Potential of Documentary Evidence to Study Fatalities of Hydrological and Meteorological Events in the Czech Republic
Abstract
:1. Introduction
2. Materials and Methods
2.1. Societal and Climatic Background
2.2. Documentary Data
2.2.1. Narrative Sources (Chronicles, “Books of Memory”)
2.2.2. Weather Diaries
2.2.3. Newspapers and Other Media
2.2.4. Parliamentary Proposals
2.2.5. Epigraphic Evidence
2.2.6. Systematic Meteorological and Hydrological Observations
2.2.7. Professional Papers
2.3. Meteorological Data
- (i)
- Daily minimum temperatures Tmin from the Prague-Klementinum station (191 m above sea level (asl)) for 1 December 1928–15 March 1929 and mean Tmin in the 1961–1990 period;
- (ii)
- Daily snow depths at the Prague-Karlov (260 m asl) and Luká (510 m asl) stations for 1 December 1928–15 March 1929;
- (iii)
- Daily precipitation totals for selected meteorological stations in southeastern Moravia for 9 June 1970;
- (iv)
- Precipitation totals for 5–8 July 1997 for selected meteorological stations in the eastern part of the Czech Republic;
- (v)
- Monthly and annual temperature and precipitation series averaged over the territory of the Czech Republic for the 1981–2018 period [68].
2.4. Methods
- (i)
- Flood: This includes rainfall-induced floods originating from single-day or multiple-day rainfall caused by precipitation-rich synoptic situations. Snow-melt floods arising after sudden melting of deep snow cover in winter/spring and mixed floods caused by a combination of snowmelt and rainfall (may be accompanied by ice jams on rivers) in winter or early spring are part of this group.
- (ii)
- Flash flood: Flash floods appear after the occurrence of torrential rains or cloudbursts (of high intensity and relatively short duration), usually accompanying thunderstorms.
- (iii)
- Windstorm: Strong winds related to large horizontal gradients of air pressure, of duration from a few hours to some days.
- (iv)
- Convective storm: Strong winds of short duration related to the development of cumulonimbus cloud (e.g., squall, tornado, downburst) with significant local/sub-regional effects.
- (v)
- Lightning: Lightning, as a phenomenon accompanying thunderstorms, may set fire to structures and trees, or kill or injure people by a direct strike.
- (vi)
- Frost: Very severe frosts when their effects may be accompanied by snowstorm or snowdrifts.
- (vii)
- Snow/glaze-ice: This includes, in particular, cases of snow calamity and the creation of glaze-ice on communications leading to car accidents.
- (viii)
- Heat: Extremely high temperatures, usually during heat waves.
- (ix)
- Other extremes: HMEs with fatalities that cannot be unequivocally attributed to any of the previous types (e.g., avalanche, thunderstorms in general).
3. Results
3.1. Spatiotemporal Variability of Fatalities
3.2. Features of Fatalities
3.2.1. Gender (Figure 8a)
3.2.2. Age (Figure 8b)
3.2.3. Cause of death (Figure 8c)
3.2.4. Place of Death (Figure 8d)
3.2.5. Type of Death (Figure 8e)
3.2.6. Behaviour (Figure 8f)
3.3. HMEs with Outstanding Numbers of Fatalities
3.3.1. Extreme Frosts and Snowdrifts in the Winter of 1928/1929
3.3.2. Flash Flood on 9 June 1970
3.3.3. Floods of July 1997
4. Discussion
4.1. Data Uncertainty
4.2. Temporal Changes in Factors Affecting Fatality
4.2.1. Lightning Fatalities
4.2.2. Transport Accidents Related to the Weather
4.2.3. Social Bias in Fatalities
4.3. The Broader Context
5. Conclusions
- (i)
- The uncertainty in documentary data used for the creation of the Czech fatality database provided only underestimated numbers of fatalities, as well as of HMEs involving fatalities. Further supplementation of this database is required, particularly with data from before 1997 and after 2011.
- (ii)
- Floods and flash floods were the predominant types of HME giving rise to fatalities in the Czech Republic, followed by windstorms with convective storms and snow/glaze-ice calamities. The other HMEs considered did not achieve comparable importance. The majority of fatalities concentrated around the summer months, followed by winter.
- (iii)
- Males and adults clearly prevailed over all other categories of fatalities classified herein. The primary cause of fatalities was drowning, associated in terms of place of death with rivers and/or their banks. Around one-quarter of fatalities may be considered indirect, and one-third were consequences of hazardous behaviour.
- (iv)
- Joining fatality trends (caused by HMEs) with climate variability/change requires the most complete database of fatalities. Temporally changeable factors influencing fatalities also have to be taken into account. The preliminary Czech fatality database, for the 1981–2018 period, does not yet permit the formulation of any such consideration with respect to observed climate change.
- (v)
- Documentary evidence constitutes an important source for the creation of databases of fatalities attributable to HMEs for the most recent period, as well as for the past. Newspaper reports are the most important source. The use of documentary data opens a new field of application for historical–climatological and historical–hydrological data worldwide.
- (vi)
- The experience and results gathered in this contribution will be further used for extensive research, in order to create a 1901–2018 chronology of fatalities attributable to HMEs over the territory of the Czech Republic. As well as traditional documentary evidence, new sources and partial databases kept by a range of institutions (e.g., the health service, the police, the fire-fighting service) will have to be used.
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Type of HME | Number of Fatalities | ||||||||
---|---|---|---|---|---|---|---|---|---|
Total | According to Reports | According to Sources | |||||||
1 | 2 | 3 | More | Newspaper | Internet | Other | Combined | ||
Flood | 91 | 66 | 17 | 8 | – | 63 | – | 13 | 15 |
Flash flood | 54 | 25 | 17 | 1 | 11 | 17 | 10 | 6 | 21 |
Windstorm | 31 | 24 | 1 | 2 | 4 | 17 | 9 | – | 5 |
Convective storm | 22 | 18 | 4 | – | – | 16 | 6 | – | – |
Lightning | 8 | 7 | 1 | – | – | 5 | 3 | – | – |
Frost | 16 | 16 | – | – | – | 16 | – | – | – |
Snow/glaze ice | 37 | 33 | 4 | – | – | 35 | 2 | – | – |
Heat | 2 | 2 | – | – | – | 2 | – | – | – |
Other HMEs | 8 | 8 | – | – | – | 6 | 2 | – | – |
Total | 269 | 199 | 44 | 11 | 15 | 177 | 32 | 19 | 41 |
% Total | 100 | 74.0 | 16.4 | 4.1 | 5.6 | 65.8 | 11.9 | 7.1 | 15.2 |
Source | Year | ||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1997 | 1998 | 1999 | 2000 | 2001 | 2002 | 2003 | 2004 | 2005 | 2006 | 2007 | 2008 | 2009 | 2010 | 2011 | 2012 | 2013 | |
A | 14 | - | - | 2 | - | 17 | - | - | - | 11 | - | - | 18 | 8 | - | - | - |
B | 60 | 10 | 0 | 2 | 0 | 16 | 0 | 0 | 0 | 9 | 0 | 0 | 15 | 8 | 0 | 0 | 15 |
C | 42 | 7 | 0 | 3 | 1 | 21 | 2 | 0 | 2 | 7 | 0 | 0 | 15 | 11 | 0 | 1 | 17 |
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Brázdil, R.; Chromá, K.; Řehoř, J.; Zahradníček, P.; Dolák, L.; Řezníčková, L.; Dobrovolný, P. Potential of Documentary Evidence to Study Fatalities of Hydrological and Meteorological Events in the Czech Republic. Water 2019, 11, 2014. https://doi.org/10.3390/w11102014
Brázdil R, Chromá K, Řehoř J, Zahradníček P, Dolák L, Řezníčková L, Dobrovolný P. Potential of Documentary Evidence to Study Fatalities of Hydrological and Meteorological Events in the Czech Republic. Water. 2019; 11(10):2014. https://doi.org/10.3390/w11102014
Chicago/Turabian StyleBrázdil, Rudolf, Kateřina Chromá, Jan Řehoř, Pavel Zahradníček, Lukáš Dolák, Ladislava Řezníčková, and Petr Dobrovolný. 2019. "Potential of Documentary Evidence to Study Fatalities of Hydrological and Meteorological Events in the Czech Republic" Water 11, no. 10: 2014. https://doi.org/10.3390/w11102014
APA StyleBrázdil, R., Chromá, K., Řehoř, J., Zahradníček, P., Dolák, L., Řezníčková, L., & Dobrovolný, P. (2019). Potential of Documentary Evidence to Study Fatalities of Hydrological and Meteorological Events in the Czech Republic. Water, 11(10), 2014. https://doi.org/10.3390/w11102014