Daily gridded datasets of snow depth and snow water equivalent for the Iberian Peninsula from 1980 to 2014
Identificadores
URI: https://hdl.handle.net/10481/88378Metadatos
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Alonso-González, Esteban; López-Moreno, J.I.; Gascoin, Simón; García Valdecasas Ojeda, Matilde María del Valle; Sanmiguel-Vallelado, Alba; Navarro-Serrano, Francisco; Revuelto, Jesús; Ceballos, Antonio; Esteban Parra, María Jesús; Essery, RichardEditorial
Copernicus
Date
2018Referencia bibliográfica
Alonso-González, E., López-Moreno, J. I., Gascoin, S., García-Valdecasas Ojeda, M., Sanmiguel-Vallelado, A., Navarro-Serrano, F., Revuelto, J., Ceballos, A., Esteban-Parra, M. J., and Essery, R.: Daily gridded datasets of snow depth and snow water equivalent for the Iberian Peninsula from 1980 to 2014, Earth Syst. Sci. Data, 10, 303–315, https://doi.org/10.5194/essd-10-303-2018, 2018.
Patrocinador
Esteban Alonso-González is supported by the Spanish Ministry of Economy and Competitiveness (BES- 2015-071466). This study was funded by the Spanish Ministry of Economy and Competitiveness projects CGL2014-52599-P 10 (Estudio del manto de nieve en la montaña española y su respuesta a la variabilidad y cambio climatico) and CGL2017- 82216-R (HIDROIBERNIEVE) and (with additional support from the European Community funds, FEDER) CGL2013-48539-R (Impactos del cambio climático en los recursos hídricos de la cuenca del Duero a alta resolución). Also, the Regional Government of Andalusia has funded this research with the project P11-RNM-7941 (Impactos del Cambio Climático en la cuenca del Guadalquivir, LICUA).Résumé
We present snow observations and a validated daily gridded snowpack dataset that was simulated
from downscaled reanalysis of data for the Iberian Peninsula. The Iberian Peninsula has long-lasting seasonal
snowpacks in its different mountain ranges, and winter snowfall occurs in most of its area. However, there are
only limited direct observations of snow depth (SD) and snow water equivalent (SWE), making it difficult to analyze
snow dynamics and the spatiotemporal patterns of snowfall. We used meteorological data from downscaled
reanalyses as input of a physically based snow energy balance model to simulate SWE and SD over the Iberian
Peninsula from 1980 to 2014. More specifically, the ERA-Interim reanalysis was downscaled to 10 km 10 km
resolution using the Weather Research and Forecasting (WRF) model. The WRF outputs were used directly, or
as input to other submodels, to obtain data needed to drive the Factorial Snow Model (FSM). We used lapse
rate coefficients and hygrobarometric adjustments to simulate snow series at 100m elevations bands for each
10 km 10 km grid cell in the Iberian Peninsula. The snow series were validated using data from MODIS satellite
sensor and ground observations. The overall simulated snow series accurately reproduced the interannual
variability of snowpack and the spatial variability of snow accumulation and melting, even in very complex topographic
terrains. Thus, the presented dataset may be useful for many applications, including land management,
hydrometeorological studies, phenology of flora and fauna, winter tourism, and risk management. The data presented
here are freely available for download from Zenodo (https://doi.org/10.5281/zenodo.854618). This paper
fully describes the work flow, data validation, uncertainty assessment, and possible applications and limitations
of the database.