An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system

Abstract A brief description of the Deterministic Modelling Hydrological System (DMHS) ‘Runoff–Erosion–Pollution’ proposed by the first author is presented. This system is being developed with the aim of giving it a universal character so that it can be applied in mountainous and flat terrain, and i...

Full description

Bibliographic Details
Published in:Hydrological Processes
Main Authors: Vinogradov, Yu. B., Semenova, O. M., Vinogradova, T. A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2010
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.7901
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.7901
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.7901
id crwiley:10.1002/hyp.7901
record_format openpolar
spelling crwiley:10.1002/hyp.7901 2024-09-09T19:51:06+00:00 An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system Vinogradov, Yu. B. Semenova, O. M. Vinogradova, T. A. 2010 http://dx.doi.org/10.1002/hyp.7901 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.7901 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.7901 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 25, issue 7, page 1055-1073 ISSN 0885-6087 1099-1085 journal-article 2010 crwiley https://doi.org/10.1002/hyp.7901 2024-07-30T04:17:46Z Abstract A brief description of the Deterministic Modelling Hydrological System (DMHS) ‘Runoff–Erosion–Pollution’ proposed by the first author is presented. This system is being developed with the aim of giving it a universal character so that it can be applied in mountainous and flat terrain, and in basins of different natural climatic zones regardless of their size. The main feature of the model is its independence of the scaling problem. The basis of our approach consists of a simple theory of runoff elements. This is different from the generally accepted use of partial differential equations such as the Saint Venant equation for surface and channel flow and the Boussinesq equation for underground waters describing the water movement from runoff formation origins to the basin outlet. The results of runoff simulation for six mountainous watersheds of different sizes across Eastern Siberia within the Lena River basin and their statistical evaluation are presented. The selected river basins ranged in size from about 40 km 2 (small scale) to the entire Lena River basin (2·4 million km 2 ), classified as a large‐scale basin. Copyright © 2010 John Wiley & Sons, Ltd. Article in Journal/Newspaper lena river Siberia Wiley Online Library Hydrological Processes 25 7 1055 1073
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract A brief description of the Deterministic Modelling Hydrological System (DMHS) ‘Runoff–Erosion–Pollution’ proposed by the first author is presented. This system is being developed with the aim of giving it a universal character so that it can be applied in mountainous and flat terrain, and in basins of different natural climatic zones regardless of their size. The main feature of the model is its independence of the scaling problem. The basis of our approach consists of a simple theory of runoff elements. This is different from the generally accepted use of partial differential equations such as the Saint Venant equation for surface and channel flow and the Boussinesq equation for underground waters describing the water movement from runoff formation origins to the basin outlet. The results of runoff simulation for six mountainous watersheds of different sizes across Eastern Siberia within the Lena River basin and their statistical evaluation are presented. The selected river basins ranged in size from about 40 km 2 (small scale) to the entire Lena River basin (2·4 million km 2 ), classified as a large‐scale basin. Copyright © 2010 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Vinogradov, Yu. B.
Semenova, O. M.
Vinogradova, T. A.
spellingShingle Vinogradov, Yu. B.
Semenova, O. M.
Vinogradova, T. A.
An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
author_facet Vinogradov, Yu. B.
Semenova, O. M.
Vinogradova, T. A.
author_sort Vinogradov, Yu. B.
title An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
title_short An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
title_full An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
title_fullStr An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
title_full_unstemmed An approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
title_sort approach to the scaling problem in hydrological modelling: the deterministic modelling hydrological system
publisher Wiley
publishDate 2010
url http://dx.doi.org/10.1002/hyp.7901
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.7901
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.7901
genre lena river
Siberia
genre_facet lena river
Siberia
op_source Hydrological Processes
volume 25, issue 7, page 1055-1073
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.7901
container_title Hydrological Processes
container_volume 25
container_issue 7
container_start_page 1055
op_container_end_page 1073
_version_ 1809920417016578048