Modeling the northern Adriatic double-gyre response to intense bora wind: A revisit
نویسندگان
چکیده
منابع مشابه
Analysis of an intense bora event in the Adriatic area
Numerical simulations of a bora event, recently occurred in the Adriatic area, are presented. Two reference runs at different horizontal resolution (about 20 km and 8 km) describe the case. Initial conditions for the atmospheric model integration are obtained from ECMWF analyses. Satellite data are used for comparisons. A further run at horizontal resolution of 8 km, using initial satellite sea...
متن کاملADRIATIC FRONTAL BORA TYPE Frontalni
The main objective of the recent Adriatic bora study by the Hydrometeorological lnstitute of Croatia was a detailed analysis of bora cases during the special observation period of Alpine experiment (SOP ALPEX) in March and April 1982. The emphasis was on local conditions described by daily courses of wind, air temperature, humidity and pressure at the surface UDK 5s1.5s5.4 Originalni znanstveni...
متن کاملSevere Bora on the mid - Adriatic
The Adriatic severe bora can partly be explained by the two-dimensional hydraulic theory, as one of the possible mechanisms of a strong surface downslope wind. A comparison of the application of the hydraulic theory shows a similar severe bora mechanism on the northern and mid-Adriatic, with the exception of the Senj area where special bora effects have been observed. As the theory could not co...
متن کاملTopographic control of wind-driven circulation in the northern Adriatic
[1] Two synoptic wind-driven situations of the circulation in the northern Adriatic were studied using the Princeton Ocean Model over the northern Adriatic Sea (NAPOM). In both situations the basin was driven by a relatively steady wind (>8 m/s) along and across the basin over three days. In the first situation (28–30 October 2008) the SSE southern jugo or scirocco wind blew along the basin, an...
متن کاملBora-induced currents corresponding to different synoptic conditions above the Adriatic
The Bora wind field is characterised by strong vorticity and divergence. Several numerical experiments, in which an oceanographic model was forced with northeasterly winds having climatological alongshore variability, were performed in order to study the influence of spatial variability in the bora wind field on the surface currents in the northern Adriatic. Numerical model results showed that ...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Journal of Geophysical Research
سال: 2006
ISSN: 0148-0227
DOI: 10.1029/2005jc003377