{"refrec":{"BRefID":367805,"RR":"(2023). Bubble bursts increase melt rates of tidewater glaciers. <i>Nature Geoscience 16(10)</i>: 835-836. <a href=\"https://dx.doi.org/10.1038/s41561-023-01271-7\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-023-01271-7</a>","BEntID":365530,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 16(10)</i>: 835-836. <a href=\"https://dx.doi.org/10.1038/s41561-023-01271-7\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-023-01271-7</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":null,"OrigTitleTranslFlag":0,"Authorstringtrunc":null,"Englishabstract":"Glacier ice contains high-pressure air bubbles, which burst into seawater as ice melts at tidewater glacier termini. Laboratory measurements found that these bubbles double the rate of ice melt. Theoretically, this effect could be even larger in a real glacier. 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