{"refrec":{"BRefID":119732,"RR":"<b>Hamilton, K.; Ohfuchi, W. (Ed.)</b> (2008). High resolution numerical modelling of the atmosphere and ocean. Springer: New York. ISBN 978-0-387-36671-5. xiv, 293 pp. <a href=\"https://dx.doi.org/10.1007/978-0-387-49791-4\" target=\"_blank\">https://dx.doi.org/10.1007/978-0-387-49791-4</a>","BEntID":113958,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Springer: New York. ISBN 978-0-387-36671-5. xiv, 293 pp. <a href=\"https://dx.doi.org/10.1007/978-0-387-49791-4\" target=\"_blank\">https://dx.doi.org/10.1007/978-0-387-49791-4</a>","DocTypID":5,"DocType":"Book/Monograph","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Hamilton, K.; Ohfuchi, W. (Ed.)","OrigTitleTranslFlag":0,"Authorstringtrunc":"Hamilton, K.; Ohfuchi, W. (Ed.)","Englishabstract":"All numerical simulations of atmospheric and oceanic phenomena are limited by the finite spatial resolution, generally requiring a parameterization of effects of motions on unresolved scales on those explicitly resolved. A goal of numerical modelers has been to resolve as many scales of the actual circulation as practically possible. With the recent advent of a new generation of high-performance computing systems such as the Earth Simulator, some notable thresholds in terms of model resolution have been approached or, in some cases, surpassed. For example, recently the first long integrations with genuinely eddy-permitting global ocean models have been reported. In atmospheric studies, decadal integrations with global models with effective horizontal resolution of about 20 km have now become possible, and shorter integrations of global models that explicitly resolve scales approaching those of individual convective elements have now been reported. 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