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A series of cross-slope transects were occupied in 2013 and 2015\udthat extended eastward from St. Anna Trough to the Lomonosov Ridge.\udHigh-resolution physical and chemical observations collected along these\udtransects revealed fronts in the potential temperature and the stable oxygen\udisotopic ratio (δ18O) that were observed north of Severnaya\udZemlya (SZ). Using linear regressions, we describe mixing regimes on either\udside of the front that characterize a transition from a seasonal halocline to\uda permanent halocline. This transition describes the formation of lower\udhalocline water (LHW) and the cold halocline layer via a mechanism that has\udbeen previously postulated by Rudels et al. (1996). Initial freshening of\udAtlantic Water (AW) by sea-ice meltwater occurs west of SZ, whereas higher\udinfluences of meteoric water and brine result in a transition to a separate\udmixing regime that alters LHW through mixing with overlying waters and shifts\udthe characteristic temperature–salinity bend from higher\ud(34.4  ≤  S  ≤  34.5) toward lower\ud(34.2  ≤  S  ≤  34.3) salinities. These mixing regimes appear to\udhave been robust since at least 2000

Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope