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Pregled bibliografske jedinice broj: 245256

A large-amplitude gravity wave over the Adriatic


Belušić, Danijel; Grisogono, Branko; Bencetić Klaić, Zvjezdana
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, 2.4.-7.4.2006

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


Projekti:
0119330
0119339

Ustanove:
Prirodoslovno-matematički fakultet, Zagreb

Citiraj ovu publikaciju:

Belušić, Danijel; Grisogono, Branko; Bencetić Klaić, Zvjezdana
A large-amplitude gravity wave over the Adriatic // Geophysical Research Abstracts, Vol. 8
Beč, 2006. (poster, nije recenziran, sažetak, znanstveni)
Belušić, D., Grisogono, B. & Bencetić Klaić, Z. (2006) A large-amplitude gravity wave over the Adriatic. U: Geophysical Research Abstracts, Vol. 8.
@article{article, year = {2006}, keywords = {front, convective instability, wave-CISK, MM5}, title = {A large-amplitude gravity wave over the Adriatic}, keyword = {front, convective instability, wave-CISK, MM5}, publisherplace = {Be\v{c}, Austrija} }
@article{article, year = {2006}, keywords = {front, convective instability, wave-CISK, MM5}, title = {A large-amplitude gravity wave over the Adriatic}, keyword = {front, convective instability, wave-CISK, MM5}, publisherplace = {Be\v{c}, Austrija} }




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