Streaming Media
Presentation Abstract
Profiling buoys take frequent (one to four times per day) measurements of water properties over the full water column. This allows characterization of short and long-term processes, including deep-water renewal events, surface influence of river runoff and heating, and tracking water mass properties. There are currently six ORCA (Oceanic Remote Chemical Analyzer) moorings in Puget Sound supported primarily by NANOOS and the Washington Ocean Acidification Center: South Hood Canal (Twanoh), central Hood Canal (Hoodsport), Dabob Bay, Admiralty Inlet (Hansville), Main Basin (Point Wells), and Southern Puget Sound (Carr Inlet). Profiling ORCA buoys have been operating in Puget Sound for over 10-15 years, depending on location. Anomalies of the real-time data (collected daily) compared to the long-term climatology illustrate times of higher than normal sea temperatures associated with marine heat waves, and times of higher than normal salinities associated with summer droughts. However, warm and salty anomalies have persisted in some years when those respective forcings (heat waves, summer droughts) were not occurring. We examine the record to elucidate annual differences and highlight basin differences in these signals. In the last six years, only 2020 and 2017 did not have predominantly warmer than average seawater temperatures. Higher than average salinities during summer have been noted for all years since 2014, except 2017. Temperature variations reflect the diverse oceanographic characteristics of Puget Sound’s sub-basins. Hood Canal, with strongly stratified waters, slow circulation, and deep water flushed by annual renewal, responds to atmospheric forcing differently than the Main Basin, which has stronger mixing that intensifies as this water feeds South Sound. Utilizing this longer view, we highlight emerging patterns and generalities in the anomalies, as well as sharp differences.
Session Title
Poster Session 1: Applied Research & Climate Change
Conference Track
SSE14: Posters
Conference Name
Salish Sea Ecosystem Conference (2022 : Online)
Document Type
Event
SSEC Identifier
SSE-posters-208
Start Date
26-4-2022 4:00 PM
End Date
26-4-2022 4:30 PM
Type of Presentation
Poster
Genre/Form
conference proceedings; presentations (communicative events)
Contributing Repository
Digital content made available by University Archives, Heritage Resources, Western Libraries, Western Washington University.
Subjects – Topical (LCSH)
Oceanographic buoys--Salish Sea (B.C. and Wash.); Seawater--Salish Sea (B.C. and Wash.); Climatic changes--Salish Sea (B.C. and Wash.); Climatology
Geographic Coverage
Salish Sea (B.C. and Wash.)
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
Format
application/pdf
Included in
Fresh Water Studies Commons, Marine Biology Commons, Natural Resources and Conservation Commons, Terrestrial and Aquatic Ecology Commons
Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence
Profiling buoys take frequent (one to four times per day) measurements of water properties over the full water column. This allows characterization of short and long-term processes, including deep-water renewal events, surface influence of river runoff and heating, and tracking water mass properties. There are currently six ORCA (Oceanic Remote Chemical Analyzer) moorings in Puget Sound supported primarily by NANOOS and the Washington Ocean Acidification Center: South Hood Canal (Twanoh), central Hood Canal (Hoodsport), Dabob Bay, Admiralty Inlet (Hansville), Main Basin (Point Wells), and Southern Puget Sound (Carr Inlet). Profiling ORCA buoys have been operating in Puget Sound for over 10-15 years, depending on location. Anomalies of the real-time data (collected daily) compared to the long-term climatology illustrate times of higher than normal sea temperatures associated with marine heat waves, and times of higher than normal salinities associated with summer droughts. However, warm and salty anomalies have persisted in some years when those respective forcings (heat waves, summer droughts) were not occurring. We examine the record to elucidate annual differences and highlight basin differences in these signals. In the last six years, only 2020 and 2017 did not have predominantly warmer than average seawater temperatures. Higher than average salinities during summer have been noted for all years since 2014, except 2017. Temperature variations reflect the diverse oceanographic characteristics of Puget Sound’s sub-basins. Hood Canal, with strongly stratified waters, slow circulation, and deep water flushed by annual renewal, responds to atmospheric forcing differently than the Main Basin, which has stronger mixing that intensifies as this water feeds South Sound. Utilizing this longer view, we highlight emerging patterns and generalities in the anomalies, as well as sharp differences.
