ocean acidification in puget sound: recent observations on water chemistry and implications for...
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Ocean acidification in Puget Sound: Recent observations on water chemistry and implications for
larval oyster success Jan Newton1,2, Simone Alin3, Richard Feely3, Chris Sabine3, Al Devol2, Andrew Suhrbier4,
Dan Cheney4, Benoit Eudeline5, Joth Davis5, Brian Allen6, Betsy Peabody6, and Christopher Krembs7
1: University of Washington, Applied Physics Laboratory2: University of Washington, School of Oceanography3: NOAA, Pacific Marine Environmental Laboratory
4: Pacific Shellfish Institute5: Taylor Shellfish
6: Puget Sound Restoration Fund7: Washington Department of Ecology
Ocean acidification (OA)Diffusion of increased atmospheric CO2 into marine waters, results in increase of aqueous CO2 (pCO2), decrease in pH and CO3
2-, and thus decreased saturation state of carbonate materials (Ω aragonite and calcite).
Wolf-Gladrow et al. (1999)
2−[CO3 ][CO2]
100−150% 50%
2100
8.2
8.1
8.0
7.9
7.81800 1900 2000 2100
50
40
30
20
10
0
300
240
180
120
60
0
pHμm
ol kg−1
Year
pH
CO2(aq)
CO32−
30% acidity16% [CO3 ]
2000
2−
OA in Puget Sound ?• Most of our OA measurements come from the open ocean• Pacific Coast estuaries susceptible to effects from OA:
– Deep Pacific Ocean waters are oldest (respiration)– Upwelling happens seasonally along west coast of U.S. – Estuaries have more carbon loading naturally, as well as loads from humans
• Estuaries host valuable economic and ecological resources• What are we learning locally re OA in Puget Sound?
– Puget Sound cruises (UW PRISM) documented OA status: • Demonstrable effect of anthropogenic OA in Puget Sound
– Buoys currently measuring OA variables: • Temporal variation is high, implies complex dynamics in estuaries
– Studies with oyster growers on OA and larvae: • Connection with biology; possible different mechanisms within Puget Sound
Observed aragonite & calcite saturation depths
The aragonite saturation horizon (Ω = 1) migrates towards the surface at the rate of 1-2 m yr-1, depending on location.
Ocean CO2 Chemistry
Feely et al. (2004)
Feely (NOAA)
Coastalupwelling - Linked to highmortality events
Figure courtesy of Alan Barton, in press
06/06 06/16 06/26 07/06 07/16 07/26-15
0
15
10 units
N S
win
d (
m/s
)06/06 06/16 06/26 07/06 07/16 07/26
28
30
32
34
Sal
init
y (p
pt)
06/06 06/16 06/26 07/06 07/16 07/26-5
0
5
Per
form
ance
of
Sm
all
Lar
vae
(<12
0 m
icro
ns)
Growth Survival
06/06 06/16 06/26 07/06 07/16 07/260.5
1
1.5
2
2.5
A
rag
on
ite
Sat
ura
tio
n S
tate
Upwelling favorable
winds
Highersalinity
High mortality
Low Ωarag
Winds from S
Lowersalinity
High survival
High Ωarag
Saturation (Ωarag)
CO2 CO2
CO2
Production−Respiration Cycle
CO2 + H2O CH2O + O2
production
CH2O + O2 CO2 + H2O
respiration
Processes that lead to hypoxia or high CO2 also yield low pH, [CO3
2-], and Ω values
Feely (NOAA)
Feely et al. (2010)
Question: How much of the corrosive conditions in Hood Canal result from ocean acidification?
* *
Respiration (DICΔR) = DICHC(deep) − DICAI(avg)
• Respiration accounts for 54 and 18 μmol kg-1 CO2 in summer and winter, respectively.
• OA accounts for 17 μmol kg-1 higher average CO2 at Admiralty Inlet in 2008 relative to pre-industrial times.
**
Ocean acidification (DICΔOA) =DICAI(avg 2008) − DICAI(avg PI)PI**
2008 ** PI = Pre-industrial AI = Admiralty InletOcean acidification accounts for 24% and 49% of corrosive conditions in summer and winter, respectively.
Under 2xCO2 conditions (atmo. CO2 = 560 ppmv), the contribution of OA to corrosive conditions would rise to
approx. 50% and 80% in summer and winter, respectively.
If humans increase deep water respiration by adding carbon or nitrogen loads, this will increase corrosiveness.
NANOOS network of autonomous observing buoys
2. OA monitoring in coastal WA and Puget SoundUW, NOAA, OSU
UW
UW
UW
NOAA
OSU
Real-time data at:
www.nanoos.org
Variability is much larger in coastal waters than the open ocean, then there are estuaries
Variability is much larger in coastal waters than the open ocean, then there are estuaries
Courtesy C. Sabine, NOAA PMEL
Gulf AK
Hawaii
WA coast
Hood Canal
Estuaries have a complex story OA to tell, but correlations with forcing functions, e.g., river input, sunlight, winds, stratification/mixing, tides, etc. are allowing interpretation of variation and, moreover, may lead to forecasting of risk.
Index Sites where shellfish monitored:
Dabob Bay: Deep, N-S fetch, stratified
Totten Inlet:Shallow, protected, mixed
Ocean Acidification Monitoring Project funded by the Puget Sound Partnership
3. OA monitoring in coastal WA and Puget SoundUW, NOAA, PSI, Taylor, Baywater, PCSGA, PSRF, Ecology
Two-year study to examine whether or not changing water conditions are affecting shellfish populations
Both upwelling and respiration processes are major contributors to the high pCO2 and low pH, undersaturated bottom waters that are highly vulnerable to further acidification in the future, there is need to better understand status, trends, and linkages with biological responses in Puget Sound.