Articles | Volume 17, issue 9
https://doi.org/10.5194/gmd-17-3815-2024
https://doi.org/10.5194/gmd-17-3815-2024
Model evaluation paper
 | 
14 May 2024
Model evaluation paper |  | 14 May 2024

Evaluation of multi-season convection-permitting atmosphere – mixed-layer ocean simulations of the Maritime Continent

Emma Howard, Steven Woolnough, Nicholas Klingaman, Daniel Shipley, Claudio Sanchez, Simon C. Peatman, Cathryn E. Birch, and Adrian J. Matthews

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Cited articles

Argueso, D., Romero, R., and Homar, V.: Precipitation Features of the Maritime Continent in Parameterized and Explicit Convection Models, J. Climate, 33, 2449–2466, https://doi.org/10.1175/JCLI-D-19-0416.1, 2020. a
Azaneu, M., Matthews, A., Lee, G., and Heywood, K.: Seaglider data from the Indian Ocean as a part of the Equatorial Line Observations (ELO), January–April 2019, Published Data Library (PDL), https://doi.org/10.5285/efcc09dc-ed05-775c-e053-6c86abc0bb49, 2022. a
Baranowski, D. B., Waliser, D. E., Jiang, X., Ridout, J. A., and Flatau, M. K.: Contemporary GCM Fidelity in Representing the Diurnal Cycle of Precipitation Over the Maritime Continent, J. Geophys. Res.-Atmos., 124, 747–769, https://doi.org/10.1029/2018JD029474, 2019. a
Beck, H. E., Wood, E. F., Pan, M., Fisher, C. K., Miralles, D. G., van Dijk, A. I. J. M., McVicar, T. R., and Adler, R. F.: MSWEP V2 Global 3-Hourly 0.1° Precipitation: Methodology and Quantitative Assessment, B. Am. Meteorol. Soc., 100, 473–500, https://doi.org/10.1175/BAMS-D-17-0138.1, 2019. a
Best, M. J., Pryor, M., Clark, D. B., Rooney, G. G., Essery, R. L. H., Ménard, C. B., Edwards, J. M., Hendry, M. A., Porson, A., Gedney, N., Mercado, L. M., Sitch, S., Blyth, E., Boucher, O., Cox, P. M., Grimmond, C. S. B., and Harding, R. J.: The Joint UK Land Environment Simulator (JULES), model description – Part 1: Energy and water fluxes, Geosci. Model Dev., 4, 677–699, https://doi.org/10.5194/gmd-4-677-2011, 2011. a, b, c
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This paper describes a coupled atmosphere–mixed-layer ocean simulation setup that will be used to study weather processes in Southeast Asia. The set-up has been used to compare high-resolution simulations, which are able to partially resolve storms, to coarser simulations, which cannot. We compare the model performance at representing variability of rainfall and sea surface temperatures across length scales between the coarse and fine models.