Results 11 to 20 of about 1,717,234 (288)
Elevation correction of ERA-Interim temperature data in complex terrain [PDF]
Hydrology 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
Blocking representation in the ERA-Interim driven EURO-CORDEX RCMs. [PDF]
Clim 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
Atmospheric conservation properties in ERA-Interim
Quarterly Journal of the Royal Meteorological Society, 2011 We study the global atmospheric budgets of mass, moisture, energy and angular momentum in the latest reanalysis from the European Centre for Medium-Range Weather Forecasts (ECMWF), ERA-Interim, for the period 1989–2008 and compare with ERA-40.
Berrisford, Paul +15 more
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Age of stratospheric air in the ERA-Interim [PDF]
Atmospheric Chemistry and Physics, 2012 Abstract. The Brewer-Dobson mean circulation and its variability are investigated in the ERA-Interim over the period 1989-2010 by using an off-line Lagrangian transport model driven by analysed winds and heating rates. At low and mid-latitudes, the mean age of air in the lower stratosphere is in good agreement with ages derived from aircraft, high ...
M. Diallo, B. Legras, A. Chédin
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Characterizing ERA-interim and ERA5 surface wind biases using ASCAT [PDF]
Ocean Science, 2019 Abstract. This paper analyses the differences between ERA-Interim and ERA5 surface winds fields relative to ASCAT ocean vector wind observations, after adjustment for the effects of atmospheric stability and density, using stress equivalent winds (U10S), and air-sea relative motion using ocean current velocities.
M. Belmonte Rivas +2 more
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The stratospheric Brewer–Dobson circulation inferred from age of air in the ERA5 reanalysis [PDF]
Atmospheric Chemistry and Physics, 2021 This paper investigates the global stratospheric Brewer–Dobson circulation (BDC) in the ERA5 meteorological reanalysis from the European Centre for Medium-Range Weather Forecasts (ECMWF).
F. Ploeger +10 more
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Spatio-temporal trends in the hydroclimate of Turkey for the last decades based on two reanalysis datasets [PDF]
Hydrology and Earth System Sciences, 2016 We present a regional assessment of the spatiotemporal trends in several hydro-climate variables from 1979 to 2010 in Turkey, one of the countries of the eastern Mediterranean vulnerable to climate change, using the two reanalysis products of the ECMWF ...
M. Gokmen
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Ice supersaturated regions: properties and validation of ERA-Interim reanalysis with IAGOS in situ water vapour measurements [PDF]
Atmospheric Chemistry and Physics, 2020 Cirrus clouds and their potential formation regions, so-called ice supersaturated regions (ISSRs), with values of relative humidity with respect to ice exceeding 100 %, occur frequently in the tropopause region. It is assumed that ISSRs and cirrus
P. Reutter +5 more
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Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet [PDF]
The Cryosphere, 2020 The ERA5 reanalysis, recently made available by the European Centre for Medium-Range Weather Forecasts (ECMWF), is a new reanalysis product at a high resolution replacing ERA-Interim and is considered to provide the best climate reanalysis over Greenland
A. Delhasse +7 more
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Earth and Space Science, 2020 Tibetan Plateau vortices (TPVs) are important rainfall triggers in southwestern and eastern China after they move off the plateau. Characteristics of the moving‐off TPVs derived from two gridded data sets, the final operational global analysis data from ...
Lun Li, Renhe Zhang, Peili Wu
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