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...
Main Authors: | , |
---|---|
Format: | Text |
Language: | English |
Published: |
Western CEDAR
2022
|
Subjects: | |
Online Access: | https://cedar.wwu.edu/ssec/2022ssec/allsessions/188 https://cedar.wwu.edu/context/ssec/article/3350/viewcontent/208_0b0d1500d5154fa19bbe7f452c0d3748.pdf |
id |
ftwestwashington:oai:cedar.wwu.edu:ssec-3350 |
---|---|
record_format |
openpolar |
spelling |
ftwestwashington:oai:cedar.wwu.edu:ssec-3350 2023-08-20T04:09:02+02:00 Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence Newton, Jan Carini, Roxanne 2022-04-26T23:00:00Z application/pdf https://cedar.wwu.edu/ssec/2022ssec/allsessions/188 https://cedar.wwu.edu/context/ssec/article/3350/viewcontent/208_0b0d1500d5154fa19bbe7f452c0d3748.pdf English eng Western CEDAR https://cedar.wwu.edu/ssec/2022ssec/allsessions/188 https://cedar.wwu.edu/context/ssec/article/3350/viewcontent/208_0b0d1500d5154fa19bbe7f452c0d3748.pdf 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. Salish Sea Ecosystem Conference text 2022 ftwestwashington 2023-07-30T16:43:11Z 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. Text Ocean acidification Orca Western Washington University: CEDAR (Contributing to Education through Digital Access to Research) Admiralty Inlet ENVELOPE(-86.000,-86.000,72.501,72.501) Carr ENVELOPE(130.717,130.717,-66.117,-66.117) |
institution |
Open Polar |
collection |
Western Washington University: CEDAR (Contributing to Education through Digital Access to Research) |
op_collection_id |
ftwestwashington |
language |
English |
description |
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. |
format |
Text |
author |
Newton, Jan Carini, Roxanne |
spellingShingle |
Newton, Jan Carini, Roxanne Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
author_facet |
Newton, Jan Carini, Roxanne |
author_sort |
Newton, Jan |
title |
Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
title_short |
Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
title_full |
Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
title_fullStr |
Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
title_full_unstemmed |
Salish Sea ORCA buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
title_sort |
salish sea orca buoy observations over the last decade: warmer and saltier than normal anomalies and their persistence |
publisher |
Western CEDAR |
publishDate |
2022 |
url |
https://cedar.wwu.edu/ssec/2022ssec/allsessions/188 https://cedar.wwu.edu/context/ssec/article/3350/viewcontent/208_0b0d1500d5154fa19bbe7f452c0d3748.pdf |
long_lat |
ENVELOPE(-86.000,-86.000,72.501,72.501) ENVELOPE(130.717,130.717,-66.117,-66.117) |
geographic |
Admiralty Inlet Carr |
geographic_facet |
Admiralty Inlet Carr |
genre |
Ocean acidification Orca |
genre_facet |
Ocean acidification Orca |
op_source |
Salish Sea Ecosystem Conference |
op_relation |
https://cedar.wwu.edu/ssec/2022ssec/allsessions/188 https://cedar.wwu.edu/context/ssec/article/3350/viewcontent/208_0b0d1500d5154fa19bbe7f452c0d3748.pdf |
op_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. |
_version_ |
1774721679043330048 |