Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China

During winter the Yellow River in China is frequently subjected to ice flood disasters. Possible dike breaking due to ice floods poses a serious threat to the part of the region located along the river, in particular the Ning–Meng reach (including Ningxia Hui and the Inner Mongolia autonomous region...

Full description

Bibliographic Details
Main Authors: C. Fu, I. Popescu, C. Wang, A. E. Mynett, F. Zhang
Format: Article
Language:English
Published: Copernicus Publications 2014-03-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/18/1225/2014/hess-18-1225-2014.pdf
id doaj-5ceeee59fe9742eb8245cab49768a937
record_format Article
spelling doaj-5ceeee59fe9742eb8245cab49768a9372020-11-24T21:32:25ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382014-03-011831225123710.5194/hess-18-1225-2014Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, ChinaC. Fu0I. Popescu1C. Wang2A. E. Mynett3F. Zhang4NARI Group Corporation, water conservancy and hydropower technology branch company, Nanjing 211000, ChinaUNESCO-IHE, Institute for Water Education, 2601DA, Delft, the NetherlandsUNESCO-IHE, Institute for Water Education, 2601DA, Delft, the NetherlandsUNESCO-IHE, Institute for Water Education, 2601DA, Delft, the NetherlandsYellow River Institute of Hydraulic Research, Zhengzhou 450003, ChinaDuring winter the Yellow River in China is frequently subjected to ice flood disasters. Possible dike breaking due to ice floods poses a serious threat to the part of the region located along the river, in particular the Ning–Meng reach (including Ningxia Hui and the Inner Mongolia autonomous regions). Due to its special geographical location and river flow direction, the ice dams and jams lead to dike breaking and overtopping on the embankment, which has resulted in huge casualties and property losses throughout history. Therefore, there is a growing need to develop capability in forecasting and analysing river ice floods. Research into ice floods along the river is taking place at the Yellow River Conservancy Commission (YRCC). A numerical model is one of the essential parts of the current research going on at the YRCC, which can be used to supplement the inadequacies in the field and lab studies which are being carried out to help understand the physical processes of river ice on the Yellow River. Based on the available data about the Ning–Meng reach of the Yellow River, the YRCC river ice dynamic model (YRIDM) has been tested for capabilities to conduct ice flood forecasting. The YRIDM can be applied to simulate water level, discharge, water temperature, and ice cover thickness under unsteady-state conditions. Different scenarios were designed to explore the model uncertainty for two bounds (5 and 95%) and probability distribution. The YRIDM is an unsteady-state flow model that can show the basic regular pattern of ice floods; hence it can be used as an important tool to support decision making. The recommendation is that data and research should be continued in order to support the model and to measure improvements.http://www.hydrol-earth-syst-sci.net/18/1225/2014/hess-18-1225-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Fu
I. Popescu
C. Wang
A. E. Mynett
F. Zhang
spellingShingle C. Fu
I. Popescu
C. Wang
A. E. Mynett
F. Zhang
Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China
Hydrology and Earth System Sciences
author_facet C. Fu
I. Popescu
C. Wang
A. E. Mynett
F. Zhang
author_sort C. Fu
title Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China
title_short Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China
title_full Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China
title_fullStr Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China
title_full_unstemmed Challenges in modelling river flow and ice regime on the Ningxia–Inner Mongolia reach of the Yellow River, China
title_sort challenges in modelling river flow and ice regime on the ningxia–inner mongolia reach of the yellow river, china
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2014-03-01
description During winter the Yellow River in China is frequently subjected to ice flood disasters. Possible dike breaking due to ice floods poses a serious threat to the part of the region located along the river, in particular the Ning–Meng reach (including Ningxia Hui and the Inner Mongolia autonomous regions). Due to its special geographical location and river flow direction, the ice dams and jams lead to dike breaking and overtopping on the embankment, which has resulted in huge casualties and property losses throughout history. Therefore, there is a growing need to develop capability in forecasting and analysing river ice floods. Research into ice floods along the river is taking place at the Yellow River Conservancy Commission (YRCC). A numerical model is one of the essential parts of the current research going on at the YRCC, which can be used to supplement the inadequacies in the field and lab studies which are being carried out to help understand the physical processes of river ice on the Yellow River. Based on the available data about the Ning–Meng reach of the Yellow River, the YRCC river ice dynamic model (YRIDM) has been tested for capabilities to conduct ice flood forecasting. The YRIDM can be applied to simulate water level, discharge, water temperature, and ice cover thickness under unsteady-state conditions. Different scenarios were designed to explore the model uncertainty for two bounds (5 and 95%) and probability distribution. The YRIDM is an unsteady-state flow model that can show the basic regular pattern of ice floods; hence it can be used as an important tool to support decision making. The recommendation is that data and research should be continued in order to support the model and to measure improvements.
url http://www.hydrol-earth-syst-sci.net/18/1225/2014/hess-18-1225-2014.pdf
work_keys_str_mv AT cfu challengesinmodellingriverflowandiceregimeontheningxiainnermongoliareachoftheyellowriverchina
AT ipopescu challengesinmodellingriverflowandiceregimeontheningxiainnermongoliareachoftheyellowriverchina
AT cwang challengesinmodellingriverflowandiceregimeontheningxiainnermongoliareachoftheyellowriverchina
AT aemynett challengesinmodellingriverflowandiceregimeontheningxiainnermongoliareachoftheyellowriverchina
AT fzhang challengesinmodellingriverflowandiceregimeontheningxiainnermongoliareachoftheyellowriverchina
_version_ 1725957752369446912