339 citations as recorded by crossref.

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25. Estimation of the Heat and Water Budgets of the Persian (Arabian) Gulf Using a Regional Climate Model*,+ P. Xue & E. Eltahir https://doi.org/10.1175/JCLI-D-14-00189.1
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55. Implementation of a multi-layer snow scheme in the GloSea6 seasonal forecast system: impacts on land–atmosphere interactions and climatological biases E. Seo et al. https://doi.org/10.5194/gmd-19-1261-2026
56. Efficient ensemble data assimilation for coupled models with the Parallel Data Assimilation Framework: example of AWI-CM (AWI-CM-PDAF 1.0) L. Nerger et al. https://doi.org/10.5194/gmd-13-4305-2020
57. Assessment of CNRM coupled ocean-atmosphere model sensitivity to the representation of aerosols L. Watson et al. https://doi.org/10.1007/s00382-017-4054-6
58. Sea-state contributions to sea-level variability in the European Seas A. Bonaduce et al. https://doi.org/10.1007/s10236-020-01404-1
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64. Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection N. Yeung et al. https://doi.org/10.1038/s43247-024-01383-x
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67. Evaluation of multi-season convection-permitting atmosphere – mixed-layer ocean simulations of the Maritime Continent E. Howard et al. https://doi.org/10.5194/gmd-17-3815-2024
68. Assessing the Future ODYSEA Satellite Mission for the Estimation of Ocean Surface Currents, Wind Stress, Energy Fluxes, and the Mechanical Coupling Between the Ocean and the Atmosphere M. Larrañaga et al. https://doi.org/10.3390/rs17020302
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73. The inter-annual variations of the significant wave height in the Western North Pacific and South China Sea region S. Li et al. https://doi.org/10.1007/s00382-021-05636-9
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87. An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea K. Wahle et al. https://doi.org/10.5194/os-13-289-2017
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89. The effect of seasonally and spatially varying chlorophyll on Bay of Bengal surface ocean properties and the South Asian monsoon J. Giddings et al. https://doi.org/10.5194/wcd-1-635-2020
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