Articles | Volume 20, issue 2
https://doi.org/10.5194/hess-20-685-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-20-685-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Technical Note: The impact of spatial scale in bias correction of climate model output for hydrologic impact studies
Santa Clara University, Civil Engineering Department, Santa Clara,
CA 95053-0563, USA
D. L. Ficklin
Indiana University, Department of Geography, Bloomington, IN 47405,
USA
W. Wang
California State University at Monterey Bay, Department of Science and
Environmental Policy and NASA Ames Research Center, Moffett Field, CA 94035,
USA
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Cited articles
Abatzoglou, J. T. and Brown, T. J.: A comparison of statistical
downscaling methods suited for wildfire applications, Int. J. Climatol., 32,
772–780, https://doi.org/10.1002/joc.2312, 2012.
Arnold, J. G., Srinivasan, R., Muttiah, R. S., and Williams, J. R.: Large
Area Hydrologic Modeling and Assessment Part I: Model Development,
J. Am. Water Resour. As., 34, 73–89,
https://doi.org/10.1111/j.1752-1688.1998.tb05961.x, 1998.
Bárdossy, A. and Pegram, G.: Multiscale spatial recorrelation of RCM
precipitation to produce unbiased climate change scenarios over large areas
and small, Water Resour. Res., 48, W09502, https://doi.org/10.1029/2011wr011524, 2012.
Barnett, T. P., Pierce, D. W., Hidalgo, H. G., Bonfils, C., Santer, B. D.,
Das, T., Bala, G., Wood, A. W., Nozawa, T., Mirin, A. A., Cayan, D. R., and
Dettinger, M. D.: Human-Induced Changes in the Hydrology of the Western
United States, Science, 319, 1080–1083, https://doi.org/10.1126/science.1152538,
2008.
Das, T., Maurer, E. P., Pierce, D. W., Dettinger, M. D., and Cayan, D. R.:
Increases in flood magnitudes in California under warming climates, J.
Hydrol., 501, 101–110, https://doi.org/10.1016/j.jhydrol.2013.07.042, 2013.
Eden, J. M., Widmann, M., Grawe, D., and Rast, S.: Skill, Correction, and
Downscaling of GCM-Simulated Precipitation, J. Climate, 25, 3970–3984,
https://doi.org/10.1175/jcli-d-11-00254.1, 2012.
Ehret, U., Zehe, E., Wulfmeyer, V., Warrach-Sagi, K., and Liebert, J.: HESS Opinions “Should we apply bias correction to global
and regional climate model data?”, Hydrol. Earth Syst. Sci., 16, 3391–3404, https://doi.org/10.5194/hess-16-3391-2012, 2012.
Ficklin, D. L. and Barnhart, B. L.: SWAT hydrologic model parameter
uncertainty and its implications for hydroclimatic projections in
snowmelt-dependent watersheds, J. Hydrol., 519, 2081–2090,
https://doi.org/10.1016/j.jhydrol.2014.09.082, 2014.
Ficklin, D. L., Stewart, I. T., and Maurer, E. P.: Projections of 21st
Century Sierra Nevada Local Hydrologic Flow Components Using an Ensemble of
General Circulation Models1, J. Am. Water Resour. As., 48, 1104–1125, https://doi.org/10.1111/j.1752-1688.2012.00675.x, 2012.
Ficklin, D. L., Stewart, I. T., and Maurer, E. P.: Climate Change Impacts on
Streamflow and Subbasin-Scale Hydrology in the Upper Colorado River Basin,
PLoS ONE, 8, e71297, https://doi.org/10.1371/journal.pone.0071297, 2013.
Ficklin, D. L., Barnhart, B. L., Knouft, J. H., Stewart, I. T., Maurer, E. P., Letsinger, S. L.,
and Whittaker, G. W.: Climate change and stream temperature projections in the Columbia
River basin: habitat implications of spatial variation in hydrologic drivers,
Hydrol. Earth Syst. Sci., 18, 4897–4912, https://doi.org/10.5194/hess-18-4897-2014, 2014.
Flato, G., Marotzke, J., Abiodun, B., Braconnot, P., Chou, S. C., Collins,
W., Cox, P., Driouech, F., Emori, S., Eyring, V., Forest, C., Gleckler, P.,
Guilyardi, E., Jakob, C., Kattsov, V., Reason, C., and Rummukainen, M.:
Evaluation of Climate Models, 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. F., Qin,
D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A.,
Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge,
United Kingdom and New York, NY, USA, 741–866, 2013.
Gudmundsson, L., Bremnes, J. B., Haugen, J. E., and Engen-Skaugen, T.: Technical Note: Downscaling RCM
precipitation to the station scale using statistical transformations – a comparison of methods,
Hydrol. Earth Syst. Sci., 16, 3383–3390, https://doi.org/10.5194/hess-16-3383-2012, 2012.
Haan, C. T.: Statistical Methods in Hydrology, second edition, Iowa State
Press, Ames, IA, USA, 496 pp., 2002.
Haerter, J. O., Eggert, B., Moseley, C., Piani, C., and Berg, P.:
Statistical precipitation bias correction of gridded model data using point
measurements, Geophys. Res. Lett., 42, 1919–1929, https://doi.org/10.1002/2015gl063188,
2015.
Hawkins, E. and Sutton, R.: The Potential to Narrow Uncertainty in Regional
Climate Predictions, B. Am. Meteorol. Soc., 90, 1095–1107,
https://doi.org/10.1175/2009BAMS2607.1, 2009.
Hawkins, E. and Sutton, R.: The potential to narrow uncertainty in
projections of regional precipitation change, Clim. Dyn., 37, 407–418,
https://doi.org/10.1007/s00382-010-0810-6, 2011.
Huth, R.: Statistical downscaling of daily temperature in Central Europe, J.
Climate, 15, 1731–1742, 2002.
Hwang, S. and Graham, W. D.: Development and comparative evaluation of a stochastic
analog method to downscale daily GCM precipitation, Hydrol. Earth Syst. Sci., 17, 4481–4502, https://doi.org/10.5194/hess-17-4481-2013, 2013.
Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L.,
Iredell, M., Saha, S., White, G., Woollen, J., Zhu, Y., Leetmaa, A., and
Reynolds, B.: The NCEP/NCAR 40-year reanalysis project, B. Am. Meteorol. Soc.,
77, 437–472, 1996.
Lafon, T., Dadson, S., Buys, G., and Prudhomme, C.: Bias correction of daily
precipitation simulated by a regional climate model: a comparison of
methods, Int. J. Climatol., 1–15, https://doi.org/10.1002/joc.3518,
2012.
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.,
115, D10101, https://doi.org/10.1029/2009jd012882, 2010.
Li, J., Sharma, A., Johnson, F., and Evans, J.: Evaluating the effect of
climate change on areal reduction factors using regional climate model
projections, J. Hydrol., 528, 419–434, https://doi.org/10.1016/j.jhydrol.2015.06.067, 2015.
Livneh, B., Rosenberg, E. A., Lin, C., Nijssen, B., Mishra, V., Andreadis,
K. M., Maurer, E. P., and Lettenmaier, D. P.: A Long-Term Hydrologically
Based Dataset of Land Surface Fluxes and States for the Conterminous United
States: Update and Extensions, J. Climate, 26, 9384–9392,
https://doi.org/10.1175/jcli-d-12-00508.1, 2013.
Maraun, D.: Nonstationarities of regional climate model biases in European
seasonal mean temperature and precipitation sums, Geophys. Res. Lett., 39,
L06706, https://doi.org/10.1029/2012gl051210, 2012.
Maraun, D.: Bias Correction, Quantile Mapping, and Downscaling: Revisiting
the Inflation Issue, J. Climate, 26, 2137–2143, https://doi.org/10.1175/jcli-d-12-00821.1,
2013.
Maraun, D.: Reply to “Comment on `Bias Correction, Quantile Mapping, and
Downscaling: Revisiting the Inflation Issue”', J. Climate, 27, 1821–1825,
https://doi.org/10.1175/jcli-d-13-00307.1, 2014.
Maraun, D. and Widmann, M.: The representation of location by a regional climate model in
complex terrain, Hydrol. Earth Syst. Sci., 19, 3449–3456, https://doi.org/10.5194/hess-19-3449-2015, 2015.
Maraun, D., Wetterhall, F., Ireson, A. M., Chandler, R. E., Kendon, E. J.,
Widmann, M., Brienen, S., Rust, H. W., Sauter, T., Themeßl, M., Venema,
V. K. C., Chun, K. P., Goodess, C. M., Jones, R. G., Onof, C., Vrac, M., and
Thiele-Eich, I.: Precipitation downscaling under climate change: Recent
developments to bridge the gap between dynamical models and the end user,
Rev. Geophys., 48, RG3003, https://doi.org/10.1029/2009rg000314, 2010.
Maurer, E. P., O'Donnell, G. M., Lettenmaier, D. P., and Roads, J. O.:
Evaluation of the land surface water budget in NCEP/NCAR and NCEP/DOE
reanalyses using an off-line hydrologic model, J. Geophys Res., 106,
17841–17862, 2001.
Maurer, E. P., Brekke, L. D., Pruitt, T., and Duffy, P. B.: Fine-resolution
climate change projections enhance regional climate change impact studies,
Eos Trans. AGU, 88, 504, https://doi.org/10.1029/2007EO470006, 2007.
Maurer, E. P., Brekke, L. D., and Pruitt, T.: Contrasting Lumped and
Distributed Hydrology Models for Estimating Climate Change Impacts on
California Watersheds1, J. Am. Water Resour. As., 46, 1024–1035, https://doi.org/10.1111/j.1752-1688.2010.00473.x, 2010a.
Maurer, E. P., Hidalgo, H. G., Das, T., Dettinger, M. D., and Cayan, D. R.: The utility of
daily large-scale climate data in the assessment of climate change impacts on daily streamflow in
California, Hydrol. Earth Syst. Sci., 14, 1125–1138, https://doi.org/10.5194/hess-14-1125-2010, 2010b.
Maurer, E. P., Das, T., and Cayan, D. R.: Errors in climate model daily precipitation and temperature
output: time invariance and implications for bias correction, Hydrol. Earth Syst. Sci., 17, 2147–2159, https://doi.org/10.5194/hess-17-2147-2013, 2013.
Maurer, E. P., Brekke, L., Pruitt, T., Thrasher, B., Long, J., Duffy, P.,
Dettinger, M., Cayan, D., and Arnold, J.: An enhanced archive facilitating
climate impacts and adaptation analysis, B. Am. Meteorol. Soc.,
https://doi.org/10.1175/bams-d-13-00126.1, 2014.
Meehl, G. A., Covey, C., Delworth, T., Latif, M., McAvaney, B., Mitchell, J.
F. B., Stouffer, R. J., and Taylor, K. E.: The WCRP CMIP3 multimodel
dataset: A new era in climate change research, B. Am. Meteorol. Soc., 88,
1383–1394, 2007.
Mehrotra, R. and Sharma, A.: An improved standardization procedure to
remove systematic low frequency variability biases in GCM simulations, Water
Resour. Res., 48, W12601, https://doi.org/10.1029/2012WR012446, 2012.
Mehrotra, R. and Sharma, A.: Correcting for systematic biases in multiple
raw GCM variables across a range of timescales, J. Hydrol., 520, 214–223,
https://doi.org/10.1016/j.jhydrol.2014.11.037, 2015.
Panofsky, H. A. and Brier, G. W.: Some Applications of Statistics to
Meteorology, The Pennsylvania State University, University Park, PA, USA,
224 pp., 1968.
Piani, C., Haerter, J., and Coppola, E.: Statistical bias correction for
daily precipitation in regional climate models over Europe, Theor. Appl.
Climatol., 99, 187–192, https://doi.org/10.1007/s00704-009-0134-9, 2010.
Pierce, D. W., Cayan, D. R., Maurer, E. P., Abatzoglou, J. T., and
Hegewisch, K. C.: Improved Bias Correction Techniques for Hydrological
Simulations of Climate Change, J. Hydrometeorology, 16, 2421–2442,
https://doi.org/10.1175/JHM-D-14-0236.1, 2015.
Reichler, T. and Kim, J.: How Well Do Coupled Models Simulate Today's
Climate?, B. Am. Meteorol. Soc., 89, 303–311,
https://doi.org/10.1175/BAMS-89-3-303, 2008.
Schmidli, J., Frei, C., and Vidale, P. L.: Downscaling from GCM
precipitation: A benchmark for dynamical and statistical downscaling, Int.
J. Climatol., 26, 679–689, 2006.
Sheffield, J., Barrett, A., Colle, B., Fernando, D. N., Fu, R., Geil, K. L.,
Hu, Q., Kinter, J., Kumar, S., Langenbrunner, B., Lombardo, K., Long, L. N.,
Maloney, E., Mariotti, A., Meyerson, J. E., Mo, K. C., Neelin, J. D., Nigam,
S., Pan, Z., Ren, T., Ruiz-Barradas, A., Serra, Y. L., Seth, A., Thibeault,
J. M., Stroeve, J. C., Yang, Z., and Yin, L.: North American Climate in
CMIP5 Experiments. Part I: Evaluation of Historical Simulations of
Continental and Regional Climatology, J. Climate, 26, 9209–9245, https://doi.org/10.1175/jcli-d-12-00592.1,
2013a.
Sheffield, J., Camargo, S. J., Fu, R., Hu, Q., Jiang, X., Johnson, N., Karnauskas, K. B., Kim, S. T.,
Kinter, J., Kumar, S., Langenbrunner, B., Maloney, E., Mariotti, A., Meyerson, J. E., Neelin, J. D., Nigam, S., Pan, Z.,
Ruiz-Barradas, A., Seager, R., Serra, Y. L., Sun, D.-Z., Wang C., Xie, S.-P., Yu, J.-Y., Zhang, T.,
and Zhao, M.: North American climate in CMIP5 experiments, Part II: Evaluation of historical simulations of
intraseasonal to decadal variability, J. Climate, 26, 9247–9290, https://doi.org/10.1175/JCLI-D-12-00593.1, 2013b.
Snover, A. K., Hamlet, A. F., and Lettenmaier, D. P.: Climate-Change
Scenarios for Water Planning Studies: Pilot Applications in the Pacific
Northwest, B. Am. Meteorol. Soc., 84, 1513–1518, https://doi.org/10.1175/BAMS-84-11-1513,
2003.
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.
Teutschbein, C. and Seibert, J.: Is bias correction of regional climate model (RCM)
simulations possible for non-stationary conditions?, Hydrol. Earth Syst. Sci., 17, 5061–5077, https://doi.org/10.5194/hess-17-5061-2013, 2013.
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.
Thrasher, B., Maurer, E. P., McKellar, C., and Duffy, P. B.: Technical Note: Bias
correcting climate model simulated daily temperature extremes with quantile mapping,
Hydrol. Earth Syst. Sci., 16, 3309–3314, https://doi.org/10.5194/hess-16-3309-2012, 2012.
Tian, D., Martinez, C. J., and Graham, W. D.: Seasonal Prediction of
Regional Reference Evapotranspiration Based on Climate Forecast System
Version 2, J. Hydrometeorol., 15, 1166–1188, https://doi.org/10.1175/jhm-d-13-087.1, 2014.
Tryhorn, L. and DeGaetano, A.: A comparison of techniques for downscaling
extreme precipitation over the Northeastern United States, Int. J.
Climatol., 31, 1975–1989, https://doi.org/10.1002/joc.2208, 2011.
Vrac, M., Stein, M., and Hayhoe, K.: Statistical downscaling of
precipitation through nonhomogeneous stochastic weather typing, Clim. Res.,
34, 169–184, https://doi.org/10.3354/cr00696, 2007.
Watterson, I. G., Bathols, J., and Heady, C.: What Influences the Skill of
Climate Models over the Continents?, B. Am. Meteorol. Soc., 95, 689–700,
https://doi.org/10.1175/bams-d-12-00136.1, 2014.
Widmann, M. and Bretherton, C. S.: Validation of mesoscale precipitation in
the NCEP reanalysis using a new grid-cell precipitation dataset for the
Northwestern United States, J. Climate, 13, 1936–1950, 2000.
Wilby, R. L., Hay, L. E., Gutowski, W. J., Arritt, R. W., Takle, E. S., Pan,
Z., Leavesley, G. H., and Clark, M. P.: Hydrological responses to
dynamically and statistically downscaled climate model output, Geophys. Res.
Lett., 27, 1199–1202, 2000.
WMO: Manual on Low-flow Estimation and Prediction, Operational Hydrology
Report No. 50, World Meteorological Organization, Geneva, Switzerland, 138,
2009.
Wood, A. W., Leung, L. R., Sridhar, V., and Lettenmaier, D. P.: Hydrologic
implications of dynamical and statistical approaches to downscaling climate
model outputs, Climatic Change, 62, 189–216, 2004.
Yuan, X. and Wood, E. F.: Downscaling precipitation or bias-correcting
streamflow? Some implications for coupled general circulation model
(CGCM)-based ensemble seasonal hydrologic forecast, Water Resour. Res., 48,
W12519, https://doi.org/10.1029/2012WR012256, 2012.
Zhang, F. and Georgakakos, A.: Joint variable spatial downscaling, Climatic
Change, 111, 945–972, https://doi.org/10.1007/s10584-011-0167-9, 2012.
Short summary
To translate climate model output from its native coarse scale to a finer scale more representative of that at which societal impacts are experienced, a common method applied is statistical downscaling. A component of many statistical downscaling techniques is quantile mapping (QM). QM can be applied at different spatial scales, and here we study how skill varies with spatial scale. We find the highest skill is generally obtained when applying QM at approximately a 50 km spatial scale.
To translate climate model output from its native coarse scale to a finer scale more...