Results 21 to 30 of about 44,233 (308)

Internal Gravity Waves [PDF]

open access: yes, 2019
The ocean's interior is filled with waves that can only exist because the ocean is vertically stratified in temperature and salinity. Like waves at the ocean surface, internal waves are restored by gravity. These internal gravity waves are generated by wind, tides, and low-frequency flows.
Buijsman, Maarten C.   +3 more
openaire   +2 more sources

Statistics of surface gravity wave turbulence in the space and time domains [PDF]

open access: yes, 2010
We present experimental results on simultaneous space–time measurements for the gravity wave turbulence in a large laboratory flume. We compare these results with predictions of the weak turbulence theory (WTT) based on random waves, as well as with ...
Nazarenko, Sergey   +3 more
core   +1 more source

Long-term MST radar observations of vertical wave number spectra of gravity waves in the tropical troposphere over Gadanki (13.5° N, 79.2° E): comparison with model spectra [PDF]

open access: yesAnnales Geophysicae, 2008
The potential utility of Mesosphere-Stratosphere-Troposphere (MST) radar measurements of zonal, meridional and vertical winds for divulging the gravity wave vertical wave number spectra is discussed. The data collected during the years 1995–2004
A. Narendra Babu   +5 more
doaj   +1 more source

The Gravity of Light-Waves [PDF]

open access: yesUniverse, 2018
Light waves carry along their own gravitational field; for simple plain electromagnetic waves, the gravitational field takes the form of a p p -wave. I present the corresponding exact solution of the Einstein–Maxwell equations and discuss the dynamics of classical particles and quantum fields in this gravitational and electromagnetic background.
openaire   +3 more sources

Gravity wave penetration into the thermosphere: sensitivity to solar cycle variations and mean winds [PDF]

open access: yesAnnales Geophysicae, 2008
We previously considered various aspects of gravity wave penetration and effects at mesospheric and thermospheric altitudes, including propagation, viscous effects on wave structure, characteristics, and damping, local body forcing, responses to solar
D. C. Fritts, S. L. Vadas
doaj   +1 more source

Effects of high-latitude atmospheric gravity wave disturbances on artificial HF radar backscatter [PDF]

open access: yes, 2006
International audienceObservations of HF radar backscatter from artificial field-aligned irregularities in an ionosphere perturbed by travelling disturbances due to atmospheric gravity waves are presented.
Tim K. Yeoman (7583066)   +14 more
core   +1 more source

Climatology, long-term variability and trend of resolved gravity wave drag in the stratosphere revealed by ERA5 [PDF]

open access: yesWeather and Climate Dynamics
Internal gravity waves have well-known importance for atmospheric dynamics, transport and coupling between atmospheric layers, and their parameterized forcing affects the circulation in climate models, especially in the stratosphere.
Z. Procházková   +2 more
doaj   +1 more source

CRITICAL GRAVITY WAVES

open access: yesThe Thirteenth Marcel Grossmann Meeting, 2015
11 pages. v2 References added.
Ayón-Beato, Eloy   +2 more
openaire   +2 more sources

Response of Ozone to a Gravity Wave Process in the UTLS Region Over the Tibetan Plateau

open access: yesFrontiers in Earth Science, 2020
In this paper, ERA5 reanalysis data from the European Center for Medium-Range Weather Forecasts and the Weather Research and Forecasting (WRF) mesoscale model are used to compare and simulate a topographic gravity wave event that occurred over the ...
Shujie Chang   +5 more
doaj   +1 more source

Satellite observations of middle atmosphere gravity wave absolute momentum flux and of its vertical gradient during recent stratospheric warmings [PDF]

open access: yesAtmospheric Chemistry and Physics, 2016
Sudden stratospheric warmings (SSWs) are circulation anomalies in the polar region during winter. They mostly occur in the Northern Hemisphere and affect also surface weather and climate.
M. Ern   +12 more
doaj   +1 more source

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