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Short-duration precipitation extremes over Canada in a warmer climate

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Abstract

Short-duration precipitation extremes are widely used in the design of engineering infrastructure systems and they also lead to high impact flash flood events and landslides. Better understanding of these events in a changing climate is therefore critical. This study assesses characteristics of short-duration precipitation extremes of 1-, 3-, 6- and 12-h durations in terms of the precipitation-temperature (P–T) relationship in current and future climates for ten Canadian climatic regions using the limited area version of the global environment multiscale (GEM) model. The GEM simulations, driven by ERA-Interim reanalysis and two coupled global climate models (CanESM2 and MPI-ESM), reproduce the general observed regional P–T relationship characteristics in current climate (1981–2010), such as sub-CC (Clausius–Clapeyron) and CC scalings for the coastal and northern, and inland regions, respectively, albeit with some underestimation. Analysis of the transient climate change simulations suggests important shifts and/or extensions of the P–T curve to higher temperature bins in future climate (2071–2100) for RCP4.5 and 8.5 scenarios, particularly for 1-h duration. Analysis of the spatial patterns of dew point depression (temperature minus dew point temperature) and convective available potential energy (CAPE) corresponding to short-duration precipitation extremes for different temperature bins show their changing relative importance from low to high temperature bins. For the low-temperature bins, short-duration precipitation extremes are largely due to high relative humidity, while for high-temperature bins, strong convection due to atmospheric instability brought by surface warming is largely responsible. The analysis thus addresses some of the key knowledge gaps related to the behavior of P–T relationship and associated mechanisms for the Canadian regions.

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References

  • Adamowski J, Adamowski K, Bougadis J (2010) Influence of trend on short duration design storms. Water Resour Manag 24:401–413

    Article  Google Scholar 

  • Arora V et al (2011) Carbon emission limits required to satisfy future representative concentration pathways of greenhouse gases. Geophys Res Lett 38:L05805. https://doi.org/10.1029/2010GL046270

    Article  Google Scholar 

  • Bao A, Sherwood JSC, Alexander LV, Evans JP (2017) Future increase in extreme precipitation exceed observed scaling rates. Nature Clim Change. https://doi.org/10.1038/NCLIMATE3201

    Article  Google Scholar 

  • Bélair S, Mailhot J, Girard C, Vaillancourt P (2005) Boundary layer and shallow cumulus coulds in a medium-range forecast of a large-scale weather system. Mon Weather Rev 133:1938–1960

    Article  Google Scholar 

  • Benoit R, Cote J, Mailhot J (1989) Inclusion of a Tke boundary-layer parameterization in the Canadian regional finite-element model. Mon Weather Rev 117(8):1726–1750

    Article  Google Scholar 

  • Berg P, Moseley C, Haeter JO (2013) Strong increase in convective precipitation in response to higher temperature. Nat Geosci 6:181–185

    Article  Google Scholar 

  • Cannon AJ, Innocenti S (2019) Projected intensification of sub-daily and daily rainfall extremes in convection-permitting climate model simulations over North America: implications for future intensity-duration-frequency curves. Nat Hazards Earth Syst Sci 19:421–440

    Article  Google Scholar 

  • Cote J, Gravel S, Methot A, Patoine A, Roch M, Staniforth A (1998) The operational CMC-MRB global environmental multiscale (GEM) model. Part I: design considerations and formulation. Mon Weather Rev 126(6):1373–1395

    Article  Google Scholar 

  • Dee DP et al (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137(656):553–597

    Article  Google Scholar 

  • Delage Y (1997) Parameterising sub-grid scale vertical transport in atmospheric models under statistically stable conditions. Bound-Layer Meteorol 82:23–48

    Article  Google Scholar 

  • Diro GT, Sushama L (2017) The role of soil moisture-atmosphere interaction on future hot spells over North America as simulated by the Canadian regional climate model (CRCM5). J Clim 30:5041–5058

    Article  Google Scholar 

  • Diro GT, Sushama L (2019) Simulating Canadian Arctic climate at convection-permitting resolution. Atmosphere. https://doi.org/10.3390/atmos10080430

    Article  Google Scholar 

  • Giorgetta MA et al (2013) Climate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the coupled model intercomparison project phase 5. J Adv Model Earth Syst 5:572–597

    Article  Google Scholar 

  • Haerter JO, Berg P (2009) Unexpected rise in extreme precipitation caused by a shift in rain type? Nat Geosci 2:372–373

    Article  Google Scholar 

  • Hogg WD, Hogg AR (2010) Historical trends in short duration rainfall in the Greater Toronto area. In: Report for the Toronto and region conservation authority. http://trca.on.ca/dotAsset/105189.pdf

  • IPCC (2013) The physical science basis. In: Contribution of working group I to the fifth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, p 1535

  • Jeong DI, Sushama L (2018) Rain-on-snow events over North America based on two Canadian regional climate models. Clim Dyn 50:303–316

    Article  Google Scholar 

  • Kain JS, Fritsch JM (1992) The role of the convective “trigger function” in numerical forecasts of mesoscale convective system. Meteorol Atmos Phys 49:93–106

    Article  Google Scholar 

  • Kendon EJ, Ban N, Roberts NM, Fowler HJ, Roberts MJ, Chan SC, Evans JP, Fosser G, Wilkinson JM (2017) Do convection-permitting regional climate models improve projections of future precipitation changes? Bull Am Meteor Soc 98:79–93

    Article  Google Scholar 

  • Khaliq MN, Sushama L, Monette A, Wheater H (2014) Seasonal and extreme precipitation characteristics for the watersheds of the Canadian Prairie Provinces as simulated by the NARCCAP multi-RCM ensemble. Clim Dyn. https://doi.org/10.1007/s00382-014-2235-0

    Article  Google Scholar 

  • Kim G, Cha D-H et al (2018) Future change in extreme precipitation indices over Korea. Int J Climatol 2018:e862–e874

    Article  Google Scholar 

  • Lenderink G, van Meijgaard E (2008) Increase in hourly precipitation extremes beyond expectations from temperature change. Nat Geosci 1:511–514

    Article  Google Scholar 

  • Lenderink G, van Meijgaard E (2010) Linking increases in hourly precipitation extremes to atmospheric temperature and moisture changes. Environ Res Lett 5:025208. https://doi.org/10.1088/1748-9326/5/2/025208

    Article  Google Scholar 

  • Li J, Barker HW (2005) A radiation algorithm with correlated-k distribution. Part I: local thermal equilibrium. J Atmos Sci 62(2):286–309

    Article  Google Scholar 

  • Martynov AR, Laprise L, Sushama K, Winger L Separovic, Dugas B (2013) Reanalysis-driven climate simulation over CORDEX North America domain using the Canadian regional climate model, version 5: model performance evaluation. Clim Dyn. https://doi.org/10.1007/s00382-013-1778-9

    Article  Google Scholar 

  • Mekis E, Donaldson N, Reid J, Zucconi A, Hoover J, Li Q, Nitu R, Melo S (2018) An overview of surface-based precipitation observation at Environment and Climate Change Canada. Atmos Ocean 56(2):71–95

    Article  Google Scholar 

  • Miao C, Sun Q, Borthwick AGL, Duan Q (2016) Linkage between hourly precipitation events and atmospheric temperature changes over China during the warm season. Sci Rep. https://doi.org/10.1038/srep22543

    Article  Google Scholar 

  • Mladjic B, Sushama L, Khaliq MN, Laprise R, Caya D, Roy R (2011) Canadian RCM projected changes to extreme precipitation characteristics over Canada. J Clim 24:2565–2584

    Article  Google Scholar 

  • Muller CJ, O’Gorman PA, Back LE (2011) Intensification of precipitation extremes with warming in a cloud resolving model. J Clim 24:2784–2800

    Article  Google Scholar 

  • Oh SG, Suh MS (2018) Changes in seasonal and diurnal precipitation types during summer over South Korea in the late twenty-first century (2081-2100) projected by the RegCM4.0 based on four RCP scenarios. Clim Dyn 51:3041–3060

    Article  Google Scholar 

  • Panthou G, Mailhot A, Laurence E, Talbot G (2014) Relationship between surface temperature and extreme rainfalls: a multi-time scale and event-based analysis. J Hydrometeorol 15:1999–2011

    Article  Google Scholar 

  • Park IH, Min SK (2017) Role of convective precipitation in the relationship between subdaily extreme precipitation and temperature. J Clim 30:9527–9537

    Article  Google Scholar 

  • Plummer DA et al (2006) Climate and climate change over North America as simulated by the Canadian RCM. J Clim 19:3112–3132

    Article  Google Scholar 

  • Prein AF, Langhans W, Fosser G, Ferrone A, Ban N, Goergen K, Keller M, Tolle M, Gutjahr O, Feser F, Brisson E, Kollet S, Schmidli J, van Lipzig NPM, Leung R (2015) A review on regional convection-permitting climate modeling: demonstrations, prospects, and challenges. Rev Geophys 53:323–361

    Article  Google Scholar 

  • Prein AF, Rasmussen RM, Ikeda K, Liu C, Clark MP (2016) The future intensification of hourly precipitation extremes. Nature Clim Change. https://doi.org/10.1038/NCLIMATE3168

    Article  Google Scholar 

  • Prein AF, Liu C, Ikeda K, Bullock R, Rasmussen RM, Holland GJ, Clark M (2017) Simulating North American mesoscale convective systems with a convection-permitting climate model. Clim Dyn. https://doi.org/10.1007/s00382-017-3993-2

    Article  Google Scholar 

  • Romps DM (2011) Response of tropical precipitation to global warming. J Atmos Sci 68:123–138

    Article  Google Scholar 

  • Schroeer K, Kirchengast G (2018) Sensitivity of extreme precipitation to temperature: the variability of scaling factors from a regional to local perspective. Clim Dyn 50:3981–3994

    Article  Google Scholar 

  • Shaw SB, Royen AA, Riha SJ (2011) The relationship between extreme hourly precipitation and surface temperature in different hydroclimatic regions of the United States. J Hydrometeorol 12:319–325

    Article  Google Scholar 

  • Shephard MW, Mekis E, Morris RJ, Feng Y, Zhang X, Kilcup K, Fleetwood R (2014) Trends in Canadian short-duration extreme rainfall: including an intensity-duration-frequency perspective. Atmos Ocean 5:398–417

    Article  Google Scholar 

  • Shuttleworth WJ (1993) Evaporation. In: Maidment DR (ed) Handbook of hydrology, chap. 4. McGraw-Hill, New York, USA, pp 4.1–4.53

    Google Scholar 

  • Sundqvist H, Berge E, Kristjánsson JE (1989) Condensation and cloud parameterization studies with a mesoscale numerical weather prediction model. Mon Weather Rev 117(8):1641–1657

    Article  Google Scholar 

  • Teufel BGT et al (2017) Investigation of the 2013 Alberta flood from weather and climate perspectives. Clim Dyn 48:2881–2899

    Article  Google Scholar 

  • United Nations (2017) World population prospects: the 2017 revision, key findings and advanced tables. Department of Economic and Social Affairs, Population Division, United Nations Press, p 47

  • Verseghy DL (2009) CLASS-The Canadian land surface scheme (version 3.4)-technical documentation (version 1.1). In: Internal report, Climate Research Division, Science and Technology Branch, Environment Canada, p 183

  • Westra S, Fowler HJ, Evans JP, Alexander LV, Berg P, Johnson F, Kendon EJ, Lenderink G, Roberts NM (2014) Future changes to the intensity and frequency of short-duration extreme rainfall. Rev Geophys 52:522–555

    Article  Google Scholar 

  • Woodhams BJ, Birch CE, Marsham JH, Bain CL, Roberts NM, Boyd DFA (2018) What is the added value of a convection-permitting model for forecasting extreme rainfall over tropical East Africa. Mon Weather Rev 146:2757–2780

    Article  Google Scholar 

  • Yeh KS, Cote J, Gravel S, Methot A, Patoine A, Roch M, Staniforth A (2002) The CMC-MRB global environmental multiscale (GEM) model. Part III: nonhydrostatic formulation. Mon Weather Rev 130(2):339–356

    Article  Google Scholar 

  • Zadra A, McTaggart-Cowan R, Roch M (2012) Recent changes to the orographic blocking. In: Seminar presentation, PRN, Dorval, Canada, 30 March 2012. http://collaboration.cmc.ec.gc.ca/science/rpn/SEM/dossiers/2012/seminaires/2012-03-30/Seminar_2012-03-30_Ayrton-Zadra.pdf. Accessed 27 Aug 2018

  • Zhang X, Zwiers FW, Li G, Wan H, Cannon AJ (2017) Complexity in estimating past and future extreme short-duration rainfall. Nat Geosci. https://doi.org/10.1038/NGEO2911

    Article  Google Scholar 

Download references

Acknowledgements

This research was funded by the Natural Sciences and Engineering Research Council of Canada and the Trottier Institute for Sustainability in Engineering and Design. The GEM simulations considered in this study were performed on the supercomputer managed by Compute Canada and Calcul Québec.

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  1. Department of Civil Engineering and Applied Mechanics and Trottier Institute for Sustainability in Engineering and Design, McGill University, Montreal, Canada

    Seok-Geun Oh & Laxmi Sushama

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  1. Seok-Geun Oh
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Correspondence to Seok-Geun Oh.

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Oh, SG., Sushama, L. Short-duration precipitation extremes over Canada in a warmer climate. Clim Dyn 54, 2493–2509 (2020). https://doi.org/10.1007/s00382-020-05126-4

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