Pregled bibliografske jedinice broj: 245256
A large-amplitude gravity wave over the Adriatic
A large-amplitude gravity wave over the Adriatic // Geophysical Research Abstracts, Vol. 8
Beč, 2006. (poster, nije recenziran, sažetak, znanstveni)
CROSBI ID: 245256 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
A large-amplitude gravity wave over the Adriatic
Autori
Belušić, Danijel ; Grisogono, Branko ; Bencetić Klaić, Zvjezdana
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Geophysical Research Abstracts, Vol. 8
/ - Beč, 2006
Skup
European Geosciences Union General Assembly
Mjesto i datum
Beč, Austrija, 02.04.2006. - 07.04.2006
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
front; convective instability; wave-CISK; MM5
Sažetak
A study of an atmospheric pressure disturbance that occurred over the Adriatic on 27 June 2003 is presented. The pressure disturbance induced exceptional sea level oscillations and strong current reversals in the eastern part of the middle Adriatic that flooded the seafront. Barographs in the area recorded pressure amplitudes over 6 hPa. The numerical simulation of the phenomenon is performed using the MM5 model. The model results show that the cold front approaching from the north together with the orographic forcing of the Alps induced the convection over the Alps and later the appearance of a gravity wave. The wave and the developed mesoscale convective system were coupled and propagated together towards southeast. When the coupled system arrived over the warm Adriatic Sea, the gravity wave deepened and obtained its maximum amplitude over the middle Adriatic. After reaching the Adriatic, the gravity wave horizontal structure started resembling dipole or even tripole, with low-high-low pressure patterns recorded also by the barographs. The 10 min digital barograph records point to even more complex structure with one more minimum and maximum, which were not resolved by the numerical model. All the results strongly suggest that the gravity wave propagation and maintenance mechanisms are consistent with the wave-CISK model which assumes a positive feedback between the gravity-wave-associated convergence forcing the convection, and the convection providing the source of wave energy.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb