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Waves and wind

Reduction of Wind and Swell Waves by Mangroves

Reduction of Wind and Swell Waves by Mangroves

... reducing wind and swell ...larger waves during storms, hurricanes and periods of high winds. Large wind and swell waves can cause flooding and damage to coastal ...

27

ANGEO - WIND observations of coherent electrostatic waves in the solar wind

ANGEO - WIND observations of coherent electrostatic waves in the solar wind

... decrease of the electrostatic energy with increasing solar wind velocity mentioned in Sect. 6.1. One would have expected that the temperature ratio T p =T e , which is related to the damping of ion acoustic ...

14

On the influence of wind and waves on underwater irradiance fluctuations

On the influence of wind and waves on underwater irradiance fluctuations

... of waves in this order of magnitude, vis- ible as clear stripes of E d ...Local wind deter- mines the steepness of these waves, affecting the depth of the (first) focal point, ...more wind, ...

17

On the excitation of ULF waves by solar wind pressure enhancements

On the excitation of ULF waves by solar wind pressure enhancements

... solar wind dynamic ...travelling waves and then suddenly change into standing ...solar wind pressure excites eigenmodes of the geomagnetic cav- ity/waveguide that propagate tailward and that these ...

12

Solar wind Alfv´en waves: a source of pulsed ionospheric convection and atmospheric gravity waves

Solar wind Alfv´en waves: a source of pulsed ionospheric convection and atmospheric gravity waves

... solar wind MHD waves can directly drive magnetospheric ...gravity waves, which then cause ...solar wind Alfv´en waves points to very direct coupling of energy in the solar wind ...

17

Magnetosheath waves under very low solar wind dynamic pressure: Wind/Geotail observations

Magnetosheath waves under very low solar wind dynamic pressure: Wind/Geotail observations

... ion waves in the magnetosheath to the low dynamic pressure ...solar wind dynamic pressure is that the resulting Alfven (and magnetosonic) Mach number weakened the bow ...solar wind, which was ...

17

Numerical Investigation of Spectral Evolution of Wind Waves. Part I: Wind-Input Source Function

Numerical Investigation of Spectral Evolution of Wind Waves. Part I: Wind-Input Source Function

... the waves; and S tot represents all energy fluxes contrib- uting to wind-wave ...that wind-wave growth is a result of three physical processes: atmospheric input from the wind to the ...

11

On the feasibility of the use of wind SAR to downscale waves on shallow water

On the feasibility of the use of wind SAR to downscale waves on shallow water

... and wind reanalysis as ...dominant wind regimes in the area: the bora (ENE direction) and sirocco (SE ...the waves forced with reanalysis wind and SAR ...SAR wind fields, can be ...

11

Ultrafast Kelvin waves in the MLT airglow and wind, and their interaction with the atmospheric tides

Ultrafast Kelvin waves in the MLT airglow and wind, and their interaction with the atmospheric tides

... meridional wind components are ...meridional wind were identified by means of the Morlet wavelet transform (Torrence and Compo, 1998), which also works as a band-pass ...planetary waves periodicities ...

11

Bed Drag Coefficient Variability under Wind Waves in a Tidal Estuary

Bed Drag Coefficient Variability under Wind Waves in a Tidal Estuary

... steady wind-sheared surface boundary layer with the steady bottom boundary layer 共driven by both wind and ...strong waves were accompanied by strong winds. During wind events, instruments high ...

12

Fast magnetoacoustic waves in non equilibrium solar wind and coronal plasmas

Fast magnetoacoustic waves in non equilibrium solar wind and coronal plasmas

... ULF waves as observed in other ...solar wind anisotropy using quasilinear plasma the- ...handed waves while the plasma was in proximity to the firehose marginal stability threshold on the (β k , T k ...

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PROFILES  OF  WIND-CREATED  WATER  WAVES  IN  THE  CAPILLARY-GRAVITY  TRANSITION  REGION

PROFILES OF WIND-CREATED WATER WAVES IN THE CAPILLARY-GRAVITY TRANSITION REGION

... (d) The wavelength of wind generated waves that first form is in the- 1 to 2 cm region corresponding to the minimum velocity in the gravity- capillary transition region. (e) As the [r] ...

10

Modeling of Wind Waves in the Bays of South-West Part of the Crimea Peninsula

Modeling of Wind Waves in the Bays of South-West Part of the Crimea Peninsula

... of wind waves in the Sevastopol ...extreme waves in the bay during devastating storm on 11 November 2007 were ...south-east wind increased to 10-15 m/s and by 9 ...south-west. Wind ...

7

Implementation and validation of a coastal forecasting system for wind waves in the Mediterranean Sea

Implementation and validation of a coastal forecasting system for wind waves in the Mediterranean Sea

... provide wind wave forecasts over the whole Mediterranean Sea area, and with the added capability to focus on selected coastal ...of waves towards the ...of waves; and the Simulating WAves ...

10

WAVES BRAND STRATEGY & IDENTITY. The answer my friend, is blowing in the wind, the answer is blowing in the wind. Bob Dylan

WAVES BRAND STRATEGY & IDENTITY. The answer my friend, is blowing in the wind, the answer is blowing in the wind. Bob Dylan

... the wind blows hard enough, and for long enough, a ‘sea’ ...the waves travel further from their origin they organise themselves into defi ned lines of ...

7

Velocity-space diffusion of solar wind protons in oblique waves and weak turbulence

Velocity-space diffusion of solar wind protons in oblique waves and weak turbulence

... Alfv´en/ion-cyclotron waves below and fast magneto-acoustic waves around the proton cyclotron ...non-dispersive waves, we may con- clude that the wave-scattering of the protons is partly inelas- tic ...

11

The response of waves to an opposing wind

The response of waves to an opposing wind

... 8.9 Phase angle between u and n as a function of U00Ie 247 wave following probe • 8.10 - Phase angle between w and n as a function of U00Ie 247 wave following probe • 8.11 ampu as a func[r] ...

21

The response of waves to an opposing wind

The response of waves to an opposing wind

... Garrett and Smith 34 conclude that the rate of energy transfer to the long waves is given by cos~ = where a~, k~ and C~ 2.57 are the long wave amplitude, wave number and phase speed, res[r] ...

116

The response of waves to an opposing wind

The response of waves to an opposing wind

... A variance expression for spectral density estimates is most conveniently obtained by direct Fourier transform operations, where the autospectral density function of a stationary ergodic[r] ...

48

The response of waves to an opposing wind

The response of waves to an opposing wind

... " Pressure transducer calibration ,~ Frequency response of tubing W Effect of wave follower oscillations ,, Low pass filters " Amplifiers " AID converters ,~ PDP-ll V Figure E.l Schemati[r] ...

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