pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021)
Ocean acidification is a global crisis that is mainly caused by too much carbon dioxide in the atmosphere being absorbed by bodies of water, altering the water chemistry. Ocean acidification has large visual consequences, such as the bleaching of coral reefs, but less obvious, small scale influences...
Main Author: | |
---|---|
Format: | Text |
Language: | English |
Published: |
Western CEDAR
2022
|
Subjects: | |
Online Access: | https://cedar.wwu.edu/ssec/2022ssec/allsessions/54 https://cedar.wwu.edu/context/ssec/article/3216/viewcontent/60_a34895e322224a6abd8fbc96d6c83b90.pdf |
id |
ftwestwashington:oai:cedar.wwu.edu:ssec-3216 |
---|---|
record_format |
openpolar |
spelling |
ftwestwashington:oai:cedar.wwu.edu:ssec-3216 2023-08-20T04:08:53+02:00 pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) Vo, Ann-marie 2022-04-26T23:00:00Z application/pdf https://cedar.wwu.edu/ssec/2022ssec/allsessions/54 https://cedar.wwu.edu/context/ssec/article/3216/viewcontent/60_a34895e322224a6abd8fbc96d6c83b90.pdf English eng Western CEDAR https://cedar.wwu.edu/ssec/2022ssec/allsessions/54 https://cedar.wwu.edu/context/ssec/article/3216/viewcontent/60_a34895e322224a6abd8fbc96d6c83b90.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 2023-07-30T16:43:03Z Ocean acidification is a global crisis that is mainly caused by too much carbon dioxide in the atmosphere being absorbed by bodies of water, altering the water chemistry. Ocean acidification has large visual consequences, such as the bleaching of coral reefs, but less obvious, small scale influences are also found in the Salish Sea. A major indication of global warming’s effects on local water systems is pH, or the measure of how acidic or basic a solution is. The goal of this study is to observe how ocean acidification has affected pH and temperature in a salt-wedge estuary in Possession Sound near Everett, Washington. We utilized pH and temperature vertical profiles collected from a YSI EXO Sonde over five years to assess the degree of ocean acidification regionally. Trends were analyzed according to depth, season, and tidal stage. Previous global studies have shown that pH has been decreasing (becoming more acidic) over the years, while the overall temperatures have been rising. Preliminary studies of this particular site have shown minor changes. Given the potential for negative impacts on the estuary, it is worth expanding the study by investigating a longer time frame. Local estuary data regarding depth, season, and tidal stage will allow people to better understand how these variables change in our environment and gain a greater understanding of climate change’s influences on ocean acidification locally. Text Ocean acidification Western Washington University: CEDAR (Contributing to Education through Digital Access to Research) |
institution |
Open Polar |
collection |
Western Washington University: CEDAR (Contributing to Education through Digital Access to Research) |
op_collection_id |
ftwestwashington |
language |
English |
description |
Ocean acidification is a global crisis that is mainly caused by too much carbon dioxide in the atmosphere being absorbed by bodies of water, altering the water chemistry. Ocean acidification has large visual consequences, such as the bleaching of coral reefs, but less obvious, small scale influences are also found in the Salish Sea. A major indication of global warming’s effects on local water systems is pH, or the measure of how acidic or basic a solution is. The goal of this study is to observe how ocean acidification has affected pH and temperature in a salt-wedge estuary in Possession Sound near Everett, Washington. We utilized pH and temperature vertical profiles collected from a YSI EXO Sonde over five years to assess the degree of ocean acidification regionally. Trends were analyzed according to depth, season, and tidal stage. Previous global studies have shown that pH has been decreasing (becoming more acidic) over the years, while the overall temperatures have been rising. Preliminary studies of this particular site have shown minor changes. Given the potential for negative impacts on the estuary, it is worth expanding the study by investigating a longer time frame. Local estuary data regarding depth, season, and tidal stage will allow people to better understand how these variables change in our environment and gain a greater understanding of climate change’s influences on ocean acidification locally. |
format |
Text |
author |
Vo, Ann-marie |
spellingShingle |
Vo, Ann-marie pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) |
author_facet |
Vo, Ann-marie |
author_sort |
Vo, Ann-marie |
title |
pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) |
title_short |
pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) |
title_full |
pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) |
title_fullStr |
pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) |
title_full_unstemmed |
pH and temperature profiles in Salish Sea in regards to Ocean Acidification (2017-2021) |
title_sort |
ph and temperature profiles in salish sea in regards to ocean acidification (2017-2021) |
publisher |
Western CEDAR |
publishDate |
2022 |
url |
https://cedar.wwu.edu/ssec/2022ssec/allsessions/54 https://cedar.wwu.edu/context/ssec/article/3216/viewcontent/60_a34895e322224a6abd8fbc96d6c83b90.pdf |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Salish Sea Ecosystem Conference |
op_relation |
https://cedar.wwu.edu/ssec/2022ssec/allsessions/54 https://cedar.wwu.edu/context/ssec/article/3216/viewcontent/60_a34895e322224a6abd8fbc96d6c83b90.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_ |
1774721446861340672 |