A Steady Regime Of Volume And Heat Transports In The Eastern Arctic Ocean In The Early 21st Century

Mooring observations in the eastern Eurasian Basin of the Arctic Ocean showed that mean 2013-2018 along-slope volume and heat (calculated relative to the freezing temperature) transports in the upper 800 m were 4.8 +/- 0.1 Sv (1 Sv = 10(6) m(3)/s) and 34.8 +/- 0.6 TW, respectively. Volume and heat transports within the Atlantic Water (AW) layer (similar to 150-800 m) in 2013-2018 lacked significant temporal shifts at annual and longer time scales: averaged over the two periods of mooring deployment in 2013-2015 and 2015-2018, volume transports were 3.1 +/- 0.1 Sv, while AW heat transports were 31.3 +/- 1.0 TW and 34.8 +/- 0.8 TW. Moreover, the reconstructed AW volume transports over longer, 2003-2018, period of time showed strong interannual variations but lacked a statistically significant trend. However, we found a weak positive trend of 0.08 +/- 0.07 Sv/year in the barotropic AW volume transport estimated using dynamic ocean topography (DOT) measurements in 2003-2014 - the longest period spanned by the DOT dataset. Vertical coherence of 2013-2018 transports in the halocline (70-140 m) and AW (similar to 150-800 m) layers was high, suggesting the essential role of the barotropic forcing in constraining along-slope transports. Quantitative estimates of transports and their variability discussed in this study help identify the role of atlantification in critical changes of the eastern Arctic Ocean.