2026-04-06T06:25:05Z http://dmoai.cloud.dkrz.de/oai/provider

oai:wdcc.dkrz.de:iso_3583467 2026-04-05T23:08:04Z iso-wdcc-doi

wdc-climate.de:3583467 eng; USA collection WaVaCurIP Jon Sáenz Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus pointOfContact Jon Sáenz Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus pointOfContact 2017-12-11T16:14:14 ISO 19115 ISO 19115-2:2009 Water vapour balance over the Iberian Peninsula 2018-03-13 publication 1 WaVaCurIP doi:10.1594/WDCC/WaVaCurIP Gabriel Ibarra-Berastegi Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: gabriel.ibarra@ehu.eus principalInvestigator Javier Díaz de Argandoña Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: javier.argandona@ehu.eus principalInvestigator Jon Sáenz Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: jon.saenz@ehu.eus principalInvestigator Santos José González-Rojí Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: santosjose.gonzalez@ehu.eus principalInvestigator Santos José González-Rojí Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: santosjose.gonzalez@ehu.eus author Jon Sáenz Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: jon.saenz@ehu.eus author Gabriel Ibarra-Berastegi Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: gabriel.ibarra@ehu.eus author Javier Díaz de Argandoña Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus Email: javier.argandona@ehu.eus author WDC Climate at DKRZ publisher These data are made available as part of paper: S. J. Gonzalez-Roji, J. Saenz, G. Ibarra-Berastegi, J. Diaz de Argandona (2018) Moisture balance over the Iberian Peninsula according to a regional climate model, Journal of Geophysical Research 123(2):708-729. The dataset holds selected postprocessed files that allow to reproduce all the results in the paper. An analysis of the atmospheric branch of the hydrological cycle by means of a 15 km resolution numerical integration performed using Weather Research and Forecasting (WRF) nested in ERA Interim is presented. Two WRF experiments covering the period 2010–2014 were prepared. The first one (N) was configured as in standard numerical downscaling experiments. The second one (D), with the same parameterizations, included a step of 3DVAR data assimilation every 6 h. Experiment D: -windowed-D-AI: Analysis increments (T2, Q2), 2010-2014 for the D experiment -windowed-wavacurip4paper-D: Netcdf files corresponding to experiment D (using 3DVAR assimilation) and years 2010-2014 holding 3-hourly outputs from the run after selecting the window covering the Iberian Peninsula. Experiment N: -windowed-wavacurip4paper-N: Netcdf files corresponding to experiment N (no data assimilation) and years 2010-2014 holding 3-hourly outputs from the run after selecting the window covering the Iberian Peninsula Jon Sáenz Universidad del País Vasco/Euskal Herriko Unibertsitatea http://www.ehu.eus pointOfContact NetCDF Precipitation WRF WRFDA evaporation hydrological cycle model evaluation regional climate simulation water cycle parameters CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA -16.4149 8.8384 33.1774 48.9286 gregorian 2010-01-01 2014-12-31 precipitation_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 surface_specific_humidity The surface called "surface" means the lower boundary of the atmosphere. "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air. [CF-Standard Name]; unit: 1 water_evaporation_flux_from_soil Water means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called sublimation.) In accordance with common usage in geophysical disciplines, flux implies per unit area, called flux density in physics. [CF-Standard Name]; unit: kg m-2 s-1 Complete list of variables: see variable-info.pdf not filled; unit: not filled time time [CF-Standard Name]; unit: h Complete list of variables: see variable-info.pdf not filled; unit: not filled height_above_mean_sea_level "Height_above_X" means the vertical distance above the named surface X. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: m eastward_atmosphere_water_vapor_transport_across_unit_distance "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Transport across_unit_distance means expressed per unit distance normal to the direction of transport. [CF-Standard Name]; unit: kg m-2 s-1 northward_atmosphere_water_vapor_transport_across_unit_distance "Northward" indicates a vector component which is positive when directed northward (negative southward). Transport across_unit_distance means expressed per unit distance normal to the direction of transport. [CF-Standard Name]; unit: kg m-2 s-1 atmosphere_mass_content_of_cloud_condensed_water alias: atmosphere_cloud_condensed_water_content "condensed_water" means liquid and ice. "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. [CF-Standard Name]; unit: kg m-2 land_binary_mask X_binary_mask has 1 where condition X is met, 0 elsewhere. 1 = land, 0 = sea. [CF-Standard Name]; unit: 1=land, 0=sea atmosphere_mass_content_of_water "Content" indicates a quantity per unit area. The "atmosphere content" of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. "Water" means water in all phases. [CF-Standard Name]; unit: kg m-2 latitude latitude [CF-Standard Name]; unit: not filled longitude longitude [CF-Standard Name]; unit: not filled longitude longitude [CF-Standard Name]; unit: degrees east latitude latitude [CF-Standard Name]; unit: degrees north air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K NetCDF 11700 https://www.wdc-climate.de/ui/entry?acronym=WaVaCurIP information collection n/a None