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When the prevailing geostrophic flow is parallel to the heterogeneity, large secondary spanwise circulations emerge within the flow that affect surface fluxes of momentum, heat, and mass. By means of wind-tunnel measurements, the influence of spanwis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e22302d087e28ceccbfef4f97864a10f
https://doi.org/10.5194/egusphere-egu22-7936
https://doi.org/10.5194/egusphere-egu22-7936
