Dynamical Flash Flood Risk Forecast
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F18%3A00506923" target="_blank" >RIV/68145535:_____/18:00506923 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/61989100:27350/17:10236721 RIV/61989100:27350/18:10236721
Výsledek na webu
<a href="http://dx.doi.org/10.1007/978-3-319-61297-3_27" target="_blank" >http://dx.doi.org/10.1007/978-3-319-61297-3_27</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/978-3-319-61297-3_27" target="_blank" >10.1007/978-3-319-61297-3_27</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Dynamical Flash Flood Risk Forecast
Popis výsledku v původním jazyce
Flash floods represent very dynamical natural phenomenon. Mostly, they are the result of torrential rains which can rise suddenly in any part of a country and are tough to predict. Of course, there are many weather forecasting systems, but their spatial and temporal resolution is usually insufficient for these purposes. There are also monitoring systems which can either register precipitation over the ground (a network of rain gauge stations) or runoff in riverbeds (a network of hydrometric stations). Again, spatial (and possibly temporal) resolution is not sufficient, and in the case of runoff monitoring, there is a substantial delay between actual rainfall and registration of runoff in riverbeds. And, of course, when the hydrometric station registers higher runoff than the flash floods is running or even over. From the point of early warning, all these systems reveal disadvantages. Aside from these systems, there is one which provides us with timely information about the spatial and temporal distribution of precipitation intensity over the ground. That is weather radar. We will demonstrate possible usage of these data for dynamic prediction of flash flood risk distribution in space and time over the monitored area. Proper processing of these data in combination with soil saturation indicator established using Flash flood guidance methodology developed by the US Hydrologic Research Center can generate timely information usable for early warning with a substantially reduced level of false warnings.
Název v anglickém jazyce
Dynamical Flash Flood Risk Forecast
Popis výsledku anglicky
Flash floods represent very dynamical natural phenomenon. Mostly, they are the result of torrential rains which can rise suddenly in any part of a country and are tough to predict. Of course, there are many weather forecasting systems, but their spatial and temporal resolution is usually insufficient for these purposes. There are also monitoring systems which can either register precipitation over the ground (a network of rain gauge stations) or runoff in riverbeds (a network of hydrometric stations). Again, spatial (and possibly temporal) resolution is not sufficient, and in the case of runoff monitoring, there is a substantial delay between actual rainfall and registration of runoff in riverbeds. And, of course, when the hydrometric station registers higher runoff than the flash floods is running or even over. From the point of early warning, all these systems reveal disadvantages. Aside from these systems, there is one which provides us with timely information about the spatial and temporal distribution of precipitation intensity over the ground. That is weather radar. We will demonstrate possible usage of these data for dynamic prediction of flash flood risk distribution in space and time over the monitored area. Proper processing of these data in combination with soil saturation indicator established using Flash flood guidance methodology developed by the US Hydrologic Research Center can generate timely information usable for early warning with a substantially reduced level of false warnings.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
—
OECD FORD obor
10508 - Physical geography
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
Dynamics in GIscience: Conference proceedings
ISBN
978-3-319-61296-6
ISSN
1863-2246
e-ISSN
1863-2351
Počet stran výsledku
9
Strana od-do
373-381
Název nakladatele
Springer
Místo vydání
Cham
Místo konání akce
Ostrava
Datum konání akce
22. 3. 2017
Typ akce podle státní příslušnosti
EUR - Evropská akce
Kód UT WoS článku
000457178200027