Cited by 1,183Climate variability and modelsMeteorological Phenomena and SimulationsAtmospheric aerosols and clouds

Sensitivity of Simulated Climate to Horizontal and Vertical Resolution in the ECHAM5 Atmosphere Model

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Roeckner, E., Brokopf, R., Esch, M., Giorgetta, M., Hagemann, S., Kornblueh, L., Manzini, E., Schlese, U. +1 more·2006·Journal of Climate

Abstract

The most recent version of the Max Planck Institute for Meteorology atmospheric general circulation model, ECHAM5, is used to study the impact of changes in horizontal and vertical resolution on seasonal mean climate. In a series of Atmospheric Model Intercomparison Project (AMIP)-style experiments with resolutions ranging between T21L19 and T159L31, the systematic errors and convergence properties are assessed for two vertical resolutions. At low vertical resolution (L19) there is no evidence for convergence to a more realistic climate state for horizontal resolutions higher than T42. At higher vertical resolution (L31), on the other hand, the root-mean-square errors decrease monotonically with increasing horizontal resolution. Furthermore, except for T42, the L31 versions are superior to their L19 counterparts, and the improvements become more evident at increasingly higher horizontal resolutions. This applies, in particular, to the zonal mean climate state and to the stationary wave patterns in boreal winter. As in previous studies, increasing horizontal resolution leads to a warming of the troposphere, most prominently at midlatitudes, and to a poleward shift and intensification of the midlatitude westerlies. Increasing the vertical resolution has the opposite effect, almost independent of horizontal resolution. Whereas the atmosphere is colder at low and middle latitudes, it is warmer at high latitudes and close to the surface. In addition, increased vertical resolution results in a pronounced warming in the polar upper troposphere and lower stratosphere, where the cold bias is reduced by up to 50% compared to L19 simulations. Consistent with these temperature changes is a decrease and equatorward shift of the midlatitude westerlies. The substantial benefits in refining both horizontal and vertical resolution give some support to scaling arguments deduced from quasigeostrophic theory implying that horizontal and vertical resolution ought to be chosen consistently.

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  1. [9]9. Gibson, J. K., P. Kallberg, S. Uppala, A. Hernandez, A. Nomura, and E. Serrano, 1997: ERA description. ECMWF Reanalysis Project Report Series, Vol. 1, European Centre for Medium- Range Weather Forecasts, Reading, United Kingdom, 72 pp.

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Authors
Roeckner, E., Brokopf, R., Esch, M., Giorgetta, M., Hagemann, S., Kornblueh, L., Manzini, E., Schlese, U., & Schulzweida, U.
Affiliations
Max Planck Society (DE)
Venue
Journal of Climate
Published
2006-08-15
Volume
19
Issue
16
Pages
3771-3791
ISSN
  • 0894-8755 (ISSN-L)
  • 1520-0442
OpenAlex
W2042290651
Cited by
1,183
References
26
Citations by year
2026: 17 · 2025: 30 · 2024: 67 · 2023: 77 · 2022: 72 · 2021: 88 · 2020: 52 · 2019: 39 · 2018: 49 · 2017: 51 · 2016: 69 · 2015: 71 · 2014: 84 · 2013: 83 · 2012: 86
FWCI
35.13
Type
journal article
Language
en
Open access
Locations
  • Journal of Climate (publishedVersion)
  • Max Planck Institute for Plasma Physics (submittedVersion)
  • Max Planck Digital Library (submittedVersion, other-oa)
  • MPG.PuRe (Max Planck Society) (submittedVersion, other-oa)
Funders
Deutsches Klimarechenzentrum
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
  • Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
Keywords
ECHAM5, horizontal resolution, vertical resolution, resolution sensitivity, standing waves, mid-latitude westerlies, tropospheric warming, atmospheric general circulation model

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