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Full Region Surface Salinity and Drifters
Full Region Bottom Oxygen
Washington Shelf Bottom Oxygen (5 days)
Puget Sound Surface Temperature
Puget Sound Surface Currents

High-Resolution Submodels

Willapa & Grays Surface Ocean Acidification
Willapa & Grays Bottom Ocean Acidification
Willapa & Grays Surface Temperature
Willapa & Grays Surface Salinity
Willapa & Grays Surface Currents
South Puget Sound Surface Temperature
South Puget Sound Surface Salinity

Interactive Tools

Drifters: Puget Sound
Drifters: Willapa & Grays
Drifters: Willapa 2025 Custom
Observation Viewer

Background

How Tides Work in Puget Sound
Observed Long-term Trends in Puget Sound Water Properties
The Estuarine Exchange Flow

About the Model

Data Access
How the Model Works
How We Test the Model
References

Gallery

A Year of Modeled Salinity
A Year of Modeled Oxygen
A Year of Modeled Phytoplankton
  1. Forecast movies
  2. Full Region Surface Salinity and Drifters

Full Region Surface Salinity and Drifters

This is a movie made from the most recent LiveOcean three-day forecast.

The movie has a panel at the bottom that shows time. The tide is evident in the twice-a-day variation of the sea surface height. Daytimes are shown as the thick yellow lines on the horizontal axis. Winds are shown by an arrow in the middle of the map, with the scale given by the circle. The black line off the coast on the map is the 200 m depth line, which marks the "shelf break" separating the coastal region from the deeper ocean beyond.

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© 2026 LiveOcean.

Last edited 07/04/2025 14:13:04
  1. Forecast movies
  2. Full Region Bottom Oxygen

Full Region Bottom Oxygen

This is a movie made from the most recent LiveOcean three-day forecast.

This is a movie made from the most recent LiveOcean three-day forecast.

The color shows the amount of dissolved oxygen predicted by the model to be in the water. We model the oxygen at all depths, but the movie is focused on the bottom water, which is where oxygen is often the lowest. When oxygen drops below 2 mg/L (the red part of the colors) that is called "hypoxia" and organisms like crabs begin to be negatively affected. In our region hypoxia typically develops every summer on the continental shelf. In part this is because the water upwelled onto the shelf is already low in oxygen, and in part it is because of phytoplankton blooms near the surface. When these blooms die the organic particles sink to the bottom and when these degrade they use up oxygen.

The movie has a panel at the bottom that shows time. The tide is evident in the twice-a-day variation of the sea surface height. Daytimes are shown as the thick yellow lines on the horizontal axis. Winds are shown by an arrow in the middle of the map, with the scale given by the circle. The black line off the coast on the map is the 200 m depth line, which marks the "shelf break" separating the coastal region from the deeper ocean beyond.

Full Region Surface Salinity and DriftersWashington Shelf Bottom Oxygen (5 days)

Content

FeedbackEdit page