Categorization of small catchments for modeling the precipitation response

Author(s):  
Petr Kavka ◽  
Luděk Strouhal ◽  
Romana Kubínová ◽  
Marek Kaspar

<p>It this contribution partial results of the project, which is focused on hydrological modelling as a tool for designing small water management construction and soil conservation measure and in the landscape are presented. For the hydrological response, design rainfall and the initial condition, the current state of the river basin as well as the characteristics of the area under consideration are important. For the hydrological response, design rainfall, the current conditions of the catchment area as well as the characteristics of the solved area are important. </p><p>Design precipitation in relation to initial conditions (soil moisture and surface condition) is one of the project goals. This data are important for hydrological modelling that is a tool for designing water management measures on small watercourses and in river basin areas is relevant for catchment size where long-term measurements and possible analogy cannot be used. The design of small hydrotechnical buildings based on hydrological modelling is used for catchments up to the area of ​​5 km2.</p><p>Basic categorization of small catchments in the Czech Republic is presented. At present, the Czech catchments are categorized into four levels. From the main river catchment to the catchment of the category IV. order (small catchments). There are considerable differences in size in the fourth category. From catchment areas of over 20 km2 to supplementary catchment areas of less than 1 km2. The categorization of these catchments in terms of their potential hydrological response is described in the past. For the categorization of the territory of the Czech Republic at the level of small catchment areas in terms of hydrological response, the different size of the area is one of the hardly definable parameters.</p><p>For these reasons, the project addresses also the delimitation of small catchments in the Czech Republic, which fall into the category of areas up to 5 km2 and significant areas outside the watercourse and their subsequent classification in terms of possible hydrological response. The activities were in this ongoing project focused on delimitation of these catchments and research of suitable data for their classification.</p><p>Detailed model of terrain in the resolution 5x5 m and watercourse layer were used as input data for delimitation of small catchments. ArcGIS tools and Python scripting language were used for processing. As it is a relatively large data set, the following analyses were gradually repeated for the catchment III. order with the extension of the boundary, so as to ensure possible discrepancies between the delimitation of the basin and the distribution boards defined on the basis of a detailed terrain model.</p><p>Nine categories were selected as significant areas ranging from contributing areas of 0,3 to 5,5 km2. In the category of the smallest catchments (categories from 0,3 to 0,7 km2) there are over 70 thousand areas defined in the Czech Republic. In the category from 4,5 to 5,5 km2 there are over 4 thousand catchments. A categorization both for individual classes and overall for the territory of the Czech Republic according to the largest contributing area is presented.</p>

2012 ◽  
Vol 50 (No. 11) ◽  
pp. 538-541
Author(s):  
M. Bíba ◽  
J. Jiřík ◽  
K. Vančura

A short introduction of historical overview and current situation refer to forestry problems of the country. Local climate is characterized and impacts of natural phenomena are described, as well as the impacts of human beings. The influence of forest management is mentioned and discussed in relation to latest catastrophic floods. The territory of the Czech Republic is damaged especially by a high intensity of atmospheric precipitation abnormal values which lead to a local or regional damage. In the catchment areas of torrents, damage leads to faster soil erosion, development of ravines, landslides, moving of soil sediments and their deposition, devastation of watercourse beds and properties, flooding while the flooding rates of flow represent a danger for the life of inhabitants. Important elements and results of respective research are described in brief. E.g. research of precipitation and its relation to the runoffs in the small mountain catchment areas with the forest stands restoration, as well as the forestry-hydrologic monitoring of forest environment, which has been taking place since 1928, and tradition of the service for torrent control. Forestry-hydrologic research gradually documents that a favorable flood-control performance of forest is limited. However, this is not a reason for not taking care of flood-control measures in the mountain afforested areas. These measures and importance of forest for the protection of land are historically verified and justified. In closing the mankind behavior to the landscape is underlined as a question mark.


2006 ◽  
Vol 5 ◽  
pp. 14-17
Author(s):  
Luboš Beran

Vertigo moulinsiana (Dupuy, 1849) was found in 2003–2005 in Northern Bohemia (Czech Republic) at 11 sites. All these sites are situated on floodplains of smaller streams in a sandstone area. The known occurrence of this endangered relict in the Czech Republic is concentrated in three areas – a large area of Bohemian Cretaceous Basin, a floodplain near villages Břežany and Božice (Dyje River Basin) in Southern Moravia and small, isolated, treeless fens in the White Carpathians (Bílé Karpaty Mts.). The principal habitats where V. moulinsiana lives in the Czech Republic are sedge marshes, Typha swamps, reed swamps (with Carex spp.), alder carrs (also with Carex spp.) and tufa-forming spring fens.


Geografie ◽  
2005 ◽  
Vol 110 (1) ◽  
pp. 32-45
Author(s):  
Zdeněk Kliment ◽  
Milada Matoušková

Recent floods in the Czech Republic raised many questions about a possible man-made impact on the outflow process. The contribution evaluates runoff changes in the Otava River basin. Attention is paid to the methodology, which is based mainly on the use of mass curves of rainfall and runoff characteristics. Results of analysis are discussed and compared with climatic factors and human activities.


2013 ◽  
Vol 1 (3) ◽  
pp. 307-322 ◽  
Author(s):  
Piotr Kowalczak ◽  
Piotr Matczak ◽  
Lenka Slavikova

1999 ◽  
Vol 30 (4) ◽  
pp. 476-481 ◽  
Author(s):  
Zdenek Kos ◽  
Eva Prenosilova

Geografie ◽  
2003 ◽  
Vol 108 (1) ◽  
pp. 1-13
Author(s):  
Jaromír Kolejka

The flood damages caused recently in the Czech Republic require additional measures both on rivers and in catchment areas. Cities and towns are especially interested in the protection because of their high vulnerability. Ecological (land use) and technical (reservoirs) measures are being planned in catchments to keep water in the landscape safe. The flood plain segmentation into sectors with different protective values and move of technical measures from rivers close to valuable objects and areas represent the vision of flood control downstream the rivers.


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