{"refrec":{"BRefID":352968,"RR":"<b>Van Liefferinge, B.; Taylor, D.; Tsutaki, S.; Fujita, S.; Gogineni, P.; Kawamura, K.; Matsuoka, K.; Moholdt, G.; Oyabu, I.; Abe-Ouchi, A.; Awasthi, A.; Buizert, C.; Gallet, J.-C.; Isaksson, E.; Motoyama, H.; Nakazawa, F.; Ohno, H.; O'Neill, C.; Pattyn, F.; Sugiura, K.</b> (2021). Surface mass balance controlled by local surface slope in inland Antarctica: implications for ice-sheet mass balance and oldest ice delineation in Dome Fuji. <i>Geophys. Res. Lett. 48(24)</i>: e2021GL094966. <a href=\"https://dx.doi.org/10.1029/2021GL094966\" target=\"_blank\">https://dx.doi.org/10.1029/2021GL094966</a>","BEntID":350677,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 48(24)</i>: e2021GL094966. <a href=\"https://dx.doi.org/10.1029/2021GL094966\" target=\"_blank\">https://dx.doi.org/10.1029/2021GL094966</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van Liefferinge, B.; Taylor, D.; Tsutaki, S.; Fujita, S.; Gogineni, P.; Kawamura, K.; Matsuoka, K.; Moholdt, G.; Oyabu, I.; Abe-Ouchi, A.; Awasthi, A.; Buizert, C.; Gallet, J.-C.; Isaksson, E.; Motoyama, H.; Nakazawa, F.; Ohno, H.; O'Neill, C.; Pattyn, F.; Sugiura, K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van Liefferinge, B. <i>et al.</i>","Englishabstract":"The limited number of surface mass balance (SMB) observations in the Antarctic inland hampers estimates of ice-sheet contribution to global sea level and locations with million-year-old ice. We present finely resolved SMB over the past three centuries in a low-accumulation region with significant depth hoar formation on Dome Fuji derived from ∼1,100&nbsp;km of microwave radar stratigraphy dated with a firn core. The regional-mean SMB over the past 264&nbsp;years is estimated to ∼22.5&nbsp;±&nbsp;3.3&nbsp;kg&nbsp;m<sup>−2</sup>&nbsp;a<sup>−1</sup>, but with large local variability of up to 30%. We found that local SMB is negatively correlated with surface slope at scales of a few hundred meters, resulting in anomalous zones of low SMB which represent as much as 8–10% of the total SMB on the inland plateau if the SMB-slope relationship is more widely valid. 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