Ecosystem Model of the Entire Beaufort Sea Marine Ecosystem: A Temporal Tool for Assessing Food-Web Structure and Marine Animal Populations from 1970 to 2014

• Main Authors: Suprenand, Paul M, Ainsworth, Cameron H., Hoover, Carie
• Format: Other/Unknown Material
• Language: unknown
• Published: Digital Commons @ University of South Florida 2018
• Subjects: Beaufort Sea; Arctic Climate Change; Ecopath with Ecosim; Ecological Model; Nature Resource Management; Life Sciences; Marine Biology; Arctic; Arctic Ocean; Tuktoyaktuk; Inuvik; Aklavik; Ulukhaktok; Sachs Harbour; Paulatuk; Climate change; ice algae; inuit; Sea ice
• Online Access: https://digitalcommons.usf.edu/msc_facpub/261; https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=1260&context=msc_facpub

The Beaufort Sea coastal-marine ecosystem is a 476,000 km2 area in the Arctic Ocean, which extends from -112.5 to -158.0° longitude to 67.5 to 75.0° latitude. Within this polar area the United States indigenous communities of Barrow, Kaktovik, and Nuiqsut, and the Canadian indigenous communities of Aklavik, Inuvik, Tuktoyaktuk, Paulatuk, Ulukhaktok, and Sachs Harbour, subsist by harvesting marine mammals, fish, and invertebrates to provide the majority of their community foods. The Beaufort Sea coastal-marine ecosystem includes many specialized marine animals whose life history is tied to the sea ice, such as polar bears that rely on sea-ice for foraging activities and denning, or ice algae that attach to the seasonal cryosphere. Changes in sea-ice extent and sea surface temperature affect the ecosystem through losses of animal habitat, alterations to trophodynamics, and/or impacts to indigenous community harvesting. The present study focuses on developing a dynamic whole-ecosystem model that can be used for natural resource management. The resulting Ecopath with Ecosim (EwE) temporal model (1970 to 2014) utilizes forcing and mediation functions that describe food web and relationships between sea-ice extent, SST, and Inuit community harvesting efforts. Following model calibrations, vulnerability estimates, trophic level validation, and sensitivity analyses, the Beaufort Sea model produces population and dietary changes over time that are analogous to observations. Changes in temporal whole-ecosystem trophodynamics highlight a potential climatological tipping point in 1993, followed by a biological tipping point in 1998.