A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer

A flow regime is influenced by the degree of hydrologic connection between surface water and groundwater. As this connection becomes more transient and the basin’s runoff response more non-linear, such as for intermittent streams, the need for explicit representation of the groundwater component inc...
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Autor*in:	Iolanda Borzì [verfasserIn] Brunella Bonaccorso [verfasserIn] Aldo Fiori [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	hydrologic response groundwater-fed basin ihacres rainfall-runoff model

Übergeordnetes Werk:	In: Water - MDPI AG, 2010, 11(2019), 10, p 2031
Übergeordnetes Werk:	volume:11 ; year:2019 ; number:10, p 2031

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/w11102031

Katalog-ID:	DOAJ011887451

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language	English
source	In Water 11(2019), 10, p 2031 volume:11 year:2019 number:10, p 2031
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topic_facet	hydrologic response groundwater-fed basin ihacres rainfall-runoff model Hydraulic engineering Water supply for domestic and industrial purposes
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authorswithroles_txt_mv	Iolanda Borzì @@aut@@ Brunella Bonaccorso @@aut@@ Aldo Fiori @@aut@@
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callnumber-first	T - Technology
author	Iolanda Borzì
spellingShingle	Iolanda Borzì misc TC1-978 misc TD201-500 misc hydrologic response misc groundwater-fed basin misc ihacres rainfall-runoff model misc Hydraulic engineering misc Water supply for domestic and industrial purposes A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer
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topic_title	TC1-978 TD201-500 A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer hydrologic response groundwater-fed basin ihacres rainfall-runoff model
topic	misc TC1-978 misc TD201-500 misc hydrologic response misc groundwater-fed basin misc ihacres rainfall-runoff model misc Hydraulic engineering misc Water supply for domestic and industrial purposes
topic_unstemmed	misc TC1-978 misc TD201-500 misc hydrologic response misc groundwater-fed basin misc ihacres rainfall-runoff model misc Hydraulic engineering misc Water supply for domestic and industrial purposes
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title	A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer
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title_full	A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer
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author_browse	Iolanda Borzì Brunella Bonaccorso Aldo Fiori
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title_sort	modified ihacres rainfall-runoff model for predicting the hydrologic response of a river basin connected with a deep groundwater aquifer
callnumber	TC1-978
title_auth	A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer
abstract	A flow regime is influenced by the degree of hydrologic connection between surface water and groundwater. As this connection becomes more transient and the basin’s runoff response more non-linear, such as for intermittent streams, the need for explicit representation of the groundwater component increases. The present study investigates the connection between Northern Etna groundwater system and the Alcantara river basin in Sicily (Italy). In particular, the upstream part of the basin, whose flow regime is essentially intermittent, is modeled through a modified version of the IHACRES rainfall-runoff model. The structure of the model includes a routing module formulated as a two-store model, with the upper store simulating the quick component of the runoff and recharging the lower store which, in turn, describes the slow component of the runoff and the groundwater extraction and losses. Both stores are conceptualized as simple linear reservoirs, with the lower one that maintains a continuous water balance account of groundwater storage volumes for the upstream basin area with respect to a control cross-section, assumed to be the stream gauging station. The model is calibrated at Moio Alcantara cross-section, where daily streamflow data are available. Model calibration and validation are carried out for the period 1980−1984 and 1986−1988, respectively. A first-order analysis is also performed to assess the sensitivity of model parameters. The adopted configuration is shown to improve model performance with respect to the original IHACRES model, with the proposed formulation able to better capture the interactions between the aquifer and the river.
abstractGer	A flow regime is influenced by the degree of hydrologic connection between surface water and groundwater. As this connection becomes more transient and the basin’s runoff response more non-linear, such as for intermittent streams, the need for explicit representation of the groundwater component increases. The present study investigates the connection between Northern Etna groundwater system and the Alcantara river basin in Sicily (Italy). In particular, the upstream part of the basin, whose flow regime is essentially intermittent, is modeled through a modified version of the IHACRES rainfall-runoff model. The structure of the model includes a routing module formulated as a two-store model, with the upper store simulating the quick component of the runoff and recharging the lower store which, in turn, describes the slow component of the runoff and the groundwater extraction and losses. Both stores are conceptualized as simple linear reservoirs, with the lower one that maintains a continuous water balance account of groundwater storage volumes for the upstream basin area with respect to a control cross-section, assumed to be the stream gauging station. The model is calibrated at Moio Alcantara cross-section, where daily streamflow data are available. Model calibration and validation are carried out for the period 1980−1984 and 1986−1988, respectively. A first-order analysis is also performed to assess the sensitivity of model parameters. The adopted configuration is shown to improve model performance with respect to the original IHACRES model, with the proposed formulation able to better capture the interactions between the aquifer and the river.
abstract_unstemmed	A flow regime is influenced by the degree of hydrologic connection between surface water and groundwater. As this connection becomes more transient and the basin’s runoff response more non-linear, such as for intermittent streams, the need for explicit representation of the groundwater component increases. The present study investigates the connection between Northern Etna groundwater system and the Alcantara river basin in Sicily (Italy). In particular, the upstream part of the basin, whose flow regime is essentially intermittent, is modeled through a modified version of the IHACRES rainfall-runoff model. The structure of the model includes a routing module formulated as a two-store model, with the upper store simulating the quick component of the runoff and recharging the lower store which, in turn, describes the slow component of the runoff and the groundwater extraction and losses. Both stores are conceptualized as simple linear reservoirs, with the lower one that maintains a continuous water balance account of groundwater storage volumes for the upstream basin area with respect to a control cross-section, assumed to be the stream gauging station. The model is calibrated at Moio Alcantara cross-section, where daily streamflow data are available. Model calibration and validation are carried out for the period 1980−1984 and 1986−1988, respectively. A first-order analysis is also performed to assess the sensitivity of model parameters. The adopted configuration is shown to improve model performance with respect to the original IHACRES model, with the proposed formulation able to better capture the interactions between the aquifer and the river.
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container_issue	10, p 2031
title_short	A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer
url	https://doi.org/10.3390/w11102031 https://doaj.org/article/cb8db57bcc58467195278a23505fb827 https://www.mdpi.com/2073-4441/11/10/2031 https://doaj.org/toc/2073-4441
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author2	Brunella Bonaccorso Aldo Fiori
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A Modified IHACRES Rainfall-Runoff Model for Predicting the Hydrologic Response of a River Basin Connected with a Deep Groundwater Aquifer

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