Atmospheric conservation properties in ERA‐Interim
By P. Berrisford, P. Kållberg, S. Kobayashi, Dick Dee, S. Uppala, A. Simmons, Paul Poli, H. Sato. 2011
368 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a58cba865a2179e96c71ca81f57b4c9720d8e10b
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Alan J. Geer
- L. Haimberger
- Dick Dee
- Ricardo Todling
- Richard G. Forbes
- P. Konopka
- S. B. Healy
- Paul Poli
In Global and Planetary Change
- Alan J. Geer
- L. Haimberger
- Dick Dee
- Ricardo Todling
- Richard G. Forbes
- P. Konopka
- S. B. Healy
- Paul Poli
Citations in the corpus
- The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2). (2017, background): “At the same time, Berrisford et al. (2011) argue that, while the observing system may not provide the data to determine exactly the total mass of the atmosphere, the degree to which dry mass is preserved in a reanalysis provides a useful diagnostic of reanalysis quality.”
- From ERA-Interim to ERA5: considerable impact of ECMWF's next-generation reanalysis on Lagrangian transport simulations (2018, result): “Global atmospheric budgets of mass, moisture, energy, and angular momentum were studied in detail by Berrisford et al. (2011), and significant improvements were reported compared with the earlier ERA-40 reanalysis (Uppala et al., 2005).”
- The ERA5 global reanalysis (2020, background): “Berrisford et al. (2011) examined the global atmospheric budgets from ERA-Interim and made comparisons with ERA-40.”
- The global energy balance from a surface perspective (2013, background): “The value of 397 Wm is also close to the upward thermal flux calculated in the ERA40 and ERA Interim (at 398 Wm) (Berrisford et al. 2011), and matches the fluxes determined in the National Center for Environmental Prediction (NRA) and the Japanese (JRA) reanalyses (Trenberth et al.”
- ERA‐20CM: a twentieth‐century atmospheric model ensemble (2015, background): “The effect is small, and is estimated to increase mass by a few tenths of a percent per year (Berrisford et al., 2011b).”