Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study

The present study aims at the evaluation of sources of uncertainty in modelling of heat transport in a river caused by the discharge coming from a cooling system of a designed gas-stem power plant. This study was a part of an Environmental Impact Assessment and was based on two-dimensional modelling...

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Main Authors: P. M. Rowiński, M. B. Kalinowska
Format: Article
Language:English
Published: Copernicus Publications 2012-11-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/16/4177/2012/hess-16-4177-2012.pdf
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spelling doaj-ce4ca46e66c745e99eaa02344c954f262020-11-24T22:46:57ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382012-11-0116114177419010.5194/hess-16-4177-2012Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case studyP. M. RowińskiM. B. KalinowskaThe present study aims at the evaluation of sources of uncertainty in modelling of heat transport in a river caused by the discharge coming from a cooling system of a designed gas-stem power plant. This study was a part of an Environmental Impact Assessment and was based on two-dimensional modelling of temperature distribution in an actual river. The problems with the proper description of the computational domain, velocity field and hydraulic characteristics were considered in the work. An in-depth discussion on the methods of evaluation of the dispersion coefficients in the model comprising of all four components of the dispersion tensor was carried out. It was shown that in natural rivers all components of a dispersion tensor should be taken into account to qualitatively reflect the proper shape of temperature distributions. The results considerably depend on the 2-D velocity field as well as hydraulic and morphometric characteristics of the flow. Numerical methods and their influence on the final results of computations were also discussed. All computations were based upon a real case study performed in Vistula River in Poland.http://www.hydrol-earth-syst-sci.net/16/4177/2012/hess-16-4177-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. M. Rowiński
M. B. Kalinowska
spellingShingle P. M. Rowiński
M. B. Kalinowska
Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study
Hydrology and Earth System Sciences
author_facet P. M. Rowiński
M. B. Kalinowska
author_sort P. M. Rowiński
title Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study
title_short Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study
title_full Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study
title_fullStr Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study
title_full_unstemmed Uncertainty in computations of the spread of warm water in a river – lessons from Environmental Impact Assessment case study
title_sort uncertainty in computations of the spread of warm water in a river – lessons from environmental impact assessment case study
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2012-11-01
description The present study aims at the evaluation of sources of uncertainty in modelling of heat transport in a river caused by the discharge coming from a cooling system of a designed gas-stem power plant. This study was a part of an Environmental Impact Assessment and was based on two-dimensional modelling of temperature distribution in an actual river. The problems with the proper description of the computational domain, velocity field and hydraulic characteristics were considered in the work. An in-depth discussion on the methods of evaluation of the dispersion coefficients in the model comprising of all four components of the dispersion tensor was carried out. It was shown that in natural rivers all components of a dispersion tensor should be taken into account to qualitatively reflect the proper shape of temperature distributions. The results considerably depend on the 2-D velocity field as well as hydraulic and morphometric characteristics of the flow. Numerical methods and their influence on the final results of computations were also discussed. All computations were based upon a real case study performed in Vistula River in Poland.
url http://www.hydrol-earth-syst-sci.net/16/4177/2012/hess-16-4177-2012.pdf
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