Effect of atmospheric pressure fluctuations on low frequency and infrasound detection

2003 ◽  
Vol 113 (4) ◽  
pp. 2247-2247
Author(s):  
Carrick L. Talmadge ◽  
Doug Shields
1992 ◽  
Vol 11 (4) ◽  
pp. 109-113
Author(s):  
A.N. Ivannikov ◽  
S.V. Makeev ◽  
V.I. Pavlov

In this paper the original results of the observation of low frequency atmospheric pressure fluctuations are presented The results have been obtained over the Pacific Ocean surface during the 17th expedition of the “Academician Nesmejanov” ship. The theoretical expressions for the degree law of the amplitude spectrum decrease and its connection with the wind velocity were found. Analysis of the experimental results was compared with the proposed theoretical model of turbulence. The spikes on the background of fluctuation spectra have been discovered.


2008 ◽  
Vol 38 (4) ◽  
pp. 862-879 ◽  
Author(s):  
Brian F. Farrell ◽  
Petros J. Ioannou

Abstract Theoretical understanding of the growth of wind-driven surface water waves has been based on two distinct mechanisms: growth due to random atmospheric pressure fluctuations unrelated to wave amplitude and growth due to wave coherent atmospheric pressure fluctuations proportional to wave amplitude. Wave-independent random pressure forcing produces wave growth linear in time, while coherent forcing proportional to wave amplitude produces exponential growth. While observed wave development can be parameterized to fit these functional forms and despite broad agreement on the underlying physical process of momentum transfer from the atmospheric boundary layer shear flow to the water waves by atmospheric pressure fluctuations, quantitative agreement between theory and field observations of wave growth has proved elusive. Notably, wave growth rates are observed to exceed laminar instability predictions under gusty conditions. In this work, a mechanism is described that produces the observed enhancement of growth rates in gusty conditions while reducing to laminar instability growth rates as gustiness vanishes. This stochastic parametric instability mechanism is an example of the universal process of destabilization of nearly all time-dependent flows.


Health ◽  
2010 ◽  
Vol 02 (05) ◽  
pp. 448-453
Author(s):  
Lyudmyla Aleksandrovna Didyk ◽  
Yuriy Pavlovich Gorgo ◽  
Joris Jan Josef Dirckx ◽  
Irina Aleksandrovna Semenova ◽  
Nataliya Petrovna Didyk ◽  
...  

1988 ◽  
Vol 123 ◽  
pp. 33-36
Author(s):  
A.B. Severny ◽  
V.A. Kotov ◽  
T.T. Tsap

The Earth atmospheric pressure fluctuations in the 5-min range of periods are analysed and their influence on observations of solar 5-min oscillations are briefly discussed. New series of observations confirmed the oscillations of the Sun with period of 160.010 min.


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