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Using jointly calibrated fine-scale drain models across Denmark to assess the influence of physical variables on spatial drain flow patterns

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Using jointly calibrated fine-scale drain models across Denmark to assess the influence of physical variables on spatial drain flow patterns. / Mahmood, Hafsa; Schneider, Raphael; Frederiksen, Rasmus Rumph et al.
I: Journal of Hydrology: Regional Studies, Bind 46, 101353, 04.2023.

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisTidsskriftartikelForskningpeer review

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@article{89b7b329713a4685be81b95cbd9cc6a1,
title = "Using jointly calibrated fine-scale drain models across Denmark to assess the influence of physical variables on spatial drain flow patterns",
abstract = "Study region: Denmark Study focus: Tile drainage, widespread across agricultural areas in Denmark, significantly impacts the hydrological cycle. Tile drain flow dynamics and their spatial patterns are crucial for water managers to address water quality and quantity issues. However, these processes are challenging to simulate accurately. In this study, we developed 10 m resolution drain models in MIKE SHE for 26 drain sites across Denmark to predict drain flow spatial and temporal dynamics. Joint calibration of all drain models was conducted by evaluating PBIAS and KGE of simulated and observed drain flow. Subsequently, we performed a correlation analysis between physical parameters and spatial patterns of simulated drain fraction (DF, ratio of drain flow to recharge per grid cell). New hydrological insights: The jointly calibrated models achieved average PBIAS and KGE of − 6.7% and 0.53 respectively, for drain flow predictions across 26 drain sites. The correlation of DF with topographical variables was highest on a national scale and on most of the drain sites, including Gyldenholm1–4, Norsminde1–11, and other Jylland drain sites. Lilleb{\ae}k drain sites showed a high correlation with average clay content in 0–30 cm layer of soil. Thus, in addition to developing scalable fine-resolution drain models for Denmark, this study also identifies the control parameters for spatial patterns of drain flows across Denmark.",
keywords = "Hydrogeological variables, Shallow groundwater modeling, Subsurface drains, Topographical variables",
author = "Hafsa Mahmood and Raphael Schneider and Frederiksen, {Rasmus Rumph} and Christiansen, {Anders Vest} and Simon Stisen",
year = "2023",
month = apr,
doi = "10.1016/j.ejrh.2023.101353",
language = "English",
volume = "46",
journal = "Journal of Hydrology: Regional Studies",
issn = "2214-5818",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Using jointly calibrated fine-scale drain models across Denmark to assess the influence of physical variables on spatial drain flow patterns

AU - Mahmood, Hafsa

AU - Schneider, Raphael

AU - Frederiksen, Rasmus Rumph

AU - Christiansen, Anders Vest

AU - Stisen, Simon

PY - 2023/4

Y1 - 2023/4

N2 - Study region: Denmark Study focus: Tile drainage, widespread across agricultural areas in Denmark, significantly impacts the hydrological cycle. Tile drain flow dynamics and their spatial patterns are crucial for water managers to address water quality and quantity issues. However, these processes are challenging to simulate accurately. In this study, we developed 10 m resolution drain models in MIKE SHE for 26 drain sites across Denmark to predict drain flow spatial and temporal dynamics. Joint calibration of all drain models was conducted by evaluating PBIAS and KGE of simulated and observed drain flow. Subsequently, we performed a correlation analysis between physical parameters and spatial patterns of simulated drain fraction (DF, ratio of drain flow to recharge per grid cell). New hydrological insights: The jointly calibrated models achieved average PBIAS and KGE of − 6.7% and 0.53 respectively, for drain flow predictions across 26 drain sites. The correlation of DF with topographical variables was highest on a national scale and on most of the drain sites, including Gyldenholm1–4, Norsminde1–11, and other Jylland drain sites. Lillebæk drain sites showed a high correlation with average clay content in 0–30 cm layer of soil. Thus, in addition to developing scalable fine-resolution drain models for Denmark, this study also identifies the control parameters for spatial patterns of drain flows across Denmark.

AB - Study region: Denmark Study focus: Tile drainage, widespread across agricultural areas in Denmark, significantly impacts the hydrological cycle. Tile drain flow dynamics and their spatial patterns are crucial for water managers to address water quality and quantity issues. However, these processes are challenging to simulate accurately. In this study, we developed 10 m resolution drain models in MIKE SHE for 26 drain sites across Denmark to predict drain flow spatial and temporal dynamics. Joint calibration of all drain models was conducted by evaluating PBIAS and KGE of simulated and observed drain flow. Subsequently, we performed a correlation analysis between physical parameters and spatial patterns of simulated drain fraction (DF, ratio of drain flow to recharge per grid cell). New hydrological insights: The jointly calibrated models achieved average PBIAS and KGE of − 6.7% and 0.53 respectively, for drain flow predictions across 26 drain sites. The correlation of DF with topographical variables was highest on a national scale and on most of the drain sites, including Gyldenholm1–4, Norsminde1–11, and other Jylland drain sites. Lillebæk drain sites showed a high correlation with average clay content in 0–30 cm layer of soil. Thus, in addition to developing scalable fine-resolution drain models for Denmark, this study also identifies the control parameters for spatial patterns of drain flows across Denmark.

KW - Hydrogeological variables

KW - Shallow groundwater modeling

KW - Subsurface drains

KW - Topographical variables

U2 - 10.1016/j.ejrh.2023.101353

DO - 10.1016/j.ejrh.2023.101353

M3 - Journal article

VL - 46

JO - Journal of Hydrology: Regional Studies

JF - Journal of Hydrology: Regional Studies

SN - 2214-5818

M1 - 101353

ER -