Atlantic Water Inflow Through the Yermak Pass Branch: Evolution Since 2007

نویسندگان

چکیده

Thirty-four months (2017–2020) of mooring data were recently obtained at 80.6°N, 7.26°E in the main branch Atlantic Water inflow to Arctic, Yermak Pass Branch. The Branch was sampled that same location during 14 a decade ago (2007–2008) when sea ice abundant (mean sea-ice concentration 74% vs. 39% recent deployment). We focus on time scales larger than 50 hr. new set shows an increase velocity variations 40% compared 2007–2008 period. Year 2018 exceptional with ice-free conditions over entire year and intensified mesoscale activity other years. Temperature salinity series 340 m showed significant trends 3 years (freshening ?0.07 g/kg cooling about ?0.9°C years). performance 1/12° Mercator-Ocean operational model precisely assessed. modeled transport average 2017–2020 (40% larger) 2007–2008. synoptic ranged between ?1 5 Sv 2007–2020 large seasonal interannual variations. winter summer. However, occasionally negative (<?0.7 Sv) through occurred winters (“Blocking events”). These blocking events are associated recirculations eddy more common last from 2016 onward. suggested Northern crossing Plateau further north (81.6°N) intermittently developed.

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ژورنال

عنوان ژورنال: Journal Of Geophysical Research: Oceans

سال: 2022

ISSN: ['2169-9275', '2169-9291']

DOI: https://doi.org/10.1029/2021jc018006