Wyniki wyszukiwania - AGRO

1

Conceptual model for rainfall-runoff computation

100%

Ignar S., Chormanski J., Warmerdam P. M. M.

Annals of Warsaw Agricultural University. Land Reclamation

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2000

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tom 30

67-76

2

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Basement of the alluvia influence on the channel pattern in example of selected reach of the Pilica River

100%

Falkowski T.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2010

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tom 42

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nr 1

93-104

The type of the channel pattern is being considered as indicative element of the fluvial environment, especially for lowland, mature rivers. Investigations carried out in the Pilica River valley (example of such river) between Inowłódz and Domaniewice (grant no 2P04E 069 29, Ministry of Science) have shown that morphological features of the valley bottom (channel zone, as well as flood terrace) depends not only on river regime, but also on channel zone geological setting. Elements of the Pilica valley geology infl uencing on fluvial processes are protrusions of alluvia basement composed of deposits resistant to erosion, crop out in the channel zone.

3

Statistical methods for trend investigation in hydrological non-seasonal series

100%

Rutkowska A.

Acta Scientiarum Polonorum. Formatio Circumiectus

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2013

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tom 12

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nr 4

In the paper some methods for identification of the monotonic deterministic trend in hydrological time series were presented and discussed: the t-test, the Mann-Kendall test with corrections, the Theil-Sen estimator with the test based on bootstrap and the prewhitening method. The tests varied in assumptions on the existence of the serial correlation and the distribution of the variables in the series. Occasionally, when assumptions were not fulfilled, the tests led to contradictory conclusions. As examples, the applications to annual maximum and minimum flows were presented.

4

A modeling framework to assess the impact of climate change on a river runoff

100%

Kuchar L., Iwanski S., Jelonek L., Szalinska W.

Meteorology Hydrology and Water Management. Research and Operational Applications

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2014

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tom 02

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nr 2

Global climate change is anticipated to have consequences on water resources and the envi-ronment both at global and local/regional levels. Efforts towards proper management of future water resources and resolving potential water-related conflicts require the formulation of appropriate techniques to downscale the output of global climate models (GCM) to local conditions for hydrologic prediction. The paper presents an integrated framework for modeling the impact of climate change on river runoff that combines methodology for downscaling climate change scenarios for a basin scale with a hydrological model to estimate the impact of climate change on a river runoff. The modeling framework uses long-term observations of meteorological and hydrological variables together with a climate change scenario to provide a projection of future flows for the specified time horizon. The framework is based on a spatial weather generator and a distributed rainfall-runoff model. Such a configuration enables a reflection of the uncertainty of future conditions by running multiple realizations of future conditions, and also take into account the spatial variability of hydrological properties in the catchment by maintaining the physical details at a given grid size. The performance of the framework was presented for the Kaczawa basin that is one of the main left bank tributaries of the Odra River – the second biggest river in Poland. The results show simulated changes of the future river flow regime caused by climatic changes for two time horizons: 2040 and 2080.

5

HydroProg: a system for hydrological forecasting in real time, based on the multimodelling approach

100%

Niedzielski T., Mizinski B., Kryza M., Netzel P., Wieczorek M., Kasprzak M., Migon P., Szymanowski M., Jeziorska J., Witek M., Kosek W.

Meteorology Hydrology and Water Management. Research and Operational Applications

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2014

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tom 02

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nr 2

The objective of this paper is to present the concept of a novel system, known as HydroProg, that aims to issue flood warnings in real time on the basis of numerous hydrological predictions computed using various models. The core infrastructure of the system is hosted by the University of Wrocław, Poland. A newly-established computational centre provides in real time, courtesy of the project Partners, various modelling groups, referred to as “project Participants”, with hydrometeorological data. The project Participants, having downloaded the most recent observations, are requested to run their hydrologic models on their machines and to provide the HydroProg system with the most up-to-date prediction of riverflow. The system gathers individual forecasts derived by the Participants and processes them in order to compute the ensemble prediction based on multiple models, following the approach known as multimodelling. The system is implemented in R and, in order to attain the above-mentioned functionality, is equipped with numerous scripts that manipulate PostgreSQL- and MySQL-managed databases and control the data quality as well as the data processing flow. As a result, the Participants are provided with multivariate hydrometeorological time series with sparse outliers and without missing values, and they may use these data to run their models. The first strategic project Partner is the County Office in Kłodzko, Poland, owner of the Local System for Flood Monitoring in Kłodzko County. The experimental implementation of the HydroProg system in the Nysa Kłodzka river basin has been completed, and six hydrologic models are run by scientists or research groups from the University of Wrocław, Poland, who act as Participants. Herein, we shows a single prediction exercise which serves as an example of the HydroProg performance.

6

Seasonal dynamics of sediment in the Ciemiega River

100%

Debicki R., Glinski P., Kuczynski A.

Zeszyty Problemowe Postępów Nauk Rolniczych

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1996

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tom 436

Dynamics of sediment amount in the Ciemiega river water during three months of the 1996 vegetative period and its comparison with similar data from 1975 are discussed in this paper. A spectrophotometric method was used to determine water turbidity as a measure of sediment concentration in water.

7

Regional climate scenarios and their applications

100%

Liszewska M., Osuch M.

Geographia Polonica

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1998

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tom 71

8

The hydrological regime of rivers in the light of scenarios of global climatic change

100%

Gutry-Korycka M., Rotnicka J.

Geographia Polonica

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1998

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tom 71

9

Characteristics of the selected hydrological parameters of the Gulf of Gdansk in the planned area of sewage discharge from the Gdansk-Wschod sewage-treatment plant

100%

Nowacki J., Matciak M.

Oceanological Studies

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2000

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tom 29

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nr 4

10

Poland's water resources in the face of climatic change

100%

Kaczmarek Z.

Geographia Polonica

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1998

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tom 71

11

Cluster analysis in determination of hydrologically homogeneous regions with low flow

86%

Cupak A., Walega A., Michalec B.

Acta Scientiarum Polonorum. Formatio Circumiectus

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2017

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tom 16

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nr 1

12

Comparison of three urban catchments in Uppsala - patterns of stormwater runoff

86%

Renman G.

Annals of Warsaw Agricultural University. Land Reclamation

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2001

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tom 31

87-94

13

An ecohydrology approach to the Danube River, and the “enviroGRIDS” project

86%

Jelev I., Jelev V.

International Journal of Ecohydrology and Hydrobiology

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2012

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tom 12

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nr 2

14

Hydric potential of selected river basins in Slovakia

86%

Lepeska T.

International Journal of Ecohydrology and Hydrobiology

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2013

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tom 13

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nr 3

15

Qualifying the geotechnical and hydrological characteristic of the Bandawaya stream valley - Northern Iraq

86%

Al-Jawadi A. S., Abdul Baqi Y. T., Sulaiman A. M.

Przegląd Naukowy. Inżynieria i Kształtowanie Środowiska

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2020

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tom 29

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nr 3[89]

16

Flood management in Azerbaijan

86%

Hasanova N., Imanov F.

Infrastruktura i Ekologia Terenów Wiejskich

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2010

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nr 11

This report examines the issues of hydrological basis and methods of flood management in the rivers of Azerbaijan and presents a review of methods of flood management applied in Azerbaijan.

17

Water balances in the smaller drainage areas of the Tywa River basin (1961-1990)

86%

Jezierski G., Zygas M., Zajner Z., Zych N.

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

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1999

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tom 03

18

Dominant discharge - an outline of theory and a case study from the Raba River

86%

Czech W., Plesinski K., Radecki-Pawlik A., Radecki-Pawlik B.

Acta Scientiarum Polonorum. Formatio Circumiectus

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2016

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tom 15

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nr 2

19

Sustainable development of the Lower Vistula

86%

Majewski W.

Meteorology Hydrology and Water Management. Research and Operational Applications

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2013

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tom 01

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nr 1

The Vistula is the Poland’s largest River. It flows from the south to the north and has its mouth in the Baltic Sea. Hydrographically the Vistula is divided into three sections: the Upper Vistula from the source to San tributary; the Middle Vistula up to the Narew tributary; and the Lower Vistula till the outlet to the sea. The Lower Vistula is 391 km in length. Along it there are several very important urban centers: Gdańsk with its harbor and container terminal, Elbląg with its harbor situated on the Vistula Lagoon, Tczew, Grudziądz, Włocławek, Płock and Warsaw, the capital of Poland. The Lower Vistula establishes part of the International Waterway E70 and E40 as it has important economic value and development potential. The Lower Vistula has important hydroenergy potential, is the source of water supply for people, industry and agriculture as well as being a very important ecological corridor. The whole length of the Lower Vistula, except for Włocławek Reservoir is included in the NATURA 2000 Program. The Włocławek hydraulic project lies along this section. It was commissioned in 1970 and has been the source of significant debate discussion between ecologists and water resources specialists. The Lower Vistula also benefits from scenic countryside and is popular for tourism and recreation. Along the Lower Vistula, a very important problem still exists in the form of flood hazard, mainly caused by ice phenomena and is also endangered by droughts. The paper begins with a short discussion about sustainable development. It then presents the current state of the management of the Lower Vistula and its catchment, its economic potential and plans for development. Possibilities regarding the construction of future hydraulic projects are also discussed, including the benefits for energy production, navigation, water supply, tourism and recreation.

20

Response of riverine ecosystem after a flood event in the Smortawa valley

86%

Adynkiewicz-Piragas M., Krzeminska A.

Journal of Water and Land Development

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2004

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nr 08

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