Scenario Changes of Atlantic Water in the Arctic Ocean

• Published in: Journal of climate Vol. 28; no. 14; pp. 5523 - 5548
• Main Authors: Long, Zhenxia, Perrie, Will
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 15-07-2015
• Subjects: Awls; Basins; Climate change; Climate change scenarios; Climate models; Climatic analysis; Climatology; Cooling; Future climates; Global climate; Global climate models; Global warming; Heat; Heat flux; Heat loss; Heat transfer; High pressure; High pressure systems; Ice; Low pressure; Low pressure systems; Modelling; Ocean circulation; Oceans; Regional climate models; Regional climates; Salinity; Sea ice; Sea transportation; Sea water; Seas; Studies; Topography; Viscosity; Volume transport; Water; Water temperature; Arctic Ocean; Fram Strait; Beaufort Sea; Barents Sea; Arctic region; Kara Sea; PNE, Kara Sea; PNW, Beaufort Sea; PNE, Barents Sea; PNE, Arctic Ocean, Fram Strait; ANE, Norwegian Sea; PN, Arctic Ocean
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-14-00522.1

The authors explore possible temperature modifications of the Atlantic Water Layer (AWL) induced by climate change, performing simulations for 1970 to 2099 with a coupled ice–ocean Arctic model (CIOM). Surface fields to drive the CIOM were provided by the Canadian Regional Climate Model (CRCM), driven by outputs from the Canadian Centre for Climate Modelling and Analysis (CCCma) Coupled Global Climate Model, version 3 (CGCM3) following the A1B climate change scenario. In the present climate, represented as 1990–2009, the CIOM can reliably reproduce the AWL compared to Polar Science Center Hydrographic Climatology (PHC) data. For the future climate, assuming the A1B climate change scenario, there is a significant increase in water volume transport into the central Arctic Ocean through Fram Strait due to the weakened atmospheric high pressure system over the western Arctic and an intensified atmospheric low pressure system over the Nordic seas. The AWL temperature tends to decrease from 0.36°C in the 2010s to 0.26°C in the 2060s. In the vertical, the warm Atlantic water core slightly expands before the 2030s, significantly shrinks after the 2050s, and essentially disappears by 2070–99, in the southern Beaufort Sea. The temperature decrease after 2030 is mainly due to the reduced heat fluxes in the Kara and Barents Seas. In the northeastern Barents and Kara Seas, the loss of sea ice increases the heat loss from the Atlantic water and reduces the water temperature near the bottom, contributing to decreased heat fluxes into the central Arctic Ocean, as well as decreased AWL temperature at central Arctic Ocean intermediate layers. In addition, the vertically integrated heat loss also plays an important role in the AWL cooling process.