Abstract
In this study we developed and examined a hybrid modeling approach integrating physically-based equations and statistical downscaling to estimate fine-scale daily-mean surface turbulent fluxes (i.e., sensible and latent heat fluxes) for a region of southern California that is extensively covered by varied vegetation types over a complex terrain. The selection of model predictors is guided by physical parameterizations of surface flux used in land surface models and analysis showing net shortwave radiation that is a major source of variability in the surface energy budget. Through a structure of multivariable regression processes with an application of near-surface wind estimates from a previous study, we successfully reproduce dynamically-downscaled 3 km resolution surface flux data. The overall error in our estimates is less than 20 % for both sensible and latent heat fluxes, while slightly larger errors are seen in high-altitude regions. The major sources of error in estimates include the limited information provided in coarse reanalysis data, the accuracy of near-surface wind estimates, and an ignorance of the nonlinear diurnal cycle of surface fluxes when using daily-mean data. However, with reasonable and acceptable errors, this hybrid modeling approach provides promising, fine-scale products of surface fluxes that are much more accurate than reanalysis data, without performing intensive dynamical simulations.
Similar content being viewed by others
References
Baldocchi D et al (2001) FLUXNET: a new tool to study the temporal and spatial variability of ecosystem-scale carbon dioxide, water vapor, and energy flux densities. Bull Am Meteorol Soc 82:2415–2434
Beljaars ACM, Holtslag AAM (1991) On flux parametrization over land surfaces for atmospheric models. J Appl Meteorol 30:327–341
Betts AK (2009) Land-surface-atmosphere coupling in observations and models. J Adv Model Earth Syst 1:4
Betts AK, Ball JH, Beljaars ACM, Miller MJ, Viterbo P (1996) The land-surface-atmosphere interaction: a review based on observational and global modeling perspectives. J Geophys Res 101:7209–7225
Bhumralkar CM (1975) Numerical experiments on the computation of ground surface temperature in an atmospheric circulation model. J Appl Meteorol 14:1246–1258
Blackadar AK (1976) Modeling the nocturnal boundary layer. In: Proceedings of the third symposium on atmospheric turbulence, diffusion and air quality, American Meteorological Society, pp 46–49
Cai J, Liu Y, Lei T, Pereira LS (2007) Estimating reference evapotranspiration with the FAO Penman-Monteith equation using daily weather forecast messages. Agric For Meteorol 145:22–35
Cai J, Liu Y, Xu D, Paredes P, Pereira L (2009) Simulation of the soil water balance of wheat using daily weather forecast messages to estimate the reference evapotranspiration. Hydrol Earth Syst Sci 13:1045–1059
Colette A, Vautard R, Vrac M (2012) Regional climate downscaling with prior statistical correction of the global climate forcing. Geophys Res Lett 39:L13707
de Rooy WC, Kok K (2004) A combined physical-statistical approach for the downscaling of model wind speed. Weather Forecast 19:485–495
Deardorff JW (1978) Efficient prediction of ground surface temperature and moisture with inclusion of a layer of vegetation. J Geophys Res 83:1889–1903
Gustafson WI Jr, Leung LR (2007) Regional downscaling for air quality assessment. A reasonable proposition? Bull Am Meteorol Soc 88:1215–1227
Hidalgo HG, Dettinger MD, Cayan DR (2008) Downscaling with constructed analogues: daily precipitation and temperature fields over the United States. Report no. CEC-500-2007-123, California Energy Commission, Sacramento, CA
Huang H-Y, Capps SB, Huang S-C, Hall A (2015) Downscaling near-surface wind over complex terrain using a physically-based statistical modeling approach. Clim Dyn 44(1–2):529-542
Ishak AM, Bray M, Remesan R, Han D (2010) Estimating reference evapotranspiration using numerical weather modelling. Hydrol Process 24:3490–3509
Kisi O (2007) Evapotranspiration modeling from climatic data using a neural computing technique. Hydrol Process 21:1925–1934
Kisi O (2009) Daily pan evaporation modelling using multi-layer perceptrons and radial basis neural networks. Hydrol Process 23:213–223
Kumar M, Bandyopadhyay A, Rahguwanshi NS, Singh R (2008) Comparative study of conventional and artificial neural networkbased ETo estimation models. Irrig Sci 26(6):531–545
Kumar M, Raghuwanshi NS, Singh R (2011) Artificial neural networks approach in evapotranspiration modeling: a review. Irrig Sci 29:11–25
Lebassi-Habtezion B, González J, Bornstein R (2011) Modeled large-scale warming impacts on summer California coastal-cooling trends. J Geophys Res 116:D20114
Lo JC-F, Yang Z-L, Pielke RA Sr (2008) Assessment of three dynamical climate downscaling methods using the Weather Research and Forecasting (WRF) model. J Geophys Res 113:D09112
Maurer E, Hidalgo H (2008) Utility of daily vs. monthly largescale climate data: an intercomparison of two statistical downscaling methods. Hydrol Earth Syst Sci 12:551–563
McNaughton KG, Jarvis PG (1984) Using the Penman–Monteith equation predictively. Agric Water Manag 8:246–263
Mesinger F, DiMego G, Kalnay E, Mitchell K, Shafran PC, Ebisuzaki W, Jović D, Woollen J, Rogers E, Berbery EH, Ek MB, Fan Y, Grumbine R, Higgins W, Li H, Lin Y, Manikin G, Parrish D, Shi W (2006) North American regional reanalysis. Bull Am Meteorol Soc 87:343–360
Monin AS, Obukhov AM (1954) Basic laws of turbulent mixing in the ground layer of the atmosphere. Tr Geofiz Inst Akad Nauk SSSR 24:163–187
Noilhan J, Planton S (1989) A simple parameterization of land surface processes for meteorological models. Mon Weather Rev 117:536–549
Plummer DA et al (2006) Climate and climate change over North America as simulated by the Canadian RCM. J Clim 19:3112–3132
Silva D, Meza FJ, Varas E (2010) Estimating reference evapotranspiration (ET0) using numerical weather forecast data in central Chile. J Hydrol 382:64–71
Skamarock WC, Klemp JB, Dudhia J, Gill DO, Barker DM, Duda M, Huang X-Y, Wang W, Power JG (2008) A description of the advanced research WRF version 3. NCAR technical note, NCAR/Tech Notes-475 + STR
Vrac M, Stein ML, Hayhoe K, Liang X-Z (2007) A general method for validating statistical downscaling methods under future climate change. Geophys Res Lett 34:L18701
Wilby RL, Wigley TML (1997) Downscaling general circulation model output: a review of methods and limitations. Prog Phys Geogr 21:530–548
Wilson KB et al (2002) Energy partitioning between latent and sensible heat flux during the warm season at FLUXNET sites. Water Resour Res 38:1294
Wood AW, Leung LR, Sridhar V, Lettenmaier DP (2004) Hydrologic implications of dynamical and statistical approaches to downscaling climate model outputs. Clim Change 62:189–216
Yoon J-H, Ruby Leung L, Correia J Jr (2012) Comparison of dynamically and statistically downscaled seasonal climate forecasts for the cold season over the United States. J Geophys Res 117:D21109
Acknowledgments
This work was supported by the California Energy Commission and the California Institute of Energy and the Environment under agreement #500-11-033. Additional funding was provided by the National Science Foundation Grant EF-1065863, as well as the City of Los Angeles and the U.S. Department of Energy as part of the American Recovery and Reinvestment Act of 2009. The authors would also like to thank the reviewers for their valuable comments.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Huang, HY., Hall, A. A physically-based hybrid framework to estimate daily-mean surface fluxes over complex terrain. Clim Dyn 46, 3883–3897 (2016). https://doi.org/10.1007/s00382-015-2810-z
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-015-2810-z