Dynamics of the Canadian Arctic Archipelago throughflow: A numerical study with a finite element sea ice and ocean model

• Main Author: Wekerle, Claudia
• Other Authors: Lemke, Peter, Wang, Qiang, Jung, Thomas
• Format: Doctoral or Postdoctoral Thesis
• Language: English
• Published: Universität Bremen 2013
• Subjects: ocean modeling; Arctic freshwater exports; 530; 530 Physics; ddc:530; Arctic; Arctic Ocean; Baffin Bay; Canadian Arctic Archipelago; Lancaster Sound; Nares; Parry; Arctic Archipelago; Arktis*; Baffin; Beaufort Sea; kanadisch-arktische Archipel; Nares strait; North Atlantic; Parry Channel; Sea ice
• Online Access: https://media.suub.uni-bremen.de/handle/elib/543; https://nbn-resolving.org/urn:nbn:de:gbv:46-00103421-10

The Canadian Arctic Archipelago (CAA) connects the Arctic Ocean and Baffin Bay through narrow channels and is one of the key gateways where freshwater leaves the Arctic. It has therefore the potential to affect the deep convection in the northern North Atlantic. Representing the CAA in traditional global models still poses a challenge due to the small scale nature of the narrow passages. In this study we apply a global, multi-resolution sea ice ocean model (the Finite Element Sea ice Ocean Model, FESOM) with refinement in the CAA up to 5 km, while keeping a coarse resolution setup otherwise. With this model setup, a hindcast simulation for the period 1968-2007 was performed. The first goal of this thesis is to assess the model behavior in the CAA region and in the Arctic Ocean. The model assessment revealed good agreement with sea ice conditions in the Arctic Ocean and with fluxes through the main gates of the Arctic Ocean. During the period 1968-2007 the mean volume transports through Lancaster Sound and Nares Strait amount to 0.86 Sv (1 Sv = 10^6 m^3/s) and 0.91 Sv, respectively. The monthly mean volume transport through western Lancaster Sound is highly correlated with the observational estimate (r=0.81). A comparison of simulated sectionally averaged velocities in Nares Strait with observational estimates reveals good agreement (r=0.57). The simulated mean CAA freshwater export rate is 123 mSv, slightly higher than the observational estimate (101 -10 mSv). The local refinement of 5 km allows to investigate the freshwater contribution of individual narrow straits to the Parry Channel. In the second part of the thesis, the mechanisms driving the interannual variability of freshwater transports through the CAA are analyzed. The interannual variability is determined by sea surface height (SSH) gradients between the Arctic Ocean and northern Baffin Bay. The variability of fluxes through Lancaster Sound and Nares Strait is mainly determined by that of the SSH on the shelf along the Beaufort Sea coast and in the ...