Abstract
Glacial debris flows (GDFs) often occur in alpine regions that are subject to rapid climate change, and pose a serious threat to road systems. However, the ways that climate change impacts GDF risks along road systems remain poorly understood. Aierkuran Gully, located in eastern Pamir along Karakoram Highway (KKH), is a hotspot for GDF activity and climate change, and was thus selected to investigate the GDF risk to road systems under climate change conditions. RegCM4.6 climate data for northwestern China were selected as climate projections during baseline (2011–2020) and future periods (2031–2040) under the Representative Concentration Pathway (RCP) 8.5. To reflect the coupling effect of rainfall and melt water that triggers GDF, a glacial hydrological model DETIM that considers both factors was applied to calculate the peak debris flow discharge. A FLO-2D model was calibrated based on high-quality data collected from a detailed field investigation and historical debris flow event. The FLO-2D model was used to simulate the debris flow depth and velocity during baseline and future periods under RCP8.5. The debris flow hazard was analyzed by integrating the maximum flow depth and momentum. Road structure vulnerability was further determined based on the economic value and susceptibility of hazard-affected objects. The GDF risk along KKH was assessed based on the GDF hazard and vulnerability analysis. Our results show that climate change would lead to amplified peak debris flow discharge, trigger higher-magnitude GDF, and induce more severe damage and threats to the road system. Compared with the baseline period, the debris flow damage risk for culverts and bridges would increase and the areas that inundate the road and pavement would expand. Our findings provide valuable insights for the development of mitigation strategies to adapt road systems to climate change, especially in alpine regions with highly active GDFs.
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References
Baker DH, Escher-Vetter H, Moser H, et al. (1982) A glacier discharge model based on results from field studies of energy balance, water storage and flow. In: Internaltional Association of Hydrological Sciences Publication 138 (Symposium at Exeter 1982-Hydological Aspects of Alpine and High Mountain Areas). pp 103–112.
Blaikie P, Cannon T, Davis I, et al. (1994) At risk: natural hazards, people’s vulnerability, and disaster. Routledge, London.
Chang M, Tang C, Asch TWJV, et al. (2017). Hazard assessment of debris flows in the Wenchuan earthquake-stricken area, South West China. Landslides 14(5): 1–10. https://doi.org/10.1007/s10346-017-0824-9
Chen XZ, Cui P, You Y, et al. (2012) Post-earthquake changes and prediction of debris flow scales in Subao River Valley, Beichuan County, Sichuan Province, China. Environ Earth Sci 65: 995–1003. https://doi.org/10.1007/s12665-011-0949-4
Chen XZ, Cui YF (2017). The formation of the Wulipo landslide and the resulting debris flow in Dujiangyan City, China. J Mt Sci 14(6): 1100–1112. https://doi.org/10.1007/s11629-017-4392-1
Chiarle M, Iannotti S, Mortara G, et al. (2007) Recent debris flow occurrences associated with glaciers in the Alps. Glob Planet Change 56(1/2): 123–136. https://doi.org/10.1016/j.gloplacha.2006.07.003
Clague JJ (2009) Climate Change and Slope Instability. In: Sassa K, Canuti P (eds) Landslides — Disaster Risk Reduction. Springer, Berlin, Heidelberg.
Cui P, Hu KH, Zhuang JQ, et al. (2011). Prediction of debris-flow danger area by combining hydrological and inundation simulation methods. J Mt Sci 8(1): 1–9. https://doi.org/10.1007/s11629-011-2040-8
Cui P, Jia Y (2015). Mountain hazards in the Tibetan Plateau: research status and prospects. Natl Sci Rev 2(4): 397–399.
Cui P, Zou Q, Xiang LZ, et al. (2013b) Risk assessment of simultaneous debris flows in mountain townships. Prog Phys Geogr 37(4): 516–542. https://doi.org/10.1177/0309133313491445
Cui YH, Ye BS, Wang J, et al. (2013a) The runoff simulations for the Glacier No.1 hydrologic section at the headwaters of the Urumqi river on the different timescales. J Arid Land Resour Environ 27(7): 119–126. (In Chinese) https://doi.org/10.13448/j.cnki.jalre.2013.07.034
Derbyshire E, Fort M, Owen LA (2001). Geomorphological hazards along the Karakoram Highway: Khunjerab Pass to the Gilgit River, Northernmost Pakistan. Erdkunde 55(1): 49–71. https://doi.org/10.3112/erdkunde.2001.01.04
Donat MG, Lowry AL, Alexander LV, et al. (2016) More extreme precipitation in the world’s dry and wet regions. Nat Clim Chang 6: 508–513. https://doi.org/10.1038/nclimate2941
Eisbacher GH (1982) Mountain torrents and debris flows. Episodes 4: 12–17. https://doi.org/10.18814/epiiugs/1982/v5i4/003
Evans SG, Clague, JJ (1994). Recent climatic change and catastrophic geomorphic processes in mountain environments. Geomorphology 10(1–4): 107–128. https://doi.org/10.1016/B978-0-444-82012-9.50012-8
Field CB, Barros V, Stocker TF, et al. (2012) Managing the risks of extreme events and disasters to advance climate change adaptation. In: Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). Cambridge: Cambridge University Press, Cambridge, UK.
FLO-2D Software Inc (2009) FLO-2D User Manual, Version 2009. Nutrioso, Arizona.
Garcia R, Rodriguez JJ, O’Brien JS (2004) Hazard zone delineation for urbanized alluvial fans. ASCE World Water and Environmental Resources Congress — Arid Lands Symposium, Salt Lake City, Utah.
Ge YG, Su FH, Chen XQ, et al. (2015). Destructions on the Karakoram Highway (KKH) from Sost to Khunjerab induced by geo-Hazards and prevention. Appl Mech Mater 744–746: 1234–1243. https://doi.org/10.4028/www.scientific.net/AMM.744-746.1234
Gobiet A, Kotlarski S, Beniston M, et al. (2014) 21st century climate change in the European Alps—A review. Sci Total Environ 493:1138–1151. https://doi.org/10.1016/j.scitotenv.2013.07.050
Guo WQ, Liu SY, Xu L, et al. (2015). The second Chinese glacier inventory: data, methods and results. J Glaciol 61(226): 357–372. https://doi.org/10.3189/2015JoG14J209
Hock R (1999). A distributed temperature index ice and snow melt model including potential direct solar radiation. J Glaciol 45(149): 101–111. https://doi.org/10.3189/s0022143000003087
Hock R, Noetzli C (1997) Areal mass balance and discharge modelling of Storglaciären, Sweden. Ann Glaciol 24: 211–217. https://doi.org/10.3189/S0260305500012192
Huggel C, Clagu JJ, Korup O (2012) Is climate change responsible for changing landslide activity in high mountains? Earth Surf Process Landf 37: 77–91. https://doi.org/10.1002/esp.2223
Hungr O (1995) A model for the runout analysis of rapid flow slides, debris flows and avalanches. Can Geotech J 32: 610–623. https://doi.org/10.1139/T95-063
Huss M, Hock R (2018) Global-scale hydrological response to future glacier mass loss. Nature Clim Change 8:135–140. https://doi.org/10.1038/s41558-017-0049-x
IPCC (2013) Summary for Policymakers. Working Group I Contribution to the IPCC Fifth Assessment Report. Climate Change: The Physical Science Basis. Cambridge University Press, Cambridge, UK
Iverson R (1997). The physics of debris flows. Rev Geophys 35(3): 245–296. https://doi.org/10.1029/97RG00426
Iverson R, Schilling M, Vallance J (1998). Objective delineation of lahar-inundation hazard zones. Geol Soc Am Bull 110(8): 972–984. https://doi.org/10.1130/0016-7606(1998)110<0972:ODOLIH>2.3.CO;2
Jenks GF (1967) The Data Model Concept in Statistical Mapping. International Yearbook of Cartography 7: 186–190.
Li M, Tian CS, Wang YK, et al. (2018). Impacts of future climate change (2030–2059) on debris flow hazard: A case study in the Upper Minjiang River basin, China. J Mt Sci 15(8): 1836–1850. https://doi.org/10.1007/s11629-017-4787-z
Liu JF, Nakatani K, Mizuyama T (2011). Effect assessment of debris flow mitigation works based on numerical simulation by using Kanako 2D. Landslides 10(2): 161–173. https://doi.org/10.1007/s10346-012-0316-x
Marzeion B, Jarosch AH, Hofer M (2012) Past and future sea-level change from the surface mass balance of glaciers. Cryosphere 6: 1295–1322. https://doi.org/10.5194/tc-6-1295-2012
O’Brien JS (2004) FLO-2D User’s Manual. Version 2004.6.1. Nutrioso, Arizona.
O’Brien JS, Julien PY, Fullerton WT (1993). Two-dimensional water flood and mudflow simulation. J Hydraul Eng 119(2): 244–261. https://doi.org/10.1061/(ASCE)0733-9429(1993)119:2(244)
Ouyang CJ, Wang ZW, An HC, et al. (2019). An example of a hazard and risk assessment for debris flows—a case study of Niwan Gully, Wudu, China. Eng Geol 263: 105351. https://doi.org/10.1016/j.enggeo.2019.105351
Owen LA, Derbyshire E (1989) The Karakoram glacial depositional system. Zeitschrift für Geomorphologie 76: 33–73.
Pan XD, Zhang L (2020) Future climate projection of China based on RegCM4.6 (2007–2099). Natl Tibetan Plateau Data Cent. https://doi.org/10.11888/Meteoro.tpdc.270998.
Pan XD, Zhang L, Huang CL (2020) Future climate projection in Northwest China with RegCM4.6. Earth Space Sci 7: e2019EA000819. https://doi.org/10.1029/2019EA000819
Qiu YB, Lu JY, Shi LJ, et al. (2018) Passive microwave remote sensing data of snow water equivalent in High Asia. Science Data Bank. https://doi.org/10.11922/sciencedb.660
Radić V, Bliss A, Beedlow AC, et al. (2014) Regional and global projections of twenty-first century glacier mass changes in response to climate scenarios from global climate models. Clim Dyn 42: 37–58. https://doi.org/10.1007/s00382-013-1719-7
Rebetez M, Lugon R, Baeriswyl PA (1997) Climatic change and debris flows in high mountain regions: the case study of the Ritigraben Torrent (Swiss Alps). Clim Change 36: 371–389. https://doi.org/10.1023/A:1005356130392
Ren Z, Su FG, Xu BQ, et al. (2018). A coupled glacier-hydrology model and its application in eastern Pamir. J Geophys Res Atmos 123(13): 692–713. https://doi.org/10.1029/2018JD028572
Rickenmann D (2016). Debris flow hazard assessment and methods applied in engineering practice. Int J Erosion Control Eng 9(3): 80–90. https://doi.org/10.13101/ijece.9.80
Rickenmann D, Laigle D, Mcardell BW, et al. (2006). Comparison of 2D debris-flow simulation models with field events. Comput Geosci 10(2): 241–264. https://doi.org/10.1007/s10596-005-9021-3
Roe GH, Baker MB, Herla F (2017). Centennial glacier retreat as categorical evidence of regional climate change. Nat Geosci 10(2): 95–99. https://doi.org/10.1038/ngeo2863
Schneeberger C, Albrecht O, Blatter H, et al. (2001) Modelling the response of glaciers to a doubling in atmospheric CO2: a case study on Storglaciären, northern Sweden. Clim Dynam 17: 825–834. https://doi.org/10.1007/s003820000147
Schwalm CR, Glendon S, Duffy PB (2020). RCP8.5 tracks cumulative CO2 emissions. Proc Nat Acad Sci India A 117(33): 19656–19657. https://doi.org/10.1073/pnas.2007117117
Shen MX, Chen J, Zhuan MJ, et al. (2018) Estimating uncertainty and its temporal variation related to global climate models in quantifying climate change impacts on hydrology. J Hydrol 556: 10–24. https://doi.org/10.1016/j.jhydrol.2017.11.004
Staffler H, Pollinger R, Zischg AP, et al. (2008) Spatial variability and potential impacts of climate change on flood and debris flow hazard zone mapping and implications for risk management. Nat Hazards Earth Syst Sci 8: 539–558. https://doi.org/10.5194/nhess-8-539-2008
Stancanelli LM, Peres DJ, Cancelliere A, et al. (2017) A combined triggering-propagation modeling approach for the assessment of rainfall induced debris flow susceptibility. J Hydrol 550:130–143. https://doi.org/10.1016/j.jhydrol.2017.04.038
Stoffel M, Mendlik T, Schneuwly-Bollschweiler M, et al. (2014). Possible impacts of climate change on debris-flow activity in the Swiss Alps. Clim Change 122:141–155. https://doi.org/10.1007/s10584-013-0993-z
Stoffel M, Beniston M (2006). On the incidence of debris flows from the early Little Ice Age to a future greenhouse climate: a case study from the Swiss Alps. Geophys Res Lett 33(16): 271–284. https://doi.org/10.1029/2006GL026805
Su LJ, Hu KH, Zhang WF, et al. (2017). Characteristics and triggering mechanism of Xinmo landslide on 24 June 2017 in Sichuan, China. J Mt Sci 14(9): 1689–1700. https://doi.org/10.1007/s11629-017-4609-3
Sun JQ, Ao J (2013). Changes in precipitation and extreme precipitation in a warming environment in China. Chin Sci Bull 58(12): 1395–1401. https://doi.org/10.1007/s11434-012-5542-z
Takebayashi H, Fujita M. (2020). Numerical simulation of a debris flow on the basis of a Two-Dimensional Continuum Body Model. Geosciences 10(2): 45. https://doi.org/10.3390/geosciences10020045
Tebaldi C, Knutti R (2007) The use of the multi-model ensemble in probabilistic climate projections. Philos Trans R Soc A 365: 2053–2075. https://doi.org/10.1098/rsta.2007.2076
Turkington T, Remaître A, Ettema J, et al. (2016) Assessing debris flow activity in a changing climate. Clim Change 137: 293–305. https://doi.org/10.1007/s10584-016-1657-6
United Nations (1991) Department of Humanitarian Affairs. Mitigating natural disaster: phenomena, effects and options-A manual for policy makers and planners. New York.
United Nations (1992) Department of Humanitarian Affairs. Internationally agreed glossary of basic terms related to disaster management. Geneva.
Wei FQ, Hu KH, Lopez JL, et al. (2003). Method and its application of the momentum model for debris flow risk zoning. Chin Sci Bull 48(6): 594–598. https://doi.org/10.1360/03tb9126
Wei K, Ouyang CJ, Duan HT, et al. (2020) Reflections on the catastrophic 2020 Yangtze River Basin flooding in southern China. The Innovation, 100038. https://doi.org/10.1016/j.xinn.2020.100038
Wei XL, Li W, Li B (2017). The type characteristics and cause Analysis of group occurring washout disaster along G314 road in 2015. Geogr Sci Res 6(2): 83–91. (In Chinese) https://doi.org/10.12677/gser.2017.62011
Westra S, Fowler HJ, Evans JP, et al. (2014). Future changes to the intensity and frequency of short-duration extreme rainfall. Rev Geophys 52(3): 522–555. https://doi.org/10.1002/2014RG000464
Woolhiser DA (1975) Simulation of unsteady overland flow. In: Mahmood K, Yevjevich V (eds) Unsteady flow in open channels. Water Resources Publications, Fort Collins, Co. Colorado, USA.
Wu YH, Liu KF, Chen YC (2013). Comparison between FLO-2D and Debris-2D on the application of assessment of granular debris flow hazards with case study. J Mt Sci 10(2): 293–304. https://doi.org/10.1007/s11629-013-2511-1
Yang TQ, Li Y, Zhang QS, et al. (2019) Calculating debris flow density based on grain-size distribution. Landslides 16: 515–522. https://doi.org/10.1007/s10346-018-01130-2
Zhang XT, Li XM, Gao P, et al. (2017). Separation of precipitation forms based on different methods in Tianshan mountainous area, Northwest China. J Glaciol Geocryol 39(2): 235–244. (In Chinese) https://doi.org/10.7522/j.issn.1000-0240.2017.0027
Zegers G, Mendoza PA, Garces A, et al. (2020). Sensitivity and identifiability of rheological parameters in debris flow modeling. Nat Hazards Earth Syst Sci 20(7): 1919–1930. https://doi.org/10.5194/nhess-20-1919-2020
Zhou BT, Wen HQ, Xu Y, et al. (2014) Projected changes in temperature and precipitation extremes in China by the CMIP5 Multimodel Ensembles. Journal of Climate 27: 6591–6611. https://doi.org/10.1175/JCLI-D-13-00761.1
Zhuang JQ, Cui P, Hu KH, et al. (2010). Characteristics of earthquake-triggered landslides and post-earthquake debris flows in Beichuan County. Journal of Mountain Science 7(3): 246–254. https://doi.org/10.1007/s11629-010-2016-0
Zimmermann M, Haeberli W (1992) Climatic change and debris flow activity in high mountain areas—a case study in the Swiss Alps. Catena Supplement 22: 59–72. https://doi.org/10.1023/A:1005356130392
Zou Q, Zhou GD, Li SS, et al. (2017). Dynamic process analysis and hazard prediction of debris flow in eastern Qinghai-Tibet Plateau area-A case study at Ridi Gully. Arctic Antarctic and Alpine Research 49(3): 373–390. https://doi.org/10.1657/AAAR0017-019
Acknowledgements
This research was jointly funded by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA20030301), the Comprehensive Investigation and Assessment of Natural Hazards in China-Pakistan Economic Corridor (Grant No. 2018FY100506), the Second Tibetan Plateau Scientific Expedition and Research Program (STEP) (Grant No. 2019QZKK0906) and the International Science & Technology Cooperation Program of China (Grant No. 2018YFE0100100). We also express our thanks to Xinjiang Uygur Autonomous Region Meteorological Service for providing historical climate data.
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Li, Ym., Su, Lj., Zou, Q. et al. Risk assessment of glacial debris flow on alpine highway under climate change: A case study of Aierkuran Gully along Karakoram Highway. J. Mt. Sci. 18, 1458–1475 (2021). https://doi.org/10.1007/s11629-021-6689-3
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DOI: https://doi.org/10.1007/s11629-021-6689-3