globalchange  > 气候变化事实与影响
DOI: 10.5194/hess-21-2187-2017
Scopus记录号: 2-s2.0-85018658691
论文题名:
Validation of a new SAFRAN-based gridded precipitation product for Spain and comparisons to Spain02 and ERA-Interim
作者: Quintana-Seguí P; , Turco M; , Herrera S; , Miguez-Macho G
刊名: Hydrology and Earth System Sciences
ISSN: 10275606
出版年: 2017
卷: 21, 期:4
起始页码: 2187
结束页码: 2201
语种: 英语
Scopus关键词: Climate models ; Gages ; Quality control ; Rain ; Rain gages ; Surface measurement ; Hydrological modeling ; Interpolation method ; Meteorological analysis ; Meteorological forcing ; Meteorological variables ; Precipitation products ; Regional climate models ; Spatial and temporal heterogeneity ; Precipitation (meteorology) ; climate modeling ; comparative study ; data interpretation ; estimation method ; heterogeneity ; hydrological cycle ; land surface ; model validation ; precipitation (climatology) ; regional climate ; Spain
英文摘要: Offline land surface model (LSM) simulations are useful for studying the continental hydrological cycle. Because of the nonlinearities in the models, the results are very sensitive to the quality of the meteorological forcing; thus, high-quality gridded datasets of screen-level meteorological variables are needed. Precipitation datasets are particularly difficult to produce due to the inherent spatial and temporal heterogeneity of that variable. They do, however, have a large impact on the simulations, and it is thus necessary to carefully evaluate their quality in great detail.

This paper reports the quality of two high-resolution precipitation datasets for Spain at the daily time scale: the new SAFRAN-based dataset and Spain02. SAFRAN is a meteorological analysis system that was designed to force LSMs and has recently been extended to the entirety of Spain for a long period of time (1979/1980–2013/2014). Spain02 is a daily precipitation dataset for Spain and was created mainly to validate regional climate models. In addition, ERA-Interim is included in the comparison to show the differences between local high-resolution and global low-resolution products. The study compares the different precipitation analyses with rain gauge data and assesses their temporal and spatial similarities to the observations.

The validation of SAFRAN with independent data shows that this is a robust product. SAFRAN and Spain02 have very similar scores, although the latter slightly surpasses the former. The scores are robust with altitude and throughout the year, save perhaps in summer when a diminished skill is observed. As expected, SAFRAN and Spain02 perform better than ERA-Interim, which has difficulty capturing the effects of the relief on precipitation due to its low resolution. However, ERA-Interim reproduces spells remarkably well in contrast to the low skill shown by the high-resolution products. The high-resolution gridded products overestimate the number of precipitation days, which is a problem that affects SAFRAN more than Spain02 and is likely caused by the interpolation method. Both SAFRAN and Spain02 underestimate high precipitation events, but SAFRAN does so more than Spain02. The overestimation of low precipitation events and the underestimation of intense episodes will probably have hydrological consequences once the data are used to force a land surface or hydrological model. © Author(s) 2017.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/79191
Appears in Collections:气候变化事实与影响

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作者单位: Observatori de l'Ebre (OE), Universitat Ramon Llull - CSIC, Horta Alta 38, Roquetes, Spain; Department of Applied Physics, University of Barcelona (UB), Av. Diagonal 647, Barcelona, Spain; Meteorology Group, Department of Applied Mathematics and Computer Science, Universidad de Cantabria, Avenida de los Castros s/n, Santander, Spain; Grupo de Física No Lineal, Universidade de Santiago Compostela, Calle Xosé María Suárez, Núñez s/n, Santiago de Compostela, Spain

Recommended Citation:
Quintana-Seguí P,, Turco M,, Herrera S,et al. Validation of a new SAFRAN-based gridded precipitation product for Spain and comparisons to Spain02 and ERA-Interim[J]. Hydrology and Earth System Sciences,2017-01-01,21(4)
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