Changes in the oxygen isotope composition of the Bering Sea contribution to the Arctic Ocean are an independent measure of increasing freshwater fluxes through the Bering Strait

A large volume of freshwater is incorporated in the relatively fresh (salinity similar to 32-33) Pacific Ocean waters that are transported north through the Bering Strait relative to deep Atlantic salinity in the Arctic Ocean (salinity similar to 34.8). These freshened waters help maintain the halocline that separates cold Arctic surface waters from warmer Arctic Ocean waters at depth. The stable oxygen isotope composition of the Bering Sea contribution to the upper Arctic Ocean halocline was established as early as the late 1980's as having a delta(18)O(V-SMOW )value of approximately -1.1 parts per thousand. More recent data indicates a shift to an isotopic composition that is more depleted in O-18 (mean delta O-18 value similar to-1.5 parts per thousand). This shift is supported by a data synthesis of >1400 water samples (salinity from 32.5 to 33.5) from the northern Bering and Chukchi seas, from the years 1987-2020, which show significant year-to-year, seasonal and regional variability. This change in the oxygen isotope composition of water in the upper halocline is consistent with observations of added freshwater in the Canada Basin, and mooring-based estimates of increased freshwater inflows through Bering Strait. Here, we use this isotopic time-series as an independent means of estimating freshwater flux changes through the Bering Strait. We employed a simple end-member mixing model that requires that the volume of freshwater (including runoff and other meteoric water, but not sea ice melt) flowing through Bering Strait has increased by similar to 40% over the past two decades to account for a change in the isotopic composition of the 33.1 salinity water from a delta O-18 value of approximately -1.1 parts per thousand to a mean of -1.5 parts per thousand. This freshwater flux change is comparable with independent published measurements made from mooring arrays in the Bering Strait (freshwater fluxes rising from 2000-2500 km(3) in 2001 to 3000-3500 km(3) in 2011).

Automated summary

Research suggests that the freshwater flux through the Bering Strait into the Arctic Ocean has increased by about 40% over the past two decades, resulting in a change in the oxygen isotope composition of water in the upper halocline. This finding is consistent with other independent measurements.