{"refrec":{"BRefID":195821,"RR":"<b>Trenberth, K.E.</b> (2010). The ocean is warming, isn't it? <i>Nature (Lond.) 465(7296)</i>: 304. <a href=\"https://dx.doi.org/10.1038/465304a\" target=\"_blank\">https://dx.doi.org/10.1038/465304a</a>","BEntID":188288,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":" <i>Nature (Lond.) 465(7296)</i>: 304. <a href=\"https://dx.doi.org/10.1038/465304a\" target=\"_blank\">https://dx.doi.org/10.1038/465304a</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Trenberth, K.E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Trenberth, K.E.","Englishabstract":"The upper ocean acts as a giant heat sink and has absorbed the majority of excess energy generated by anthropogenic greenhouse gasses. This makes ocean heat content, potentially, a key indicator of climate change. But to be useful for evaluating the global energy balance and as a constraint on climate models, the measurement uncertainties of such a key indicator need to be well understood. At present the magnitude of the oceanic heat uptake is highly uncertain, with patterns of inter-annual variability in particular differing among estimates. In a major international collaboration, Lyman et al. compare the available upper-ocean heat content anomaly curves and examine the sources of uncertainly attached to them — including the difficulties in correcting bias in expendable bathythermograph data. 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