Articles | Volume 10, issue 1
https://doi.org/10.5194/gmd-10-57-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-10-57-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Methods for assessment of models
| 
05 Jan 2017
Methods for assessment of models |
| 05 Jan 2017
ASoP (v1.0): a set of methods for analyzing scales of precipitation in general circulation models
Nicholas P. Klingaman
CORRESPONDING AUTHOR
National Centre for Atmospheric Science–Climate and Department of Meteorology, University of Reading, Earley Gate, P.O. Box 243, Reading, Berkshire RG6 6BB, UK
Gill M. Martin
Met Office, Exeter, UK
Aurel Moise
Bureau of Meteorology, Melbourne, Australia
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- Evaluation of the Tail of the Probability Distribution of Daily and Subdaily Precipitation in CMIP6 Models J. Norris et al. 10.1175/JCLI-D-20-0182.1
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- A Pan-African Convection-Permitting Regional Climate Simulation with the Met Office Unified Model: CP4-Africa R. Stratton et al. 10.1175/JCLI-D-17-0503.1
- Relationships between subseasonal‐to‐seasonal predictability and spatial scales in tropical rainfall V. Moron & A. Robertson 10.1002/joc.7143
- Intraseasonal summer rainfall variability over China in the MetUM GA6 and GC2 configurations C. Stephan et al. 10.5194/gmd-11-3215-2018
- The importance of horizontal model resolution on simulated precipitation in Europe – from global to regional models G. Strandberg & P. Lind 10.5194/wcd-2-181-2021
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- Role of convection–circulation coupling in the propagation mechanism of the Madden–Julian Oscillation over the Maritime Continent in a climate model Y. Wang et al. 10.1007/s00382-021-06013-2
- Climate Models Permit Convection at Much Coarser Resolutions Than Previously Considered J. Vergara-Temprado et al. 10.1175/JCLI-D-19-0286.1
- Physical processes driving intensification of future precipitation in the mid- to high latitudes B. Poujol et al. 10.1088/1748-9326/abdd5b
- Larger Future Intensification of Rainfall in the West African Sahel in a Convection‐Permitting Model S. Berthou et al. 10.1029/2019GL083544
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- Evaluation of Asian summer precipitation in different configurations of a high-resolution general circulation model in a range of decision-relevant spatial scales M. Muetzelfeldt et al. 10.5194/hess-25-6381-2021
- Evaluation of climate simulations produced with the Brazilian global atmospheric model version 1.2 C. Coelho et al. 10.1007/s00382-020-05508-8
- Contrasting contributions of surface hydrological pathways in convection permitting and parameterised climate simulations over Africa and their feedbacks on the atmosphere S. Folwell et al. 10.1007/s00382-022-06144-0
- UKESM1: Description and Evaluation of the U.K. Earth System Model A. Sellar et al. 10.1029/2019MS001739
- Connecting spatial and temporal scales of tropical precipitation in observations and the MetUM-GA6 G. Martin et al. 10.5194/gmd-10-105-2017
- A perspective for advancing climate prediction services in Brazil C. Coelho et al. 10.1002/cli2.29
- Subhourly rainfall in a convection-permitting model E. Meredith et al. 10.1088/1748-9326/ab6787
- Assessing Two Approaches for Enhancing the Range of Simulated Scales in the E3SMv1 and the Impact on the Character of Hourly US Precipitation G. Kooperman et al. 10.1029/2021GL096717
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Latest update: 02 Nov 2024
Short summary
Weather and climate models show large errors in the frequency, intensity and persistence of daily rainfall, particularly in the tropics. We introduce a set of diagnostics to reveal the spatial and temporal scales of precipitation in models and compare them to satellite observations to inform development efforts. Although models show similar errors in 3 h precipitation, at the time step and gridpoint level some produce coherent precipitation and others exhibit worrying quasi-random behavior.
Weather and climate models show large errors in the frequency, intensity and persistence of...
