The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model
Determining an optimal calibration strategy for hydrological models is essential for a robust and accurate water balance assessment, in particular, for catchments with limited observed data. In the present study, the hydrological model Bilan was used to simulate hydrological balance for 20 catchment...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2020-12-01
|
Series: | Water |
Subjects: | |
Online Access: | https://www.mdpi.com/2073-4441/12/12/3401 |
_version_ | 1797545880327290880 |
---|---|
author | Eva Melišová Adam Vizina Linda R. Staponites Martin Hanel |
author_facet | Eva Melišová Adam Vizina Linda R. Staponites Martin Hanel |
author_sort | Eva Melišová |
collection | DOAJ |
description | Determining an optimal calibration strategy for hydrological models is essential for a robust and accurate water balance assessment, in particular, for catchments with limited observed data. In the present study, the hydrological model Bilan was used to simulate hydrological balance for 20 catchments throughout the Czech Republic during the period 1981–2016. Calibration strategies utilizing observed runoff and estimated soil moisture time series were compared with those using only long-term statistics (signatures) of runoff and soil moisture as well as a combination of signatures and time series. Calibration strategies were evaluated considering the goodness-of-fit, the bias in flow duration curve and runoff signatures and uncertainty of the Bilan model. Results indicate that the expert calibration and calibration with observed runoff time series are, in general, preferred. On the other hand, we show that, in many cases, the extension of the calibration criteria to also include runoff or soil moisture signatures is beneficial, particularly for decreasing the uncertainty in parameters of the hydrological model. Moreover, in many cases, fitting the model with hydrological signatures only provides a comparable fit to that of the calibration strategies employing runoff time series. |
first_indexed | 2024-03-10T14:21:12Z |
format | Article |
id | doaj.art-375ba6e0622d4b9581c39703a14358d1 |
institution | Directory Open Access Journal |
issn | 2073-4441 |
language | English |
last_indexed | 2024-03-10T14:21:12Z |
publishDate | 2020-12-01 |
publisher | MDPI AG |
record_format | Article |
series | Water |
spelling | doaj.art-375ba6e0622d4b9581c39703a14358d12023-11-20T23:19:55ZengMDPI AGWater2073-44412020-12-011212340110.3390/w12123401The Role of Hydrological Signatures in Calibration of Conceptual Hydrological ModelEva Melišová0Adam Vizina1Linda R. Staponites2Martin Hanel3Department of Hydrology, T. G. Masaryk Water Research Institute, Podbabska 2582/30, 160 00 Prague 6, Czech RepublicDepartment of Hydrology, T. G. Masaryk Water Research Institute, Podbabska 2582/30, 160 00 Prague 6, Czech RepublicDepartment of Hydrology, T. G. Masaryk Water Research Institute, Podbabska 2582/30, 160 00 Prague 6, Czech RepublicDepartment of Hydrology, T. G. Masaryk Water Research Institute, Podbabska 2582/30, 160 00 Prague 6, Czech RepublicDetermining an optimal calibration strategy for hydrological models is essential for a robust and accurate water balance assessment, in particular, for catchments with limited observed data. In the present study, the hydrological model Bilan was used to simulate hydrological balance for 20 catchments throughout the Czech Republic during the period 1981–2016. Calibration strategies utilizing observed runoff and estimated soil moisture time series were compared with those using only long-term statistics (signatures) of runoff and soil moisture as well as a combination of signatures and time series. Calibration strategies were evaluated considering the goodness-of-fit, the bias in flow duration curve and runoff signatures and uncertainty of the Bilan model. Results indicate that the expert calibration and calibration with observed runoff time series are, in general, preferred. On the other hand, we show that, in many cases, the extension of the calibration criteria to also include runoff or soil moisture signatures is beneficial, particularly for decreasing the uncertainty in parameters of the hydrological model. Moreover, in many cases, fitting the model with hydrological signatures only provides a comparable fit to that of the calibration strategies employing runoff time series.https://www.mdpi.com/2073-4441/12/12/3401hydrological modelmodel calibrationmodel validationhydrological balancesoil moistureungauged catchments |
spellingShingle | Eva Melišová Adam Vizina Linda R. Staponites Martin Hanel The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model Water hydrological model model calibration model validation hydrological balance soil moisture ungauged catchments |
title | The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model |
title_full | The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model |
title_fullStr | The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model |
title_full_unstemmed | The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model |
title_short | The Role of Hydrological Signatures in Calibration of Conceptual Hydrological Model |
title_sort | role of hydrological signatures in calibration of conceptual hydrological model |
topic | hydrological model model calibration model validation hydrological balance soil moisture ungauged catchments |
url | https://www.mdpi.com/2073-4441/12/12/3401 |
work_keys_str_mv | AT evamelisova theroleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT adamvizina theroleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT lindarstaponites theroleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT martinhanel theroleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT evamelisova roleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT adamvizina roleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT lindarstaponites roleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel AT martinhanel roleofhydrologicalsignaturesincalibrationofconceptualhydrologicalmodel |