Articles | Volume 24, issue 12
https://doi.org/10.5194/hess-24-5745-2020
© Author(s) 2020. 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-24-5745-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
| 
01 Dec 2020
Review article |
| 01 Dec 2020
| 01 Dec 2020
Last-decade progress in understanding and modeling the land surface processes on the Tibetan Plateau
Ministry of Education Key Laboratory for Earth System Modeling,
Department of Earth System Science, Tsinghua University, Beijing 100084,
China
Ministry of Education Ecological Field Station for East Asian
Migratory Birds, Beijing 100084, China
Donghai Zheng
National Tibetan Plateau Data Center, Key Laboratory of Tibetan
Environmental Changes and Land Surface Processes, Institute of Tibetan
Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
Ministry of Education Key Laboratory for Earth System Modeling,
Department of Earth System Science, Tsinghua University, Beijing 100084,
China
Center for Excellence in Tibetan Plateau Earth Sciences, Chinese
Academy of Sciences, Beijing 100101, China
Fan Yang
Ministry of Education Key Laboratory for Earth System Modeling,
Department of Earth System Science, Tsinghua University, Beijing 100084,
China
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Wenjun Tang, Kun Yang, Jun Qin, Xin Li, and Xiaolei Niu
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Yanbin Lei, Tandong Yao, Kun Yang, Zhu La, Yaoming Ma, and Broxton W. Bird
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-421, https://doi.org/10.5194/hess-2019-421, 2019
Revised manuscript not accepted
Yvan Orsolini, Martin Wegmann, Emanuel Dutra, Boqi Liu, Gianpaolo Balsamo, Kun Yang, Patricia de Rosnay, Congwen Zhu, Wenli Wang, Retish Senan, and Gabriele Arduini
The Cryosphere, 13, 2221–2239, https://doi.org/10.5194/tc-13-2221-2019, https://doi.org/10.5194/tc-13-2221-2019, 2019
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The Tibetan Plateau region exerts a considerable influence on regional climate, yet the snowpack over that region is poorly represented in both climate and forecast models due a large precipitation and snowfall bias. We evaluate the snowpack in state-of-the-art atmospheric reanalyses against in situ observations and satellite remote sensing products. Improved snow initialisation through better use of snow observations in reanalyses may improve medium-range to seasonal weather forecasts.
W. Qu, N. Hu, J. Fu, J. Lu, H. Lu, T. Lei, Z. Pang, X. Li, and L. Li
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLII-3, 1461–1465, https://doi.org/10.5194/isprs-archives-XLII-3-1461-2018, https://doi.org/10.5194/isprs-archives-XLII-3-1461-2018, 2018
Fan Yang, Hui Lu, Kun Yang, Jie He, Wei Wang, Jonathon S. Wright, Chengwei Li, Menglei Han, and Yishan Li
Hydrol. Earth Syst. Sci., 21, 5805–5821, https://doi.org/10.5194/hess-21-5805-2017, https://doi.org/10.5194/hess-21-5805-2017, 2017
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Wenjun Tang, Jun Qin, Kun Yang, Shaomin Liu, Ning Lu, and Xiaolei Niu
Atmos. Chem. Phys., 16, 2543–2557, https://doi.org/10.5194/acp-16-2543-2016, https://doi.org/10.5194/acp-16-2543-2016, 2016
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C. Xu, Y. M. Ma, A. Panday, Z. Y. Cong, K. Yang, Z. K. Zhu, J. M. Wang, P. M. Amatya, and L. Zhao
Atmos. Chem. Phys., 14, 3133–3149, https://doi.org/10.5194/acp-14-3133-2014, https://doi.org/10.5194/acp-14-3133-2014, 2014
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Subject: Hydrometeorology | Techniques and Approaches: Modelling approaches
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Hydrol. Earth Syst. Sci., 29, 45–65, https://doi.org/10.5194/hess-29-45-2025, https://doi.org/10.5194/hess-29-45-2025, 2025
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We present a new method to calculate the chance of heavy downpour and the maximum rainfall expected over a 25-year period. It is designed to analyse global climate models' reproduction of past and future climates. For the Nordic countries, it projects a wetter climate in the future with increased intensity but not necessarily more wet days. The analysis also shows that rainfall intensity is sensitive to future greenhouse gas emissions, while the number of wet days appears to be less affected.
Chien-Yu Tseng, Li-Pen Wang, and Christian Onof
Hydrol. Earth Syst. Sci., 29, 1–25, https://doi.org/10.5194/hess-29-1-2025, https://doi.org/10.5194/hess-29-1-2025, 2025
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This study presents a new algorithm to model convective storms. We used advanced tracking methods to analyse 165 storm events in Birmingham (UK) and reconstruct storm cell life cycles. We found that cell properties like intensity and size are interrelated and vary over time. The new algorithm, based on vine copulas, accurately simulates these properties and their evolution. It also integrates an exponential shape function for realistic rainfall patterns, enhancing its hydrological applicability.
Kenza Tazi, Andrew Orr, Javier Hernandez-González, Scott Hosking, and Richard E. Turner
Hydrol. Earth Syst. Sci., 28, 4903–4925, https://doi.org/10.5194/hess-28-4903-2024, https://doi.org/10.5194/hess-28-4903-2024, 2024
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This work aims to improve the understanding of precipitation patterns in High-mountain Asia, a crucial water source for around 1.9 billion people. Through a novel machine learning method, we generate high-resolution precipitation predictions, including the likelihoods of floods and droughts. Compared to state-of-the-art methods, our method is simpler to implement and more suitable for small datasets. The method also shows accuracy comparable to or better than existing benchmark datasets.
Peter E. Levy and the COSMOS-UK team
Hydrol. Earth Syst. Sci., 28, 4819–4836, https://doi.org/10.5194/hess-28-4819-2024, https://doi.org/10.5194/hess-28-4819-2024, 2024
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Having accurate up-to-date maps of soil moisture is important for many purposes. However, current modelled and remotely sensed maps are rather coarse and not very accurate. Here, we demonstrate a simple but accurate approach that is closely linked to direct measurements of soil moisture at a network sites across the UK, to the water balance (precipitation minus drainage and evaporation) measured at a large number of catchments (1212) and to remotely sensed satellite estimates.
Amy C. Green, Chris Kilsby, and András Bárdossy
Hydrol. Earth Syst. Sci., 28, 4539–4558, https://doi.org/10.5194/hess-28-4539-2024, https://doi.org/10.5194/hess-28-4539-2024, 2024
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Weather radar is a crucial tool in rainfall estimation, but radar rainfall estimates are subject to many error sources, with the true rainfall field unknown. A flexible model for simulating errors relating to the radar rainfall estimation process is implemented, inverting standard processing methods. This flexible and efficient model performs well in generating realistic weather radar images visually for a large range of event types.
Peng Huang, Agnès Ducharne, Lucia Rinchiuso, Jan Polcher, Laure Baratgin, Vladislav Bastrikov, and Eric Sauquet
Hydrol. Earth Syst. Sci., 28, 4455–4476, https://doi.org/10.5194/hess-28-4455-2024, https://doi.org/10.5194/hess-28-4455-2024, 2024
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We conducted a high-resolution hydrological simulation from 1959 to 2020 across France. We used a simple trial-and-error calibration to reduce the biases of the simulated water budget compared to observations. The selected simulation satisfactorily reproduces water fluxes, including their spatial contrasts and temporal trends. This work offers a reliable historical overview of water resources and a robust configuration for climate change impact analysis at the nationwide scale of France.
He Sun, Tandong Yao, Fengge Su, Wei Yang, and Deliang Chen
Hydrol. Earth Syst. Sci., 28, 4361–4381, https://doi.org/10.5194/hess-28-4361-2024, https://doi.org/10.5194/hess-28-4361-2024, 2024
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Our findings show that runoff in the Yarlung Zangbo (YZ) basin is primarily driven by rainfall, with the largest glacier runoff contribution in the downstream sub-basin. Annual runoff increased in the upper stream but decreased downstream due to varying precipitation patterns. It is expected to rise throughout the 21st century, mainly driven by increased rainfall.
Louise Arnal, Martyn P. Clark, Alain Pietroniro, Vincent Vionnet, David R. Casson, Paul H. Whitfield, Vincent Fortin, Andrew W. Wood, Wouter J. M. Knoben, Brandi W. Newton, and Colleen Walford
Hydrol. Earth Syst. Sci., 28, 4127–4155, https://doi.org/10.5194/hess-28-4127-2024, https://doi.org/10.5194/hess-28-4127-2024, 2024
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Forecasting river flow months in advance is crucial for water sectors and society. In North America, snowmelt is a key driver of flow. This study presents a statistical workflow using snow data to forecast flow months ahead in North American snow-fed rivers. Variations in the river flow predictability across the continent are evident, raising concerns about future predictability in a changing (snow) climate. The reproducible workflow hosted on GitHub supports collaborative and open science.
Annalina Lombardi, Barbara Tomassetti, Valentina Colaiuda, Ludovico Di Antonio, Paolo Tuccella, Mario Montopoli, Giovanni Ravazzani, Frank Silvio Marzano, Raffaele Lidori, and Giulia Panegrossi
Hydrol. Earth Syst. Sci., 28, 3777–3797, https://doi.org/10.5194/hess-28-3777-2024, https://doi.org/10.5194/hess-28-3777-2024, 2024
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The accurate estimation of precipitation and its spatial variability within a watershed is crucial for reliable discharge simulations. The study is the first detailed analysis of the potential usage of the cellular automata technique to merge different rainfall data inputs to hydrological models. This work shows an improvement in the performance of hydrological simulations when satellite and rain gauge data are merged.
Beijing Fang, Emanuele Bevacqua, Oldrich Rakovec, and Jakob Zscheischler
Hydrol. Earth Syst. Sci., 28, 3755–3775, https://doi.org/10.5194/hess-28-3755-2024, https://doi.org/10.5194/hess-28-3755-2024, 2024
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We use grid-based runoff from a hydrological model to identify large spatiotemporally connected flood events in Europe, assess extent trends over the last 70 years, and attribute the trends to different drivers. Our findings reveal a general increase in flood extent, with regional variations driven by diverse factors. The study not only enables a thorough examination of flood events across multiple basins but also highlights the potential challenges arising from changing flood extents.
Alexandre Devers, Jean-Philippe Vidal, Claire Lauvernet, Olivier Vannier, and Laurie Caillouet
Hydrol. Earth Syst. Sci., 28, 3457–3474, https://doi.org/10.5194/hess-28-3457-2024, https://doi.org/10.5194/hess-28-3457-2024, 2024
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Daily streamflow series for 661 near-natural French catchments are reconstructed over 1871–2012 using two ensemble datasets: HydRE and HydREM. They include uncertainties coming from climate forcings, streamflow measurement, and hydrological model error (for HydrREM). Comparisons with other hydrological reconstructions and independent/dependent observations show the added value of the two reconstructions in terms of quality, uncertainty estimation, and representation of extremes.
María Agostina Bracalenti, Omar V. Müller, Miguel A. Lovino, and Ernesto Hugo Berbery
Hydrol. Earth Syst. Sci., 28, 3281–3303, https://doi.org/10.5194/hess-28-3281-2024, https://doi.org/10.5194/hess-28-3281-2024, 2024
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The Gran Chaco is a large, dry forest in South America that has been heavily deforested, particularly in the dry Chaco subregion. This deforestation, mainly driven by the expansion of the agricultural frontier, has changed the land's characteristics, affecting the local and regional climate. The study reveals that deforestation has resulted in reduced precipitation, soil moisture, and runoff, and if intensive agriculture continues, it could make summers in this arid region even drier and hotter.
Rutong Liu, Jiabo Yin, Louise Slater, Shengyu Kang, Yuanhang Yang, Pan Liu, Jiali Guo, Xihui Gu, Xiang Zhang, and Aliaksandr Volchak
Hydrol. Earth Syst. Sci., 28, 3305–3326, https://doi.org/10.5194/hess-28-3305-2024, https://doi.org/10.5194/hess-28-3305-2024, 2024
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Climate change accelerates the water cycle and alters the spatiotemporal distribution of hydrological variables, thus complicating the projection of future streamflow and hydrological droughts. We develop a cascade modeling chain to project future bivariate hydrological drought characteristics over China, using five bias-corrected global climate model outputs under three shared socioeconomic pathways, five hydrological models, and a deep-learning model.
Lu Su, Dennis P. Lettenmaier, Ming Pan, and Benjamin Bass
Hydrol. Earth Syst. Sci., 28, 3079–3097, https://doi.org/10.5194/hess-28-3079-2024, https://doi.org/10.5194/hess-28-3079-2024, 2024
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We fine-tuned the variable infiltration capacity (VIC) and Noah-MP models across 263 river basins in the Western US. We developed transfer relationships to similar basins and extended the fine-tuned parameters to ungauged basins. Both models performed best in humid areas, and the skills improved post-calibration. VIC outperforms Noah-MP in all but interior dry basins following regionalization. VIC simulates annual mean streamflow and high flow well, while Noah-MP performs better for low flows.
Iván Noguera, Jamie Hannaford, and Maliko Tanguy
EGUsphere, https://doi.org/10.5194/egusphere-2024-1969, https://doi.org/10.5194/egusphere-2024-1969, 2024
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In this study, we present a detailed characterisation of flash drought in United Kingdom over the period 1969–2021.The spatiotemporal distribution of flash droughts is highly variable, with important regional and seasonal contrasts. In the UK, flash drought occurrence responds primarily to precipitation variability, although the atmospheric evaporative demand (AED) is important as a secondary driver. The atmospheric and oceanic conditions during flash droughts development were also analyzed.
Geert Lenderink, Nikolina Ban, Erwan Brisson, Ségolène Berthou, Virginia Edith Cortés-Hernández, Elizabeth Kendon, Hayley Fowler, and Hylke de Vries
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-132, https://doi.org/10.5194/hess-2024-132, 2024
Revised manuscript accepted for HESS
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Future extreme rainfall events are influenced by changes in both absolute and relative humidity. The impact of increasing absolute humidity is reasonably well understood, but the role of relative humidity decreases over land remains largely unknown. Using hourly observations from France and The Netherlands, we find that lower relative humidity generally leads to more intense rainfall extremes. This relation is only captured well in recently developed convection-permitting climate models.
Valentin Dura, Guillaume Evin, Anne-Catherine Favre, and David Penot
Hydrol. Earth Syst. Sci., 28, 2579–2601, https://doi.org/10.5194/hess-28-2579-2024, https://doi.org/10.5194/hess-28-2579-2024, 2024
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The increase in precipitation as a function of elevation is poorly understood in areas with complex topography. In this article, the reproduction of these orographic gradients is assessed with several precipitation products. The best product is a simulation from a convection-permitting regional climate model. The corresponding seasonal gradients vary significantly in space, with higher values for the first topographical barriers exposed to the dominant air mass circulations.
Mohammad Ali Farmani, Ali Behrangi, Aniket Gupta, Ahmad Tavakoly, Matthew Geheran, and Guo-Yue Niu
EGUsphere, https://doi.org/10.5194/egusphere-2024-1256, https://doi.org/10.5194/egusphere-2024-1256, 2024
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This study investigates how key hydrological processes enhance soil water retention and release in land surface models, crucial for accurate weather and climate forecasting. Experiments show that soil hydraulics effectively sustain soil moisture. Additionally, allowing surface water ponding and improving soil permeability through macropores both enhance soil moisture persistency in the models.
Caroline Legrand, Benoît Hingray, Bruno Wilhelm, and Martin Ménégoz
Hydrol. Earth Syst. Sci., 28, 2139–2166, https://doi.org/10.5194/hess-28-2139-2024, https://doi.org/10.5194/hess-28-2139-2024, 2024
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Climate change is expected to increase flood hazard worldwide. The evolution is typically estimated from multi-model chains, where regional hydrological scenarios are simulated from weather scenarios derived from coarse-resolution atmospheric outputs of climate models. We show that two such chains are able to reproduce, from an atmospheric reanalysis, the 1902–2009 discharge variations and floods of the upper Rhône alpine river, provided that the weather scenarios are bias-corrected.
Nenghan Wan, Xiaomao Lin, Roger A. Pielke Sr., Xubin Zeng, and Amanda M. Nelson
Hydrol. Earth Syst. Sci., 28, 2123–2137, https://doi.org/10.5194/hess-28-2123-2024, https://doi.org/10.5194/hess-28-2123-2024, 2024
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Global warming occurs at a rate of 0.21 K per decade, resulting in about 9.5 % K−1 of water vapor response to temperature from 1993 to 2021. Terrestrial areas experienced greater warming than the ocean, with a ratio of 2 : 1. The total precipitable water change in response to surface temperature changes showed a variation around 6 % K−1–8 % K−1 in the 15–55° N latitude band. Further studies are needed to identify the mechanisms leading to different water vapor responses.
Kyungmin Sung, Max C. A. Torbenson, and James H. Stagge
Hydrol. Earth Syst. Sci., 28, 2047–2063, https://doi.org/10.5194/hess-28-2047-2024, https://doi.org/10.5194/hess-28-2047-2024, 2024
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This study examines centuries of nonstationary trends in meteorological drought and pluvial climatology. A novel approach merges tree-ring proxy data (North American Seasonal Precipitation Atlas – NASPA) with instrumental precipitation datasets by temporally downscaling proxy data, correcting biases, and analyzing shared trends in normal and extreme precipitation anomalies. We identify regions experiencing recent unprecedented shifts towards drier or wetter conditions and shifts in seasonality.
Baoying Shan, Niko E. C. Verhoest, and Bernard De Baets
Hydrol. Earth Syst. Sci., 28, 2065–2080, https://doi.org/10.5194/hess-28-2065-2024, https://doi.org/10.5194/hess-28-2065-2024, 2024
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This study developed a convenient and new method to identify the occurrence of droughts, heatwaves, and co-occurring droughts and heatwaves (CDHW) across four seasons. Using this method, we could establish the start and/or end dates of drought (or heatwave) events. We found an increase in the frequency of heatwaves and CDHW events in Belgium caused by climate change. We also found that different months have different chances of CDHW events.
Alexis Bédard-Therrien, François Anctil, Julie M. Thériault, Olivier Chalifour, Fanny Payette, Alexandre Vidal, and Daniel F. Nadeau
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-78, https://doi.org/10.5194/hess-2024-78, 2024
Preprint under review for HESS
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Observations from a study site network in eastern Canada showed a temperature interval the overlapping probabilities for rain, snow or a mix of both. Models using random forest algorithms were developed to classify the precipitation phase using meteorological data to evaluate operational applications. They showed significantly improved phase classification compared to benchmarks, but misclassification led to costlier errors. However, accurate prediction of mixed phase remains a challenge.
Felipe Lobos-Roco, Jordi Vilà-Guerau de Arellano, and Camilo de Rio
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-110, https://doi.org/10.5194/hess-2024-110, 2024
Revised manuscript accepted for HESS
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Water resources are fundamental for social, economic, and natural development of (semi-)arid regions. Precipitation decreases due to climate change obligates us to find new water resources. Fog harvesting emerges as a complementary one in regions where it is abundant but untapped. This research proposes a model to estimate fog harvesting potential in coastal (semi-)arid regions. This model could have broader applicability worldwide in regions where fog harvesting could be a viable water source.
Lorenzo Silvestri, Miriam Saraceni, Giulia Passadore, and Paolina Bongioannini Cerlini
EGUsphere, https://doi.org/10.5194/egusphere-2024-889, https://doi.org/10.5194/egusphere-2024-889, 2024
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This work demonstrates that seasonal forecasts of soil moisture are a valuable resource for groundwater management in certain areas of the Central Mediterranean. In particular, they show significant correlation coefficients and forecast skill for the deepest soil moisture at 289 cm depth. Wet and dry events can be predicted 6 months in advance and, in general, dry events are better captured than wet events.
Georgina M. Falster, Nicky M. Wright, Nerilie J. Abram, Anna M. Ukkola, and Benjamin J. Henley
Hydrol. Earth Syst. Sci., 28, 1383–1401, https://doi.org/10.5194/hess-28-1383-2024, https://doi.org/10.5194/hess-28-1383-2024, 2024
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Multi-year droughts have severe environmental and economic impacts, but the instrumental record is too short to characterise multi-year drought variability. We assessed the nature of Australian multi-year droughts using simulations of the past millennium from 11 climate models. We show that multi-decadal
megadroughtsare a natural feature of the Australian hydroclimate. Human-caused climate change is also driving a tendency towards longer droughts in eastern and southwestern Australia.
Kyle R. Mankin, Sushant Mehan, Timothy R. Green, and David M. Barnard
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-58, https://doi.org/10.5194/hess-2024-58, 2024
Revised manuscript accepted for HESS
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We assess 60 gridded climate datasets [ground- (G), satellite- (S), reanalysis-based (R)]. Higher-density station data and less-hilly terrain improved climate data. In mountainous and humid regions, dataset types performed similarly; but R outperformed G when underlying data had low station density. G outperformed S or R datasets, though better streamflow modeling did not always follow. Hydrologic analyses need datasets that better represent climate variable dependencies and complex topography.
Urmin Vegad, Yadu Pokhrel, and Vimal Mishra
Hydrol. Earth Syst. Sci., 28, 1107–1126, https://doi.org/10.5194/hess-28-1107-2024, https://doi.org/10.5194/hess-28-1107-2024, 2024
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A large population is affected by floods, which leave their footprints through human mortality, migration, and damage to agriculture and infrastructure, during almost every summer monsoon season in India. Despite the massive damage of floods, sub-basin level flood risk assessment is still in its infancy and needs to be improved. Using hydrological and hydrodynamic models, we reconstructed sub-basin level observed floods for the 1901–2020 period.
Qi Sun, Patrick Olschewski, Jianhui Wei, Zhan Tian, Laixiang Sun, Harald Kunstmann, and Patrick Laux
Hydrol. Earth Syst. Sci., 28, 761–780, https://doi.org/10.5194/hess-28-761-2024, https://doi.org/10.5194/hess-28-761-2024, 2024
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Tropical cyclones (TCs) often cause high economic loss due to heavy winds and rainfall, particularly in densely populated regions such as the Pearl River Delta (China). This study provides a reference to set up regional climate models for TC simulations. They contribute to a better TC process understanding and assess the potential changes and risks of TCs in the future. This lays the foundation for hydrodynamical modelling, from which the cities' disaster management and defence could benefit.
Simon Parry, Jonathan D. Mackay, Thomas Chitson, Jamie Hannaford, Eugene Magee, Maliko Tanguy, Victoria A. Bell, Katie Facer-Childs, Alison Kay, Rosanna Lane, Robert J. Moore, Stephen Turner, and John Wallbank
Hydrol. Earth Syst. Sci., 28, 417–440, https://doi.org/10.5194/hess-28-417-2024, https://doi.org/10.5194/hess-28-417-2024, 2024
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We studied drought in a dataset of possible future river flows and groundwater levels in the UK and found different outcomes for these two sources of water. Throughout the UK, river flows are likely to be lower in future, with droughts more prolonged and severe. However, whilst these changes are also found in some boreholes, in others, higher levels and less severe drought are indicated for the future. This has implications for the future balance between surface water and groundwater below.
Francesco Marra, Marika Koukoula, Antonio Canale, and Nadav Peleg
Hydrol. Earth Syst. Sci., 28, 375–389, https://doi.org/10.5194/hess-28-375-2024, https://doi.org/10.5194/hess-28-375-2024, 2024
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We present a new physical-based method for estimating extreme sub-hourly precipitation return levels (i.e., intensity–duration–frequency, IDF, curves), which are critical for the estimation of future floods. The proposed model, named TENAX, incorporates temperature as a covariate in a physically consistent manner. It has only a few parameters and can be easily set for any climate station given sub-hourly precipitation and temperature data are available.
Alexander Gelfan, Andrey Panin, Andrey Kalugin, Polina Morozova, Vladimir Semenov, Alexey Sidorchuk, Vadim Ukraintsev, and Konstantin Ushakov
Hydrol. Earth Syst. Sci., 28, 241–259, https://doi.org/10.5194/hess-28-241-2024, https://doi.org/10.5194/hess-28-241-2024, 2024
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Paleogeographical data show that 17–13 ka BP, the Caspian Sea level was 80 m above the current level. There are large disagreements on the genesis of this “Great” Khvalynian transgression of the sea, and we tried to shed light on this issue. Using climate and hydrological models as well as the paleo-reconstructions, we proved that the transgression could be initiated solely by hydroclimatic factors within the deglaciation period in the absence of the glacial meltwater effect.
Joeri B. Reinders and Samuel E. Munoz
Hydrol. Earth Syst. Sci., 28, 217–227, https://doi.org/10.5194/hess-28-217-2024, https://doi.org/10.5194/hess-28-217-2024, 2024
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Flooding presents a major hazard for people and infrastructure along waterways; however, it is challenging to study the likelihood of a flood magnitude occurring regionally due to a lack of long discharge records. We show that hydroclimatic variables like Köppen climate regions and precipitation intensity explain part of the variance in flood frequency distributions and thus reduce the uncertainty of flood probability estimates. This gives water managers a tool to locally improve flood analysis.
Mehrad Rahimpour Asenjan, Francois Brissette, Jean-Luc Martel, and Richard Arsenault
Hydrol. Earth Syst. Sci., 27, 4355–4367, https://doi.org/10.5194/hess-27-4355-2023, https://doi.org/10.5194/hess-27-4355-2023, 2023
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Climate models are central to climate change impact studies. Some models project a future deemed too hot by many. We looked at how including hot models may skew the result of impact studies. Applied to hydrology, this study shows that hot models do not systematically produce hydrological outliers.
Ross Pidoto and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 3957–3975, https://doi.org/10.5194/hess-27-3957-2023, https://doi.org/10.5194/hess-27-3957-2023, 2023
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Long continuous time series of meteorological variables (i.e. rainfall, temperature) are required for the modelling of floods. Observed time series are generally too short or not available. Weather generators are models that reproduce observed weather time series. This study extends an existing station-based rainfall model into space by enforcing observed spatial rainfall characteristics. To model other variables (i.e. temperature) the model is then coupled to a simple resampling approach.
Kajsa Maria Parding, Rasmus Emil Benestad, Anita Verpe Dyrrdal, and Julia Lutz
Hydrol. Earth Syst. Sci., 27, 3719–3732, https://doi.org/10.5194/hess-27-3719-2023, https://doi.org/10.5194/hess-27-3719-2023, 2023
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Intensity–duration–frequency (IDF) curves describe the likelihood of extreme rainfall and are used in hydrology and engineering, for example, for flood forecasting and water management. We develop a model to estimate IDF curves from daily meteorological observations, which are more widely available than the observations on finer timescales (minutes to hours) that are needed for IDF calculations. The method is applied to all data at once, making it efficient and robust to individual errors.
Kaltrina Maloku, Benoit Hingray, and Guillaume Evin
Hydrol. Earth Syst. Sci., 27, 3643–3661, https://doi.org/10.5194/hess-27-3643-2023, https://doi.org/10.5194/hess-27-3643-2023, 2023
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High-resolution precipitation data, needed for many applications in hydrology, are typically rare. Such data can be simulated from daily precipitation with stochastic disaggregation. In this work, multiplicative random cascades are used to disaggregate time series of 40 min precipitation from daily precipitation for 81 Swiss stations. We show that very relevant statistics of precipitation are obtained when precipitation asymmetry is accounted for in a continuous way in the cascade generator.
Theresa Boas, Heye Reemt Bogena, Dongryeol Ryu, Harry Vereecken, Andrew Western, and Harrie-Jan Hendricks Franssen
Hydrol. Earth Syst. Sci., 27, 3143–3167, https://doi.org/10.5194/hess-27-3143-2023, https://doi.org/10.5194/hess-27-3143-2023, 2023
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In our study, we tested the utility and skill of a state-of-the-art forecasting product for the prediction of regional crop productivity using a land surface model. Our results illustrate the potential value and skill of combining seasonal forecasts with modelling applications to generate variables of interest for stakeholders, such as annual crop yield for specific cash crops and regions. In addition, this study provides useful insights for future technical model evaluations and improvements.
Yuanhong You, Chunlin Huang, Zuo Wang, Jinliang Hou, Ying Zhang, and Peipei Xu
Hydrol. Earth Syst. Sci., 27, 2919–2933, https://doi.org/10.5194/hess-27-2919-2023, https://doi.org/10.5194/hess-27-2919-2023, 2023
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This study aims to investigate the performance of a genetic particle filter which was used as a snow data assimilation scheme across different snow climates. The results demonstrated that the genetic algorithm can effectively solve the problem of particle degeneration and impoverishment in a particle filter algorithm. The system has revealed a low sensitivity to the particle number in point-scale application of the ground snow depth measurement.
Patricia Lawston-Parker, Joseph A. Santanello Jr., and Nathaniel W. Chaney
Hydrol. Earth Syst. Sci., 27, 2787–2805, https://doi.org/10.5194/hess-27-2787-2023, https://doi.org/10.5194/hess-27-2787-2023, 2023
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Irrigation has been shown to impact weather and climate, but it has only recently been considered in prediction models. Prescribing where (globally) irrigation takes place is important to accurately simulate its impacts on temperature, humidity, and precipitation. Here, we evaluated three different irrigation maps in a weather model and found that the extent and intensity of irrigated areas and their boundaries are important drivers of weather impacts resulting from human practices.
Marcos Julien Alexopoulos, Hannes Müller-Thomy, Patrick Nistahl, Mojca Šraj, and Nejc Bezak
Hydrol. Earth Syst. Sci., 27, 2559–2578, https://doi.org/10.5194/hess-27-2559-2023, https://doi.org/10.5194/hess-27-2559-2023, 2023
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For rainfall-runoff simulation of a certain area, hydrological models are used, which requires precipitation data and temperature data as input. Since these are often not available as observations, we have tested simulation results from atmospheric models. ERA5-Land and COSMO-REA6 were tested for Slovenian catchments. Both lead to good simulations results. Their usage enables the use of rainfall-runoff simulation in unobserved catchments as a requisite for, e.g., flood protection measures.
Tuantuan Zhang, Zhongmin Liang, Wentao Li, Jun Wang, Yiming Hu, and Binquan Li
Hydrol. Earth Syst. Sci., 27, 1945–1960, https://doi.org/10.5194/hess-27-1945-2023, https://doi.org/10.5194/hess-27-1945-2023, 2023
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We use circulation classifications and spatiotemporal deep neural networks to correct raw daily forecast precipitation by combining large-scale circulation patterns with local spatiotemporal information. We find that the method not only captures the westward and northward movement of the western Pacific subtropical high but also shows substantially higher bias-correction capabilities than existing standard methods in terms of spatial scale, timescale, and intensity.
Zeyu Xue, Paul Ullrich, and Lai-Yung Ruby Leung
Hydrol. Earth Syst. Sci., 27, 1909–1927, https://doi.org/10.5194/hess-27-1909-2023, https://doi.org/10.5194/hess-27-1909-2023, 2023
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We examine the sensitivity and robustness of conclusions drawn from the PGW method over the NEUS by conducting multiple PGW experiments and varying the perturbation spatial scales and choice of perturbed meteorological variables to provide a guideline for this increasingly popular regional modeling method. Overall, we recommend PGW experiments be performed with perturbations to temperature or the combination of temperature and wind at the gridpoint scale, depending on the research question.
Louise J. Slater, Louise Arnal, Marie-Amélie Boucher, Annie Y.-Y. Chang, Simon Moulds, Conor Murphy, Grey Nearing, Guy Shalev, Chaopeng Shen, Linda Speight, Gabriele Villarini, Robert L. Wilby, Andrew Wood, and Massimiliano Zappa
Hydrol. Earth Syst. Sci., 27, 1865–1889, https://doi.org/10.5194/hess-27-1865-2023, https://doi.org/10.5194/hess-27-1865-2023, 2023
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Hybrid forecasting systems combine data-driven methods with physics-based weather and climate models to improve the accuracy of predictions for meteorological and hydroclimatic events such as rainfall, temperature, streamflow, floods, droughts, tropical cyclones, or atmospheric rivers. We review recent developments in hybrid forecasting and outline key challenges and opportunities in the field.
Zexuan Xu, Erica R. Siirila-Woodburn, Alan M. Rhoades, and Daniel Feldman
Hydrol. Earth Syst. Sci., 27, 1771–1789, https://doi.org/10.5194/hess-27-1771-2023, https://doi.org/10.5194/hess-27-1771-2023, 2023
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The goal of this study is to understand the uncertainties of different modeling configurations for simulating hydroclimate responses in the mountainous watershed. We run a group of climate models with various configurations and evaluate them against various reference datasets. This paper integrates a climate model and a hydrology model to have a full understanding of the atmospheric-through-bedrock hydrological processes.
Jolanda J. E. Theeuwen, Arie Staal, Obbe A. Tuinenburg, Bert V. M. Hamelers, and Stefan C. Dekker
Hydrol. Earth Syst. Sci., 27, 1457–1476, https://doi.org/10.5194/hess-27-1457-2023, https://doi.org/10.5194/hess-27-1457-2023, 2023
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Evaporation changes over land affect rainfall over land via moisture recycling. We calculated the local moisture recycling ratio globally, which describes the fraction of evaporated moisture that rains out within approx. 50 km of its source location. This recycling peaks in summer as well as over wet and elevated regions. Local moisture recycling provides insight into the local impacts of evaporation changes and can be used to study the influence of regreening on local rainfall.
Eleonora Dallan, Francesco Marra, Giorgia Fosser, Marco Marani, Giuseppe Formetta, Christoph Schär, and Marco Borga
Hydrol. Earth Syst. Sci., 27, 1133–1149, https://doi.org/10.5194/hess-27-1133-2023, https://doi.org/10.5194/hess-27-1133-2023, 2023
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Convection-permitting climate models could represent future changes in extreme short-duration precipitation, which is critical for risk management. We use a non-asymptotic statistical method to estimate extremes from 10 years of simulations in an orographically complex area. Despite overall good agreement with rain gauges, the observed decrease of hourly extremes with elevation is not fully represented by the model. Climate model adjustment methods should consider the role of orography.
Bora Shehu, Winfried Willems, Henrike Stockel, Luisa-Bianca Thiele, and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 1109–1132, https://doi.org/10.5194/hess-27-1109-2023, https://doi.org/10.5194/hess-27-1109-2023, 2023
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Rainfall volumes at varying duration and frequencies are required for many engineering water works. These design volumes have been provided by KOSTRA-DWD in Germany. However, a revision of the KOSTRA-DWD is required, in order to consider the recent state-of-the-art and additional data. For this purpose, in our study, we investigate different methods and data available to achieve the best procedure that will serve as a basis for the development of the new KOSTRA-DWD product.
Sandra M. Hauswirth, Marc F. P. Bierkens, Vincent Beijk, and Niko Wanders
Hydrol. Earth Syst. Sci., 27, 501–517, https://doi.org/10.5194/hess-27-501-2023, https://doi.org/10.5194/hess-27-501-2023, 2023
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Forecasts on water availability are important for water managers. We test a hybrid framework based on machine learning models and global input data for generating seasonal forecasts. Our evaluation shows that our discharge and surface water level predictions are able to create reliable forecasts up to 2 months ahead. We show that a hybrid framework, developed for local purposes and combined and rerun with global data, can create valuable information similar to large-scale forecasting models.
Richard Arsenault, Jean-Luc Martel, Frédéric Brunet, François Brissette, and Juliane Mai
Hydrol. Earth Syst. Sci., 27, 139–157, https://doi.org/10.5194/hess-27-139-2023, https://doi.org/10.5194/hess-27-139-2023, 2023
Short summary
Short summary
Predicting flow in rivers where no observation records are available is a daunting task. For decades, hydrological models were set up on these gauges, and their parameters were estimated based on the hydrological response of similar or nearby catchments where records exist. New developments in machine learning have now made it possible to estimate flows at ungauged locations more precisely than with hydrological models. This study confirms the performance superiority of machine learning models.
Cited articles
Bai, P., Liu, X. M., Yang, T. T., Liang, K., and Liu, C. M.: Evaluation of
streamflow simulation results of land surface models in GLDAS on the Tibetan
plateau, J. Geophys. Res.-Atmos., 121, 12180–12197,
2016.
Bao, H., Koike, T., Yang, K., Wang, L., Shrestha, M., and Lawford, P.:
Development of an enthalpy-based frozen soil model and its validation in a
cold region in China, J. Geophys. Res.-Atmos., 121,
5259–5280, https://doi.org/10.1002/2015jd024451, 2016.
Beljaars, A. C. M., Brown, A. R., and Wood, N.: A new parametrization of
turbulent orographic form drag, Q. J. Roy. Meteor. Soc., 130, 1327–1347,
https://doi.org/10.1256/qj.03.73, 2004.
Boone, A., de Rosnay, P., Balsamo, G., Beljaars, A., Chopin, F., Decharme,
B., Delire, C., Ducharne, A., Gascoin, S., Grippa, M., Guichard, F., Gusev,
Y., Harris, P., Jarlan, L., Kergoat, L., Mougin, E., Nasonova, O., Norgaard,
A., Orgeval, T., Ottle, C., Poccard-Leclercq, I., Polcher, J., Sandholt, I.,
Saux-Picart, S., Taylor, C., and Xue, Y. K.: The Amma Land Surface Model
Intercomparison Project (Almip), B. Am. Meteorol. Soc., 90, 1865–1880, 2009.
Chen, Y. Y., Yang, K., He, J., Qin, J., Shi, J. C., Du, J. Y., and He, Q.:
Improving land surface temperature modeling for dry land of China, J. Geophys. Res.-Atmos., 116, D20104, https://doi.org/10.1029/2011JD015921, 2011.
Chen, Y. Y., Yang, K., Tang, W. J., Qin, J., and Zhao, L.: Parameterizing
soil organic carbon's impacts on soil porosity and thermal parameters for
Eastern Tibet grasslands, Sci. China Earth Sci., 55, 1001–1011, 2012.
Chen, Y. Y., Yang, K., Qin, J., Zhao, L., Tang, W. J., and Han, M. L.:
Evaluation of AMSR-E retrievals and GLDAS simulations against observations
of a soil moisture network on the central Tibetan Plateau, J.
Geophys. Res.-Atmos., 118, 4466–4475, 2013.
Corbari, C., Mancini, M., Li, J., and Su, Z.: Can satellite land surface
temperature data be used similarly to river discharge measurements for
distributed hydrological model calibration?, Hydrolog. Sci.
J., 60, 202–217, https://doi.org/10.1080/02626667.2013.866709, 2015.
Dai, Y., Wei, N., Huang, A., Zhu, S., Shangguan, W., Yuan, H., Zhang, S.,
and Liu, S.: The lake scheme of the Common Land Model and its performance
evaluation, Chinese Sci. Bull., 63, 3002–3021, 2018.
Dai, Y., Xin, Q., Wei, N., Zhang, Y., Wei, S., Yuan, H., Zhang, S., Liu, S.,
and Lu, X.: A Global High-Resolution Data Set of Soil Hydraulic and Thermal
Properties for Land Surface Modeling, J. Adv. Model. Earth Sy., 11, 2996–3023,
https://doi.org/10.1029/2019ms001784, 2019.
Dai, Y. J., Zeng, X. B., Dickinson, R. E., Baker, I., Bonan, G. B.,
Bosilovich, M. G., Denning, A. S., Dirmeyer, P. A., Houser, P. R., Niu, G.
Y., Oleson, K. W., Schlosser, C. A., and Yang, Z. L.: The Common Land Model,
B. Am. Meteorol. Soc., 84, 1013–1023, 2003.
Dai, Y. J., Shangguan, W., Duan, Q. Y., Liu, B. Y., Fu, S. H., and Niu, G.:
Development of a China Dataset of Soil Hydraulic Parameters Using
Pedotransfer Functions for Land Surface Modeling, J. Hydrometeorol., 14,
869–887, 2013.
Dee, D. P., Uppala, S. M., Simmons, A. J., Berrisford, P., Poli, P., Kobayashi, S.,
Andrae, U., Balmaseda, M. A., Balsamo, G., Bauer, P., Bechtold, P., Beljaars,
A. C. M., van de Berg, L., Bidlot, J., Bormann, N., Delsol, C., Dragani, R.,
Fuentes, M., Geer, A. J., Haimberger, L., Healy, S. B., Hersbach, H., Hólm, E. V.,
Isaksen, L., Kållberg, P., Köhler, M., Matricardi, M., McNally, A. P.,
Monge-Sanz, B. M., Morcrette, J.-J., Park, B.-K., Peubey, C., de Rosnay, P.,
Tavolato, C., Thépaut, J.-N., and Vitart, F.: The ERA-Interim reanalysis:
configuration and performance of the data assimilation system, Q.
J. Roy. Meteor. Soc., 137, 553–597, https://doi.org/10.1002/qj.828,
2011 (data available at: http://apps.ecmwf.int/datasets/, last access: 01 November 2020).
Dickinson, R. E., Kennedy, P. J., and Henderson-Sellers, A.:
Biosphere-Atmosphere Transfer Scheme (BATS) version 1e as coupled to the
NCAR community climate model, National Center for Atmospheric Research,
Climate and Global Dynamics Division, 1993.
Dickinson, R. E., Oleson, K. W., Bonan, G., Hoffman, F., Thornton, P.,
Vertenstein, M., Yang, Z. L., and Zeng, X. B.: The Community Land Model and
its climate statistics as a component of the Community Climate System Model,
J. Climate, 19, 2302–2324, 2006.
Ding, B. H., Yang, K., Qin, J., Wang, L., Chen, Y. Y., and He, X. B.: The
dependence of precipitation types on surface elevation and meteorological
conditions and its parameterization, J. Hydrol., 513, 154–163, https://doi.org/10.1016/j.jhydrol.2014.03.038, 2014.
Ding, B. H., Yang, K., Yang, W., He, X. B., Chen, Y. Y., Lazhu, Guo, X. F.,
Wang, L., Wu, H., and Yao, T. D.: Development of a Water and Enthalpy
Budget-based Glacier mass balance Model (WEB-GM) and its preliminary
validation, Water Resour. Res., 53, 3146–3178, 2017.
Dirmeyer, P. A.: A History and Review of the Global Soil Wetness Project
(GSWP), J. Hydrometeorol., 12, 729–749, 2011.
Dirmeyer, P. A., Dolman, A. J., and Sato, N.: The pilot phase of the Global
Soil Wetness Project, B. Am. Meteorol. Soc., 80, 851–878, 1999.
Fang, N., Yang, K., Lazhu, Chen, Y., Wang, J., and Zhu, L.: Research on the
Application of WRF-Lake Modeling at Nam Co Lake on the Qinghai-Tibetan
Plateau, Plateau Meteorology, 36, 610–618, 2017.
FAO: The Digitized Soil Map of the World Including Derived Soil Properties
(version 3.6), available at: http://www.fao.org/geonetwork/srv/en/metadata.show?id=14116&currTab=distribution, last access: 01 November 2020), FAO, Rome, Italy, 2003.
FAO/IIASA/ISRIC/ISS-CAS/JRC: Harmonized World Soil Database (version 1.2), available at: http://webarchive.iiasa.ac.at/Research/LUC/External-World-soil-database/HTML/ (last access: 1 November 2020), FAO, Rome, Italy and IIASA, Laxenburg, Austria, 2012.
Farouki, O. T.: The Thermal-Properties of Soils in Cold Regions, Cold Reg.
Sci. Technol., 5, 67–75, 1981.
Gao, Y. H., Li, K., Chen, F., Jiang, Y. S., and Lu, C. G.: Assessing and
improving Noah-MP land model simulations for the central Tibetan Plateau,
J. Geophys. Rese.-Atmos., 120, 9258–9278, 2015.
Gelaro, R., McCarty, W., Suarez, M. J., Todling, R., Molod, A., Takacs, L.,
Randles, C. A., Darmenov, A., Bosilovich, M. G., Reichle, R., Wargan, K.,
Coy, L., Cullather, R., Draper, C., Akella, S., Buchard, V., Conaty, A., da
Silva, A. M., Gu, W., Kim, G. K., Koster, R., Lucchesi, R., Merkova, D.,
Nielsen, J. E., Partyka, G., Pawson, S., Putman, W., Rienecker, M.,
Schubert, S. D., Sienkiewicz, M., and Zhao, B.: The Modern-Era Retrospective
Analysis for Research and Applications, Version 2 (MERRA-2), J. Climate, 30,
5419–5454, https://doi.org/10.1175/JCLI-D-16-0758.1, 2017 (data available at: https://disc.gsfc.nasa.gov/datasets?keywords=MERRA-2&page=1, last access: 1 November 2020).
Gu, C., Huang, A., Wu, Y., Yang, B., Mu, X., Zhang, X., and Cai, S.: Effects
of Subgrid Terrain Radiative Forcing on the Ability of RegCM4.1 in the
Simulation of Summer Precipitation Over China, J. Geophys.
Res.-Atmos., 125, e2019JD032215, https://doi.org/10.1029/2019jd032215, 2020.
Gu, H., Jin, J., Wu, Y., Ek, M. B., and Subin, Z. M.: Calibration and
validation of lake surface temperature simulations with the coupled WRF-lake
model, Climatic Change, 129, 471–483, https://doi.org/10.1007/s10584-013-0978-y, 2015.
Guo, D. L. and Wang, H. J.: Simulation of permafrost and seasonally frozen
ground conditions on the Tibetan Plateau, 1981–2010, J. Geophys.
Res.-Atmos., 118, 5216–5230, https://doi.org/10.1002/jgrd.50457, 2013.
Guo, H.: Big Earth data: A new frontier in Earth and information sciences,
Big Earth Data, 1, 4–20, https://doi.org/10.1080/20964471.2017.1403062, 2017.
Han, C. B., Ma, Y. M., Su, Z. B., Chen, X. L., Zhang, L., Li, M. S., and
Sun, F. L.: Estimates of effective aerodynamic roughness length over
mountainous areas of the Tibetan Plateau, Q. J. Roy. Meteor. Soc., 141,
1457–1465, https://doi.org/10.1002/qj.2462, 2015.
He, J., Yang, K., Tang, W., Lu, H., Qin, J., Chen, Y., and Li, X.: The first
high-resolution meteorological forcing dataset for land process studies over
China, Scientific Data, 7, 25, https://doi.org/10.1038/s41597-020-0369-y, 2020.
He, S. W., Nan, Z. T., and Hou, Y. T.: Accuracy evaluation of two
precipitation datasets over upper reach of Heihe River Basin, northwestern
China, available at: http://www.scar.ac.cn/EN/10.3724/SP.J.1226.2015.00157 (last access: 1 November 2020), Sci. Cold Arid. Reg., 7, 157–169, 2015.
Henderson-Sellers, A., Yang, Z. L., and Dickinson, R. E.: The Project for
Intercomparison of Land-Surface Parameterization Schemes, B. Am. Meteorol. Soc.,
74, 1335–1349, 1993.
Henderson-Sellers, A., Pitman, A. J., Love, P. K., Irannejad, P., and Chen,
T. H.: The Project for Intercomparison of Land Surface Parameterization Schemes (PILPS): Phase 2 and Phase 3, B. Am. Meteorol. Soc., 76, 489–503, 1995.
Hengl, T., de Jesus, J. M., MacMillan, R. A., Batjes, N. H., Heuvelink, G.
B. M., Ribeiro, E., Samuel-Rosa, A., Kempen, B., Leenaars, J. G. B., Walsh,
M. G., and Gonzalez, M. R.: SoilGrids1km – Global Soil Information Based on
Automated Mapping, PLOS One, 9, e114788, https://doi.org/10.1371/journal.pone.0105992, 2014.
Huang, A., Lazhu, Wang, J., Dai, Y., Yang, K., Wei, N., Wen, L., Wu, Y.,
Zhu, X., Zhang, X., and Cai, S.: Evaluating and Improving the Performance of
Three 1-D Lake Models in a Large Deep Lake of the Central Tibetan Plateau,
J. Geophys. Res.-Atmos., 124, 3143–3167,
https://doi.org/10.1029/2018jd029610, 2019.
Hurrell, J. W., Holland, M. M., Gent, P. R., Ghan, S., Kay, J. E., Kushner,
P. J., Lamarque, J. F., Large, W. G., Lawrence, D., Lindsay, K., Lipscomb,
W. H., Long, M. C., Mahowald, N., Marsh, D. R., Neale, R. B., Rasch, P.,
Vavrus, S., Vertenstein, M., Bader, D., Collins, W. D., Hack, J. J., Kiehl,
J., and Marshall, S.: The Community Earth System Model A Framework for
Collaborative Research, B. Am. Meteorol. Soc., 94, 1339–1360, 2013.
Jimenez, C., Prigent, C., Mueller, B., Seneviratne, S. I., McCabe, M. F.,
Wood, E. F., Rossow, W. B., Balsamo, G., Betts, A. K., Dirmeyer, P. A.,
Fisher, J. B., Jung, M., Kanamitsu, M., Reichle, R. H., Reichstein, M.,
Rodell, M., Sheffield, J., Tu, K., and Wang, K.: Global intercomparison of
12 land surface heat flux estimates, J. Geophys.
Res.-Atmos., 116, D02102, https://doi.org/10.1029/2010jd014545, 2011.
Jing, W. L., Di, L. P., Zhao, X. D., Yao, L., Xia, X. L., Liu, Y. X., Yang,
J., Li, Y., and Zhou, C. H.: A data-driven approach to generate past
GRACE-like terrestrial water storage solution by calibrating the land
surface model simulations, Adv. Water Resour., 143, 103683,
https://doi.org/10.1016/j.advwatres.2020.103683, 2020.
Johansen, O.: Thermal conductivity of soils, PhD dissertation,
University of Trondheim, Trondheim, Norway, 236 pp., 1975.
Lazhu, Yang, K., Wang, J. B., Lei, Y. B., Chen, Y. Y., Zhu, L. P., Ding, B.
H., and Qin, J.: Quantifying evaporation and its decadal change for Lake Nam
Co, central Tibetan Plateau, J. Geophys. Res.-Atmos.,
121, 7578–7591, 2016.
Lee, W.-L., Liou, K. N., and Wang, C.-c.: Impact of 3-D topography on
surface radiation budget over the Tibetan Plateau, Theor. Appl.
Climatol., 113, 95–103, https://doi.org/10.1007/s00704-012-0767-y, 2013.
Lee, W.-L., Liou, K.-N., Wang, C.-c., Gu, Y., Hsu, H.-H., and Li, J.-L. F.:
Impact of 3-D Radiation-Topography Interactions on Surface Temperature and
Energy Budget Over the Tibetan Plateau in Winter, J. Geophys.
Res.-Atmos., 124, 1537–1549, https://doi.org/10.1029/2018jd029592, 2019.
Li, C., Lu, H., Leung, L. R., Yang, K., Li, H., Wang, W., Han, M., and Chen,
Y.: Improving Land Surface Temperature Simulation in CoLM Over the Tibetan
Plateau Through Fractional Vegetation Cover Derived From a Remotely Sensed
Clumping Index and Model-Simulated Leaf Area Index, J. Geophys.
Res.-Atmos., 124, 2620–2642, https://doi.org/10.1029/2018jd028640, 2019.
Li, C. W., Lu, H., Yang, K., Wright, J. S., Yu, L., Chen, Y. Y., Huang, X.
M., and Xu, S. M.: Evaluation of the Common Land Model (CoLM) from the
Perspective of Water and Energy Budget Simulation: Towards Inclusion in
CMIP6, Atmosphere-Basel, 8, 141, https://doi.org/10.3390/atmos8080141, 2017.
Li, C. W., Lu, H., Yang, K., Han, M. L., Wright, J. S., Chen, Y. Y., Yu, L.,
Xu, S. M., Huang, X. M., and Gong, W.: The Evaluation of SMAP Enhanced Soil
Moisture Products Using High-Resolution Model Simulations and In-Situ
Observations on the Tibetan Plateau, Remote Sens.-Basel, 10, 535, https://doi.org/10.3390/rs10040535, 2018.
Li, D., Yang, K., Tang, W. J., Li, X., Zhou, X., and Guo, D. L.:
Characterizing precipitation in high altitudes of the western Tibetan
plateau with a focus on major glacier areas, Int. J.
Climatol., 40, 5114–5127, https://doi.org/10.1002/joc.6509, 2020.
Li, J. D., Chen, F., Zhang, G., Barlage, M., Gan, Y. J., Xin, Y. F., and
Wang, C.: Impacts of Land Cover and Soil Texture Uncertainty on Land Model
Simulations Over the Central Tibetan Plateau, J. Adv. Model. Earth Sy., 10, 2121–2146, https://doi.org/10.1029/2018MS001377,
2018.
Li, Q. and Sun, S.: Development of the universal and simplified soil model
coupling heat and water transport, Sci. China Ser. D,
51, 88–102, https://doi.org/10.1007/s11430-007-0153-2, 2008.
Lin, C. G., Chen, D. L., Yang, K., and Ou, T. H.: Impact of model resolution
on simulating the water vapor transport through the central Himalayas:
implication for models' wet bias over the Tibetan Plateau, Clim. Dynam.,
51, 3195–3207, https://doi.org/10.1007/s00382-018-4074-x, 2018.
Liou, K. N., Lee, W.-L., and Hall, A.: Radiative transfer in mountains:
Application to the Tibetan Plateau, Geophys. Res. Lett., 34,
L23809, https://doi.org/10.1029/2007GL031762, 2007.
Liu, W., Sun, F., Li, Y., Zhang, G., Sang, Y.-F., Lim, W. H., Liu, J., Wang, H., and Bai, P.: Investigating water budget dynamics in 18 river basins across the Tibetan Plateau through multiple datasets, Hydrol. Earth Syst. Sci., 22, 351–371, https://doi.org/10.5194/hess-22-351-2018, 2018.
Lu, H., Koike, T., Yang, K., Hu, Z. Y., Xu, X. D., Rasmy, M., Kuria, D., and
Tamagawa, K.: Improving land surface soil moisture and energy flux
simulations over the Tibetan plateau by the assimilation of the microwave
remote sensing data and the GCM output into a land surface model,
Int. J. Appl. Earth Obs., 17,
43–54, https://doi.org/10.1016/j.jag.2011.09.006, 2012.
Luo, Q., Yang, K., Chen, Y., and Zhou, X.: Method development for estimating
soil organic carbon content in an alpine region using soil moisture data,
Sci. China Earth Sci., 63, 591–601, https://doi.org/10.1007/s11430-019-9554-8, 2020.
Luo, S. Q., Fang, X. W., Lyu, S. H., Zhang, Y., and Chen, B. L.: Improving
CLM4.5 Simulations of Land-Atmosphere Exchange during Freeze-Thaw Processes
on the Tibetan Plateau, J. Meteorol. Res.-Prc., 31, 916–930, 2017.
Luo, S. Q., Chen, B. L., Lyu, S. H., Fang, X. W., Wang, J. Y., Meng, X. H.,
Shang, L. Y., Wang, S. Y., and Ma, D.: An improvement of soil temperature
simulations on the Tibetan Plateau, available at: http://www.scar.ac.cn/EN/10.3724/SP.J.1226.2018.00080 (last access: 1 November 2020), Sci. Cold Arid. Reg., 10, 80–94, 2018.
Manabe, S.: Climate and Ocean Circulation: I. The Atmospheric Circulation and
Hydrology of the Earth's Surface, Mon. Weather Rev., 97, 739–774, https://doi.org/10.1175/1520-0493(1969)097<0739:CATOC>2.3.CO;2, 1969.
Oleson, K. W., Lawrence, D. M., Gordon, B., Flanner, M. G., Kluzek, E.,
Peter, J., Levis, S., Swenson, S. C., Thornton, E., and Feddema, J.:
Technical description of version 4.0 of the Community Land model (CLM), The
National Center for Atmospheric Research (NCAR), 2010.
Pan, M., Sahoo, A. K., Troy, T. J., Vinukollu, R. K., Sheffield, J., and
Wood, E. F.: Multisource Estimation of Long-Term Terrestrial Water Budget
for Major Global River Basins, J. Climate, 25, 3191–3206, 2012.
Pan, Y. J., Lyu, S. H., Li, S. S., Gao, Y. H., Meng, X. H., Ao, Y. H., and
Wang, S. J.: Simulating the role of gravel in freeze-thaw process on the
Qinghai-Tibet Plateau, Theor. Appl. Climatol., 127, 1011–1022, 2017.
Pinnington, E., Quaife, T., and Black, E.: Impact of remotely sensed soil moisture and precipitation on soil moisture prediction in a data assimilation system with the JULES land surface model, Hydrol. Earth Syst. Sci., 22, 2575–2588, https://doi.org/10.5194/hess-22-2575-2018, 2018.
Qi, W., Liu, J. G., and Chen, D. L.: Evaluations and Improvements of
GLDAS2.0 and GLDAS2.1 Forcing Data's Applicability for Basin Scale
Hydrological Simulations in the Tibetan Plateau, J. Geophys.
Res.-Atmos., 123, 13128–13148, https://doi.org/10.1029/2018jd029116, 2018.
Reichstein, M., Camps-Valls, G., Stevens, B., Jung, M., Denzler, J.,
Carvalhais, N., and Prabhat: Deep learning and process understanding for
data-driven Earth system science, Nature, 566, 195–204, https://doi.org/10.1038/s41586-019-0912-1, 2019.
Rienecker, M. M., Suarez, M. J., Gelaro, R., Todling, R., Bacmeister, J.,
Liu, E., Bosilovich, M. G., Schubert, S. D., Takacs, L., Kim, G. K., Bloom,
S., Chen, J. Y., Collins, D., Conaty, A., Da Silva, A., Gu, W., Joiner, J.,
Koster, R. D., Lucchesi, R., Molod, A., Owens, T., Pawson, S., Pegion, P.,
Redder, C. R., Reichle, R., Robertson, F. R., Ruddick, A. G., Sienkiewicz,
M., and Woollen, J.: MERRA: NASA's Modern-Era Retrospective Analysis for
Research and Applications, J. Climate, 24, 3624–3648, 2011.
Rodell, M., Houser, P. R., Jambor, U., Gottschalck, J., Mitchell, K., Meng,
C. J., Arsenault, K., Cosgrove, B., Radakovich, J., Bosilovich, M., Entin,
J. K., Walker, J. P., Lohmann, D., and Toll, D.: The global land data
assimilation system, B. Am. Meteorol. Soc., 85, 381–394, https://doi.org/10.1175/BAMS-85-3-381, 2004 (data available at: https://disc.gsfc.nasa.gov/datasets?page=1&keywords=GLDAS, last access: 1 November 2020).
Sellers, P. J., Mintz, Y., Sud, Y. C., and Dalcher, A.: A Simple Biosphere
Model (Sib) for Use within General-Circulation Models, J. Atmos. Sci., 43,
505–531, 1986.
Sellers, P. J., Randall, D. A., Collatz, G. J., Berry, J. A., Field, C. B.,
Dazlich, D. A., Zhang, C., Collelo, G. D., and Bounoua, L.: A revised land surface parameterization (SiB2) for atmospheric GCMs .1. Model formulation,
J. Climate, 9, 676–705, 1996.
Shangguan, W., Dai, Y. J., Liu, B. Y., Ye, A. Z., and Yuan, H.: A soil
particle-size distribution dataset for regional land and climate modelling
in China, Geoderma, 171, 85–91, 2012.
Shangguan, W., Dai, Y. J., Liu, B. Y., Zhu, A. X., Duan, Q. Y., Wu, L. Z.,
Ji, D. Y., Ye, A. Z., Yuan, H., Zhang, Q., Chen, D. D., Chen, M., Chu, J.
T., Dou, Y. J., Guo, J. X., Li, H. Q., Li, J. J., Liang, L., Liang, X., Liu,
H. P., Liu, S. Y., Miao, C. Y., and Zhang, Y. Z.: A China data set of soil
properties for land surface modeling, J. Adv. Model. Earth Sy., 5, 212–224,
2013.
Shangguan, W., Dai, Y. J., Duan, Q. Y., Liu, B. Y., and Yuan, H.: A global
soil data set for earth system modeling, J. Adv. Model. Earth Sy., 6, 249–263,
2014.
Shangguan, W., Hengl, T., de Jesus, J. M., Yuan, H., and Dai, Y. J.: Mapping
the global depth to bedrock for land surface modeling, J. Adv. Model. Earth Sy.,
9, 65–88, https://doi.org/10.1002/2016MS000686, 2017 (data available at: http://globalchange.bnu.edu.cn/research/data, last access: 1 November 2020).
Su, D., Hu, X., Wen, L., Lyu, S., Gao, X., Zhao, L., Li, Z., Du, J., and Kirillin, G.: Numerical study on the response of the largest lake in China to climate change, Hydrol. Earth Syst. Sci., 23, 2093–2109, https://doi.org/10.5194/hess-23-2093-2019, 2019.
Su, Z., Wen, J., Dente, L., van der Velde, R., Wang, L., Ma, Y., Yang, K., and Hu, Z.: The Tibetan Plateau observatory of plateau scale soil moisture and soil temperature (Tibet-Obs) for quantifying uncertainties in coarse resolution satellite and model products, Hydrol. Earth Syst. Sci., 15, 2303–2316, https://doi.org/10.5194/hess-15-2303-2011, 2011.
Su, Z., de Rosnay, P., Wen, J., Wang, L., and Zeng, Y.: Evaluation of
ECMWF's soil moisture analyses using observations on the Tibetan Plateau,
J. Geophys. Res.-Atmos., 118, 5304–5318,
https://doi.org/10.1002/jgrd.50468, 2013.
Sun, S., Yan, J., Xia, N., and Sun, C.: Development of a model for water and
heat exchange between the atmosphere and a water body, Adv.
Atmos. Sci., 24, 927–938, https://doi.org/10.1007/s00376-007-0927-7, 2007.
Sun, S. F., Jin, J. M., and Xue, Y. K.: A simple snow-atmosphere-soil
transfer model, J. Geophys. Res.-Atmos., 104,
19587–19597, https://doi.org/10.1029/1999jd900305, 1999.
Tong, K., Su, F. G., Yang, D. Q., and Hao, Z. C.: Evaluation of satellite
precipitation retrievals and their potential utilities in hydrologic
modeling over the Tibetan Plateau, J. Hydrol., 519, 423–437,
https://doi.org/10.1016/j.jhydrol.2014.07.044, 2014.
Wang, A. H. and Zeng, X. B.: Evaluation of multireanalysis products with in
situ observations over the Tibetan Plateau, J. Geophys.
Res.-Atmos., 117, D05102, https://doi.org/10.1029/2011JD016553, 2012.
Wang, A. H., Zeng, X. B., and Guo, D. L.: Estimates of Global Surface
Hydrology and Heat Fluxes from the Community Land Model (CLM4.5) with Four
Atmospheric Forcing Datasets, J. Hydrometeorol., 17, 2493–2510, 2016.
Wang, B., Ma, Y., Chen, X., Ma, W., Su, Z., and Menenti, M.: Observation and
simulation of lake-air heat and water transfer processes in a high-altitude
shallow lake on the Tibetan Plateau, J. Geophys.
Res.-Atmos., 120, 12327–12344, https://doi.org/10.1002/2015jd023863, 2015.
Wang, C. H. and Yang, K.: A New Scheme for Considering Soil Water-Heat
Transport Coupling Based on Community Land Model: Model Description and
Preliminary Validation, J. Adv. Model. Earth Sy., 10, 927–950, 2018.
Wang, L., Li, X. P., Chen, Y. Y., Yang, K., Chen, D. L., Zhou, J., Liu, W.
B., Qi, J., and Huang, J. B.: Validation of the global land data
assimilation system based on measurements of soil temperature profiles, Agr.
Forest Meteorol., 218, 288–297, 2016.
Wang, L., Zhou, J., Qi, J., Sun, L. T., Yang, K., Tian, L. D., Lin, Y. L.,
Liu, W. B., Shrestha, M., Xue, Y. K., Koike, T., Ma, Y. M., Li, X. P., Chen,
Y. Y., Chen, D. L., Piao, S. L., and Lu, H.: Development of a land surface
model with coupled snow and frozen soil physics, Water Resour. Res., 53,
5085–5103, 2017.
Wang, S., Liu, S. X., Mo, X. G., Peng, B., Qiu, J. X., Li, M. X., Liu, C.
M., Wang, Z. G., and Bauer-Gottwein, P.: Evaluation of Remotely Sensed
Precipitation and Its Performance for Streamflow Simulations in Basins of
the Southeast Tibetan Plateau, J. Hydrometeorol., 16, 2577–2594,
https://doi.org/10.1175/Jhm-D-14-0166.1, 2015.
Wang, W., Cui, W., Wang, X. J., and Chen, X.: Evaluation of GLDAS-1 and
GLDAS-2 Forcing Data and Noah Model Simulations over China at the Monthly
Scale, J. Hydrometeorol., 17, 2815–2833, 2016.
Wang, W., Yang, K., Zhao, L., Zheng, Z., Lu, H., Mamtimin, A., Ding, B., Li,
X., Zhao, L., Li, H., Che, T., and Moore, J. C.: Characterizing surface
albedo of shallow fresh snow and its importance for snow ablation on the
interior of the Tibetan Plateau, J. Hydrometeorol., 21, 815–827,
https://doi.org/10.1175/JHM-D-19-0193.1, 2020.
Wang, Y., Yang, K., Pan, Z. Y., Qin, J., Chen, D. L., Lin, C. G., Chen, Y.
Y., Lazhu, Tang, W. J., Han, M. L., Lu, N., and Wu, H.: Evaluation of
Precipitable Water Vapor from Four Satellite Products and Four Reanalysis
Datasets against GPS Measurements on the Southern Tibetan Plateau, J.
Climate, 30, 5699–5713, https://doi.org/10.1175/Jcli-D-16-0630.1, 2017.
Wang, Y., Yang, K., Zhou, X., Chen, D. L., Lu, H., Ouyang, L., Chen, Y. Y.,
Lazhu, and Wang, B. B.: Synergy of orographic drag parameterization and high
resolution greatly reduces biases of WRF-simulated precipitation in central
Himalaya, Clim. Dynam., 54, 1729–1740, 2020.
Wu, G., Duan, A., Liu, Y., Mao, J., Ren, R., Bao, Q., He, B., Liu, B., and
Hu, W.: Tibetan Plateau climate dynamics: recent research progress and
outlook, Natl. Sci. Rev., 2, 100–116, https://doi.org/10.1093/nsr/nwu045, 2015.
Wu, J. and Gao, X.-J.: A gridded daily observation dataset over China
region and comparison with the other datasets, available at: http://www.geophy.cn/EN/10.6038/cjg20130406 (last access: 1 November 2020), Chinese Journal of
Geophysics-Chinese Edition, 56, 1102–1111, 2013.
Xia, Y., Sheffield, J., Ek, M. B., Dong, J., Chaney, N., Wei, H., Meng, J.,
and Wood, E. F.: Evaluation of multi-model simulated soil moisture in
NLDAS-2, J. Hydrol., 512, 107–125, https://doi.org/10.1016/j.jhydrol.2014.02.027,
2014.
Xie, Z., Hu, Z., Gu, L., Sun, G., Du, Y., and Yan, X.: Meteorological
Forcing Datasets for Blowing Snow Modeling on the Tibetan Plateau:
Evaluation and Intercomparison, J. Hydrometeorol., 18, 2761–2780,
https://doi.org/10.1175/JHM-D-17-0075.1, 2017.
Xie, Z. H., Di, Z. H., Luo, Z. D., and Ma, Q.: A Quasi-Three-Dimensional
Variably Saturated Groundwater Flow Model for Climate Modeling, J.
Hydrometeorol., 13, 27–46, 2012.
Xie, Z. H., Liu, S., Zeng, Y. J., Gao, J. Q., Qin, P. H., Jia, B. H., Xie,
J. B., Liu, B., Li, R. C., Wang, Y., and Wang, L. H.: A High-Resolution Land
Model With Groundwater Lateral Flow, Water Use, and Soil Freeze-Thaw Front
Dynamics and its Applications in an Endorheic Basin, J. Geophys.
Res.-Atmos., 123, 7204–7222, https://doi.org/10.1029/2018JD028369, 2018.
Yang, F., Lu, H., Yang, K., He, J., Wang, W., Wright, J. S., Li, C., Han, M., and Li, Y.: Evaluation of multiple forcing data sets for precipitation and shortwave radiation over major land areas of China, Hydrol. Earth Syst. Sci., 21, 5805–5821, https://doi.org/10.5194/hess-21-5805-2017, 2017.
Yang, K. and He J.: China meteorological forcing dataset (1979-2018), National Tibetan Plateau Data Center, https://doi.org/10.11888/AtmosphericPhysics.tpe.249369.file, 2019.
Yang, K., Koike, T., Ye, B. S., and Bastidas, L.: Inverse analysis of the
role of soil vertical heterogeneity in controlling surface soil state and
energy partition, J. Geophys. Res.-Atmos., 110, D08101, https://doi.org/10.1029/2004JD005500, 2005.
Yang, K., Koike, T., Ishikawa, H., Kim, J., Li, X., Liu, H. Z., Liu, S. M.,
Ma, Y. M., and Wang, J. M.: Turbulent flux transfer over bare-soil surfaces:
Characteristics and parameterization, J. Appl. Meteorol. Clim., 47, 276–290, 2008.
Yang, K., Chen, Y.-Y., and Qin, J.: Some practical notes on the land surface modeling in the Tibetan Plateau, Hydrol. Earth Syst. Sci., 13, 687–701, https://doi.org/10.5194/hess-13-687-2009, 2009.
Yang, K., Qin, J., Zhao, L., Chen, Y. Y., Tang, W. J., Han, M. L., Lazhu,
Chen, Z. Q., Lv, N., Ding, B. H., Wu, H., and Lin, C. G.: A Multiscale Soil Moisture and Freeze–Thaw Monitoring Network on the Third Pole, B. Am. Meteorol. Soc., 94, 1907–1916, https://doi.org/10.1175/bams-d-12-00203.1, 2013.
Yang, K., Zhu, L., Chen, Y. Y., Zhao, L., Qin, J., Lu, H., Tang, W. J., Han,
M. L., Ding, B. H., and Fang, N.: Land surface model calibration through
microwave data assimilation for improving soil moisture simulations, J. Hydrol., 533, 266–276, 2016.
Yang, K., Wang, C. H., and Li, S. Y.: Improved Simulation of Frozen-Thawing
Process in Land Surface Model (CLM4.5), J. Geophys.
Res.-Atmos., 123, 13238–13258, https://doi.org/10.1029/2017jd028260, 2018.
Yang, K., Chen, Y. Y., He, J., Zhao, L., Lu, H., Qin, J., Zheng, D. H., and
Li, X.: Development of a daily soil moisture product for the period of
2002–2011 in Chinese Mainland, Sci. China Earth Sci., 63, 1113–1125,
https://doi.org/10.1007/s11430-019-9588-5, 2020.
Yao, T., Wu, F., Ding, L., Sun, J., Zhu, L., Piao, S. L., Deng, T., Ni, X.,
Zheng, H., and Ouyang, H.: Multispherical interactions and their effects on
the Tibetan Plateau's earth system: a review of the recent researches,
Natl. Sci. Rev., 2, 468–488, https://doi.org/10.1093/nsr/nwv070, 2015.
Yi, S., He, Y., Guo, X., Chen, J., Wu, Q., Qin, Y., and Ding, Y.: The physical properties of coarse-fragment soils and their effects on permafrost dynamics: a case study on the central Qinghai–Tibetan Plateau, The Cryosphere, 12, 3067–3083, https://doi.org/10.5194/tc-12-3067-2018, 2018.
Yuan, H., Dai, Y. J., Xiao, Z. Q., Ji, D. Y., and Shangguan, W.:
Reprocessing the MODIS Leaf Area Index products for land surface and climate
modelling, Remote Sens. Environ., 115, 1171–1187, 2011.
Yuan, X., Ji, P., Wang, L., Liang, X.-Z., Yang, K., Ye, A., Su, Z., and Wen,
J.: High-Resolution Land Surface Modeling of Hydrological Changes Over the
Sanjiangyuan Region in the Eastern Tibetan Plateau: 1. Model Development and
Evaluation, J. Adv. Model. Earth Sy., 10, 2806–2828, https://doi.org/10.1029/2018ms001412, 2018.
Zeng, Y., Xie, Z., Yu, Y., Liu, S., Wang, L., Jia, B., Qin, P., and Chen, Y.: Ecohydrological effects of stream–aquifer water interaction: a case study of the Heihe River basin, northwestern China, Hydrol. Earth Syst. Sci., 20, 2333–2352, https://doi.org/10.5194/hess-20-2333-2016, 2016.
Zeng, Y. J., Xie, Z. H., Yu, Y., Liu, S., Wang, L. Y., Zou, J., Qin, P. H.,
and Jia, B. H.: Effects of anthropogenic water regulation and groundwater
lateral flow on land processes, J. Adv. Model. Earth Sy., 8, 1106–1131, 2016.
Zhang, Q., Jin, J., Wang, X., Budy, P., Barrett, N., and Null, S. E.: Improving lake mixing process simulations in the Community Land Model by using K profile parameterization, Hydrol. Earth Syst. Sci., 23, 4969–4982, https://doi.org/10.5194/hess-23-4969-2019, 2019.
Zhao, P., Xu, X., Chen, F., Guo, X., Zheng, X., Liu, L., Hong, Y., Li, Y.,
La, Z., Peng, H., Zhong, L., Ma, Y., Tang, S., Liu, Y., Liu, H., Li, Y.,
Zhang, Q., Hu, Z., Sun, J., Zhang, S., Dong, L., Zhang, H., Zhao, Y., Yan,
X., Xiao, A., Wan, W., Liu, Y., Chen, J., Liu, G., Zhaxi, Y., and Zhou, X.:
The third atmospheric scientific experiment for understanding the
Earth-atmosphere coupled system over the Tibetan Plateau and its effects, B.
Am. Meteorol. Soc., 99, 757–776, https://doi.org/10.1175/bams-d-16-0050.1, 2018.
Zheng, D., van der Velde, R., Su, Z., Wang, X., Wen, J., Booij, M. J.,
Hoekstra, A. Y., and Chen, Y.: Augmentations to the Noah Model Physics for
Application to the Yellow River Source Area. Part I: Soil Water Flow, J.
Hydrometeorol., 16, 2659–2676, https://doi.org/10.1175/jhm-d-14-0198.1, 2015a.
Zheng, D., van der Velde, R., Su, Z., Wang, X., Wen, J., Booij, M. J.,
Hoekstra, A. Y., and Chen, Y.: Augmentations to the Noah Model Physics for
Application to the Yellow River Source Area. Part II: Turbulent Heat Fluxes
and Soil Heat Transport, J. Hydrometeorol., 16, 2677–2694,
https://doi.org/10.1175/jhm-d-14-0199.1, 2015b.
Zheng, D., Van der Velde, R., Su, Z., Wen, J., Booij, M. J., Hoekstra, A.
Y., and Wang, X.: Under-canopy turbulence and root water uptake of a Tibetan
meadow ecosystem modeled by Noah-MP, Water Resour. Res., 51, 5735–5755,
https://doi.org/10.1002/2015wr017115, 2015c.
Zheng, D., Van der Velde, R., Su, Z., Wen, J., and Wang, X.: Assessment of
Noah land surface model with various runoff parameterizations over a Tibetan
river, J. Geophys. Res.-Atmos., 122, 1488–1504,
https://doi.org/10.1002/2016jd025572, 2017a.
Zheng, D., van der Velde, R., Su, Z., Wen, J., Wang, X., and Yang, K.:
Evaluation of Noah Frozen Soil Parameterization for Application to a Tibetan
Meadow Ecosystem, J. Hydrometeorol., 18, 1749–1763, https://doi.org/10.1175/jhm-d-16-0199.1,
2017b.
Zheng, D., van der Velde, R., Su, Z., Wen, J., Wang, X., and Yang, K.:
Impact of soil freeze-thaw mechanism on the runoff dynamics of two Tibetan
rivers, J. Hydrol., 563, 382–394, https://doi.org/10.1016/j.jhydrol.2018.06.024,
2018.
Zheng, D. H., Van der Velde, R., Su, Z. B., Wen, J., Wang, X., Booij, M. J.,
Hoekstra, A. Y., Lv, S. H., Zhang, Y., and Ek, M. B.: Impacts of Noah model
physics on catchment-scale runoff simulations, J. Geophys.
Res.-Atmos., 121, 807–832, 2016.
Zhou, X., Yang, K., and Wang, Y.: Implementation of a turbulent orographic
form drag scheme in WRF and its application to the Tibetan Plateau, Clim.
Dynam., 50, 2443–2455, https://doi.org/10.1007/s00382-017-3677-y, 2018.
Zhou, X., Yang, K., Beljaars, A., Li, H., Lin, C., Huang, B., and Wang, Y.:
Dynamical impact of parameterized turbulent orographic form drag on the
simulation of winter precipitation over the western Tibetan Plateau, Clim.
Dynam., 53, 707–720, https://doi.org/10.1007/s00382-019-04628-0, 2019.
Zhu, S. G., Chen, H. S., Zhang, X. X., Wei, N., Wei, S. G., Yuan, H., Zhang,
S. P., Wang, L. L., Zhou, L. H., and Dai, Y. J.: Incorporating root
hydraulic redistribution and compensatory water uptake in the Common Land
Model: Effects on site level and global land modeling, J. Geophys. Res.-Atmos., 122, 7308–7322, 2017.
Short summary
The Tibetan Plateau (TP), known as the Asian water tower, plays an important role in the regional climate system, while the land surface process is a key component through which the TP impacts the water and energy cycles. In this paper, we reviewed the progress achieved in the last decade in understanding and modeling the land surface processes on the TP. Based on this review, perspectives on the further improvement of land surface modelling on the TP are also provided.
The Tibetan Plateau (TP), known as the Asian water tower, plays an important role in the...
