{"refrec":{"BRefID":209485,"RR":"<b>McGillicuddy Jr., D.J.</b> (2011). Eddies masquerade as planetary waves. <i>Science (Wash.) 334(6054)</i>: 318-319. <a href=\"https://dx.doi.org/10.1126/science.1208892\" target=\"_blank\">https://dx.doi.org/10.1126/science.1208892</a>","BEntID":201467,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 334(6054)</i>: 318-319. <a href=\"https://dx.doi.org/10.1126/science.1208892\" target=\"_blank\">https://dx.doi.org/10.1126/science.1208892</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"McGillicuddy Jr., D.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"McGillicuddy Jr., D.J.","Englishabstract":"The advent of satellite-based remote sensing of ocean color in the late 1970s (1) provided the first largescale views of chlorophyll distributions in the upper ocean. These distributions are a proxy for the biomass of phytoplankton, which drive oceanic productivity. More recently, ocean color measurements have been combined with satellite data on sea-surface height (SSH) and other physical properties of the ocean to elucidate the processes that regulate primary production in the sea. On page 328 of this issue, Chelton et al. 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