scholarly journals Properties of Phase Solitons in an Optically Driven Semiconductor Ring Laser

2019 ◽  
Vol 9 (20) ◽  
pp. 4351
Author(s):  
Ghafour Hashemvand Shakarab ◽  
Reza Kheradmand ◽  
Mohammad Agha Bolorizadeh ◽  
Franco Prati

A semiconductor ring laser with a long cavity supports propagating localised structures with a chiral charge, named phase solitons. In this paper we study the dependence of the velocity and of the duration of the phase solitons on the characteristic time scales of the laser, namely the photon lifetime and the carrier lifetime. We show numerically that phase solitons are stable over a large range of those parameters and verify that the propagation velocity decreases linearly with the ratio of the carrier lifetime to the photon lifetime, while the duration is proportional to the ratio of the carrier lifetime to the cavity roundtrip time.

2009 ◽  
Author(s):  
Bin Zhang ◽  
Lu-Hong Mao ◽  
Sheng Xie ◽  
Wei-Lian Guo ◽  
Yan Chen ◽  
...  

Author(s):  
Zhuoran Wang ◽  
Guy Verschaffelt ◽  
Gabor Mezosi ◽  
Marc Sorel ◽  
Jan Danckaert ◽  
...  

Author(s):  
Andrea Trita ◽  
Gabor Mezosi ◽  
Maria J. Latorre Vidal ◽  
Marco Zanola ◽  
Ilaria Cristiani ◽  
...  

2009 ◽  
Vol 27 (19) ◽  
pp. 4233-4240 ◽  
Author(s):  
Bei Li ◽  
M.I. Memon ◽  
G. Mezosi ◽  
Zhuoran Wang ◽  
M. Sorel ◽  
...  

2011 ◽  
Vol 12 (1) ◽  
pp. 27-44 ◽  
Author(s):  
Michael Kunz

Abstract Simulations of orographic precipitation over the low mountain ranges of southwestern Germany and eastern France with two different physics-based linear precipitation models are presented. Both models are based on 3D airflow dynamics from linear theory and consider advection of condensed water and leeside drying. Sensitivity studies for idealized conditions and a real case study show that the amount and spatial distribution of orographic precipitation is strongly controlled by characteristic time scales for cloud and hydrometeor advection and background precipitation due to large-scale lifting. These parameters are estimated by adjusting the model results on a 2.5-km grid to observed precipitation patterns for a sample of 40 representative orography-dominated stratiform events (24 h) during a calibration period (1971–80). In general, the best results in terms of lowest rmse and bias are obtained for characteristic time scales of 1600 s and background precipitation of 0.4 mm h−1. Model simulations of a sample of 84 events during an application period (1981–2000) with fixed parameters demonstrate that both models are able to reproduce quantitatively precipitation patterns obtained from observations and reanalyses from a numerical model [Consortium for Small-scale Modeling (COSMO)]. Combining model results with observation data shows that heavy precipitations over mountains are restricted to situations with strong atmospheric forcings in terms of synoptic-scale lifting, horizontal wind speed, and moisture content.


2017 ◽  
Vol 35 (16) ◽  
pp. 3555-3561 ◽  
Author(s):  
Arpit Khandelwal ◽  
Azeemuddin Syed ◽  
Jagannath Nayak

2009 ◽  
Vol 27 (6) ◽  
pp. 631-638 ◽  
Author(s):  
Kornkamol Thakulsukanant ◽  
Bei Li ◽  
Irfan Memon ◽  
Gabor Mezosi ◽  
Zhuoran Wang ◽  
...  

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