Results 31 to 40 of about 110,240 (298)

climatology [PDF]

open access: yes, 2020
Energy and momentum deposition from planetary-scale Rossby waves as well as from small-scale gravity waves (GWs) largely control stratospheric dynamics.
Danker, Jessica   +5 more
core   +1 more source

More evidence for a planetary wave link with midlatitude E region coherent backscatter and sporadic E layers [PDF]

open access: yesAnnales Geophysicae, 2000
Measurements of midlatitude E region coherent backscatter obtained during four summers with SESCAT, a 50 MHz Doppler system operating in Crete, Greece, and concurrent ionosonde recordings from the same ionospheric volume obtained with a CADI for one ...
M. Voiculescu   +5 more
doaj   +1 more source

Spontaneous generation of inertial waves from boundary turbulence in a librating sphere [PDF]

open access: yes, 2013
In this work, we report the excitation of inertial waves in a librating sphere even for libration frequencies where these waves are not directly forced.
Bars, Michael Le   +2 more
core   +3 more sources

Properties of internal planetary-scale inertio gravity waves in the mesosphere [PDF]

open access: yesAnnales Geophysicae, 2004
At high latitudes in the upper mesosphere, horizontal wind oscillations have been observed with periods around 10h. Waves with such a period are generated in our Numerical Spectral Model (NSM), and they are identified as planetary-scale inertio ...
H. G. Mayr   +4 more
doaj   +1 more source

Arctic amplification: does it impact the polar jet stream?

open access: yesTellus: Series A, Dynamic Meteorology and Oceanography, 2016
It has been hypothesised that the Arctic amplification of temperature changes causes a decrease in the northward temperature gradient in the troposphere, thereby enhancing the oscillation of planetary waves leading to extreme weather in mid-latitudes. To
Valentin P. Meleshko   +4 more
doaj   +1 more source

Tropopause-level planetary wave source and its role in two-way troposphere–stratosphere coupling [PDF]

open access: yesWeather and Climate Dynamics, 2020
Atmospheric planetary waves play a fundamental role in driving stratospheric dynamics, including sudden stratospheric warming (SSW) events. It is well established that the bulk of the planetary wave activity originates near the surface.
L. Boljka, T. Birner
doaj   +1 more source

A phase-space study of jet formation in planetary-scale fluids

open access: yes, 2009
The interaction between planetary waves and an arbitrary zonal flow is studied from a phase-space viewpoint. Using the Wigner distribution, a planetary wave Vlasov equation is derived that includes the contribution of the mean flow to the zonal potential
Wordsworth, Robin D.
core   +2 more sources

A model of mid-latitude E-region plasma convergence inside a planetary wave cyclonic vortex [PDF]

open access: yesAnnales Geophysicae, 2002
Recently, Shalimov et al. (1999) proposed a new mechanism for large-scale accumulation of long-lived metallic ions in the mid-latitude ionosphere driven by planetary waves in the lower thermosphere.
S. Shalimov   +3 more
doaj   +1 more source

Stratospheric control of planetary waves [PDF]

open access: yesGeophysical Research Letters, 2016
AbstractThe effects of imposing at various altitudes in the stratosphere zonally symmetric circulation anomalies associated with a stratospheric sudden warming are investigated in a mechanistic circulation model. A shift of the tropospheric jet is found even when the anomalies are imposed only above 2 hPa.
Peter Hitchcock, Peter H. Haynes
openaire   +1 more source

Nanothermometry in Living Cells: Physical Limits, Conceptual and Material Challenges

open access: yesAdvanced Functional Materials, EarlyView.
Heat and temperature are fundamental to life. When nanothermometers began probing regions as small as a living cell, they triggered controversial claims of large intracellular temperature gradients. We review physical constraints energy‐conservation, entropy production, thermodynamic fluctuations, and molecular dynamics.
Taras Plakhotnik
wiley   +1 more source

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