A polar low observed over the Norwegian Sea on 3-4 March 2008: high-resolution numerical experiments

2012 ◽  
Vol 138 (669) ◽  
pp. 1983-1998 ◽  
Author(s):  
Ivan Føre ◽  
Thor Erik Nordeng
2011 ◽  
Vol 68 (8) ◽  
pp. 1607-1619 ◽  
Author(s):  
Agnieszka A. Mrowiec ◽  
Stephen T. Garner ◽  
Olivier M. Pauluis

Abstract This paper discusses the possible existence of hurricanes in an atmosphere without water vapor and analyzes the dynamic and thermodynamic structures of simulated hurricane-like storms in moist and dry environments. It is first shown that the “potential intensity” theory for axisymmetric hurricanes is directly applicable to the maintenance of a balanced vortex sustained by a combination of surface energy and momentum flux, even in the absence of water vapor. This theoretical insight is confirmed by simulations with a high-resolution numerical model. The same model is then used to compare dry and moist hurricanes. While it is found that both types of storms exhibit many similarities and fit well within the theoretical framework, there are several differences, most notably in the storm inflow and in the relationship between hurricane size and intensity. Such differences indicate that while water vapor is not necessary for the maintenance of hurricane-like vortices, moist processes directly affect the structure of these storms.


2011 ◽  
Vol 137 (660) ◽  
pp. 1688-1699 ◽  
Author(s):  
E. A. Irvine ◽  
S. L. Gray ◽  
J. Methven

2017 ◽  
Vol 17 (3) ◽  
pp. 55-67 ◽  
Author(s):  
Yujin Kim ◽  
◽  
Mirae Hong ◽  
Jae Gyoo Lee ◽  
◽  
...  

1997 ◽  
Vol 78 (11) ◽  
pp. 2643-2658 ◽  
Author(s):  
Gunther Heinemann ◽  
Chantal Claud

A workshop on theoretical and observational studies of polar lows was held in St. Petersburg, Russia, 23–26 September 1996. An international group with scientists and students from Canada, Denmark, Germany, Norway, Russia, the United Kingdom, and the United States participated in the workshop. The papers presented covered the fields of climatological studies, studies using numerical models, and satellite studies for the Northern and Southern Hemispheres. Two polar low cases were investigated in more detail during working groups sessions: The polar low “Le Cygne” occurring 13–16 October 1993 over the Norwegian Sea, and a Southern Hemisphere polar low occurring 30 July–1 August 1986 over the Weddell Sea. Programs related to polar low research were presented in order to coordinate the international efforts in investigating polar mesocyclones. The workshop showed the progress achieved by using 1) the synergetic combination of the satellite data presently available, and 2) mesoscale numerical models for the understanding of the development and the physical processes of polar mesocyclones.


1990 ◽  
Vol 14 (1) ◽  
pp. 57-76 ◽  
Author(s):  
Frédérique Blanc ◽  
Sabine Houry ◽  
Pierre Mazzega ◽  
Jean François Minster

Fluids ◽  
2019 ◽  
Vol 4 (2) ◽  
pp. 78 ◽  
Author(s):  
Sk. Mashfiqur Rahman ◽  
Omer San

In this paper, we investigate the performance of a relaxation filtering approach for the Euler turbulence using a central seven-point stencil reconstruction scheme. High-resolution numerical experiments are performed for both multi-mode and single-mode


Author(s):  
Antonina Polezhayeva ◽  
Antonina Polezhayeva

Polar lows are generally characterized by severe weather in the form of strong winds, showers and occasionally heavy snow, which have sometimes resulted in the loss of life, especially at sea. Numerical simulations with mesoscale atmospheric models is a good alternative to investigate polar low phenomenon, because they produce temporally and spatially regular-spaced fields of atmospheric variables with high resolution. To describe the evolution of atmospheric processes the Advanced Weather Research and Forecasting (WRF-ARW) model was used. The principal objectives of this study were 1) the understanding of mesoscale WRF model and adapting the model for the Barents Sea region; 2) to conduct numerical experiments using WRF model with different Planetary Boundary Layer parameterization (PBLs) schemes and investigate the impact of each scheme on the quality of forecast; and 3) the investigation of the capability of WRF model to successfully simulate evolution of polar lows. The impact on the quality of forecast was investigated. The results of the study, obtained by numerical modeling of polar mesoscale low over the Barents Sea. One polar low, near Spitsbergen, from 24 of March to 26 of March 2014 were targeted. The results of numerical experiments showed that each of Planetary Boundary Layer parameterization scheme isn't successful for simulation of polar low.


Author(s):  
Jørn Kristiansen ◽  
Silje Lund Sørland ◽  
Trond Iversen ◽  
Dag Bjørge ◽  
Morten Ødegaard Køltzow

2015 ◽  
Vol 70 (1) ◽  
pp. 53-61 ◽  
Author(s):  
A. A. Shmatkova ◽  
A. A. Shmatkov ◽  
V. G. Gainanov ◽  
S. Buenz

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