Speaker

Su Kyong Yun

Streaming Media

Presentation Abstract

The Salih Sea is a complex estuarine system crossing over the U.S and Canadian waters. It has high cultural, environmental, and economic importance, but the increasing levels of nutrient pollution have threatened its values and caused hypoxia, algal blooms, and fish kills. To understand the impact of nutrient loading on the Salish Sea, we used a diagnostic hydrodynamic and biogeochemical model of the Salish Sea (Salish Sea Model) which has been developed to simulate circulation and biogeochemical cycling. For a deeper understanding of the interaction between land-based nutrient loading and circulation characteristic of the Salish Sea, we conducted initial components of a sensitivity analysis of different nutrient loading scenarios, with the nutrient reduction from non-point source loads to those from marine wastewater outfalls. We focused the analysis on the sub-basins in the Salish Sea such as Hood Canal Basin, Admiralty Inlet, Bellingham Bay, Whidbey Basin, Central Basin, and South Sound. We found that sub-basins respond differently to scenarios, likely driven by underlying differences in their physical and biogeochemical characteristics. To consider both temporal and spatial Dissolved Oxygen variation, we applied a novel analysis of calculated Dissolved Oxygen, including calculations of cumulative noncompliance-volume-days and hypoxic-volume-days. The cumulative volume days calculation is an extension of the method of marine water quality criteria of State of Washington, to provide further detail within the water column. The hypoxic volume days calculation is based on classic representations of hypoxia volume (dissolved oxygen < 2 mg/L).

Session Title

Innovations and Emerging Science 1

Conference Track

SSE1: Science for the Future

Conference Name

Salish Sea Ecosystem Conference (2022 : Online)

Document Type

Event

SSEC Identifier

SSE-traditionals-468

Start Date

27-4-2022 9:45 AM

End Date

27-4-2022 11:15 AM

Rights

Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this document for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.

Type

Text

Language

English

COinS
 
Apr 27th, 9:45 AM Apr 27th, 11:15 AM

Initial sensitivity analysis of nutrient loading to understand hypoxia in the Salish Sea sub-basins

The Salih Sea is a complex estuarine system crossing over the U.S and Canadian waters. It has high cultural, environmental, and economic importance, but the increasing levels of nutrient pollution have threatened its values and caused hypoxia, algal blooms, and fish kills. To understand the impact of nutrient loading on the Salish Sea, we used a diagnostic hydrodynamic and biogeochemical model of the Salish Sea (Salish Sea Model) which has been developed to simulate circulation and biogeochemical cycling. For a deeper understanding of the interaction between land-based nutrient loading and circulation characteristic of the Salish Sea, we conducted initial components of a sensitivity analysis of different nutrient loading scenarios, with the nutrient reduction from non-point source loads to those from marine wastewater outfalls. We focused the analysis on the sub-basins in the Salish Sea such as Hood Canal Basin, Admiralty Inlet, Bellingham Bay, Whidbey Basin, Central Basin, and South Sound. We found that sub-basins respond differently to scenarios, likely driven by underlying differences in their physical and biogeochemical characteristics. To consider both temporal and spatial Dissolved Oxygen variation, we applied a novel analysis of calculated Dissolved Oxygen, including calculations of cumulative noncompliance-volume-days and hypoxic-volume-days. The cumulative volume days calculation is an extension of the method of marine water quality criteria of State of Washington, to provide further detail within the water column. The hypoxic volume days calculation is based on classic representations of hypoxia volume (dissolved oxygen < 2 mg/L).