Putting It Together - NSTA Learning Center
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Transcript Putting It Together - NSTA Learning Center
OA is the consequence of rising anthropogenic
emissions of CO2 since 1750, and the uptake
of 30-40% of that carbon by the ocean This
process is driven by CO2
Process of ocean water becoming less basic
(but not acidic)
CO2 affects both climate change and
acidification, but via different mechanisms
CO2 in the atmosphere: it warms it
CO2 in the ocean: it acidifies it
2
≈ 48% of anthropogenic
CO2 taken up by the ocean
CO2
Sabine et al. Science (2004)
CO2
(photosynthesis
& respiration)
H2CO3 Carbonic
CO2 + H2O
pH
acid
H+
Hydrogen
ion
H+
Hydrogen
ion
HCO3Bicarbonate ion
+ CO32Carbonate
ion
+ = CaCO
X
X
3 =
Ca
2+
pH
NOAA CMDL CCGG CO2
data at Mauna Loa, HI
4
5
Invention: Students will design an
investigation into ocean acidification using
real data on conditions in the Caribbean
study area.
4 Interactivity: Students will use online data to
support or disprove a simple hypothesis about
increased atmospheric CO2 and the health of marine
calcifieres, such as coral reefs.
3 Adaptation: Students will use online tools to recreate
climate change model scenarios and examine effects of
increased CO2 on ocean acidity and carbonate saturation
levels.
Adoption: Students will use data graphs of ocean pH, sea-surface
temperature, and CO2 data to find the driving factor behind ocean
acidification.
Levels of
scaled
interaction
2
1
5
Entry: Students will examine data maps and graphs to look for patterns and
relationships that would explain variations in ocean pH.
1.
2.
3.
4.
5.
Measuring Ocean pH
The Ocean-Carbon Connection
Carbonate Buffering System
Aragonite Saturation & Marine Calcifiers
Design Your Own Investigation
Adaptation: Students use online tools to
recreate climate change model scenarios
and examine effects of increased CO2 on
ocean acidity and carbonate saturation
levels.
Interactivity: Students use online data to
support or disprove a simple hypothesis
about increased atmospheric CO2 and the
health of marine calcifieres, such as coral
reefs.
How does dissolved CO2 relate
to levels of atmospheric CO2?
Describe the pattern of change
in aragonite concentration (Ω) in
the study area over time.
If you assume a steady rate of
aragonite saturation decrease
over time, when will coral reefs
reach the critical 3.3 Ω level?
Friday 8AM-9AM: NOAA Data Education
Project
Saturday 3:30PM-4:30: Corals, Tech, and
Carbon (bleaching and OA)
[email protected]