Abstract
This paper presents the basis for the design of streamflow prediction systems for the hydroelectric dams of Rincón del Bonete (Uruguay) and Salto Grande (Uruguay–Argentina). The prediction is made, independently, for each reservoir and each month of the year with two methodologies: data-driven statistical models and hybrid downscaling that includes atmospheric predictors. We determine a set of potential predictors and then fit linear models coupled with variable selection techniques, under the hypothesis of perfectly known predictors. The predictive skill of the schemes outperforms the climatological forecast throughout the year in both reservoirs (except August in Rincón del Bonete). This remains the case even when the forecast lead does not allow for the use of preceding flows as predictors. While in Rincón del Bonete it is not possible to distinguish a period of high predictability, in Salto Grande, there is a robust signal in March–May and October–December.
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References
Aceituno P (1988) On the functioning of the southern oscillation in the South American sector. Part I: surface climate. Mon Weather Rev 116:505–524
Aceituno P (1989) On the functioning of the southern oscillation in the South American sector. Part II. Upper-air circulation. J Clim 2:341–355
Barnston AG (1994) Linear statistical short-term climate predictive skill in the Northern Hemisphere. J Clim 7:1513–1564
Cazes-Boezio G, Robertson A, Mechoso R (2003) Seasonal dependence of ENSO teleconnections over South America and relationships with precipitation in Uruguay. J Clim 16:1159–1176
Farrara JD, Mechoso CR, Robertson AW (2000) Ensembles of AGCM two-tier predictions and simulations of the circulation anomalies during winter 1997–1998. Mon Weather Rev 128:3589–3604
Goddard L, Mason SJ, Zebiak SE, Ropelewski CF, Basher R, Cane MA (2001) Current approaches to seasonal-to-interannual climate predictions. Int J Clim 21:1111–1152
Grimm AM, Pal JS, Giorgi F (2007) Connection between spring conditions and peak summer monsoon rainfall in South America: role of soil moisture, surface temperature and topography in eastern Brazil. J Clim 20:5929–5945
Izenman AJ (2008) Modern multivariate statistical techniques, Springer texts in statistics. Springer, New York
Kalnay E et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–470
Konor CS, Cazes-Boezio G, Mechoso CR, Arakawa A (2009) Parameterization of PBL processes in an atmospheric general circulation model: description and preliminary assessment. Mon Weather Rev 137:1061–1082
Koster R et al (2011) The second phase of the global land–atmosphere coupling experiment: soil moisture contributions to subseasonal forecast skill. J Hydrometeorol 12:805–822
Kumar A, Hoerling MP (2003) The nature and causes for the delayed atmospheric response to El Niño. J Clim 16:1391–1403
Landman WA, Mason SJ, Tyson PD, Tennat WJ (2001) Statistical downscaling of GCM simulations to streamflow. J Hydrol 252:221–236
Lima CH, Lall U (2010) Climate informed monthly streamflow forecasts for the Brazilian hydropower network using a periodic ridge regression model. J Hydrol 380:438–449
Lorenz EN (1963) Deterministic nonperiodic flow. J Atmos Sci 20:130–141
Lumley T (2009) Package leaps. http://cran.r-project.org/
Mechoso CR, Pérez-Irribarren G (1992) Streamflow in southeastern South America and the southern oscillation. J Clim 5:1535–1539
Miller AJ, Cayan DR, Barnett TP, Graham EN, Oberhuber JM (1994) The 1976–1977 climate shift of the Pacific Ocean. J Oceanogr 7:21–26
Pisciottano G, Díaz A, Cazes G, Mechoso R (1994) El Niño—southern oscillation impact on rainfall in Uruguay. J Clim 7:1286–1302
Reynolds RW, Rayner NA, Smith TM, Stokes DC, Wang W (2002) An improved in situ and satellite SST analysis for climate. J Clim 15:1609–1625
Richman MB (1986) Rotation of principal components. J Climatol 6:293–335
Ropelewski CF, Halpert MS (1987) Global and regional scale precipitation patterns associated with the El Niño/southern oscillation. Mon Weather Rev 115:1606–1626
Ropelewski CF, Halpert MS (1989) Precipitation patterns associated with the high index phase of the southern oscillation. J Clim 2:268–284
Soukup TL, Aziz OA, Tootle GA, Piechota TC, Wulff SS (2009) Long lead-time streamflow forecasting of the North Platte River incorporating oceanic-atmospheric climate variability. J Hydrol 368:131–142
Stone M (1974) Cross-validatory choice and assessment of statistical predictions. J R Stat Soc Ser B (Methodol) 36:111–147
Su H, Neelin JD, Meyerson JE (2005) Mechanisms for lagged atmospheric response to ENSO forcing. J Clim 18:4195–4215
Trenberth KE (1990) Recent observed interdecadal climate changes in the Northern Hemisphere. Bull Am Meteorol Soc 71:988–993
Wang W (2006) Stochasticity, nonlinearity and forecasting of streamflow processes. IOS, Amsterdam
Westra S, Brown C, Lall U, Sharma A (2007) Modeling multivariable hydrological series: principal component analysis or independent component analysis? Water Resources Res 43:W06429
Westra S, Sharma A (2009) Probabilistic estimation of multivariate streamflow using independent component analysis and climate information. J Hydrometeorol 10:1479–1492
Westra S, Sharma A (2010) An upper limit to seasonal rainfall predictability? J Clim 7:3332–3351
Wood AW, Maurer EP, Kumar A, Lettenmaier DP (2002) Long-range experimental hydrologic forecasting for the eastern United States. J Geophys Res 107:4429. doi:10.1029/2001JD000659
Acknowledgements
Part of this work was performed while the first author was supported by a grant from Agencia Nacional de Investigación e Innovación (ANII). We thank Marco Scavino for insightful discussions and Gabriel Cazes for helping with the simulations.
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Appendix
Appendix
In Figs. 17 and 18, we show, for each month of the year, the variables selected for the model lmAUCLAOQ-optimal for Rincón del Bonete and Salto Grande, respectively. Variables not available for selection (those not included in the AUCLA group) are indicated in white, variables available but not selected are indicated in grey and variables selected are indicated in black.
For Rincón del Bonete (Fig. 17), the most selected variable is Q1; N3.4 is persistently selected from November to February, and the only season in which atmospheric variables were selected is from February to July.
For Salto Grande (Fig. 18), in every month of the year, at least one of the variables of precedent flow is selected. N3.4 is selected in a continuous manner from October to January and, similar to what happened for Rincón del Bonete, the selection of atmospheric variables is restricted to the period March–July.
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Talento, S., Terra, R. Basis for a streamflow forecasting system to Rincón del Bonete and Salto Grande (Uruguay). Theor Appl Climatol 114, 73–93 (2013). https://doi.org/10.1007/s00704-012-0822-8
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DOI: https://doi.org/10.1007/s00704-012-0822-8