The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions

<p>The Split wildfire in July 2017, which was one of the most severe wildfires in the history of this Croatian World Heritage Site, is the focus in this study. The Split fire is a good example of a wildfire–urban interface, with unexpected fire behavior including rapid downslope spread to the...

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Main Authors: I. Čavlina Tomašević, K. K. W. Cheung, V. Vučetić, P. Fox-Hughes, K. Horvath, M. Telišman Prtenjak, P. J. Beggs, B. Malečić, V. Milić
Format: Article
Language:English
Published: Copernicus Publications 2022-10-01
Series:Natural Hazards and Earth System Sciences
Online Access:https://nhess.copernicus.org/articles/22/3143/2022/nhess-22-3143-2022.pdf
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author I. Čavlina Tomašević
I. Čavlina Tomašević
I. Čavlina Tomašević
K. K. W. Cheung
V. Vučetić
P. Fox-Hughes
K. Horvath
M. Telišman Prtenjak
P. J. Beggs
B. Malečić
V. Milić
author_facet I. Čavlina Tomašević
I. Čavlina Tomašević
I. Čavlina Tomašević
K. K. W. Cheung
V. Vučetić
P. Fox-Hughes
K. Horvath
M. Telišman Prtenjak
P. J. Beggs
B. Malečić
V. Milić
author_sort I. Čavlina Tomašević
collection DOAJ
description <p>The Split wildfire in July 2017, which was one of the most severe wildfires in the history of this Croatian World Heritage Site, is the focus in this study. The Split fire is a good example of a wildfire–urban interface, with unexpected fire behavior including rapid downslope spread to the coastal populated area. This study clarifies the meteorological conditions behind the fire event, those that have limited the effectiveness of firefighting operations, and the rapid escalation and expansion of the fire zones within 30 h. The Split fire propagation was first reconstructed using radio logs, interviews with firefighters and pilots involved in the intervention, eyewitness statements, digital photographs from fire detection cameras, media, and the monthly firefighting journal. Four phases of fire development have been identified.</p> <p>Then, weather observations and numerical simulations using an enhanced-resolution operational model are utilized to analyze the dynamics in each phase of the fire runs. The synoptic background of the event includes large surface pressure gradient between the Azores anticyclone accompanied by a cold front and a cyclone over the southeastern Balkan Peninsula. At the upper level, there was a deep shortwave trough extending from the Baltic Sea to the Adriatic Sea, which developed into a cut-off low. Such synoptic conditions have resulted in the maximum fire weather index in 2017. Combined with topography, they also locally provoke the formation of the strong northeasterly <i>bura</i> wind along the Adriatic coast, which has been accompanied by a low-level jet (LLJ). The bura (downslope wind), with mid- to low-level gravity-wave breaking and turbulence mixing (as in the hydraulic jump theory), also facilitated the subsidence of dry air from the upper troposphere and rapid drying at the surface.</p> <p>This study demonstrates that numerical guidance that indicates the spatial and temporal occurrence of a LLJ is highly capable of explaining the Split fire evolution from the ignition potential to its extinguishment stage. Thus, in addition to the conventional fire weather indices, such products are able to improve fire weather behavior forecasting and in general more effective decision-making in fire management.</p>
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spelling doaj.art-c5c1f49a40d04a70a374779697288a402022-12-22T04:07:42ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812022-10-01223143316510.5194/nhess-22-3143-2022The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditionsI. Čavlina Tomašević0I. Čavlina Tomašević1I. Čavlina Tomašević2K. K. W. Cheung3V. Vučetić4P. Fox-Hughes5K. Horvath6M. Telišman Prtenjak7P. J. Beggs8B. Malečić9V. Milić10School of Natural Sciences, Faculty of Science and Engineering, Macquarie University, Sydney, NSW 2109, AustraliaCroatian Meteorological and Hydrological Service, Ravnice 48, 10 000 Zagreb, CroatiaDepartment of Geophysics, Faculty of Science, University of Zagreb, Horvatovac 95, 10 000 Zagreb, CroatiaE-Complexity Consultant, Eastwood, NSW 2122, AustraliaCroatian Meteorological and Hydrological Service, Ravnice 48, 10 000 Zagreb, CroatiaBureau of Meteorology, Level 5, 111 Macquarie St., Hobart, TAS 7001, AustraliaCroatian Meteorological and Hydrological Service, Ravnice 48, 10 000 Zagreb, CroatiaDepartment of Geophysics, Faculty of Science, University of Zagreb, Horvatovac 95, 10 000 Zagreb, CroatiaSchool of Natural Sciences, Faculty of Science and Engineering, Macquarie University, Sydney, NSW 2109, AustraliaDepartment of Geophysics, Faculty of Science, University of Zagreb, Horvatovac 95, 10 000 Zagreb, CroatiaCroatian Meteorological and Hydrological Service, Ravnice 48, 10 000 Zagreb, Croatia<p>The Split wildfire in July 2017, which was one of the most severe wildfires in the history of this Croatian World Heritage Site, is the focus in this study. The Split fire is a good example of a wildfire–urban interface, with unexpected fire behavior including rapid downslope spread to the coastal populated area. This study clarifies the meteorological conditions behind the fire event, those that have limited the effectiveness of firefighting operations, and the rapid escalation and expansion of the fire zones within 30 h. The Split fire propagation was first reconstructed using radio logs, interviews with firefighters and pilots involved in the intervention, eyewitness statements, digital photographs from fire detection cameras, media, and the monthly firefighting journal. Four phases of fire development have been identified.</p> <p>Then, weather observations and numerical simulations using an enhanced-resolution operational model are utilized to analyze the dynamics in each phase of the fire runs. The synoptic background of the event includes large surface pressure gradient between the Azores anticyclone accompanied by a cold front and a cyclone over the southeastern Balkan Peninsula. At the upper level, there was a deep shortwave trough extending from the Baltic Sea to the Adriatic Sea, which developed into a cut-off low. Such synoptic conditions have resulted in the maximum fire weather index in 2017. Combined with topography, they also locally provoke the formation of the strong northeasterly <i>bura</i> wind along the Adriatic coast, which has been accompanied by a low-level jet (LLJ). The bura (downslope wind), with mid- to low-level gravity-wave breaking and turbulence mixing (as in the hydraulic jump theory), also facilitated the subsidence of dry air from the upper troposphere and rapid drying at the surface.</p> <p>This study demonstrates that numerical guidance that indicates the spatial and temporal occurrence of a LLJ is highly capable of explaining the Split fire evolution from the ignition potential to its extinguishment stage. Thus, in addition to the conventional fire weather indices, such products are able to improve fire weather behavior forecasting and in general more effective decision-making in fire management.</p>https://nhess.copernicus.org/articles/22/3143/2022/nhess-22-3143-2022.pdf
spellingShingle I. Čavlina Tomašević
I. Čavlina Tomašević
I. Čavlina Tomašević
K. K. W. Cheung
V. Vučetić
P. Fox-Hughes
K. Horvath
M. Telišman Prtenjak
P. J. Beggs
B. Malečić
V. Milić
The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions
Natural Hazards and Earth System Sciences
title The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions
title_full The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions
title_fullStr The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions
title_full_unstemmed The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions
title_short The 2017 Split wildfire in Croatia: evolution and the role of meteorological conditions
title_sort 2017 split wildfire in croatia evolution and the role of meteorological conditions
url https://nhess.copernicus.org/articles/22/3143/2022/nhess-22-3143-2022.pdf
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