Articles | Volume 23, issue 7
https://doi.org/10.5194/hess-23-2877-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-2877-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Jul 2019
Research article |
| 10 Jul 2019
| 10 Jul 2019
Bayesian performance evaluation of evapotranspiration models based on eddy covariance systems in an arid region
Guoxiao Wei
Key Laboratory of Western China's Environmental System (Ministry of
Education), Lanzhou University, Lanzhou, 730000, China
School of Earth and Environmental Sciences, Lanzhou University,
Lanzhou, 730000, China
Xiaoying Zhang
CORRESPONDING AUTHOR
College of Construction Engineering, Jilin University, Changchun, 130400, China
Ming Ye
Department of Earth, Ocean, and Atmospheric Science, Florida State
University, Tallahassee, FL 32306, USA
Ning Yue
Key Laboratory of Western China's Environmental System (Ministry of
Education), Lanzhou University, Lanzhou, 730000, China
School of Earth and Environmental Sciences, Lanzhou University,
Lanzhou, 730000, China
Fei Kan
Key Laboratory of Western China's Environmental System (Ministry of
Education), Lanzhou University, Lanzhou, 730000, China
School of Earth and Environmental Sciences, Lanzhou University,
Lanzhou, 730000, China
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Xiaoying Zhang, Fan Dong, Guangquan Chen, and Zhenxue Dai
Hydrol. Earth Syst. Sci., 27, 83–96, https://doi.org/10.5194/hess-27-83-2023, https://doi.org/10.5194/hess-27-83-2023, 2023
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In a data-driven framework, groundwater levels can generally only be calculated 1 time step ahead. We discuss the advance prediction with longer forecast periods rather than single time steps by constructing a model based on a temporal convolutional network. Model accuracy and efficiency were further compared with an LSTM-based model. The two models derived in this study can help people cope with the uncertainty of what might occur in hydrological scenarios under the threat of climate change.
Haifan Liu, Heng Dai, Jie Niu, Bill X. Hu, Dongwei Gui, Han Qiu, Ming Ye, Xingyuan Chen, Chuanhao Wu, Jin Zhang, and William Riley
Hydrol. Earth Syst. Sci., 24, 4971–4996, https://doi.org/10.5194/hess-24-4971-2020, https://doi.org/10.5194/hess-24-4971-2020, 2020
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It is still challenging to apply the quantitative and comprehensive global sensitivity analysis method to complex large-scale process-based hydrological models because of variant uncertainty sources and high computational cost. This work developed a new tool and demonstrate its implementation to a pilot example for comprehensive global sensitivity analysis of large-scale hydrological modelling. This method is mathematically rigorous and can be applied to other large-scale hydrological models.
Wei Mao, Yan Zhu, Heng Dai, Ming Ye, Jinzhong Yang, and Jingwei Wu
Hydrol. Earth Syst. Sci., 23, 3481–3502, https://doi.org/10.5194/hess-23-3481-2019, https://doi.org/10.5194/hess-23-3481-2019, 2019
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A new quasi-3-D model was developed by coupling a soil water balance model with MODFLOW iteratively for regional-scale water flow modeling. The model was tested to be effective and efficient with well-maintained mass balance. A modeling framework was developed to organize the coupling scheme and to handle the pre- and post-processing information. The model is then used to evaluate groundwater recharge in a real-world application, which shows the model practicability in regional-scale problems.
Haifan Liu, Heng Dai, Jie Niu, Bill X. Hu, Han Qiu, Dongwei Gui, Ming Ye, Xingyuan Chen, Chuanhao Wu, Jin Zhang, and William Riley
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-246, https://doi.org/10.5194/hess-2019-246, 2019
Manuscript not accepted for further review
Ahmed S. Elshall, Ming Ye, Guo-Yue Niu, and Greg A. Barron-Gafford
Geosci. Model Dev., 12, 2009–2032, https://doi.org/10.5194/gmd-12-2009-2019, https://doi.org/10.5194/gmd-12-2009-2019, 2019
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The assumptions that the residuals are independent, identically distributed, and have constant variance tend to simplify the underlying mathematics of data models for Bayesian inference. We relax these three assumptions step-wise, resulting in eight data models. Using three mechanistic soil respiration models with different levels of model discrepancy, we discuss the impacts of data models on parameter estimation and predictive performance, and provide recommendations for data model selection.
Anthony P. Walker, Ming Ye, Dan Lu, Martin G. De Kauwe, Lianhong Gu, Belinda E. Medlyn, Alistair Rogers, and Shawn P. Serbin
Geosci. Model Dev., 11, 3159–3185, https://doi.org/10.5194/gmd-11-3159-2018, https://doi.org/10.5194/gmd-11-3159-2018, 2018
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Large uncertainty is inherent in model predictions due to imperfect knowledge of how to describe the processes that a model is intended to represent. Yet methods to quantify and evaluate this model hypothesis uncertainty are limited. To address this, the multi-assumption architecture and testbed (MAAT) automates the generation of all possible models by combining multiple representations of multiple processes. MAAT provides a formal framework for quantification of model hypothesis uncertainty.
Zexuan Xu, Bill X. Hu, and Ming Ye
Hydrol. Earth Syst. Sci., 22, 221–239, https://doi.org/10.5194/hess-22-221-2018, https://doi.org/10.5194/hess-22-221-2018, 2018
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This study helps hydrologists better understand the parameters in modeling seawater intrusion in a coastal karst aquifer. Local and global sensitivity studies are conducted to evaluate a density-dependent numerical model of seawater intrusion. The sensitivity analysis indicates that karst features are critical for seawater intrusion modeling, and the evaluation of hydraulic conductivity is biased in continuum SEAWAT model. Dispervisity is no longer important in the advection-dominated aquifer.
Related subject area
Subject: Hydrometeorology | Techniques and Approaches: Mathematical applications
Using statistical models to depict the response of multi-timescale drought to forest cover change across climate zones
Past, present and future rainfall erosivity in central Europe based on convection-permitting climate simulations
The most extreme rainfall erosivity event ever recorded in China up to 2022: the 7.20 storm in Henan Province
The role of atmospheric rivers in the distribution of heavy precipitation events over North America
Study on a mother wavelet optimization framework based on change-point detection of hydrological time series
Projected changes in droughts and extreme droughts in Great Britain strongly influenced by the choice of drought index
Atmospheric water transport connectivity within and between ocean basins and land
Technical Note: Space–time statistical quality control of extreme precipitation observations
The relative importance of antecedent soil moisture and precipitation in flood generation in the middle and lower Yangtze River basin
Rainfall pattern analysis in 24 East Asian megacities using a complex network
Comparison between canonical vine copulas and a meta-Gaussian model for forecasting agricultural drought over China
Analysis of flash droughts in China using machine learning
Performance-based comparison of regionalization methods to improve the at-site estimates of daily precipitation
The use of personal weather station observations to improve precipitation estimation and interpolation
The 2018 northern European hydrological drought and its drivers in a historical perspective
Assimilating shallow soil moisture observations into land models with a water budget constraint
Emerging climate signals in the Lena River catchment: a non-parametric statistical approach
Near-0 °C surface temperature and precipitation type patterns across Canada
A universal multifractal approach to assessment of spatiotemporal extreme precipitation over the Loess Plateau of China
Significant spatial patterns from the GCM seasonal forecasts of global precipitation
Technical note: An improved Grassberger–Procaccia algorithm for analysis of climate system complexity
The influence of long-term changes in canopy structure on rainfall interception loss: a case study in Speulderbos, the Netherlands
Geostatistical assessment of warm-season precipitation observations in Korea based on the composite precipitation and satellite water vapor data
Investigating water budget dynamics in 18 river basins across the Tibetan Plateau through multiple datasets
Does the GPM mission improve the systematic error component in satellite rainfall estimates over TRMM? An evaluation at a pan-India scale
Assessment of an ensemble seasonal streamflow forecasting system for Australia
Technical note: Combining quantile forecasts and predictive distributions of streamflows
Scaled distribution mapping: a bias correction method that preserves raw climate model projected changes
Temporal and spatial changes of rainfall and streamflow in the Upper Tekezē–Atbara river basin, Ethiopia
Seasonal streamflow forecasting by conditioning climatology with precipitation indices
Bias correcting precipitation forecasts to improve the skill of seasonal streamflow forecasts
Flood triggering in Switzerland: the role of daily to monthly preceding precipitation
Comparing bias correction methods in downscaling meteorological variables for a hydrologic impact study in an arid area in China
Explaining and forecasting interannual variability in the flow of the Nile River
Drought severity–duration–frequency curves: a foundation for risk assessment and planning tool for ecosystem establishment in post-mining landscapes
Characterising the space–time structure of rainfall in the Sahel with a view to estimating IDAF curves
Spatial analysis of precipitation in a high-mountain region: exploring methods with multi-scale topographic predictors and circulation types
Variability of extreme precipitation over Europe and its relationships with teleconnection patterns
Drought evolution characteristics and precipitation intensity changes during alternating dry–wet changes in the Huang–Huai–Hai River basin
Structural break or long memory: an empirical survey on daily rainfall data sets across Malaysia
Calibration of aerodynamic roughness over the Tibetan Plateau with Ensemble Kalman Filter analysed heat flux
Technical Note: Downscaling RCM precipitation to the station scale using statistical transformations – a comparison of methods
Spectral representation of the annual cycle in the climate change signal
Simultaneous estimation of land surface scheme states and parameters using the ensemble Kalman filter: identical twin experiments
Downscaling of surface moisture flux and precipitation in the Ebro Valley (Spain) using analogues and analogues followed by random forests and multiple linear regression
Geostatistical radar-raingauge combination with nonparametric correlograms: methodological considerations and application in Switzerland
El Niño-Southern Oscillation and water resources in the headwaters region of the Yellow River: links and potential for forecasting
A summer climate regime over Europe modulated by the North Atlantic Oscillation
Introducing a rainfall compound distribution model based on weather patterns sub-sampling
Yan Li, Bo Huang, and Henning W. Rust
Hydrol. Earth Syst. Sci., 28, 321–339, https://doi.org/10.5194/hess-28-321-2024, https://doi.org/10.5194/hess-28-321-2024, 2024
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The inconsistent changes in temperature and precipitation induced by forest cover change are very likely to affect drought condition. We use a set of statistical models to explore the relationship between forest cover change and drought change in different timescales and climate zones. We find that the influence of forest cover on droughts varies under different precipitation and temperature quantiles. Forest cover also could modulate the impacts of precipitation and temperature on drought.
Magdalena Uber, Michael Haller, Christoph Brendel, Gudrun Hillebrand, and Thomas Hoffmann
Hydrol. Earth Syst. Sci., 28, 87–102, https://doi.org/10.5194/hess-28-87-2024, https://doi.org/10.5194/hess-28-87-2024, 2024
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We calculated past, present and future rainfall erosivity in central Europe from high-resolution precipitation data (3 km and 1 h) generated by the COSMO-CLM convection-permitting climate model. Future rainfall erosivity can be up to 84 % higher than it was in the past. Such increases are much higher than estimated previously from regional climate model output. Convection-permitting simulations have an enormous and, to date, unexploited potential for the calculation of future rainfall erosivity.
Yuanyuan Xiao, Shuiqing Yin, Bofu Yu, Conghui Fan, Wenting Wang, and Yun Xie
Hydrol. Earth Syst. Sci., 27, 4563–4577, https://doi.org/10.5194/hess-27-4563-2023, https://doi.org/10.5194/hess-27-4563-2023, 2023
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An exceptionally heavy rainfall event occurred on 20 July 2021 in central China (the 7.20 storm). The storm presents a rare opportunity to examine the extreme rainfall erosivity. The storm, with an average recurrence interval of at least 10 000 years, was the largest in terms of its rainfall erosivity on record over the past 70 years in China. The study suggests that extreme erosive events can occur anywhere in eastern China and are not necessarily concentrated in low latitudes.
Sara M. Vallejo-Bernal, Frederik Wolf, Niklas Boers, Dominik Traxl, Norbert Marwan, and Jürgen Kurths
Hydrol. Earth Syst. Sci., 27, 2645–2660, https://doi.org/10.5194/hess-27-2645-2023, https://doi.org/10.5194/hess-27-2645-2023, 2023
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Employing event synchronization and complex networks analysis, we reveal a cascade of heavy rainfall events, related to intense atmospheric rivers (ARs): heavy precipitation events (HPEs) in western North America (NA) that occur in the aftermath of land-falling ARs are synchronized with HPEs in central and eastern Canada with a delay of up to 12 d. Understanding the effects of ARs in the rainfall over NA will lead to better anticipating the evolution of the climate dynamics in the region.
Jiqing Li, Jing Huang, Lei Zheng, and Wei Zheng
Hydrol. Earth Syst. Sci., 27, 2325–2339, https://doi.org/10.5194/hess-27-2325-2023, https://doi.org/10.5194/hess-27-2325-2023, 2023
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Under the joint action of climate–human activities the use of runoff data whose mathematical properties have changed has become the key to watershed management. To determine whether the data have been changed, the number and the location of changes, we proposed a change-point detection framework. The problem of determining the parameters of wavelet transform has been solved by comparing the accuracy of identifying change points. This study helps traditional models adapt to environmental changes.
Nele Reyniers, Timothy J. Osborn, Nans Addor, and Geoff Darch
Hydrol. Earth Syst. Sci., 27, 1151–1171, https://doi.org/10.5194/hess-27-1151-2023, https://doi.org/10.5194/hess-27-1151-2023, 2023
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In an analysis of future drought projections for Great Britain based on the Standardised Precipitation Index and the Standardised Precipitation Evapotranspiration Index, we show that the choice of drought indicator has a decisive influence on the resulting projected changes in drought characteristics, although both result in increased drying. This highlights the need to understand the interplay between increasing atmospheric evaporative demand and drought impacts under a changing climate.
Dipanjan Dey, Aitor Aldama Campino, and Kristofer Döös
Hydrol. Earth Syst. Sci., 27, 481–493, https://doi.org/10.5194/hess-27-481-2023, https://doi.org/10.5194/hess-27-481-2023, 2023
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One of the most striking and robust features of climate change is the acceleration of the atmospheric water cycle branch. Earlier studies were able to provide a quantification of the global atmospheric water cycle, but they missed addressing the atmospheric water transport connectivity within and between ocean basins and land. These shortcomings were overcome in the present study and presented a complete synthesised and quantitative view of the atmospheric water cycle.
Abbas El Hachem, Jochen Seidel, Florian Imbery, Thomas Junghänel, and András Bárdossy
Hydrol. Earth Syst. Sci., 26, 6137–6146, https://doi.org/10.5194/hess-26-6137-2022, https://doi.org/10.5194/hess-26-6137-2022, 2022
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Through this work, a methodology to identify outliers in intense precipitation data was presented. The results show the presence of several suspicious observations that strongly differ from their surroundings. Many identified outliers did not have unusually high values but disagreed with their neighboring values at the corresponding time steps. Weather radar and discharge data were used to distinguish between single events and false observations.
Qihua Ran, Jin Wang, Xiuxiu Chen, Lin Liu, Jiyu Li, and Sheng Ye
Hydrol. Earth Syst. Sci., 26, 4919–4931, https://doi.org/10.5194/hess-26-4919-2022, https://doi.org/10.5194/hess-26-4919-2022, 2022
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This study aims to further evaluate the relative importance of antecedent soil moisture and rainfall on flood generation and the controlling factors. The relative importance of antecedent soil moisture and daily rainfall present a significant correlation with drainage area; the larger the watershed, and the more essential the antecedent soil saturation rate is in flood generation, the less important daily rainfall will be.
Kyunghun Kim, Jaewon Jung, Hung Soo Kim, Masahiko Haraguchi, and Soojun Kim
Hydrol. Earth Syst. Sci., 26, 4823–4836, https://doi.org/10.5194/hess-26-4823-2022, https://doi.org/10.5194/hess-26-4823-2022, 2022
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This study applied a new methodology (complex network), instead of using classic methods, to establish the relationships between rainfall events in large East Asian cities. The relationships show that western China and Southeast Asia have a lot of influence on each other. Moreover, it is confirmed that the relationships arise from the effect of the East Asian monsoon. In future, complex network may be able to be applied to analyze the concurrent relationships between extreme rainfall events.
Haijiang Wu, Xiaoling Su, Vijay P. Singh, Te Zhang, Jixia Qi, and Shengzhi Huang
Hydrol. Earth Syst. Sci., 26, 3847–3861, https://doi.org/10.5194/hess-26-3847-2022, https://doi.org/10.5194/hess-26-3847-2022, 2022
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Agricultural drought forecasting lies at the core of overall drought risk management and is critical for food security and drought early warning. Using three-dimensional scenarios, we attempted to compare the agricultural drought forecast performance of a canonical vine copula (3C-vine) model and meta-Gaussian (MG) model over China. The findings show that the 3C-vine model exhibits more skill than the MG model when using 1– to 3-month lead times for forecasting agricultural drought.
Linqi Zhang, Yi Liu, Liliang Ren, Adriaan J. Teuling, Ye Zhu, Linyong Wei, Linyan Zhang, Shanhu Jiang, Xiaoli Yang, Xiuqin Fang, and Hang Yin
Hydrol. Earth Syst. Sci., 26, 3241–3261, https://doi.org/10.5194/hess-26-3241-2022, https://doi.org/10.5194/hess-26-3241-2022, 2022
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In this study, three machine learning methods displayed a good detection capacity of flash droughts. The RF model was recommended to estimate the depletion rate of soil moisture and simulate flash drought by considering the multiple meteorological variable anomalies in the adjacent time to drought onset. The anomalies of precipitation and potential evapotranspiration exhibited a stronger synergistic but asymmetrical effect on flash droughts compared to slowly developing droughts.
Abubakar Haruna, Juliette Blanchet, and Anne-Catherine Favre
Hydrol. Earth Syst. Sci., 26, 2797–2811, https://doi.org/10.5194/hess-26-2797-2022, https://doi.org/10.5194/hess-26-2797-2022, 2022
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Reliable prediction of floods depends on the quality of the input data such as precipitation. However, estimation of precipitation from the local measurements is known to be difficult, especially for extremes. Regionalization improves the estimates by increasing the quantity of data available for estimation. Here, we compare three regionalization methods based on their robustness and reliability. We apply the comparison to a dense network of daily stations within and outside Switzerland.
András Bárdossy, Jochen Seidel, and Abbas El Hachem
Hydrol. Earth Syst. Sci., 25, 583–601, https://doi.org/10.5194/hess-25-583-2021, https://doi.org/10.5194/hess-25-583-2021, 2021
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In this study, the applicability of data from private weather stations (PWS) for precipitation interpolation was investigated. Due to unknown errors and biases in these observations, a two-step filter was developed that uses indicator correlations and event-based spatial precipitation patterns. The procedure was tested and cross validated for the state of Baden-Württemberg (Germany). The biggest improvement is achieved for the shortest time aggregations.
Sigrid J. Bakke, Monica Ionita, and Lena M. Tallaksen
Hydrol. Earth Syst. Sci., 24, 5621–5653, https://doi.org/10.5194/hess-24-5621-2020, https://doi.org/10.5194/hess-24-5621-2020, 2020
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This study provides an in-depth analysis of the 2018 northern European drought. Large parts of the region experienced 60-year record-breaking temperatures, linked to high-pressure systems and warm surrounding seas. Meteorological drought developed from May and, depending on local conditions, led to extreme low flows and groundwater drought in the following months. The 2018 event was unique in that it affected most of Fennoscandia as compared to previous droughts.
Bo Dan, Xiaogu Zheng, Guocan Wu, and Tao Li
Hydrol. Earth Syst. Sci., 24, 5187–5201, https://doi.org/10.5194/hess-24-5187-2020, https://doi.org/10.5194/hess-24-5187-2020, 2020
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Data assimilation is a procedure to generate an optimal combination of the state variable in geoscience, based on the model outputs and observations. The ensemble Kalman filter (EnKF) scheme is a widely used assimilation method in soil moisture estimation. This study proposed several modifications of EnKF for improving this assimilation. The study shows that the quality of the assimilation result is improved, while the degree of water budget imbalance is reduced.
Eric Pohl, Christophe Grenier, Mathieu Vrac, and Masa Kageyama
Hydrol. Earth Syst. Sci., 24, 2817–2839, https://doi.org/10.5194/hess-24-2817-2020, https://doi.org/10.5194/hess-24-2817-2020, 2020
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Existing approaches to quantify the emergence of climate change require several user choices that make these approaches less objective. We present an approach that uses a minimum number of choices and showcase its application in the extremely sensitive, permafrost-dominated region of eastern Siberia. Designed as a Python toolbox, it allows for incorporating climate model, reanalysis, and in situ data to make use of numerous existing data sources and reduce uncertainties in obtained estimates.
Eva Mekis, Ronald E. Stewart, Julie M. Theriault, Bohdan Kochtubajda, Barrie R. Bonsal, and Zhuo Liu
Hydrol. Earth Syst. Sci., 24, 1741–1761, https://doi.org/10.5194/hess-24-1741-2020, https://doi.org/10.5194/hess-24-1741-2020, 2020
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This article provides a Canada-wide analysis of near-0°C temperature conditions (±2°C) using hourly surface temperature and precipitation type observations from 92 locations for the 1981–2011 period. Higher annual occurrences were found in Atlantic Canada, although high values also occur in other regions. Trends of most indicators show little or no change despite a systematic warming over Canada. A higher than expected tendency for near-0°C conditions was also found at some stations.
Jianjun Zhang, Guangyao Gao, Bojie Fu, Cong Wang, Hoshin V. Gupta, Xiaoping Zhang, and Rui Li
Hydrol. Earth Syst. Sci., 24, 809–826, https://doi.org/10.5194/hess-24-809-2020, https://doi.org/10.5194/hess-24-809-2020, 2020
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We proposed an approach that integrates universal multifractals and a segmentation algorithm to precisely identify extreme precipitation (EP) and assess spatiotemporal EP variation over the Loess Plateau, using daily data. Our results explain how EP contributes to the widely distributed severe natural hazards. These findings are of great significance for ecological management in the Loess Plateau. Our approach is also helpful for spatiotemporal EP assessment at the regional scale.
Tongtiegang Zhao, Wei Zhang, Yongyong Zhang, Zhiyong Liu, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 24, 1–16, https://doi.org/10.5194/hess-24-1-2020, https://doi.org/10.5194/hess-24-1-2020, 2020
Chongli Di, Tiejun Wang, Xiaohua Yang, and Siliang Li
Hydrol. Earth Syst. Sci., 22, 5069–5079, https://doi.org/10.5194/hess-22-5069-2018, https://doi.org/10.5194/hess-22-5069-2018, 2018
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The original Grassberger–Procaccia algorithm for complex analysis was modified by incorporating the normal-based K-means clustering technique and the RANSAC algorithm. The calculation accuracy of the proposed method was shown to outperform traditional algorithms. The proposed algorithm was used to diagnose climate system complexity in the Hai He basin. The spatial patterns of the complexity of precipitation and air temperature reflected the influence of the dominant climate system.
César Cisneros Vaca, Christiaan van der Tol, and Chandra Prasad Ghimire
Hydrol. Earth Syst. Sci., 22, 3701–3719, https://doi.org/10.5194/hess-22-3701-2018, https://doi.org/10.5194/hess-22-3701-2018, 2018
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The influence of long-term changes in canopy structure on rainfall interception loss was studied in a 55-year old forest. Interception loss was similar at the same site (38 %), when the forest was 29 years old. In the past, the forest was denser and had a higher storage capacity, but the evaporation rates were lower. We emphasize the importance of quantifying downward sensible heat flux and heat release from canopy biomass in tall forest in order to improve the quantification of evaporation.
Sojung Park, Seon Ki Park, Jeung Whan Lee, and Yunho Park
Hydrol. Earth Syst. Sci., 22, 3435–3452, https://doi.org/10.5194/hess-22-3435-2018, https://doi.org/10.5194/hess-22-3435-2018, 2018
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Understanding the precipitation characteristics is essential to design an optimal observation network. We studied the spatial and temporal characteristics of summertime precipitation systems in Korea via geostatistical analyses on the ground-based precipitation and satellite water vapor data. We found that, under a strict standard, an observation network with higher resolution is required in local areas with frequent heavy rainfalls, depending on directional features of precipitation systems.
Wenbin Liu, Fubao Sun, Yanzhong Li, Guoqing Zhang, Yan-Fang Sang, Wee Ho Lim, Jiahong Liu, Hong Wang, and Peng Bai
Hydrol. Earth Syst. Sci., 22, 351–371, https://doi.org/10.5194/hess-22-351-2018, https://doi.org/10.5194/hess-22-351-2018, 2018
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The dynamics of basin-scale water budgets over the Tibetan Plateau (TP) are not well understood nowadays due to the lack of hydro-climatic observations. In this study, we investigate seasonal cycles and trends of water budget components (e.g. precipitation P, evapotranspiration ET and runoff Q) in 18 TP river basins during the period 1982–2011 through the use of multi-source datasets (e.g. in situ observations, satellite retrievals, reanalysis outputs and land surface model simulations).
Harsh Beria, Trushnamayee Nanda, Deepak Singh Bisht, and Chandranath Chatterjee
Hydrol. Earth Syst. Sci., 21, 6117–6134, https://doi.org/10.5194/hess-21-6117-2017, https://doi.org/10.5194/hess-21-6117-2017, 2017
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High-quality satellite precipitation forcings have provided a viable alternative to hydrologic modeling in data-scarce regions. Ageing TRMM sensors have recently been upgraded to GPM, promising enhanced spatio-temporal resolutions. Statistical and hydrologic evaluation of GPM measurements across 86 Indian river basins revealed improved low rainfall estimates with reduced effects of climatology and topography.
James C. Bennett, Quan J. Wang, David E. Robertson, Andrew Schepen, Ming Li, and Kelvin Michael
Hydrol. Earth Syst. Sci., 21, 6007–6030, https://doi.org/10.5194/hess-21-6007-2017, https://doi.org/10.5194/hess-21-6007-2017, 2017
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We assess a new streamflow forecasting system in Australia. The system is designed to meet the need of water agencies for 12-month forecasts. The forecasts perform well in a wide range of rivers. Forecasts for shorter periods (up to 6 months) are generally informative. Forecasts sometimes did not perform well in a few very dry rivers. We test several techniques for improving streamflow forecasts in drylands, with mixed success.
Konrad Bogner, Katharina Liechti, and Massimiliano Zappa
Hydrol. Earth Syst. Sci., 21, 5493–5502, https://doi.org/10.5194/hess-21-5493-2017, https://doi.org/10.5194/hess-21-5493-2017, 2017
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The enhanced availability of many different weather prediction systems nowadays makes it very difficult for flood and water resource managers to choose the most reliable and accurate forecast. In order to circumvent this problem of choice, different approaches for combining this information have been applied at the Sihl River (CH) and the results have been verified. The outcome of this study highlights the importance of forecast combination in order to improve the quality of forecast systems.
Matthew B. Switanek, Peter A. Troch, Christopher L. Castro, Armin Leuprecht, Hsin-I Chang, Rajarshi Mukherjee, and Eleonora M. C. Demaria
Hydrol. Earth Syst. Sci., 21, 2649–2666, https://doi.org/10.5194/hess-21-2649-2017, https://doi.org/10.5194/hess-21-2649-2017, 2017
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The commonly used bias correction method called quantile mapping assumes a constant function of error correction values between modeled and observed distributions. Our article finds that this function cannot be assumed to be constant. We propose a new bias correction method, called scaled distribution mapping, that does not rely on this assumption. Furthermore, the proposed method more explicitly accounts for the frequency of rain days and the likelihood of individual events.
Tesfay G. Gebremicael, Yasir A. Mohamed, Pieter v. Zaag, and Eyasu Y. Hagos
Hydrol. Earth Syst. Sci., 21, 2127–2142, https://doi.org/10.5194/hess-21-2127-2017, https://doi.org/10.5194/hess-21-2127-2017, 2017
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This study was conducted to understand the spatio-temporal variations of streamflow in the Tekezē basin. Results showed rainfall over the basin did not significantly change. However, streamflow experienced high variabilities at seasonal and annual scales. Further studies are needed to verify hydrological changes by identifying the physical mechanisms behind those changes. Findings are useful as prerequisite for studying the effects of catchment management dynamics on the hydrological processes.
Louise Crochemore, Maria-Helena Ramos, Florian Pappenberger, and Charles Perrin
Hydrol. Earth Syst. Sci., 21, 1573–1591, https://doi.org/10.5194/hess-21-1573-2017, https://doi.org/10.5194/hess-21-1573-2017, 2017
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The use of general circulation model outputs for streamflow forecasting has developed in the last decade. In parallel, traditional streamflow forecasting is commonly based on historical data. This study investigates the impact of conditioning historical data based on circulation model precipitation forecasts on seasonal streamflow forecast quality. Results highlighted a trade-off between the sharpness and reliability of forecasts.
Louise Crochemore, Maria-Helena Ramos, and Florian Pappenberger
Hydrol. Earth Syst. Sci., 20, 3601–3618, https://doi.org/10.5194/hess-20-3601-2016, https://doi.org/10.5194/hess-20-3601-2016, 2016
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This study investigates the way bias correcting precipitation forecasts can improve the skill of streamflow forecasts at extended lead times. Eight variants of bias correction approaches based on the linear scaling and the distribution mapping methods are applied to the precipitation forecasts prior to generating the streamflow forecasts. One of the main results of the study is that distribution mapping of daily values is successful in improving forecast reliability.
P. Froidevaux, J. Schwanbeck, R. Weingartner, C. Chevalier, and O. Martius
Hydrol. Earth Syst. Sci., 19, 3903–3924, https://doi.org/10.5194/hess-19-3903-2015, https://doi.org/10.5194/hess-19-3903-2015, 2015
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We investigate precipitation characteristics prior to 4000 annual floods in Switzerland since 1961. The floods were preceded by heavy precipitation, but in most catchments extreme precipitation occurred only during the last 3 days prior to the flood events. Precipitation sums for earlier time periods (like e.g. 4-14 days prior to floods) were mostly average and do not correlate with the return period of the floods.
G. H. Fang, J. Yang, Y. N. Chen, and C. Zammit
Hydrol. Earth Syst. Sci., 19, 2547–2559, https://doi.org/10.5194/hess-19-2547-2015, https://doi.org/10.5194/hess-19-2547-2015, 2015
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This study compares the effects of five precipitation and three temperature correction methods on precipitation, temperature, and streamflow through loosely coupling RCM (RegCM) and a distributed hydrological model (SWAT) in terms of frequency-based indices and time-series-based indices. The methodology and results can be used for other regions and other RCM and hydrologic models, and for impact studies of climate change on water resources at a regional scale.
M. S. Siam and E. A. B. Eltahir
Hydrol. Earth Syst. Sci., 19, 1181–1192, https://doi.org/10.5194/hess-19-1181-2015, https://doi.org/10.5194/hess-19-1181-2015, 2015
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This paper explains the different natural modes of interannual variability in the flow of the Nile River and also presents a new index based on the sea surface temperature (SST) over the southern Indian Ocean to forecast the flow of the Nile River. It also presents a new hybrid forecasting algorithm that can be used to predict the Nile flow based on indices of the SST in the eastern Pacific and southern Indian oceans.
D. Halwatura, A. M. Lechner, and S. Arnold
Hydrol. Earth Syst. Sci., 19, 1069–1091, https://doi.org/10.5194/hess-19-1069-2015, https://doi.org/10.5194/hess-19-1069-2015, 2015
G. Panthou, T. Vischel, T. Lebel, G. Quantin, and G. Molinié
Hydrol. Earth Syst. Sci., 18, 5093–5107, https://doi.org/10.5194/hess-18-5093-2014, https://doi.org/10.5194/hess-18-5093-2014, 2014
D. Masson and C. Frei
Hydrol. Earth Syst. Sci., 18, 4543–4563, https://doi.org/10.5194/hess-18-4543-2014, https://doi.org/10.5194/hess-18-4543-2014, 2014
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The question of how to utilize information from the physiography/topography in the spatial interpolation of rainfall is a long-standing discussion in the literature. In this study we test ideas that go beyond the approach in popular interpolation schemes today. The key message of our study is that these ideas can at best marginally improve interpolation accuracy, even in a region where a clear benefit would intuitively be expected.
A. Casanueva, C. Rodríguez-Puebla, M. D. Frías, and N. González-Reviriego
Hydrol. Earth Syst. Sci., 18, 709–725, https://doi.org/10.5194/hess-18-709-2014, https://doi.org/10.5194/hess-18-709-2014, 2014
D. H. Yan, D. Wu, R. Huang, L. N. Wang, and G. Y. Yang
Hydrol. Earth Syst. Sci., 17, 2859–2871, https://doi.org/10.5194/hess-17-2859-2013, https://doi.org/10.5194/hess-17-2859-2013, 2013
F. Yusof, I. L. Kane, and Z. Yusop
Hydrol. Earth Syst. Sci., 17, 1311–1318, https://doi.org/10.5194/hess-17-1311-2013, https://doi.org/10.5194/hess-17-1311-2013, 2013
J. H. Lee, J. Timmermans, Z. Su, and M. Mancini
Hydrol. Earth Syst. Sci., 16, 4291–4302, https://doi.org/10.5194/hess-16-4291-2012, https://doi.org/10.5194/hess-16-4291-2012, 2012
L. Gudmundsson, J. B. Bremnes, J. E. Haugen, and T. Engen-Skaugen
Hydrol. Earth Syst. Sci., 16, 3383–3390, https://doi.org/10.5194/hess-16-3383-2012, https://doi.org/10.5194/hess-16-3383-2012, 2012
T. Bosshard, S. Kotlarski, T. Ewen, and C. Schär
Hydrol. Earth Syst. Sci., 15, 2777–2788, https://doi.org/10.5194/hess-15-2777-2011, https://doi.org/10.5194/hess-15-2777-2011, 2011
S. Nie, J. Zhu, and Y. Luo
Hydrol. Earth Syst. Sci., 15, 2437–2457, https://doi.org/10.5194/hess-15-2437-2011, https://doi.org/10.5194/hess-15-2437-2011, 2011
G. Ibarra-Berastegi, J. Saénz, A. Ezcurra, A. Elías, J. Diaz Argandoña, and I. Errasti
Hydrol. Earth Syst. Sci., 15, 1895–1907, https://doi.org/10.5194/hess-15-1895-2011, https://doi.org/10.5194/hess-15-1895-2011, 2011
R. Schiemann, R. Erdin, M. Willi, C. Frei, M. Berenguer, and D. Sempere-Torres
Hydrol. Earth Syst. Sci., 15, 1515–1536, https://doi.org/10.5194/hess-15-1515-2011, https://doi.org/10.5194/hess-15-1515-2011, 2011
A. Lü, S. Jia, W. Zhu, H. Yan, S. Duan, and Z. Yao
Hydrol. Earth Syst. Sci., 15, 1273–1281, https://doi.org/10.5194/hess-15-1273-2011, https://doi.org/10.5194/hess-15-1273-2011, 2011
G. Wang, A. J. Dolman, and A. Alessandri
Hydrol. Earth Syst. Sci., 15, 57–64, https://doi.org/10.5194/hess-15-57-2011, https://doi.org/10.5194/hess-15-57-2011, 2011
F. Garavaglia, J. Gailhard, E. Paquet, M. Lang, R. Garçon, and P. Bernardara
Hydrol. Earth Syst. Sci., 14, 951–964, https://doi.org/10.5194/hess-14-951-2010, https://doi.org/10.5194/hess-14-951-2010, 2010
Cited articles
Allen, R. G., Perista, L. S., Raes, D., and Smith, M.: Crop
Evapotranspiration – Guidelines for Computing Crop Water Requirements; FAO
Irrigation and Drainage papers 56, FAO – Food and Agriculture Organization of the United Nations, Rome, 1998.
Alves, I. and Pereira, L. S.: Modeling surface resistance from climatic
variables?, Agr. Water Manage., 42, 371–385, 2000.
Aubinet, M., Grelle, A., Ibrom, A., Rannik, Ü., Moncrieff, J., and
Foken, T.: Estimates of the annual net carbon and water exchange of forests:
the euroflux methodology, Adv. Ecol. Res., 30, 113–175, 2000.
Baldocchi, D. D.: Assessing the eddy covariance technique for evaluating
carbon dioxide exchange rates of ecosystems: past, present and future, Global
Change. Biol., 9, 479–492, 2003.
Bardossy, A. and Das, T.: Influence of rainfall observation network on model calibration and application, Hydrol. Earth Syst. Sci., 12, 77–89,
https://doi.org/10.5194/hess-12-77-2008, 2008.
Barton, I. J.: A Parameterization of the Evaporation from Nonsaturated
Surfaces, J. Appl. Meteorol., 18, 43–47, 1979.
Beyrich, F., Richter, S. H., Weisensee, U., Kohsiek, W., Lohse, H., de Bruin, H. A. R., Foken, T., Göckede, M., Berger, F., Vogt, R., and Batchvarova, E.: Experimental determination of turbulent fluxes over the heterogeneous litfass area: selected results from the litfass-98 experiment, Theor. Appl. Climatol., 73, 19–34, https://doi.org/10.1007/s00704-002-0691-7, 2002.
Bohn, T. J. and Vivoni, E. R.: Process-based characterization of
evapotranspiration sources over the North American monsoon region, Water
Resour. Res., 52, 358–384, https://doi.org/10.1002/2015WR017934, 2016.
Bonan, G.: Ecological climatology: concepts and applications, Cambridge
University Press, Cambridge, 2008.
Braswell, B. H., Sacks, W. J., Linder, E., and Schimel, D. S.: Estimating
diurnal to annual ecosystem parameters by synthesis of a carbon flux model
with eddy covariance net ecosystem exchange observations, Global Change
Biol., 11, 335–355, 2005.
Brutsaert, W.: Hydrology: An Introduction, Cambridge University Press,
Cambridge, 2005.
Brutsaert, W. and Stricker, H.: An advection-aridity approach to estimate actual regional evapotranspiration, Water Resour. Res., 15, 443–450, 1979.
Chen, D. Y., Wang, X., Liu, S. Y., Wang, Y. K., Gao, Z. Y., Zhang, L. L.,
Wei, X. G., and Wei, X. D.: Using Bayesian analysis to compare the
performance of three evapotranspiration models for rainfed jujube (Ziziphus
jujuba Mill.) plantations in the Loess Plateau, Agr. Water. Manage., 159,
341–357, 2015.
Elshall, A. S., Ye, M., Pei, Y., Zhang, F., Niu, G. Y., and Barron-Gafford,
G. A.: Relative model score: A scoring rule for evaluating ensemble
simulations with application to microbial soil respiration modeling, Stoch.
Environ. Res. A., https://doi.org/10.1007/s00477-018-1592-3, in press, 2018.
Ershadi, A., Mccabe, M. F., Evans, J. P., Chaney, N. W., and Wood, E. F.:
Multi-site evaluation of terrestrial evaporation models using fluxnet data,
Agr. Forest Meteorol., 187, 46–61, 2014.
Ershadi, A., McCabe, M .F., Evans, J. P., and Wood, E. F.: Impact of model
structure and parameterization on Penman–Monteith type evaporation models,
J. Hydrol., 525, 521–535, 2015.
Fisher, J. B., DeBiase, T. A., Qi, Y., Xu, M., and Goldstein, A. H.:
Evapotranspiration models compared on a Sierra Nevada forest ecosystem,
Environ. Model. Softw., 20, 783–796, 2005.
Flint A. L. and Childs, S. W.: Use of the Priestley–Taylor evaporation
equation for soil water limited conditions in a small forest clearcut,
Agr. Forest Meteorol., 56, 247–260, 1991.
Foken, T., Mauder, M., Liebethal, C., Wimmer, F., Beyrich, F., Leps, J. P.,
Raasch, S., DeBruin, H. A. R., Meijninger, W. M. L., and Bange, J.: Energy
balance closure for the LITFASS-2003 experiment, Theor. Appl. Climatol.,
101, 149–160, https://doi.org/10.1007/s00704-009-0216-8, 2010.
Franssen, H. J. H., Stöckli, R., Lehner, I., Rotenberg, E., and
Seneviratne S. I.: Energy balance closure of eddy-covariance data: A
multisite analysis for European FLUXNET stations, Agr. Forest Meteorol.,
150, 1553–1567, https://doi.org/10.1016/j.agrformet.2010.08.005, 2010.
Gelman, A. and Meng, X. L.: Simulating normalizing constants: From importance sampling to bridge sampling to path sampling, Stat. Sci., 13, 163–185, 1998.
Gelman, A. and Rubin, D. B.: Inference from iterative simulation using
multiple sequences, Stat. Sci., 7, 457–472, 1992.
Giudice, D., Albert, C., Rieckermann, J., and Reichert, P.: Describing the
catchment-averaged precipitation as a stochastic process improves parameter
and input estimation, Water Resour. Res., 52, 3162–3186,
https://doi.org/10.1002/2015WR017871, 2016.
Höge, M., Wöhling, T., and Nowak, W.: A primer for model selection:
The decisive role of model complexity, Water Resour. Res., 54, 1688–1715,
https://doi.org/10.1002/2017WR021902, 2018.
Jefferys, W. H. and Berger, J. O.: Sharpening Ockham's razor on a Bayesian
strop, Am. Sci., 89, 64–72, 1992.
Kashyap, R. L.: Optimal choice of AR and MA parts in autoregressive moving
average models, IEEE T. Pattern Anal. Mach. Intell., 4, 99–104, 1982.
Katerji, N. and Rana, G.: Modelling evapotranspiration of six irrigated crops under Mediterranean climate conditions, Agr. Forest Meteorol., 138, 142–155, 2006.
Katerji, N., Rana, G., and Fahed, S.: Parameterizing canopy resistance using
mechanistic and semi-empirical estimates of hourly evapotranspiration:
critical evaluation for irrigated crops in the Mediterranean, Hydrol. Process., 25, 117–129, 2011.
Kato, T., Kimura, R., and Kamichika, M.: Estimation of evapotranspiration,
transpiration ratio and water-use efficiency from a sparse canopy using a
compartment model, Agr. Water Manage., 65, 173–191, 2004.
Kelliher, F. M., Leunig, R., Raupach, M. R., and Schulze, E. D.: Maximum conductances for evaporation from global vegetation types, Agr. Forest Meteorol., 73, 1–16, 1995.
Kessler, E. and Neas, B.: On correlation, with applications to the radar
and raingage measurement of rainfall, Atmos. Res., 34, 217–229, 1994.
Laloy, E., Linde, N., Jacques, D., and Vrugt, J. A.: Probabilistic inference
of multi-Gaussian fields from indirect hydrological data using circulant
embedding and dimensionality reduction, Water Resour. Res., 51, 4224–4243,
https://doi.org/10.1002/2014WR016395, 2015.
Lartillot, N. and Philippe, H.: Computing Bayes factors using thermodynamic
integration, Syst. Biol., 55, 195–207, 2006.
Leeb, H. and Pötscher, B. M.: Model selection, Springer, Berlin, Germany,
889–925, https://doi.org/10.1007/978-3-540-71297-8-39, 2009.
Legates, D. R. and McCabe, G. J.: Evaluating the use of “goodnessof-fit”
measures in hydrologic and hydroclimatic model validation, Water Resour.
Res., 35, 233–241, 1999.
Leuning, R., Zhang, Y. Q., Rajaud, A., Cleugh, H., and Tu, K.: A simple
surface conductance model to estimate regional evaporation using MODIS leaf
area index and the Penman–Monteith equation, Water Resour. Res., 44, W10419, https://doi.org/10.1029/2007WR006562, 2008.
Liang, J., Zhang, L., Cao, X., Wen, J., Wang, J., and Wang, G.: Energy
balance in the semiarid area of the Loess Plateau, China, J. Geophys. Res.-Atmos., 122, 2155–2168, https://doi.org/10.1002/2015JD024572, 2017.
Li, S., Kang, S., Zhang, L., Ortega-Farias, S., Li, F., Du, T., Tong, L.,
Wang, S., Ingman, M., and Guo, W.: Measuring and modeling maize
evapotranspiration under plastic film-mulching condition, J. Hydrol., 503,
153–168, 2013.
Li, S., Zhang, L., Kang, S., Tong, L., Du, T., Hao, X., and Zhao, P.: Comparison of several surface resistance models for estimating crop evapotranspiration over the entire growing season in arid regions, Agr. Forest Meteorol., 208, 1–15, 2015.
Li, X., Cheng, G. D., Liu, S. M., Xiao, Q., Ma, M. G., Jin, R., Che, T.,
Liu, Q. H., Wang, W. Z., Qi, Y., Wen, J. G., Li, H. Y., Zhu, G. F., Guo, J.
W., Ran, Y. H., Wang, S. G., Zhu, Z. L., Zhou, J., Hu, X. L., and Xu, Z. W.:
Heihe Watershed Allied Telemetry Experimental Research (HiWATER): Scientific
objectives and experimental design, B. Am. Meteorol. Soc., 94, 1145–1160,
2013.
Liu, G., Liu, Y., Hafeez, M., Xu, D., and Vote, C.: Comparison of two methods to derive time series of actual evapotranspiration using eddy covariance
measurements in the southeastern Australia, J. Hydrol., 454–455, 1–6, 2012.
Liu, P., Elshall, A. S., Ye, M., Beerli, P., Zeng, X., Lu, D., and Tao, Y.:
Evaluating marginal likelihood with thermodynamic integration method and
comparison with several other numerical methods, Water Resour. Res., 52,
734–758, https://doi.org/10.1002/2014WR016718, 2016.
Liu, S. M., Xu, Z. W.,Wang,W. Z., Jia, Z. Z., Zhu, M. J., Bai, J., and Wang,
J. M.: A comparison of eddy-covariance and large aperture scintillometer
measurements with respect to the energy balanceclosure problem, Hydrol. Earth Syst. Sci., 15, 1291–1306, https://doi.org/10.5194/hess-15-1291-2011, 2011.
Marshall, L., Nott, D., and Sharma, A.: Hydrological model selection: A
Bayesian alternative, Water Resour. Res., 41, 3092–3100, https://doi.org/10.1029/2004WR003719, 2005.
Matheny, A. M., Bohrer, G., Stoy, P. C., Baker, I. T., Black, A. T., Desai,
A. R., Dietze, M. C., Gough, C. M., Ivanov, V. Y., Jassal, R. S., Novick, K. A., Schäfer, K. V. R., and Verbeeck, H.: Characterizing the diurnal
patterns of errors in the prediction of evapotranspiration by several
land-surface models: An NACP analysis, J. Geophys. Res.-Biogeo., 119,
1458–1473, 2014.
Monteith, J. L.: Evaporation and environment, Symp. Soc. Exp. Biol., 19,
205–234, 1965.
Morison, J. I. L., Baker, N. R., Mullineaux, P. M., and Davies, W. J.:
Improving water use in crop production, Philos. T. Roy. Soc. B, 363,
639–658, 2008.
Neal, R. M.: Markov chain sampling methods for Dirichlet process mixture
models, J. Comput. Graph. Stat., 9, 249–265, 2000.
Oncley, S. P., Foken, T., Vogt, R., Kohsiek, W., DeBruin, H., Bernhofer, C.,
Christen, A., Van Gorsel, E., Grantz, D., and Feigenwinter, C.: The energy
balance experiment EBEX-2000. Part I: Overview and energy balance, Bound.-Lay. Meteorol., 123, 1–28, https://doi.org/10.1007/s10546-007-9161-1, 2007.
Ortega-Farias, S., Olioso, A., Fuentes, S., and Valdes, H.: Latent heat flux
over a furrow-irrigated tomato crop using Penman–Monteith equation with a
variable surface canopy resistance, Agr. Water Manage., 82, 421–432, 2006.
Parlange, M. B. and Katul, G. G.: An advection-aridity evaporation model,
Water Resour. Res., 28, 127–132, 1992.
Poblete-Echeverria, C. and Ortega-Farias, S.: Estimation of actual
evapotranspiration for a drip-irrigated Merlot vineyard using a three-source
model, Irrig. Sci., 28, 65–78, 2009.
Priestley, C. H. B. and Taylor, R. J.: On the assessment of surface heat
flux and evaporation using large-scale parameters, Mon. Weather Rev., 100, 81–92, 1972.
Rana, G., Katerji, N., Ferrara, R. M., and Martinelli, N.: An operational
model to estimate hourly and daily crop evapotranspiration in hilly terrain:
validation on wheat and oat crops, Theor. Appl. Climatol., 103, 413–426, 2011.
Sadegh, M. and Vrugt J. A.: Approximate Bayesian Computation using Markov Chain Monte Carlo simulation: DREAM(ABC), Water Resour. Res., 50,
6767–6787, https://doi.org/10.1002/2014WR015386, 2014.
Samani, S., Ye, M., Zhang, F., Pei, Y. Z., Tang, G. P., Elshall, A. S., and
Moghaddam, A. A.: Impacts of prior parameter distributions on bayesian
evaluation of groundwater model complexity, Water Sci. Eng., 11, 89–100, https://doi.org/10.1016/j.wse.2018.06.001, 2018.
Schöniger, A., Wohling, T., Samaniego, L., and Nowak, W.: Model
selection on solid ground: Rigorous comparison of nine ways to evaluate
Bayesian model evidence, Water Resour. Res., 50, 9484–9513,
https://doi.org/10.1002/2014WR016062, 2014.
Schwarz, G.: Estimating the dimension of a model, Ann. Stat., 6, 461–464, https://doi.org/10.1214/aos/1176344136, 1978.
Sellers, P. J., Heiser, M. D., and Hall, F. G.: Relations between surface conductance and spectral vegetation indices at intermediate (100 m2 to 15 km2) length scales, J. Geophys. Res., 97, 19033–19059, 1992.
Shao, J.: An asymptotic theory for linear model selection, Statist. Sin., 7, 221–242, 1997.
Shuttleworth, W. J. and Gurney, R. J.: The theoretical relationship between
foliage temperature and canopy resistance in sparse crops, Q. J. Roy.
Meteorol. Soc., 116, 497–519, 1990.
Stannard, D. I.: Comparison of Penman-Monteith, Shuttleworth–Wallace, and
modified Priestley-Taylor evapotranspiration models for wildland vegetation
in semiarid rangeland, Water Resour. Res., 29, 1379–1392, 1993.
Stull, R. B.: An introduction to boundary layer meteorology, Kluwer Academic
Publ., the Netherlands, 255 pp., 1988.
Sumner, D. M. and Jacobs, J. M.: Utility of Penman–Monteith
Priestley–Taylor reference evapotranspiration, and pan evaporation methods
to estimate pasture evapotranspiration, J. Hydrol., 308, 81–104, 2005.
Szilagyi, J. and Jozsa, J.: New findings about the complementary relationship based evaporation estimation methods, J. Hydrol., 354, 171–186, 2008.
Thomsen, J., Bohrer, G., Matheny, M. V., Ivanov, Y., He, L., Renninger, H.,
and Schäfer, K.: Contrasting hydraulic strategies during dry soil
conditions in Quercus rubra and Acer rubrum in a sandy site in Michigan,
Forests, 4, 1106–1120, 2013.
Tsvang, L., Fedorov, M., Kader, B., Zubkovskii, S., Foken, T., Richter, S.,
and Zeleny, Y.: Turbulent exchange over a surface with chessboardtype
inhomogeneities, Bound.-Lay. Meteorol., 55, 141–160, 1991.
Vinukollu R, K., Wood, E. F., Ferguson, C. R., and Fisher, J. B.: Global
estimates of evapotranspiration for climate studies using multi-sensor
remote sensing data: evaluation of three process-based approaches, Remote
Sens. Environ., 115, 801–823, 2011.
Vrugt, J. A., ter Braak, C. J. F., Clark, M. P. J., Hyman, M., and Robinson,
B. A.: Treatment of input uncertainty in hydrologic modeling: Doing
hydrology backward with Markov chain Monte Carlo simulation, Water Resour.
Res., 44, W00B09, https://doi.org/10.1029/2007WR006720, 2008.
Vrugt, J. A., ter Braak, C. J. F., Diks, C. G. H., Higdon, D., Robinson, B.
A., and Hyman, J. M.: Accelerating Markov chain Monte Carlo simulation by
differential evolution with self-adaptive randomized subspace sampling, Int.
J. Nonlin. Sci. Numer. Simul., 10, 273–290, 2009.
Webb, E. K., Pearman, G. I., and Leuning, R.: Correction of flux measurements for density effects due to heat and water-vapor transfer, Q. J. Roy. Meteorol. Soc., 106, 85–100, 1980.
Willmott, C. J.: On the validation of models, Phys. Geogr., 2, 184–194, 1981.
Xie, W., Lewis, P. O., Fan, Y., Kuo, L., and Chen, M. H.: Improving marginal
likelihood estimaton for Bayesian phylogenetic model selection, Syst. Biol.,
60, 150–160, 2011.
Xu, C. Y. and Singh, V. P.: A review on monthly water balance models for
water resources investigations, Water Resour. Manage., 12, 31–50, 1998.
Xu, Z. W., Liu, S. M., Li, X., Shi, S. J.,Wang, J. M., Zhu, Z. L., Xu, T.
R., Wang, W. Z., and Ma, M. G.: Intercomparison of surface energy flux
measurement systems used during the HiWATERUSOEXE, J. Geophys. Res., 118,
13140–13157, 2014.
Ye, M., Neuman, S. P., and Meyer, P. D.: Maximum likelihood Bayesian
averaging of spatial variability models in unsaturated fractured tuff, Water
Resour. Res., 40, W05113, https://doi.org/10.1029/2003WR002557, 2004.
Ye, M., Meyer, P. D., and Neuman, S. P.: On model selection criteria in
multimodel analysis, Water Resour. Res., 44, W03428, https://doi.org/10.1029/2008WR006803, 2008.
Zhang, B., Kang, S., Li, F.,and Zhang, L.: Comparison of three
evapotranspiration models to Bowen ratio-energy balance method for vineyard
in an arid desert region of northwest China, Agr. Forest Meteorol., 148,
1629–1640, 2008.
Zhang, K., Ma, J., Zhu, G., Ma, T., Han, T., and Feng, L. L.: Parameter
sensitivity analysis and optimization for a satellite-based
evapotranspiration model across multiple sites using moderate resolution
imaging spectroradiometer and flux data, J. Geophys. Res.-Atmos., 122, 230–245, 2017.
Zhang, X. Y., Liu, C. X., Hu, B. X., and Zhang, G. N.: Uncertainty analysis
of multi-rate kinetics of uranium desorption from sediments, J. Contam.
Hydrol., 156, 1–15, 2014.
Zhu, G. F., Su, Y. H., Li, X., Zhang, K., and Li, C. B.: Estimating actual
evapotranspiration from an alpine grassland on Qinghai–Tibetan plateau
using a two-source model and parameter uncertainty analysis by Bayesian
approach, J. Hydrol., 476, 42–51, 2013.
Zhu, G. F., Li, X., Su, Y. H., Zhang, K., Bai, Y., Ma, J. Z., Li, C. B., Hu, X. L., and He, J. H.: Simultaneously assimilating multivariate data sets into the two-source evapotranspiration model by Bayesian approach: application to spring maize in an arid region of northwestern China, Geosci. Model Dev., 7, 1467–1482, https://doi.org/10.5194/gmd-7-1467-2014, 2014.
Short summary
Accurately evaluating evapotranspiration (ET) is a critical challenge in improving hydrological process modeling. Here we evaluated four ET models (PM, SW, PT–FC, and AA) under the Bayesian framework. Our results reveal that the SW model has the best performance. This is in part because the SW model captures the main physical mechanism in ET; the other part is that the key parameters, such as the extinction factor, could be well constrained with observation data.
Accurately evaluating evapotranspiration (ET) is a critical challenge in improving hydrological...
