Articles | Volume 23, issue 4
https://doi.org/10.5194/hess-23-1833-2019
© 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-23-1833-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Future evolution and uncertainty of river flow regime change in a deglaciating river basin
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG, UK
Nicholas E. Barrand
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
David M. Hannah
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Stefan Krause
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Christopher R. Jackson
British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG, UK
Jez Everest
British Geological Survey, Lyell Centre, Research Avenue South, Edinburgh, EH14 4AS, UK
Guðfinna Aðalgeirsdóttir
Institute of Earth Sciences, University of Iceland, 101 Reykjavík, Iceland
Andrew R. Black
Geography and Environmental Science, University of Dundee, Dundee, DD1 4HN, UK
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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.
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Louisa D. Oldham, Jim Freer, Gemma Coxon, Nicholas Howden, John P. Bloomfield, and Christopher Jackson
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loss functionsmay be used in conceptual rainfall–runoff models but should be supported by perceptualisation of IGF processes and connectivities.
Lizz Ultee, Sloan Coats, and Jonathan Mackay
Earth Syst. Dynam., 13, 935–959, https://doi.org/10.5194/esd-13-935-2022, https://doi.org/10.5194/esd-13-935-2022, 2022
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Global climate models suggest that droughts could worsen over the coming century. In mountain basins with glaciers, glacial runoff can ease droughts, but glaciers are retreating worldwide. We analyzed how one measure of drought conditions changes when accounting for glacial runoff that changes over time. Surprisingly, we found that glacial runoff can continue to buffer drought throughout the 21st century in most cases, even as the total amount of runoff declines.
Doris E. Wendt, John P. Bloomfield, Anne F. Van Loon, Margaret Garcia, Benedikt Heudorfer, Joshua Larsen, and David M. Hannah
Nat. Hazards Earth Syst. Sci., 21, 3113–3139, https://doi.org/10.5194/nhess-21-3113-2021, https://doi.org/10.5194/nhess-21-3113-2021, 2021
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Liwen Wu, Jesus D. Gomez-Velez, Stefan Krause, Anders Wörman, Tanu Singh, Gunnar Nützmann, and Jörg Lewandowski
Hydrol. Earth Syst. Sci., 25, 1905–1921, https://doi.org/10.5194/hess-25-1905-2021, https://doi.org/10.5194/hess-25-1905-2021, 2021
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Kate E. Ashley, Robert McKay, Johan Etourneau, Francisco J. Jimenez-Espejo, Alan Condron, Anna Albot, Xavier Crosta, Christina Riesselman, Osamu Seki, Guillaume Massé, Nicholas R. Golledge, Edward Gasson, Daniel P. Lowry, Nicholas E. Barrand, Katelyn Johnson, Nancy Bertler, Carlota Escutia, Robert Dunbar, and James A. Bendle
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Doris E. Wendt, Anne F. Van Loon, John P. Bloomfield, and David M. Hannah
Hydrol. Earth Syst. Sci., 24, 4853–4868, https://doi.org/10.5194/hess-24-4853-2020, https://doi.org/10.5194/hess-24-4853-2020, 2020
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Groundwater use changes the availability of groundwater, especially during droughts. This study investigates the impact of groundwater use on groundwater droughts. A methodological framework is presented that was developed and applied to the UK. We identified an asymmetric impact of groundwater use on droughts, which highlights the relation between short-term and long-term strategies for sustainable groundwater use.
Nicolas Massei, Daniel G. Kingston, David M. Hannah, Jean-Philippe Vidal, Bastien Dieppois, Manuel Fossa, Andreas Hartmann, David A. Lavers, and Benoit Laignel
Proc. IAHS, 383, 141–149, https://doi.org/10.5194/piahs-383-141-2020, https://doi.org/10.5194/piahs-383-141-2020, 2020
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Bentje Brauns, Daniela Cuba, John P. Bloomfield, David M. Hannah, Christopher Jackson, Ben P. Marchant, Benedikt Heudorfer, Anne F. Van Loon, Hélène Bessière, Bo Thunholm, and Gerhard Schubert
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Hydrol. Earth Syst. Sci., 23, 5199–5225, https://doi.org/10.5194/hess-23-5199-2019, https://doi.org/10.5194/hess-23-5199-2019, 2019
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The movement of water and solutes between streams and their shallow, connected subsurface is important to many ecosystem functions. These exchanges are widely expected to vary with stream flow across space and time, but these assumptions are seldom tested across basin scales. We completed more than 60 experiments across a 5th-order river basin to document these changes, finding patterns in space but not time. We conclude space-for-time and time-for-space substitutions are not good assumptions.
Brighid É. Ó Dochartaigh, Alan M. MacDonald, Andrew R. Black, Jez Everest, Paul Wilson, W. George Darling, Lee Jones, and Mike Raines
Hydrol. Earth Syst. Sci., 23, 4527–4539, https://doi.org/10.5194/hess-23-4527-2019, https://doi.org/10.5194/hess-23-4527-2019, 2019
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We provide evidence of high groundwater storage and flow in catchments with active glaciers. Groundwater is found within gravels at the front of glaciers and replenished by both ice melt and precipitation. We studied a glacier in Iceland for 3 years, characterising the aquifer properties and measuring groundwater, river flow and precipitation. The results are important for accurately measuring meltwater and show that groundwater can provide strategic water supplies in de-glaciating catchments.
Adam S. Ward, Jay P. Zarnetske, Viktor Baranov, Phillip J. Blaen, Nicolai Brekenfeld, Rosalie Chu, Romain Derelle, Jennifer Drummond, Jan H. Fleckenstein, Vanessa Garayburu-Caruso, Emily Graham, David Hannah, Ciaran J. Harman, Skuyler Herzog, Jase Hixson, Julia L. A. Knapp, Stefan Krause, Marie J. Kurz, Jörg Lewandowski, Angang Li, Eugènia Martí, Melinda Miller, Alexander M. Milner, Kerry Neil, Luisa Orsini, Aaron I. Packman, Stephen Plont, Lupita Renteria, Kevin Roche, Todd Royer, Noah M. Schmadel, Catalina Segura, James Stegen, Jason Toyoda, Jacqueline Hager, Nathan I. Wisnoski, and Steven M. Wondzell
Earth Syst. Sci. Data, 11, 1567–1581, https://doi.org/10.5194/essd-11-1567-2019, https://doi.org/10.5194/essd-11-1567-2019, 2019
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Studies of river corridor exchange commonly focus on characterization of the physical, chemical, or biological system. As a result, complimentary systems and context are often lacking, which may limit interpretation. Here, we present a characterization of all three systems at 62 sites in a 5th-order river basin, including samples of surface water, hyporheic water, and sediment. These data will allow assessment of interacting processes in the river corridor.
Chiara Magliozzi, Robert C. Grabowski, Aaron I. Packman, and Stefan Krause
Hydrol. Earth Syst. Sci., 22, 6163–6185, https://doi.org/10.5194/hess-22-6163-2018, https://doi.org/10.5194/hess-22-6163-2018, 2018
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The hyporheic zone is the area below riverbeds where surfacewater and groundwater mix. Hyporheic flow is linked to river processes and functions, but research to date has not sufficiently addressed how factors operating at different scales in time and space drive hyporheic flow variations at reach and larger scales. This review presents the scale-specific processes and interactions that control hyporheic flow, and a case study showing how valley factors affect its expression at the reach scale.
Clemens Schannwell, Stephen Cornford, David Pollard, and Nicholas E. Barrand
The Cryosphere, 12, 2307–2326, https://doi.org/10.5194/tc-12-2307-2018, https://doi.org/10.5194/tc-12-2307-2018, 2018
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Despite the speculation on the state and fate of Larsen C Ice Shelf, a key unknown factor remains: what would be the effects of ice-shelf collapse on upstream drainage basins and thus global sea levels? In our paper three state-of-the-art numerical ice-sheet models were used to simulate the volume evolution of the inland ice sheet to ice-shelf collapse at Larsen C and George VI ice shelves. Our results suggest sea-level rise of up to ~ 4 mm for Larsen C ice shelf and ~ 22 for George VI ice shelf.
Giri Gopalan, Birgir Hrafnkelsson, Guðfinna Aðalgeirsdóttir, Alexander H. Jarosch, and Finnur Pálsson
The Cryosphere, 12, 2229–2248, https://doi.org/10.5194/tc-12-2229-2018, https://doi.org/10.5194/tc-12-2229-2018, 2018
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Geophysical systems can often contain scientific parameters whose values are uncertain, complex underlying dynamics, and field measurements with errors. These components are naturally modeled together within what is known as a Bayesian hierarchical model (BHM). This paper constructs such a model for shallow glaciers based on an approximation of the underlying dynamics. The evaluation of this model is aided by the use of exact analytical solutions from the literature.
Jonathan D. Mackay, Nicholas E. Barrand, David M. Hannah, Stefan Krause, Christopher R. Jackson, Jez Everest, and Guðfinna Aðalgeirsdóttir
The Cryosphere, 12, 2175–2210, https://doi.org/10.5194/tc-12-2175-2018, https://doi.org/10.5194/tc-12-2175-2018, 2018
Short summary
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We apply a framework to compare and objectively accept or reject competing melt and run-off process models. We found no acceptable models. Furthermore, increasing model complexity does not guarantee better predictions. The results highlight model selection uncertainty and the need for rigorous frameworks to identify deficiencies in competing models. The application of this approach in the future will help to better quantify model prediction uncertainty and develop improved process models.
Faye L. Jackson, Robert J. Fryer, David M. Hannah, and Iain A. Malcolm
Hydrol. Earth Syst. Sci., 21, 4727–4745, https://doi.org/10.5194/hess-21-4727-2017, https://doi.org/10.5194/hess-21-4727-2017, 2017
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River temperature (Tw) is important to fish populations, but one cannot monitor everywhere. Thus, models are used to predict Tw, sometimes in rivers with no data. To date, the accuracy of these predictions has not been determined. We found that models including landscape predictors (e.g. altitude, tree cover) could describe spatial patterns in Tw in other rivers better than those including air temperature. Such findings are critical for developing Tw models that have management application.
Feng Mao, Julian Clark, Timothy Karpouzoglou, Art Dewulf, Wouter Buytaert, and David Hannah
Hydrol. Earth Syst. Sci., 21, 3655–3670, https://doi.org/10.5194/hess-21-3655-2017, https://doi.org/10.5194/hess-21-3655-2017, 2017
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The paper aims to propose a conceptual framework that supports nuanced understanding and analytical assessment of resilience in socio-hydrological contexts. We identify three framings of resilience for different human–water couplings, which have distinct application fields and are used for different water management challenges. To assess and improve socio-hydrological resilience in each type, we introduce a
resilience canvasas a heuristic tool to design bespoke management strategies.
Louise Steffensen Schmidt, Guðfinna Aðalgeirsdóttir, Sverrir Guðmundsson, Peter L. Langen, Finnur Pálsson, Ruth Mottram, Simon Gascoin, and Helgi Björnsson
The Cryosphere, 11, 1665–1684, https://doi.org/10.5194/tc-11-1665-2017, https://doi.org/10.5194/tc-11-1665-2017, 2017
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The regional climate model HIRHAM5 is evaluated over Vatnajökull, Iceland, using automatic weather stations and mass balance observations from 1995 to 2014. From this we asses whether the model can be used to reconstruct the mass balance of the glacier. We find that the simulated energy balance is underestimated overall, but it has been improved by using a new albedo scheme. The specific mass balance is reconstructed back to 1980, thus expanding on the observational records of the mass balance.
Cédric L. R. Laizé, Cristian Bruna Meredith, Michael J. Dunbar, and David M. Hannah
Hydrol. Earth Syst. Sci., 21, 3231–3247, https://doi.org/10.5194/hess-21-3231-2017, https://doi.org/10.5194/hess-21-3231-2017, 2017
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Stream temperature controls many river processes, making it vital to know how climate affects it. Climate and stream temperatures at 35 British sites and associated basin properties were used to model climate–water temperature associations and to assess how they are influenced by basins. Associations vary with season and water temperature range. Basin permeability, size, and elevation have the main influence; smaller upland or impermeable basins are the most sensitive to climate.
Joaquín M. C. Belart, Etienne Berthier, Eyjólfur Magnússon, Leif S. Anderson, Finnur Pálsson, Thorsteinn Thorsteinsson, Ian M. Howat, Guðfinna Aðalgeirsdóttir, Tómas Jóhannesson, and Alexander H. Jarosch
The Cryosphere, 11, 1501–1517, https://doi.org/10.5194/tc-11-1501-2017, https://doi.org/10.5194/tc-11-1501-2017, 2017
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Sub-meter satellite stereo images (Pléiades and WorldView2) are used to accurately measure snow accumulation and winter mass balance of Drangajökull ice cap. This is done by creating and comparing accurate digital elevation models. A glacier-wide geodetic mass balance of 3.33 ± 0.23 m w.e. is derived between October 2014 and May 2015. This method could be easily transposable to remote glaciated areas where seasonal mass balance measurements (especially winter accumulation) are lacking.
Nicholas E. Barrand, Robert G. Way, Trevor Bell, and Martin J. Sharp
The Cryosphere, 11, 157–168, https://doi.org/10.5194/tc-11-157-2017, https://doi.org/10.5194/tc-11-157-2017, 2017
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This paper provides a comprehensive assessment of the state of small glaciers in the Canadian province of Labrador. These glaciers, the last in continental northeast North America, exist in heavily shaded locations within the remote Torngat Mountains National Park. Fieldwork, and airborne and spaceborne remote-sensing analyses were used to measure regional glacier area changes and individual glacier thinning rates. These results were then linked to trends in prevailing climatic conditions.
Chiara Magliozzi, Robert Grabowski, Aaron I. Packman, and Stefan Krause
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2016-683, https://doi.org/10.5194/hess-2016-683, 2017
Manuscript not accepted for further review
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A critical review of recent literature details how drivers operating at catchment, valley and reach scales are responsible of variations in space and time in the hyporheic exchange. It is based on cross-disciplinary understanding of environmental topics from published reviews and field studies placed within a hierarchical framework. The outcomes will benefit hyporheic research and catchment managers by providing an integrated approach of the drivers of hyporheic exchange in space and time.
Sally Rangecroft, Anne F. Van Loon, Héctor Maureira, Koen Verbist, and David M. Hannah
Earth Syst. Dynam. Discuss., https://doi.org/10.5194/esd-2016-57, https://doi.org/10.5194/esd-2016-57, 2016
Preprint withdrawn
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This paper on anthropogenic droughts looks at the interactions of human activity and "natural" processes. Using a case study of the introduction of a reservoir in a Chilean river basin and a new methodology, we established the most effective way forward for quantifying human activities on hydrological drought: the "threshold level" method with an "undisturbed" time period as the threshold. This will increase our understanding on how human activities are impacting the hydrological system.
Anne F. Van Loon, Kerstin Stahl, Giuliano Di Baldassarre, Julian Clark, Sally Rangecroft, Niko Wanders, Tom Gleeson, Albert I. J. M. Van Dijk, Lena M. Tallaksen, Jamie Hannaford, Remko Uijlenhoet, Adriaan J. Teuling, David M. Hannah, Justin Sheffield, Mark Svoboda, Boud Verbeiren, Thorsten Wagener, and Henny A. J. Van Lanen
Hydrol. Earth Syst. Sci., 20, 3631–3650, https://doi.org/10.5194/hess-20-3631-2016, https://doi.org/10.5194/hess-20-3631-2016, 2016
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In the Anthropocene, drought cannot be viewed as a natural hazard independent of people. Drought can be alleviated or made worse by human activities and drought impacts are dependent on a myriad of factors. In this paper, we identify research gaps and suggest a framework that will allow us to adequately analyse and manage drought in the Anthropocene. We need to focus on attribution of drought to different drivers, linking drought to its impacts, and feedbacks between drought and society.
N. A. L. Archer, B. R. Rawlins, B. P. Machant, J. D. Mackay, and P. I. Meldrum
SOIL Discuss., https://doi.org/10.5194/soil-2016-40, https://doi.org/10.5194/soil-2016-40, 2016
Preprint withdrawn
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This study investigates the importance of using techniques, such as soil water release curves, soil shrinkage measurements and field observations to create reference points to determine the best-fit calibrations for estimating volumetric water content (VWC). We also show that calibrating soil moisture sensors in disturbed clay soils over-estimates VWC and we suggest that undisturbed soil cores provide better calibrations to estimate VWC in clay soils.
J. M. van Wessem, S. R. M. Ligtenberg, C. H. Reijmer, W. J. van de Berg, M. R. van den Broeke, N. E. Barrand, E. R. Thomas, J. Turner, J. Wuite, T. A. Scambos, and E. van Meijgaard
The Cryosphere, 10, 271–285, https://doi.org/10.5194/tc-10-271-2016, https://doi.org/10.5194/tc-10-271-2016, 2016
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This study presents the first high-resolution (5.5 km) modelled estimate of surface mass balance (SMB) over the period 1979–2014 for the Antarctic Peninsula (AP). Precipitation (snowfall and rain) largely determines the SMB, and is exceptionally high over the western mountain slopes, with annual values > 4 m water equivalent. Snowmelt is widespread over the AP, but only runs off into the ocean at some locations: the Larsen B,C, and Wilkins ice shelves, and along the north-western mountains.
N. Le Vine, A. Butler, N. McIntyre, and C. Jackson
Hydrol. Earth Syst. Sci., 20, 143–159, https://doi.org/10.5194/hess-20-143-2016, https://doi.org/10.5194/hess-20-143-2016, 2016
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– A strategy to diagnose hydrological limitations of a Land Surface Model
– Land Surface Model adaptation for hydrological applications
– Highlights challenges faced while moving towards high resolution modelling
I. Giuntoli, J.-P. Vidal, C. Prudhomme, and D. M. Hannah
Earth Syst. Dynam., 6, 267–285, https://doi.org/10.5194/esd-6-267-2015, https://doi.org/10.5194/esd-6-267-2015, 2015
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We assessed future changes in high and low flows globally using runoff projections from global hydrological models (GHMs) driven by global climate models (GCMs) under the RCP8.5 scenario. Further, we quantified the relative size of uncertainty from GHMs and from GCMs using ANOVA. We show that GCMs are the major contributors to uncertainty overall, but GHMs increase their contribution for low flows and can equal or outweigh GCM uncertainty in snow-dominated areas for both high and low flows.
H. Hannesdóttir, H. Björnsson, F. Pálsson, G. Aðalgeirsdóttir, and Sv. Guðmundsson
The Cryosphere, 9, 565–585, https://doi.org/10.5194/tc-9-565-2015, https://doi.org/10.5194/tc-9-565-2015, 2015
G. Garner, I. A. Malcolm, J. P. Sadler, and D. M. Hannah
Hydrol. Earth Syst. Sci., 18, 5361–5376, https://doi.org/10.5194/hess-18-5361-2014, https://doi.org/10.5194/hess-18-5361-2014, 2014
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This study demonstrates the processes by which instantaneous longitudinal water temperature gradients may be generated in a stream reach that transitions from moorland to semi-natural forest in the absence of substantial groundwater inflows. Water did not cool as it flowed downstream. Instead, temperature gradients were generated by a combination of reduced rates of heating in the forested reach and advection of cooler (overnight and early morning) water from the upstream moorland catchment.
C. Prudhomme, T. Haxton, S. Crooks, C. Jackson, A. Barkwith, J. Williamson, J. Kelvin, J. Mackay, L. Wang, A. Young, and G. Watts
Earth Syst. Sci. Data, 5, 101–107, https://doi.org/10.5194/essd-5-101-2013, https://doi.org/10.5194/essd-5-101-2013, 2013
P. Fretwell, H. D. Pritchard, D. G. Vaughan, J. L. Bamber, N. E. Barrand, R. Bell, C. Bianchi, R. G. Bingham, D. D. Blankenship, G. Casassa, G. Catania, D. Callens, H. Conway, A. J. Cook, H. F. J. Corr, D. Damaske, V. Damm, F. Ferraccioli, R. Forsberg, S. Fujita, Y. Gim, P. Gogineni, J. A. Griggs, R. C. A. Hindmarsh, P. Holmlund, J. W. Holt, R. W. Jacobel, A. Jenkins, W. Jokat, T. Jordan, E. C. King, J. Kohler, W. Krabill, M. Riger-Kusk, K. A. Langley, G. Leitchenkov, C. Leuschen, B. P. Luyendyk, K. Matsuoka, J. Mouginot, F. O. Nitsche, Y. Nogi, O. A. Nost, S. V. Popov, E. Rignot, D. M. Rippin, A. Rivera, J. Roberts, N. Ross, M. J. Siegert, A. M. Smith, D. Steinhage, M. Studinger, B. Sun, B. K. Tinto, B. C. Welch, D. Wilson, D. A. Young, C. Xiangbin, and A. Zirizzotti
The Cryosphere, 7, 375–393, https://doi.org/10.5194/tc-7-375-2013, https://doi.org/10.5194/tc-7-375-2013, 2013
Related subject area
Subject: Snow and Ice | Techniques and Approaches: Uncertainty analysis
Interactions between thresholds and spatial discretizations of snow: insights from estimates of wolverine denning habitat in the Colorado Rocky Mountains
Role of forcing uncertainty and background model error characterization in snow data assimilation
Justin M. Pflug, Yiwen Fang, Steven A. Margulis, and Ben Livneh
Hydrol. Earth Syst. Sci., 27, 2747–2762, https://doi.org/10.5194/hess-27-2747-2023, https://doi.org/10.5194/hess-27-2747-2023, 2023
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Wolverine denning habitat inferred using a snow threshold differed for three different spatial representations of snow. These differences were based on the annual volume of snow and the elevation of the snow line. While denning habitat was most influenced by winter meteorological conditions, our results show that studies applying thresholds to environmental datasets should report uncertainties stemming from different spatial resolutions and uncertainties introduced by the thresholds themselves.
Sujay V. Kumar, Jiarui Dong, Christa D. Peters-Lidard, David Mocko, and Breogán Gómez
Hydrol. Earth Syst. Sci., 21, 2637–2647, https://doi.org/10.5194/hess-21-2637-2017, https://doi.org/10.5194/hess-21-2637-2017, 2017
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Data assimilation deals with the blending of model forecasts and observations based on their relative errors. This paper addresses the importance of accurately representing the errors in the model forecasts for skillful data assimilation performance.
Cited articles
Ali, G., Tetzlaff, D., Soulsby, C., McDonnell, J. J., and Capell, R.: A
comparison of similarity indices for catchment classification using a
cross-regional dataset, Adv. Water Resour., 40, 11–22,
https://doi.org/10.1016/j.advwatres.2012.01.008, 2012. a
Allen, R., Pereira, L., Raes, D., and Smith, M.: Crop evapotranspiration –
Guidelines for computing crop water requirements – FAO Irrigation and
drainage paper 56, Tech. rep., Food and Agriculture Organization of the
United Nations, Rome, Italy, 1998. a
Baraer, M., Mckenzie, J., Mark, B. G., Gordon, R., Bury, J., Condom, T., Gomez,
J., Knox, S., and Fortner, S. K.: Contribution of groundwater to the outflow
from ungauged glacierized catchments: A multi-site study in the tropical
Cordillera Blanca, Peru, Hydrol. Process., 29, 2561–2581,
https://doi.org/10.1002/hyp.10386, 2015. a
Bartók, B., Wild, M., Folini, D., Lüthi, D., Kotlarski, S.,
Schär, C., Vautard, R., Jerez, S., and Imecs, Z.: Projected changes in
surface solar radiation in CMIP5 global climate models and in EURO-CORDEX
regional climate models for Europe, Clim. Dynam., 49, 2665–2683,
https://doi.org/10.1007/s00382-016-3471-2, 2017. a
Beamer, J. P., Hill, D. F., McGrath, D., Arendt, A., and Kienholz, C.:
Hydrologic impacts of changes in climate and glacier extent in the Gulf of
Alaska watershed, Water Resour. Res., 53, 7502–7520,
https://doi.org/10.1002/2016WR020033, 2017. a
Beer, C., Porada, P., Ekici, A., and Brakebusch, M.: Effects of short-term
variability of meteorological variables on soil temperature in permafrost
regions, The Cryosphere, 12, 741–757,
https://doi.org/10.5194/tc-12-741-2018, 2018. a
Björnsson, H. and Pálsson, F.: Icelandic glaciers, Jökull,
58, 365–386, 2008. a
Bliss, A., Hock, R., and Radić, V.: Global response of glacier runoff to
twenty-first century climate change, J. Geophys. Res., 119,
717–730, https://doi.org/10.1002/2013JF002931, 2014. a
Braithwaite, R. J.: Positive degree-day factors for ablation on the Greenland
Ice-sheet studied by energy balance modeling, J. Glaciol., 41,
153–160, 1995. a
Brately, P. and Fox, B. L.: Algorithm 659: Implementing Sobol's quasirandom
sequence generator, ACM T. Math. Software, 14, 88–100,
1988. a
Brock, B. W., Willis, I. C., and Sharp, M. J.: Measurement and
parameterisation of albedo variations at Haut Glacier d'Arolla,
Switzerland, J. Glaciol., 46, 675–688,
https://doi.org/10.3189/172756500781832675, 2000. a, b
Bunn, S. E. and Arthington, A. H.: Basic principles and ecological
consequences of altered flow regimes for aquatic biodiversity, Environ.
Manage., 30, 492–507, https://doi.org/10.1007/s00267-002-2737-0, 2002. a
Carey, M., Baraer, M., Mark, B. G., French, A., Bury, J., Young, K. R., and
McKenzie, J. M.: Toward hydro-social modeling: Merging human variables and
the social sciences with climate-glacier runoff models (Santa River, Peru),
J. Hydrol., 518, 60–70, https://doi.org/10.1016/j.jhydrol.2013.11.006, 2014. a
Carvajal, P. E., Anandarajah, G., Mulugetta, Y., and Dessens, O.: Assessing
uncertainty of climate change impacts on long-term hydropower generation
using the CMIP5 ensemble – the case of Ecuador, Climatic Change, 144,
611–624, https://doi.org/10.1007/s10584-017-2055-4, 2017. a
Casper, M. C., Grigoryan, G., Gronz, O., Gutjahr, O., Heinemann, G., Ley, R.,
and Rock, A.: Analysis of projected hydrological behavior of catchments based
on signature indices, Hydrol. Earth Syst. Sci., 16, 409–421,
https://doi.org/10.5194/hess-16-409-2012, 2012. a
Chen, J. and Ohmura, A.: On the influence of Alpine glaciers on runoff,
IAHS-AISH P., 193, 117–126, 1990. a
Collins, M., Knutti, R., Arblaster, J., Dufresne, J.-L., Fichefet, T.,
Friedlingstein, P., Gao, X., Gutowski, W., Johns, T., Krinner, G., Shongwe,
M., Tebaldi, C., Weaver, A., and Wehner, M.: Long-term Climate Change:
Projections, Commitments and Irreversibility, in: Climate Change 2013: The
Physical Science Basis. Contribution of Working Group I to the Fifth
Assessment Report of the Intergovernmental Panel on Climate Change, edited
by:
Stocker, T., Qin, D., Plattner, G.-K., Tignor, M., Allen, S., Boschung, J.,
Nauels, A., Xia, Y., Bex, V., and Midgley, P., Cambridge
University Press, Cambridge, United Kingdom and New York, USA, 1029–1136, 2013. a
Coxon, G., Freer, J., Wagener, T., Odoni, N. A., and Clark, M.: Diagnostic
evaluation of multiple hypotheses of hydrological behaviour in a
limits-of-acceptability framework for 24 UK catchments, Hydrol.
Process., 28, 6135–6150, https://doi.org/10.1002/hyp.10096, 2014. a, b
Daron, J. D. and Stainforth, D. A.: On predicting climate under climate
change, Environ. Res. Lett., 8, 034021,
https://doi.org/10.1088/1748-9326/8/3/034021, 2013. a
Duethmann, D., Menz, C., Jiang, T., and Vorogushyn, S.: Projections for
headwater catchments of the Tarim River reveal glacier retreat and decreasing
surface water availability but uncertainties are large, Environ.
Res. Lett., 11, 054024, https://doi.org/10.1088/1748-9326/11/5/054024, 2016. a, b
Euser, T., Winsemius, H. C., Hrachowitz, M., Fenicia, F., Uhlenbrook, S., and
Savenije, H. H. G.: A framework to assess the realism of model structures
using hydrological signatures, Hydrol. Earth Syst. Sci., 17, 1893–1912,
https://doi.org/10.5194/hess-17-1893-2013, 2013. a
Farinotti, D., Usselmann, S., Huss, M., Bauder, A., and Funk, M.: Runoff
evolution in the Swiss Alps: projections for selected high-alpine catchments
based on ENSEMBLES scenarios, Hydrol. Process., 26, 1909–1924,
https://doi.org/10.1002/hyp.8276, 2012. a, b
Finger, D., Pellicciotti, F., Konz, M., Rimkus, S., and Burlando, P.: The
value of glacier mass balance, satellite snow cover images, and hourly
discharge for improving the performance of a physically based distributed
hydrological model, Water Resour. Res., 47, W07519,
https://doi.org/10.1029/2010WR009824, 2011. a
Flett, V., Maurice, L., Finlayson, A., Black, A. R., MacDonald, A. M., Everest,
J., and Kirkbride, M. P.: Meltwater flow through a rapidly deglaciating
glacier and foreland catchment system: Virkisjökull, SE Iceland,
Hydrol. Res., 1, nh2017205, https://doi.org/10.2166/nh.2017.205, 2017. a
Flett, V. T.: Glacier retreat and projected river regime changes in the
hydrologically highly-coupled Virkisjökull catchment, SE Iceland,
Doctor of philosophy, University of Dundee, Dundee, Scotland, 2016. a
Fountain, A. G. and Tangborn, W. V.: The Effect of Glaciers on Streamflow
Variations, Water Resour. Res., 21, 579–586,
https://doi.org/10.1029/WR021i004p00579, 1985. a
Fyke, J. and Matthews, H. D.: A probabilistic analysis of cumulative carbon
emissions and long-term planetary warming, Environ. Res. Lett.,
10, 115007, https://doi.org/10.1088/1748-9326/10/11/115007, 2015. a
Garee, K., Chen, X., Bao, A., Wang, Y., and Meng, F.: Hydrological Modeling of
the Upper Indus Basin: A Case Study from a High-Altitude Glacierized
Catchment Hunza, Water, 9, 1–20, https://doi.org/10.3390/w9010017, 2017. a
Gaudard, L., Romerio, F., Dalla Valle, F., Gorret, R., Maran, S., Ravazzani,
G., Stoffel, M., and Volonterio, M.: Climate change impacts on hydropower in
the Swiss and Italian Alps, Sci. Total Environ., 493,
1211–1221, https://doi.org/10.1016/j.scitotenv.2013.10.012, 2014. a
Giuntoli, I., Vidal, J.-P., Prudhomme, C., and Hannah, D. M.: Future
hydrological extremes: the uncertainty from multiple global climate and
global hydrological models, Earth Syst. Dynam., 6, 267–285,
https://doi.org/10.5194/esd-6-267-2015, 2015. a, b, c
Gosseling, M.: CORDEX climate trends for Iceland in the 21st century, Tech.
rep., Icelandic Meteorological Office, Reykjavik, Iceland, 2017. a
Griffiths, J., Keller, V., Morris, D., and Young, A. R.: Continuous
Estimation
of River Flows (CERF), Tech. rep., Environment Agency, Bristol, UK, 2008. a
Hanzer, F., Helfricht, K., Marke, T., and Strasser, U.: Multilevel
spatiotemporal validation of snow/ice mass balance and runoff modeling in
glacierized catchments, The Cryosphere, 10, 1859–1881,
https://doi.org/10.5194/tc-10-1859-2016, 2016. a
Hernández-Henríquez, M. A., Sharma, A. R., and Déry, S. J.:
Variability and trends in runoff in the rivers of British Columbia's Coast
and Insular Mountains, Hydrol. Process., 31, 3269–3282,
https://doi.org/10.1002/hyp.11257, 2017. a
Hingray, B., Schaefli, B., Mezghani, A., and Hamdi, Y.: Signature-based model
calibration for hydrological prediction in mesoscale Alpine catchments,
Hydrolog. Sci. J., 55, 1002–1016,
https://doi.org/10.1080/02626667.2010.505572, 2010. a
Hrachowitz, M., Fovet, O., Ruiz, L., Euser, T., Gharari, S., Nijzink, R.,
Freer, J., Savenije, H., and Gascuel-Odoux, C.: Process consistency in
models: The importance of system signatures, expert knowledge, and process
complexity, Water Resour. Res., 50, 7445–7469, 2014. a
Huss, M. and Hock, R.: Global-scale hydrological response to future glacier
mass loss, Nat. Clim. Change, 8, 135–140,
https://doi.org/10.1038/s41558-017-0049-x, 2018. a, b
Huss, M., Bauder, A., Funk, M., and Hock, R.: Determination of the seasonal
mass balance of four Alpine glaciers since 1865, J. Geophys.
Res.-Earth, 113, F01015, https://doi.org/10.1029/2007JF000803, 2008. a
Huss, M., Jouvet, G., Farinotti, D., and Bauder, A.: Future high-mountain
hydrology: a new parameterization of glacier retreat, Hydrol. Earth Syst.
Sci., 14, 815–829, https://doi.org/10.5194/hess-14-815-2010, 2010. a
Immerzeel, W. W., Pellicciotti, F., and Bierkens, M. F. P.: Rising river flows
throughout the twenty-first century in two Himalayan glacierized watersheds,
Nat. Geosci., 6, 742–745, https://doi.org/10.1038/ngeo1896, 2013. a, b
Jackson, C., Wang, L., Pachocka, M., Mackay, J., and Bloomfield, J.:
Reconstruction of multi-decadal groundwater level time-series using a lumped
conceptual model, Hydrol. Process., 30, 3107–3125, https://doi.org/10.1002/hyp.10850, 2016. a
Jakob Themeßl, M., Gobiet, A., and Leuprecht, A.: Empirical-statistical
downscaling and error correction of daily precipitation from regional climate
models, Int. J. Climatol., 31, 1530–1544,
https://doi.org/10.1002/joc.2168, 2011. a
Jansson, P., Hock, R., and Schneider, T.: The concept of glacier storage: a
review, J. Hydrol., 282, 116–129,
https://doi.org/10.1016/S0022-1694(03)00258-0, 2003. a
Jobst, A. M., Kingston, D. G., Cullen, N. J., and Schmid, J.: Intercomparison
of different uncertainty sources in hydrological climate change projections
for an alpine catchment (upper Clutha River, New Zealand), Hydrol. Earth
Syst. Sci., 22, 3125–3142, https://doi.org/10.5194/hess-22-3125-2018, 2018. a, b, c, d, e, f
Jóhannesson, T., Aðlgeirsdóttir, G., Björnsson, H., and
Crochet, P.: Effect of climate change on hydrology and hydro-resources in
Iceland, Tech. rep., National Energy Authority, Orkugarður, 2007. a
Kelleher, C., McGlynn, B., and Wagener, T.: Characterizing and reducing
equifinality by constraining a distributed catchment model with regional
signatures, local observations, and process understanding, Hydrol. Earth
Syst. Sci., 21, 3325–3352, https://doi.org/10.5194/hess-21-3325-2017, 2017. a
Kiesel, J., Guse, B., Pfannerstill, M., Kakouei, K., Jähnig, S. C., and
Fohrer, N.: Improving hydrological model optimization for riverine species,
Ecol. Indic., 80, 376–385, https://doi.org/10.1016/j.ecolind.2017.04.032,
2017. a
Kobierska, F., Jonas, T., Zappa, M., Bavay, M., Magnusson, J., and Bernasconi,
S. M.: Future runoff from a partly glacierized watershed in Central
Switzerland: A two-model approach, Adv. Water Resour., 55,
204–214, https://doi.org/10.1016/j.advwatres.2012.07.024, 2013. a, b
Konz, M. and Seibert, J.: On the value of glacier mass balances for
hydrological model calibration, J. Hydrol., 385, 238–246,
https://doi.org/10.1016/j.jhydrol.2010.02.025, 2010. a
Laghari., J. R.: Melting glaciers bring energy uncertainty, Nature, 502,
617–618, https://doi.org/10.1038/502617a, 2013. a, b
Li, H., Sheffield, J., and Wood, E. F.: Bias correction of monthly
precipitation and temperature fields from Intergovernmental Panel on Climate
Change AR4 models using equidistant quantile matching, J.
Geophys. Res.-Atmos., 115, D10101, https://doi.org/10.1029/2009JD012882,
2010. a
Luce, C. H. and Holden, Z. A.: Declining annual streamflow distributions in
the Pacific Northwest United States, 1948–2006, Geophys. Res.
Lett., 36, L16401, https://doi.org/10.1029/2009GL039407, 2009. a
Lutz, a. F., Immerzeel, W. W., Shrestha, A. B., and Bierkens, M. F. P.:
Consistent increase in High Asia's runoff due to increasing glacier melt and
precipitation, Nat. Clim. Change, 4, 587–592,
https://doi.org/10.1038/nclimate2237, 2014. a
Macdonald, A. M., Black, A. R., Dochartaigh, B. É. Ó., Everest, J.,
Darling, W. G., Flett, V., and Peach, D. W.: Using stable isotopes and
continuous meltwater river monitoring to investigate the hydrology of a
rapidly retreating Icelandic outlet glacier, Ann. Glaciol., 57, 1–8,
https://doi.org/10.1017/aog.2016.22, 2016. a
Mackay, J., Jackson, C., and Wang, L.: A lumped conceptual model to simulate
groundwater level time-series, Environ. Modell. Softw., 61,
229–245, https://doi.org/10.1016/j.envsoft.2014.06.003, 2014. a
Mackay, J., Jackson, C., Brookshaw, A., Scaife, A., Cook, J., and Ward, R.:
Seasonal forecasting of groundwater levels in principal aquifers of the
United Kingdom, J. Hydrol., 530, 815–828,
https://doi.org/10.1016/j.jhydrol.2015.10.018, 2015. a
Mackay, J. D., Barrand, N. E., Hannah, D. M., Krause, S., Jackson, C. R.,
Everest, J., and Aðalgeirsdóttir, G.: Glacio-hydrological melt and
run-off modelling: application of a limits of acceptability framework for
model comparison and selection, The Cryosphere, 12, 2175–2210,
https://doi.org/10.5194/tc-12-2175-2018, 2018. a, b, c, d, e, f, g, h, i, j
Magnússon, E., Muñoz-Cobo Belart, J., Pálsson, F.,
Ágústsson, H., and Crochet, P.: Geodetic mass balance record with
rigorous uncertainty estimates deduced from aerial photographs and lidar data
– Case study from Drangajökull ice cap, NW Iceland, The Cryosphere, 10,
159–177, https://doi.org/10.5194/tc-10-159-2016, 2016. a
Mandal, S. and Simonovic, S. P.: Quantification of uncertainty in the
assessment of future streamflow under changing climate conditions,
Hydrol. Process., 31, 2076–2094, https://doi.org/10.1002/hyp.11174, 2017. a
Mankin, J. S., Viviroli, D., Singh, D., Hoekstra, A. Y., and Diffenbaugh,
N. S.: The potential for snow to supply human water demand in the present
and future, Environ. Res. Lett., 10, 114016,
https://doi.org/10.1088/1748-9326/10/11/114016, 2015. a
Mansour, M. M., Wang, L., Whiteman, M., and Hughes, A. G.: Estimation of
spatially distributed groundwater potential recharge for the United Kingdom,
Q. J. Eng. Geol., 51, 247–263,
2018. a
Marren, P. M.: Magnitude and frequency in proglacial rivers: a
geomorphological and sedimentological perspective, Earth-Sci. Rev.,
70, 203–251, https://doi.org/10.1016/j.earscirev.2004.12.002, 2005. a
Matti, B., Dahlke, H. E., Dieppois, B., Lawler, D. M., and Lyon, S. W.: Flood
seasonality across Scandinavia – Evidence of a shifting hydrograph?,
Hydrol. Process., 31, 4354–4370, https://doi.org/10.1002/hyp.11365, 2017. a
McDowell, J. Z. and Hess, J. J.: Accessing adaptation: Multiple stressors on
livelihoods in the Bolivian highlands under a changing climate, Global
Environ. Chang., 22, 342–352, https://doi.org/10.1016/j.gloenvcha.2011.11.002,
2012. a
Meresa, H. K. and Romanowicz, R. J.: The critical role of uncertainty in
projections of hydrological extremes, Hydrol. Earth Syst. Sci., 21,
4245–4258, https://doi.org/10.5194/hess-21-4245-2017, 2017. a
Mora, C., Frazier, A. G., Longman, R. J., Dacks, R. S., Walton, M. M., Tong,
E. J., Sanchez, J. J., Kaiser, L. R., Stender, Y. O., Anderson, J. M.,
Ambrosino, C. M., Fernandez-Silva, I., Giuseffi, L. M., and Giambelluca,
T. W.: The projected timing of climate departure from recent variability,
Nature, 502, 183–187, https://doi.org/10.1038/nature12540,
2013. a
Naiman, R. J., Latterell, J. J., Pettit, N. E., and Olden, J. D.: Flow
variability and the biophysical vitality of river systems, C. R.
Geosci., 340, 629–643, https://doi.org/10.1016/j.crte.2008.01.002, 2008. a
Nolin, A. W., Phillippe, J., Jefferson, A., and Lewis, S. L.: Present-day and
future contributions of glacier runoff to summertime flows in a Pacific
Northwest watershed: Implications for water resources, Water Resour. Res.,
46, W12509, https://doi.org/10.1029/2009WR008968, 2010. a
Phillips, E., Finlayson, A., Bradwell, T., Everest, J., and Jones, L.:
Structural evolution triggers a dynamic reduction in active glacier length
during rapid retreat: Evidence from Falljökull, SE Iceland, J.
Geophys. Res.-Earth, 119, 2194–2208,
https://doi.org/10.1002/2014JF003165, 2014. a
Pianosi, F., Beven, K., Freer, J., Hall, J. W., Rougier, J., Stephenson, D. B.,
and Wagener, T.: Sensitivity analysis of environmental models: A systematic
review with practical workflow, Environ. Modell. Softw., 79,
214–232, https://doi.org/10.1016/j.envsoft.2016.02.008, 2016. a
Ponce, V. M.: Engineering hydrology: Principles and practices, Prentice-Hall,
Englewood Cliffs, New Jersey, 1989. a
Pool, S., Vis, M. J. P., Knight, R. R., and Seibert, J.: Streamflow
characteristics from modeled runoff time series – importance of calibration
criteria selection, Hydrol. Earth Syst. Sci., 21, 5443–5457,
https://doi.org/10.5194/hess-21-5443-2017, 2017. a
Ragettli, S., Pellicciotti, F., Bordoy, R., and Immerzeel, W. W.: Sources of
uncertainty in modeling the glaciohydrological response of a Karakoram
watershed to climate change, Water Resour. Res., 49, 6048–6066,
https://doi.org/10.1002/wrcr.20450, 2013. a, b
Ragettli, S., Immerzeel, W. W., and Pellicciotti, F.: Contrasting climate
change impact on river flows from high-altitude catchments in the Himalayan
and Andes Mountains., P. Natl. Acad. Sci.
USA, 113, 9222–9227, https://doi.org/10.1073/pnas.1606526113,
2016. a, b
Riggs, G. and Hall, D.: MODIS Snow Products Collection 6 User Guide, Tech.
rep., available at: https://nsidc.org/sites/nsidc.org/files/files/MODIS-snow-user-guide-C6.pdf (last access:
6 October 2016), 2015. a
Samaniego, L., Kumar, R., Breuer, L., Chamorro, A., Flörke, M.,
Pechlivanidis, I. G., Schäfer, D., Shah, H., Vetter, T., Wortmann, M.,
and Zeng, X.: Propagation of forcing and model uncertainties on to
hydrological drought characteristics in a multi-model century-long experiment
in large river basins, Climatic Change, 141, 435–449,
https://doi.org/10.1007/s10584-016-1778-y, 2017. a
Sanford, T., Frumhoff, P. C., Luers, A., and Gulledge, J.: The climate policy
narrative for a dangerously warming world, Nat. Clim. Change, 4, 164–166,
https://doi.org/10.1038/nclimate2148,
2014. a
Sawicz, K. A., Kelleher, C., Wagener, T., Troch, P., Sivapalan, M., and
Carrillo, G.: Characterizing hydrologic change through catchment
classification, Hydrol. Earth Syst. Sci., 18, 273–285,
https://doi.org/10.5194/hess-18-273-2014, 2014. a
Schaefli, B.: Snow hydrology signatures for model identification within a
limits-of-acceptability approach, Hydrol. Process., 30, 4019–4035,
https://doi.org/10.1002/hyp.10972, 2016. a, b
Schaefli, B. and Huss, M.: Integrating point glacier mass balance
observations into hydrologic model identification, Hydrol. Earth Syst. Sci.,
15, 1227–1241, https://doi.org/10.5194/hess-15-1227-2011, 2011. a
Seibert, J., Vis, M. J. P., Kohn, I., Weiler, M., and Stahl, K.: Technical
note: Representing glacier geometry changes in a semi-distributed
hydrological model, Hydrol. Earth Syst. Sci., 22, 2211–2224,
https://doi.org/10.5194/hess-22-2211-2018, 2018. a, b
Shea, J. M. and Immerzeel, W. W.: An assessment of basin-scale glaciological
and hydrological sensitivities in the Hindu Kush-Himalaya, Ann.
Glaciol., 57, 308–318, https://doi.org/10.3189/2016AoG71A073, 2016. a
Shea, J. M. and Moore, R. D.: Prediction of spatially distributed
regional-scale fields of air temperature and vapor pressure over mountain
glaciers, J. Geophys. Res.-Atmos., 115, D23107,
https://doi.org/10.1029/2010JD014351, 2010. a
Singh, S., Kumar, R., Bhardwaj, A., Sam, L., Shekhar, M., Singh, A., Kumar, R.,
and Gupta, A.: Changing climate and glacio-hydrology in Indian Himalayan
Region: A review, Wiley Interdisciplinary Reviews: Climate Change, 7,
393–410, https://doi.org/10.1002/wcc.393, 2016. a
Sorensen, J. P. R., Finch, J. W., Ireson, A. M., and Jackson, C. R.:
Comparison of varied complexity models simulating recharge at the field
scale, Hydrol. Process., 28, 2091–2102, https://doi.org/10.1002/hyp.9752, 2014. a
Stewart, I. T., Ficklin, D. L., Carrillo, C. A., and McIntosh, R.: 21st
century increases in the likelihood of extreme hydrologic conditions for the
mountainous basins of the Southwestern United States, J. Hydrol.,
529, 340–353, https://doi.org/10.1016/j.jhydrol.2015.07.043, 2015. a, b
Stoffel, M., Wyżga, B., and Marston, R. A.: Floods in mountain
environments: A synthesis, Geomorphology, 272, 1–9,
https://doi.org/10.1016/j.geomorph.2016.07.008, 2016. a
Tabachnick, B. G. and Fidell, L. S.: Using Multivariate Statistics Sixth
Edition, Pearson Education Limited, Essex, United Kingdom, sixth edn., 2014. a
Taylor, K. E., Stouffer, R. J., and Meehl, G. a.: An Overview of CMIP5 and the
Experiment Design, B. Am. Meteorol. Soc., 93,
485–498, https://doi.org/10.1175/BAMS-D-11-00094.1, 2012. a
Teutschbein, C., Grabs, T., Karlsen, R. H., Laudon, H., and Bishop, K.:
Hydrological response to changing climate conditions: Spatial streamflow
variability in the boreal region, Water Resour. Res., 51, 9425–9446,
https://doi.org/10.1002/2015WR017337, 2015. a
Thorsteinsson, T. and Björnsson, H.: Climate Change and Energy Systems:
Impacts, Risks and Adaptation in the Nordic and Baltic countries, Tech.
rep., Nordic Council of Ministers, Copenhagen, 2012. a
Vaughan, D., Comiso, J., Allison, I., Carrasco, J., Kaser, G., Kwok, R., Mote,
P., Murray, T., Paul, F., Ren, J., Rignot, E., Solomina, O., Steffen, K., and
Zhang, T.: Observations: Cryosphere, in: Climate Change 2013: The Physical
Science Basis. Contribution of Working Group I to the Fifth Assessment Report
of the Intergovernmental Panel on Climate Change, edited by: Stocker, T., Qin,
D., Plattner, G.-K., Tignor, M., Allen, S., Boschung, J., Nauels, A., Xia,
Y., Bex, V., and Midgley, P., Cambridge University Press,
Cambridge, United Kingdom and New York, NY, USA, 358–359, 2013. a
Vetter, T., Huang, S., Aich, V., Yang, T., Wang, X., Krysanova, V., and
Hattermann, F.: Multi-model climate impact assessment and intercomparison for
three large-scale river basins on three continents, Earth Syst. Dynam., 6,
17–43, https://doi.org/10.5194/esd-6-17-2015, 2015. a, b, c, d
Vetter, T., Reinhardt, J., Flörke, M., van Griensven, A., Hattermann, F.,
Huang, S., Koch, H., Pechlivanidis, I. G., Plötner, S., Seidou, O., Su,
B., Vervoort, R. W., and Krysanova, V.: Evaluation of sources of uncertainty
in projected hydrological changes under climate change in 12 large-scale
river basins, Climatic Change, 141, 419–433,
https://doi.org/10.1007/s10584-016-1794-y, 2017. a, b, c
Viviroli, D. and Weingartner, R.: The hydrological significance of mountains:
from regional to global scale, Hydrol. Earth Syst. Sci., 8, 1017–1030, https://doi.org/10.5194/hess-8-1017-2004, 2004. a
Viviroli, D., Dürr, H. H., Messerli, B., Meybeck, M., and Weingartner,
R.: Mountains of the world, water towers for humanity: Typology, mapping,
and global significance, Water Resour. Res., 43, 1–13,
https://doi.org/10.1029/2006WR005653, 2007. a
von Storch, H. and Zwiers, F. W.: Statistical Analysis in Climate Research,
Cambridge University Press, Cambridge, United Kingdom, 1999. a
Wijngaard, R. R., Lutz, A. F., Nepal, S., Khanal, S., Pradhananga, S.,
Shrestha, A. B., and Immerzeel, W. W.: Future changes in hydro-climatic
extremes in the Upper Indus, Ganges, and Brahmaputra River basins, PLOS ONE,
12, e0190224, https://doi.org/10.1371/journal.pone.0190224, 2017. a, b
Willis, I.: 168: Hydrology of Glacierized Basins, in: Encyclopedia of
Hydrological Sciences: Part 14. Snow and Glacier Hydrology, edited by:
Anderson, M. G. and McDonnell, J. J., John Wiley & Sons, Ltd, Chichester,
UK, 2005. a
Yadav, M., Wagener, T., and Gupta, H.: Regionalization of constraints on
expected watershed response behavior for improved predictions in ungauged
basins, Adv. Water Resour., 30, 1756–1774,
https://doi.org/10.1016/j.advwatres.2007.01.005, 2007.
a, b
Yilmaz, K. K., Gupta, H. V., and Wagener, T.: A process-based diagnostic
approach to model evaluation: Application to the NWS distributed hydrologic
model, Water Resour. Res., 44, W09417, https://doi.org/10.1029/2007WR006716,
2008. a
Yuan, F., Zhao, C., Jiang, Y., Ren, L., Shan, H., Zhang, L., Zhu, Y., Chen, T.,
Jiang, S., Yang, X., and Shen, H.: Evaluation on uncertainty sources in
projecting hydrological changes over the Xijiang River basin in South China,
J. Hydrol., 554, 434–450, https://doi.org/10.1016/j.jhydrol.2017.08.034,
2017. a, b
Zappa, M. and Kan, C.: Extreme heat and runoff extremes in the Swiss Alps,
Nat. Hazards Earth Syst. Sci., 7, 375–389,
https://doi.org/10.5194/nhess-7-375-2007, 2007. a
Zemp, M., Frey, H., Gärtner-Roer, I., Nussbaumer, S. U., Hoelzle, M.,
Paul, F., Haeberli, W., Denzinger, F., Ahlstrøm, A. P., Anderson, B.,
Bajracharya, S., Baroni, C., Braun, L. N., Càceres, B. E., Casassa, G.,
Cobos, G., Dàvila, L. R., Delgado Granados, H., Demuth, M. N.,
Espizua, L., Fischer, A., Fujita, K., Gadek, B., Ghazanfar, A., Hagen, J. O.,
Holmlund, P., Karimi, N., Li, Z., Pelto, M., Pitte, P., Popovnin, V. V.,
Portocarrero, C. A., Prinz, R., Sangewar, C. V., Severskiy, I., Sigurdsson,
O., Soruco, A., Usubaliev, R., and Vincent, C.: Historically unprecedented
global glacier decline in the early 21st century, J. Glaciol., 61,
745–762, https://doi.org/10.3189/2015JoG15J017, 2015. a
Short summary
We project 21st century change and uncertainty in 25 river flow regime metrics (signatures) for a deglaciating river basin. The results show that glacier-fed river flow magnitude, timing and variability are sensitive to climate change and that projection uncertainty stems from incomplete understanding of future climate and glacier-hydrology processes. These findings indicate how impact studies can be better designed to provide more robust projections of river flow regime in glaciated basins.
We project 21st century change and uncertainty in 25 river flow regime metrics (signatures) for...