Irreversible thermodynamics of nonlinear transport processes and instability: Application to the current fluctuation phenomena in semiconductors

1984 ◽  
Vol 80 (5) ◽  
pp. 2063-2075 ◽  
Author(s):  
Jaleel Ali ◽  
Byung Chan Eu
Keyword(s):  
Irreversible Thermodynamics ◽  
Fluctuation Phenomena ◽  
Transport Processes ◽  
Nonlinear Transport ◽  
Current Fluctuation

scholarly journals Nonlinear transport processes in tokamak plasmas. I. The collisional regimes

2008 ◽  
Vol 15 (6) ◽  
pp. 062309 ◽  
Author(s):  
Giorgio Sonnino ◽  
Philippe Peeters
Keyword(s):  
Transport Processes ◽  
Tokamak Plasmas ◽  
Nonlinear Transport

scholarly journals An Atlantic streamer in stratospheric ozone observations and SD-WACCM simulation data

2016 ◽  
Author(s):  
Klemens Hocke ◽  
Franziska Schranz ◽  
Eliane Maillard Barras ◽  
Lorena Moreira ◽  
Niklaus Kämpfer
Keyword(s):  
Water Vapour ◽  
Central Europe ◽  
Large Scale ◽  
Surf Zone ◽  
Middle Atmosphere ◽  
Stratospheric Ozone ◽  
Polar Vortex ◽  
Transport Processes ◽  
Sudden Increase ◽  
Nonlinear Transport

Abstract. Observation and simulation of individual ozone streamers are important for the description and understanding of nonlinear transport processes in the middle atmosphere. A sudden increase in mid-stratospheric ozone occurred above Central Europe on December 4, 2015. The GROunbased Millimeter-wave Ozone Spectrometer (GROMOS) and the Stratospheric Ozone MOnitoring RAdiometer (SOMORA) in Switzerland measured an ozone enhancement of about 30 % at 34 km altitude from December 1 to December 4. A similar ozone increase is simulated by the Specified Dynamics-Whole Atmosphere Community Climate (SD-WACCM) model. Further, the global ozone fields at 34 km altitude from SD-WACCM and the satellite experiment Aura/MLS show a remarkable agreement for the location and the timing of an ozone streamer (large-scale tongue like structure) extending from the subtropics in Northern America over the Atlantic to Central Europe. This agreement indicates that SD-WACCM can inform us about the wind inside the Atlantic ozone streamer. SD-WACCM shows an eastward wind of about 100 m/s inside the Atlantic streamer in the mid-stratosphere. SD-WACCM shows that the Atlantic streamer flows along the edge region of the polar vortex. The Atlantic streamer turns southward at an erosion region of the polar vortex located above the Caspian Sea. The spatial distribution of stratospheric water vapour indicates a filament outgoing from this erosion region. The Atlantic streamer, the polar vortex erosion region and the water vapour filament belong to the process of planetary wave breaking in the so-called surf zone of the Northern mid-latitude winter stratosphere.

Nonlinear transport processes in gases

1981 ◽  
Vol 74 (5) ◽  
pp. 3006-3015 ◽  
Author(s):  
Byung Chan Eu
Keyword(s):  
Transport Processes ◽  
Nonlinear Transport

Nonlinear Transport Processes in Non-Ideal Media

2014 ◽  
Vol 55 (2-3) ◽  
pp. 254-263 ◽  
Author(s):  
G. A. Pavlov ◽  
Yu. V. Troshchiev
Keyword(s):  
Transport Processes ◽  
Nonlinear Transport
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