Tornadic waterspout event in Split (Croatia) - analysis of meteorological environment
Апстракт
The aim of this paper is the waterspout in Split (phi 43.51 degrees N, lambda 16.45 degrees E, h = 0 m) observed on January 6, 2016, which swept over the city at 15:40-16:00 CET (14:40-15:00 UTC). There were convective developments in upper-level south-west flow within the cloudiness which followed the low-level cyclone and associated frontal disturbances. There was an intense thermodynamic instability in lower and mid layers of the atmosphere-the passage of the cold front as a main synoptic feature over the warm Adriatic water, pronounced directional and speed wind shear, as well as the presence of jet stream and a pronounced horizontal field of positive divergence above the observed area. The aim of this paper is to investigate synoptic and mesoscale situation, and meteorological conditions which created favourable thermodynamic environment which preceded the waterspout development.
Кључне речи:
waterspout / synoptic types / instability indices / the Adriatic Sea / SplitИзвор:
Zbornik radova Geografskog instituta "Jovan Cvijić", SANU, 2016, 66, 2, 185-202Издавач:
- Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"
Колекције
Институција/група
Geografski fakultetTY - JOUR AU - Mihajlović, Jovan AU - Ducić, Vladan AU - Burić, Dragan PY - 2016 UR - https://gery.gef.bg.ac.rs/handle/123456789/785 AB - The aim of this paper is the waterspout in Split (phi 43.51 degrees N, lambda 16.45 degrees E, h = 0 m) observed on January 6, 2016, which swept over the city at 15:40-16:00 CET (14:40-15:00 UTC). There were convective developments in upper-level south-west flow within the cloudiness which followed the low-level cyclone and associated frontal disturbances. There was an intense thermodynamic instability in lower and mid layers of the atmosphere-the passage of the cold front as a main synoptic feature over the warm Adriatic water, pronounced directional and speed wind shear, as well as the presence of jet stream and a pronounced horizontal field of positive divergence above the observed area. The aim of this paper is to investigate synoptic and mesoscale situation, and meteorological conditions which created favourable thermodynamic environment which preceded the waterspout development. PB - Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić" T2 - Zbornik radova Geografskog instituta "Jovan Cvijić", SANU T1 - Tornadic waterspout event in Split (Croatia) - analysis of meteorological environment VL - 66 IS - 2 SP - 185 EP - 202 DO - 10.2298/IJGI1602185M UR - https://hdl.handle.net/21.15107/rcub_gery_785 ER -
@article{ author = "Mihajlović, Jovan and Ducić, Vladan and Burić, Dragan", year = "2016", abstract = "The aim of this paper is the waterspout in Split (phi 43.51 degrees N, lambda 16.45 degrees E, h = 0 m) observed on January 6, 2016, which swept over the city at 15:40-16:00 CET (14:40-15:00 UTC). There were convective developments in upper-level south-west flow within the cloudiness which followed the low-level cyclone and associated frontal disturbances. There was an intense thermodynamic instability in lower and mid layers of the atmosphere-the passage of the cold front as a main synoptic feature over the warm Adriatic water, pronounced directional and speed wind shear, as well as the presence of jet stream and a pronounced horizontal field of positive divergence above the observed area. The aim of this paper is to investigate synoptic and mesoscale situation, and meteorological conditions which created favourable thermodynamic environment which preceded the waterspout development.", publisher = "Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"", journal = "Zbornik radova Geografskog instituta "Jovan Cvijić", SANU", title = "Tornadic waterspout event in Split (Croatia) - analysis of meteorological environment", volume = "66", number = "2", pages = "185-202", doi = "10.2298/IJGI1602185M", url = "https://hdl.handle.net/21.15107/rcub_gery_785" }
Mihajlović, J., Ducić, V.,& Burić, D.. (2016). Tornadic waterspout event in Split (Croatia) - analysis of meteorological environment. in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"., 66(2), 185-202. https://doi.org/10.2298/IJGI1602185M https://hdl.handle.net/21.15107/rcub_gery_785
Mihajlović J, Ducić V, Burić D. Tornadic waterspout event in Split (Croatia) - analysis of meteorological environment. in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU. 2016;66(2):185-202. doi:10.2298/IJGI1602185M https://hdl.handle.net/21.15107/rcub_gery_785 .
Mihajlović, Jovan, Ducić, Vladan, Burić, Dragan, "Tornadic waterspout event in Split (Croatia) - analysis of meteorological environment" in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU, 66, no. 2 (2016):185-202, https://doi.org/10.2298/IJGI1602185M ., https://hdl.handle.net/21.15107/rcub_gery_785 .