seismic Waves You learned earlier that rocks move past each other along faults, creating stress at points where the rocks’ irregular surfaces catch each other. The stress continues to build up until the elastic limit is exceeded and energy is released in the form of seismic waves. The poin ...
The Marine Environment
... Large breaking waves can hurl thousands of metric tons of water, along with suspended rock fragments, against a shore with such force that they are capable of eroding solid rock. Erosional features Waves move faster in deep water than in shallow water. This difference in wave speed causes initially ...
... Large breaking waves can hurl thousands of metric tons of water, along with suspended rock fragments, against a shore with such force that they are capable of eroding solid rock. Erosional features Waves move faster in deep water than in shallow water. This difference in wave speed causes initially ...
Oceanic lithosphereasthenosphere boundary from surface wave
... maximum in the asthenosphere, while the elastic lithosphere jointly moves with the plate. As a part of the adiabatic convecting mantle, the LAB within the upper thermal boundary layer can be considered as the limit between a conductive lithosphere and a convective asthenosphere. The LAB is classical ...
... maximum in the asthenosphere, while the elastic lithosphere jointly moves with the plate. As a part of the adiabatic convecting mantle, the LAB within the upper thermal boundary layer can be considered as the limit between a conductive lithosphere and a convective asthenosphere. The LAB is classical ...
Using Animations to Enhance Understanding of - ASEE
... Yarden and Yarden [11] offer a comprehensive review (containing fifty-eight citations) and assessment of the cognitive literature related to animation effectiveness. Even though they specifically address issues related to animations in biotechnology, the suggestions they make and the conclusions the ...
... Yarden and Yarden [11] offer a comprehensive review (containing fifty-eight citations) and assessment of the cognitive literature related to animation effectiveness. Even though they specifically address issues related to animations in biotechnology, the suggestions they make and the conclusions the ...
Oceanic lithosphere-asthenosphere boundary from - HAL
... maximum in the asthenosphere, while the elastic lithosphere jointly moves with the plate. As a part of the adiabatic convecting mantle, the LAB within the upper thermal boundary layer can be considered as the limit between a conductive lithosphere and a convective asthenosphere. The LAB is classical ...
... maximum in the asthenosphere, while the elastic lithosphere jointly moves with the plate. As a part of the adiabatic convecting mantle, the LAB within the upper thermal boundary layer can be considered as the limit between a conductive lithosphere and a convective asthenosphere. The LAB is classical ...
16 - Glencoe
... Large breaking waves can hurl thousands of metric tons of water, along with suspended rock fragments, against a shore with such force that they are capable of eroding solid rock. Erosional features Waves move faster in deep water than in shallow water. This difference in wave speed causes initially ...
... Large breaking waves can hurl thousands of metric tons of water, along with suspended rock fragments, against a shore with such force that they are capable of eroding solid rock. Erosional features Waves move faster in deep water than in shallow water. This difference in wave speed causes initially ...
Development of an operational coastal flooding early warning system
... and Fordham, 1996; Wang and Du, 2003; Plessis, 2002; Kaya et al., 2005; Basha and Rus, 2007). For coastal areas, substantial efforts have been invested into the different management systems (Solomon and Forbes, 1999; Doornkamp, 1998; Thumerer et al., 2000). In the aftermath of the 2004 Indian Ocean ...
... and Fordham, 1996; Wang and Du, 2003; Plessis, 2002; Kaya et al., 2005; Basha and Rus, 2007). For coastal areas, substantial efforts have been invested into the different management systems (Solomon and Forbes, 1999; Doornkamp, 1998; Thumerer et al., 2000). In the aftermath of the 2004 Indian Ocean ...
Tank Testing of Wave Energy Conversion Systems
... empirical equation defining the one dimensional spectral shape of the distribution of variance over a frequency range, based on the assumption that the input wind is in equilibrium with the waves, also known as fully developed f 4 5 p α g2 1 S( f )PM = exp − ...
... empirical equation defining the one dimensional spectral shape of the distribution of variance over a frequency range, based on the assumption that the input wind is in equilibrium with the waves, also known as fully developed f 4 5 p α g2 1 S( f )PM = exp − ...
Earthquakes
... Folding Earth’s Crust • Anticline – upward fold in rock formed by compression of Earth’s crust. • Syncline – downward fold in rock formed by compression in Earth’s crust. • Folding produced some of the world’s largest mountain ...
... Folding Earth’s Crust • Anticline – upward fold in rock formed by compression of Earth’s crust. • Syncline – downward fold in rock formed by compression in Earth’s crust. • Folding produced some of the world’s largest mountain ...
Earthquakes
... Folding Earth’s Crust • Anticline – upward fold in rock formed by compression of Earth’s crust. • Syncline – downward fold in rock formed by compression in Earth’s crust. • Folding produced some of the world’s largest mountain ...
... Folding Earth’s Crust • Anticline – upward fold in rock formed by compression of Earth’s crust. • Syncline – downward fold in rock formed by compression in Earth’s crust. • Folding produced some of the world’s largest mountain ...
Wind wave
![](https://commons.wikimedia.org/wiki/Special:FilePath/Wedge_Newport_Hurricane_Marie_photo_D_Ramey_Logan.jpg?width=300)
In fluid dynamics, wind waves, or wind-generated waves, are surface waves that occur on the free surface of oceans, seas, lakes, rivers, and canals or even on small puddles and ponds. They result from the wind blowing over an area of fluid surface. Waves in the oceans can travel thousands of miles before reaching land. Wind waves range in size from small ripples, to waves over 100 ft (30 m) high.When directly generated and affected by local winds, a wind wave system is called a wind sea. After the wind ceases to blow, wind waves are called swells. More generally, a swell consists of wind-generated waves that are not significantly affected by the local wind at that time. They have been generated elsewhere or some time ago. Wind waves in the ocean are called ocean surface waves.Wind waves have a certain amount of randomness: subsequent waves differ in height, duration, and shape with limited predictability. They can be described as a stochastic process, in combination with the physics governing their generation, growth, propagation and decay—as well as governing the interdependence between flow quantities such as: the water surface movements, flow velocities and water pressure. The key statistics of wind waves (both seas and swells) in evolving sea states can be predicted with wind wave models.Although waves are usually considered in the water seas of Earth, the hydrocarbon seas of Titan may also have wind-driven waves.