A climatological study of the strongest local winds of Japan “Inami‐kaze”

2019 ◽  
Vol 40 (2) ◽  
pp. 1007-1021
Author(s):  
Takuma Koyanagi ◽  
Hiroyuki Kusaka
Keyword(s):  
1957 ◽  
Vol 3 (22) ◽  
pp. 104-110
Author(s):  
Terence Armstrong

AbstractRecent investigations of the ice of the central polar basin have been largely done by Russians, and some of their results are given here. General characteristics of the ice and of the currents and bathymetry of the area are outlined. Attention is directed to advances in knowledge in two spheres; the effect of currents and local winds on ice drift, and the growth and structure of floes. To illustrate the latter, an explanation of the stratification of a 3 m. vertical section is quoted. In conclusion, the prospects of the work continuing, and of its results being made available, are assessed.


1985 ◽  
Vol 5 (2) ◽  
pp. 145-160 ◽  
Author(s):  
A. P. Sturman ◽  
S. J. Fitzsimons ◽  
L. M. Holland

2016 ◽  
Vol 6 (1) ◽  
Author(s):  
Takao Yoshikane ◽  
Kei Yoshimura ◽  
Eun-Chul Chang ◽  
Akane Saya ◽  
Taikan Oki

1990 ◽  
Vol 51 (4) ◽  
pp. 321-342 ◽  
Author(s):  
Ian G. McKendry ◽  
Errol W. D. Lewthwaite

2002 ◽  
pp. 295-318
Author(s):  
Edward Linacre ◽  
Bart Geerts
Keyword(s):  

2017 ◽  
Vol 47 (6) ◽  
pp. 1367-1387 ◽  
Author(s):  
S. Djakouré ◽  
P. Penven ◽  
B. Bourlès ◽  
V. Koné ◽  
J. Veitch

AbstractThe northern Gulf of Guinea is a part of the eastern tropical Atlantic where oceanic conditions due to the presence of coastal upwelling may influence the regional climate and fisheries. The dynamics of this coastal upwelling is still poorly understood. A sensitivity experiment based on the Regional Oceanic Modeling System (ROMS) is carried out to assess the role of the detachment of the Guinea Current as a potential mechanism for coastal upwelling. This idealized experiment is performed by canceling the inertia terms responsible for the advection of momentum in the equations and comparing with a realistic experiment. The results exhibit two major differences. First, the Guinea Current is found to be highly sensitive to inertia, as it is no longer detached from the coast in the idealized experiment. The Guinea Current adjusts on an inertial boundary layer, the inertial terms defining its lateral extension. Second, the upwelling east of Cape Palmas disappears in absence of the Guinea Current detachment. This is in contrast with the upwelling east of Cape Three Points, which is still present. The results suggest that two different generation processes of the coastal upwelling need to be considered: the upwelling east of Cape Palmas (which is due to inertia, topographic variations, and advective terms effects resulting in important vertical pumping) and the upwelling east of Cape Three Points (which is principally induced by local winds). In addition to recent work ruling out the role of eddies, this study clarifies the processes responsible for this coastal upwelling.


Author(s):  
Storm Dunlop

Although certain weather events, such as violent tornadoes, affect relatively small areas on the ground, there are a number of effects that are localized in their influence. ‘Localized weather’ first considers fog, which may be associated with widespread anticyclonic conditions leading to a significant drop in temperature at night, and relatively quiet, or windless, conditions. The two common forms of fog are radiation fog and advection fog. Haze and smog are also discussed along with local winds divided into two groups: sea, land, and lake breezes; and valley and mountain winds. Katabatic winds, föhn conditions, lake effect snow, ice storms, and glaze (or ‘black ice’) are also considered.


2018 ◽  
Vol 39 (1) ◽  
pp. 1-17 ◽  
Author(s):  
Djordje Romanic
Keyword(s):  

1951 ◽  
pp. 655-672 ◽  
Author(s):  
Friedrich Defant
Keyword(s):  

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