Fluctuations of floods of the River Morava (Czech Republic) in the 1691- 2009 period: interactions of natural and anthropogenic factors

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00027073%3A_____%2F11%3A%230001120" target="_blank" >RIV/00027073:_____/11:#0001120 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/11:00049428 RIV/00020699:_____/11:#0000545

Výsledek na webu

<a href="http://dx.doi.org/10.1080/02626667.2011.564175" target="_blank" >http://dx.doi.org/10.1080/02626667.2011.564175</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1080/02626667.2011.564175" target="_blank" >10.1080/02626667.2011.564175</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Fluctuations of floods of the River Morava (Czech Republic) in the 1691- 2009 period: interactions of natural and anthropogenic factors

Popis výsledku v původním jazyce

Floods from the middle part of the River Morava are considered over the course of the past three centuries, the study being based on data derived from documentary evidence (1691?1880), measured peak water stages (1881?1920) and peak discharges (1916?2009), evaluated with respect to their N-year return period. Changes in land use and water management are discussed, as are factors influencing runoff conditions in the Morava catchment. Decadal synthesis of flood series identifies the highest flood activityin the decades of 1911?1920 and 1961?1970 (11 floods each), 1831?1840, 1891?1900, 1901?1910 and 1931?1940 (10). Uncertainty in this series is related to some incompleteness of documentary data in the pre-1881 period. Very low flood frequency occurred inthe 1990s?2000s, although the most disastrous floods were recorded in this particular period (July 1997 at Q100 and March/April 2006 at Q20?Q50). Changes in flood frequency correspond partly to long-term changes in temperature and precip

Název v anglickém jazyce

Fluctuations of floods of the River Morava (Czech Republic) in the 1691- 2009 period: interactions of natural and anthropogenic factors

Popis výsledku anglicky

Floods from the middle part of the River Morava are considered over the course of the past three centuries, the study being based on data derived from documentary evidence (1691?1880), measured peak water stages (1881?1920) and peak discharges (1916?2009), evaluated with respect to their N-year return period. Changes in land use and water management are discussed, as are factors influencing runoff conditions in the Morava catchment. Decadal synthesis of flood series identifies the highest flood activityin the decades of 1911?1920 and 1961?1970 (11 floods each), 1831?1840, 1891?1900, 1901?1910 and 1931?1940 (10). Uncertainty in this series is related to some incompleteness of documentary data in the pre-1881 period. Very low flood frequency occurred inthe 1990s?2000s, although the most disastrous floods were recorded in this particular period (July 1997 at Q100 and March/April 2006 at Q20?Q50). Changes in flood frequency correspond partly to long-term changes in temperature and precip

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

<a href="/cs/project/IAAX00130801" target="_blank" >IAAX00130801: Vztahy mezi klimatem, antropogenní činností a erozí krajiny zaznamenané v přírodních archívech Strážnického Pomoraví (ČR)</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Hydrological Sciences Journal

ISSN

0262-6667

e-ISSN

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Svazek periodika

56

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

18

Strana od-do

468-485

Kód UT WoS článku

000291263600008

EID výsledku v databázi Scopus

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