Results 1 to 10 of about 16,481 (158)

Validation of ERA-Interim Precipitation Estimates over the Baltic Sea [PDF]

open access: yesAtmosphere, 2016
European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-Interim reanalysis total precipitation estimates are validated against ten years of in situ precipitation measurements onboard of ships over the Baltic Sea.
Karl Bumke
doaj   +4 more sources

Blocking representation in the ERA-Interim driven EURO-CORDEX RCMs. [PDF]

open access: yesClim Dyn, 2019
While Regional Climate Models (RCMs) have been shown to yield improved simulations compared to General Circulation Model (GCM), their representation of large-scale phenomena like atmospheric blocking has been hardly addressed. Here, we evaluate the ability of RCMs to simulate blocking situations present in their reanalysis driving data and analyse the ...
Jury MW   +3 more
europepmc   +6 more sources

ERA-Interim/Land: a global land surface reanalysis data set [PDF]

open access: yesHydrology and Earth System Sciences, 2015
ERA-Interim/Land is a global land surface reanalysis data set covering the period 1979–2010. It describes the evolution of soil moisture, soil temperature and snowpack.
G. Balsamo   +12 more
doaj   +8 more sources

An assessment of tropopause characteristics of the ERA5 and ERA-Interim meteorological reanalyses [PDF]

open access: yesAtmospheric Chemistry and Physics, 2022
The tropopause layer plays a key role in manifold processes in atmospheric chemistry and physics. Here we compare the representation and characteristics of the lapse rate tropopause according to the definition of the World Meteorological Organization ...
L. Hoffmann   +3 more
doaj   +6 more sources

The ERA‐Interim reanalysis: configuration and performance of the data assimilation system [PDF]

open access: yesQuarterly Journal of the Royal Meteorological Society, 2011
Abstract ERA‐Interim is the latest global atmospheric reanalysis produced by the European Centre for Medium‐Range Weather Forecasts (ECMWF). The ERA‐Interim project was conducted in part to prepare for a new atmospheric reanalysis to replace ERA‐40, which will extend back to the early part of the twentieth century.
Frédéric Vitart   +2 more
exaly   +2 more sources

Elevation correction of ERA-Interim temperature data in complex terrain [PDF]

open access: yesHydrology and Earth System Sciences, 2012
Air temperature controls a large variety of environmental processes, and is an essential input parameter for land surface models, for example in hydrology, ecology and climatology.
L. Gao, M. Bernhardt, K. Schulz
doaj   +5 more sources

Real‐time correction of ERA‐Interim monthly rainfall [PDF]

open access: yesGeophysical Research Letters, 2013
Gridded precipitation from reanalysis can be a valid proxy for observations in many regions where local measurements are not available. Despite the continuous improvements in assimilation systems and the growing availability of in situ and remote observations, model errors can nevertheless still affect reanalysis quality.
Francesca Di Giuseppe   +2 more
exaly   +2 more sources

Using ERA-INTERIM for regional crop yield forecasting in Europe [PDF]

open access: yesClimate Research, 2010
Agrometeorological systems for regional crop yield forecasting have traditionally relied on weather data derived from weather stations for crop simulation and yield prediction. In recent years, numerical weather prediction (NWP) models have become an interesting source of weather data with the potential to replace observed weather data.
Allard De Wit, Iwan Supit, B Baruth
exaly   +2 more sources

Verification of the new ECMWF ERA-Interim reanalysis over France [PDF]

open access: yesHydrology and Earth System Sciences, 2011
An evaluation of the global ECMWF atmospheric reanalysis ERA-Interim (with a 0.5° grid) is performed over France, based on the high resolution (8 km) SAFRAN atmospheric reanalysis.
C. Szczypta   +7 more
doaj   +1 more source

Evaluation of ERA5 reanalysis atmospheric water vapor variation in Algeria

open access: yesGeodetski Vestnik, 2022
In climate change context, the precipitable water vapour (PW) is key parameter of atmospheric process and dynamics and its variation is very high in space and time. It's accuracy is paramount for any geodetic or climatic study. The main objective of this
Houaria Namaoui
doaj   +1 more source

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