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Correcting lateral boundary biases in regional climate modelling: the effect of the relaxation zone

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Abstract

Regional climate models (RCM) are an important tool for simulating atmospheric information at finer resolutions often of greater relevance to local scale climate change impact assessment studies. The lateral and lower boundary conditions, which form the inputs to the RCM downscaling application, are outputs from the global climate model (GCM). These boundary variables are known to be biased in GCMs, providing the potential to use a statistical approach that corrects these biases before use in downscaling. An array of bias correction techniques have been developed to remove these biases before being used to drive the RCM, but questions remain on their efficacy in terms of the final downscaled output. This study assesses the impact of these bias correction strategies by focussing on how these corrections are translated as one proceeds from the lateral boundaries into the model interior. Of specific interest is the change in the correction from generation of the lateral boundary conditions as well as how correction information moves through the relaxation zone and into the interior of the model. Here we show that bias correction information passing into the regional climate model is limited by interpolations required to generate lateral boundary conditions and dominant outflow wind conditions in the boundaries. This work suggests that these limitations should be addressed in order for bias correction of lateral boundary conditions to robustly influence RCM simulations of climate in the interior of the model domain.

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References

  • Bruyère CL, Done JM, Holland GJ, Fredrick S (2014) Bias corrections of global models for regional climate simulations of high-impact weather. Clim Dyn 43(7–8):1847–1856

    Article  Google Scholar 

  • Davies HC, Turner RE (1977) Updating prediction models by dynamical relaxation: an examination of the technique. Q J R Meteorol Soc 103(436):225–245

    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 

  • Di Virgilio G et al (2019) Evaluating reanalysis-driven CORDEX regional climate models over Australia: model performance and errors. Clim Dyn. https://doi.org/10.1007/s00382-019-04672-w

    Article  Google Scholar 

  • Errico RM, VukiĆEviĆ T, Raeder K (1993) Comparison of initial and lateral boundary condition sensitivity for a limited-area model. Tellus A 45(5):539–557

    Article  Google Scholar 

  • Evans JP, McCabe MF (2013) Effect of model resolution on a regional climate model simulation over southeast Australia. Clim Res 56(2):131–145

    Article  Google Scholar 

  • Evans JP, Ekström M, Ji F (2012) Evaluating the performance of a WRF physics ensemble over South-East Australia. Clim Dyn 39(6):1241–1258

    Article  Google Scholar 

  • Giorgi F, Bi X (2000) A study of internal variability of a regional climate model. J Geophys Res Atmos 105(D24):29503–29521

    Article  Google Scholar 

  • Johnson F, Sharma A (2011) Accounting for interannual variability: a comparison of options for water resources climate change impact assessments. Water Resour Res 47(4):1–20

    Article  Google Scholar 

  • Maraun D (2016) Bias correcting climate change simulations—a critical review. Curr Clim Change Rep 2:211–220

    Article  Google Scholar 

  • Marbaix P, Gallée H, Brasseur O, Ypersele J-PV (2003) Lateral boundary conditions in regional climate models: a detailed study of the relaxation procedure. Mon Weather Rev 131(3):461–479

    Article  Google Scholar 

  • Meehl GA, Covey C, Taylor KE, Delworth T, Stouffer RJ, Latif M, McAvaney B, Mitchell JFB (2007) The WCRP CMIP3 multimodel dataset: a new era in climate change research. Bull Am Meteorol Soc 88(9):1383–1394

    Article  Google Scholar 

  • Moalafhi DB, Sharma A, Evans JP, Mehrotra R, Rocheta E (2017) Impact of bias-corrected reanalysis-derived lateral boundary conditions on WRF simulations. J Adv Model Earth Syst 9(4):1828–1846

    Article  Google Scholar 

  • Olson R, Evans JP, Di Luca A, Argueso D (2016) The NARCliM project: model agreement and significance of climate projections. Clim Res 69:209–227

    Article  Google Scholar 

  • Rocheta E, Evans JP, Sharma A (2014a) Assessing atmospheric bias correction for dynamical consistency using potential vorticity. Environ Res Lett 9(12):124010

    Article  Google Scholar 

  • Rocheta E, Sugiyanto M, Johnson F, Evans J, Sharma A (2014b) How well do general circulation models represent low-frequency rainfall variability? Water Resour Res 50:2108–2123. https://doi.org/10.1002/2012WR013085

    Article  Google Scholar 

  • Rocheta E, Evans JP, Sharma A (2017) Can bias correction of regional climate model lateral boundary conditions improve low-frequency rainfall variability? J Clim 30:9785–9806

    Article  Google Scholar 

  • Seth A, Giorgi F (1998) The effects of domain choice on summer precipitation simulation and sensitivity in a regional climate model. J Clim 11(10):2698–2712

    Article  Google Scholar 

  • Skamarock WC, Klemp JB, Dudhia J, Gill DO, Barker DM, Duda MG, Huang XY, Wang W, Powers JG (2008) A description of the advanced research WRF Version 3

  • Vukicevic T, Errico RM (1990) The influence of artificial and physical factors upon predictability estimates using a complex limited-area model. Mon Weather Rev 118(7):1460–1482

    Article  Google Scholar 

  • Warner TT, Peterson RA, Treadon RE (1997) A tutorial on lateral boundary conditions as a basic and potentially serious limitation to regional numerical weather prediction. Bull Am Meteorol Soc 78(11):2599–2617

    Article  Google Scholar 

  • White RH, Toumi R (2013) The limitations of bias correcting regional climate model inputs. Geophys Res Lett 40(12):2907–2912

    Article  Google Scholar 

  • Wu W, Lynch AH, Rivers A (2005) Estimating the uncertainty in a regional climate model related to initial and lateral boundary conditions. J Clim 18(7):917–933

    Article  Google Scholar 

  • Xu Z, Yang ZL (2012) An improved dynamical downscaling method with GCM bias corrections and its validation with 30 years of climate simulations. J Clim 25:6271–6286

    Article  Google Scholar 

Download references

Acknowledgements

Funding for this research came from the Australian Research Council (FT110100576 and FT100100197) and the Peter Cullen Postgraduate Scholarship. This research was undertaken with the assistance of resources provided at the NCI National Facility systems at the Australian National University through the National Computational Merit Allocation Scheme supported by the Australian Government. We acknowledge the modeling groups for making their model output available for analysis, the PCMDI for collecting and archiving, and the WGCM for organizing this data. ERA-Interim data was obtained from the European Centre for Medium-Range Weather Forecasts (ECMWF) online archive catalogue. Thanks also to the anonymous reviewers who shared their expertise and provided useful commentary which improved the quality of this paper.

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Correspondence to Ashish Sharma.

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Rocheta, E., Evans, J.P. & Sharma, A. Correcting lateral boundary biases in regional climate modelling: the effect of the relaxation zone. Clim Dyn 55, 2511–2521 (2020). https://doi.org/10.1007/s00382-020-05393-1

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