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Čeština (Czech)
The research project of the Technology Agency of the Czech Republic SS02030027 „Water systems and water management in the Czech Republic in conditions of climate change“, whose guarantor is the Ministry of the Environment, tries to answer the question of whether we will continue to have enough quality water. Climate change and the associated drought, as well as human behaviour and demands threaten water, and solutions must be sought for the immediate future.
BILAN je celistvý konceptuální model v denní/měsíční struktuře (schéma je uvedeno na obr. 1), simulující složky hydrologické bilance na povodí. Přestože jeho vývoj byl nastartován ve VÚV TGM již počátkem devadesátých let minulého století, jde o model, který je v České republice stále standardně používán a zůstává přístupný laické i odborné veřejnosti. Například je nedílnou součástí řešení aplikace/systému HAMR [1], ale byl použit i jinde [2–4]. Mezi hlavní výhody modelu oproti jiným řešením patří interní kalibrační algoritmy, možnost přímého vkládání dat o užívání vod a nízká výpočetní náročnost vhodná pro variantní simulování (např. dopadů klimatické změny na vodní režim).
The Výrovka river basin, as a compact area covering 542.5 km2, is very suitable for monitoring hydrological characteristics and comparing them in different landscape types. It is located on the border of the Lower Vltava and Upper and Middle Elbe sub-basins, extending in a range of 175–555 m above sea level, with a total of six landscape types according to the typology of the contemporary landscape of the Czech Republic. Simultane-ously, there is a varied mosaic in terms of geological subsoil and soil types. There have also been major changes in land use in this basin, mainly due to intensive agricultural activity and related watercourse modifications and amelioration. Monitoring activities within the project SS02030027 ”Water systems and water management in the Czech Republic in conditions of climate change” are currently taking place in the Výrovka river basin.
According to the Czech technical standard ČSN 75 1400 Hydrological data of surface waters, M-day discharges are a part of the Basic hydrological data [1]. The values of M-day discharges in water gauging stations are derived from time series of observed mean daily discharges over a defined reference period. The reference period 1981–2010 is currently used for design purposes [2]. With the end of the second decade of the 21st century, a change in the reference period for 1991–2020 is being considered. In the past, the Czech Hydrometeorological Institute (CHMI) provided hydrological data for the reference periods 1931–1940, 1931–1960, and 1931–1980.
Since December 2012, during every winter season, the altitude of the zero isochion (snowline) has been determined at the Czech Hydrometeorological Institute for the purposes of operational hydrology. The reason is the estimation of the amount of water stored in snow cover, which is inevitable activity for Czech hydrologists who naturally want their forecasting models to give relevant results. In order to get a better idea about current spatial distribution of snow cover in Czechia, the information on the zero isochion has been extracted from the MODIS imagery coming from the Terra satellite.
GIS technologies are widely used in the Hydrology Department of the Czech Hydrometeorological Institute (CHMI). The processing of geospatial data, which are used in hydrology for analytical tasks, and the development of GIS technologies in the last two decades have contributed to the spread of GIS in the CHMI practice. The use of GIS tools is shown in four examples. The first one focuses on the creation of GIS data. The second example concerns the preparation of input source data for the derivation of the hydrological characteristics of M-day discharge, which, according to Czech Standard 75 1400 Surface water hydrological data, are among the basic hydrological data. The third example describes the use of GIS in the preparation of hydrological assessments according to the above-mentioned standard (75 1400), which usually result in M-day or N-year-flood discharges in a specified profile of a certain watercourse. The fourth example focuses on the use of GIS in operational hydrological service, specifically in the development of the Flash Flood Indicator, which determines the level of risk of flash flood formation or occurrence based on current land saturation and radar rainfall estimates.
The International Commission on Remote Sensing (ICRS), as one of the current ten scientific commissions under the umbrella of the International Association of Hydrological Sciences (IAHS; [1]), has emerged as a logical response to the availability of spatial data associated with the launch of the first satellites in the 1970s that were designed to observe the Earth’s landscape sphere from space, providing a completely new perspective in which the spatial extent of the territory under observation played the major role.
This article is available in Czech only. For translation or more information on this topic, please contact author. Souhrn V poslední době se velmi diskutuje – a to nejen mezi odbornou veřejností – o dopadech změny klimatu na vodní režim v přírodní krajině. Řešení OP Praha – pól růstu se zaměřilo i na krajinu… Read more »
