scaling up carbon and carbonate production to regional scales with landsat 7 etm+ christopher s....
TRANSCRIPT
Scaling Up Carbon and Carbonate Production to
Regional Scales with Landsat 7 ETM+
Christopher S. Moses (USF)Serge Andréfouët (IRD)
Frank Muller-Karger (UMass)Christine Kranenburg (USF)
NOAA Think Tank #5: Ocean Acidification3-7 Dec. 2007, Little Cayman Research Center
C.S. Moses, Think Tank #5, Dec. 2007
Outline• Driving questions• Millennium Coral Reef Map• Location• Scaling up carbon and carbonate production• Conclusions• What’s next and what’s needed
C.S. Moses, Think Tank #5, Dec. 2007
Questions• Can remote sensing produce reasonably
accurate estimates of production over regional scales (103-104 km2)?
• Can the Millennium Map geomorphologic classes serve as proxies for production in areas with poor imagery or no data for validation?
C.S. Moses, Think Tank #5, Dec. 2007
Previous Scaling-up Work• Atkinson & Grigg (1984)
– French Frigate Shoals– Aerial photography– 3 classes
• Andréfouët & Payri (2001)– Moorea– SPOT (20 m resolution)– 9 classes
• Brock et al. (2006)– Biscayne National Park– ASTER (15 m), IKONOS (4 m), AISA (~1.5 m)– 4 classes
Andréfouët & Payri (2001)
C.S. Moses, Think Tank #5, Dec. 2007
Landsat 7 ETM+: Full Scene
~180 km
Path 14, Row 46
14 Feb. 2000
C.S. Moses, Think Tank #5, Dec. 2007
Measuring Production• Several methods
– Geochemical– Growth rate, density
• aka: census based
– Net accretion
• Geochemical measurements– Single points or arrays– Total alkalinity (TA), pH
– pCO2, HCO3-, or CO2
O2
Yates & Halley (2003)
C.S. Moses, Think Tank #5, Dec. 2007
Scaling-Up Production
• Assumptions:– In situ values are
representative over larger areas
– Production is linearly scalable
Ppatch reef = (Fsand x Psand) + (Fdense live x Pdense live )… + (Fi x Pi)
C.S. Moses, Think Tank #5, Dec. 2007
In situ Production Values
P R E P/R G
Class (g C m-2 d-1) (g C m-2 d-1) (g C m-2 d-1) (g CaCO3 m-2 d-1)
Sand 1.76 1.96 -0.20 0.90 0.11
Seagrass 2.88 3.32 -0.44 0.87 -0.19
Sparse seagrass* 1.98 2.23 -0.25 0.89 0.05
Dense live substrate 6.43 8.09 -1.66 0.79 1.29
Sparse live substrate 4.23 5.31 -1.08 0.80 -0.04
C.S. Moses, Think Tank #5, Dec. 2007
Unit P, R, P/R, and G
Sensor P R E P/R G(g C m-2 d-1) (g C m-2 d-1) (g C m-2 d-1) (g CaCO3 m-2 d-1)
AISA 3.15 3.71 -0.57 0.85 0.04
IKONOS 3.52 4.20 -0.68 0.84 0.15
ASTER 4.05 4.91 -0.86 0.82 0.36
AISA corrected
3.11 3.67 -0.56 0.85 0.07
L7 NFRT total
3.03 3.61 -0.58 0.84 -0.002
Net heterotrophic
Net CO2 sink
Net Dissolution
Comparative Estimates
-1
0
1
2
3
4
5
P R E P/R G
g C m
-2 d
-1
IKONOS
AISA corrected
Landsat 7
C.S. Moses, Think Tank #5, Dec. 2007
Accuracy of L7• 86.2 (±2.3%) accuracy
over entire NFRT• Most TD >1.80• Lowest TD (0.63)
between shallow dense live and deep sparse live
• Sand is most easily misclassified
C.S. Moses, Think Tank #5, Dec. 2007
Proxy Stability
Millennium Coral Reef Map
P R E P/R G
Class (g C m-2 d-1) (g C m-2 d-1) (g C m-2 d-1) (g CaCO3 m-2 d-1)
Intra-seas patch reef complex (#568)
3.84 4.68 -0.84 0.84 0.30
Shelf terrace (#781)
3.46 4.19 -0.73 0.83 0.25
Cross shelf (#793) 2.90 3.43 -0.53 0.85 -0.07
C.S. Moses, Think Tank #5, Dec. 2007
Conclusions• Landsat 7 ETM+ imagery can produce
accurate biotope classifications and production estimates at regional scales
• Millennium Map classes can be used as proxies in areas with poor bathymetric control and little validation
• Limitations:– Dependent on accuracy of in situ observations– Greater numbers of classes decrease accuracy– MM classes only regionally applicable
C.S. Moses, Think Tank #5, Dec. 2007
Needs and Next Steps• Better spatial
coverage of in situ measurements of production– Keystone sites??
• Accurate measurements in deeper (>10 m) water depths– New technologies
• Integration into more complex models
Hochberg & Atkinson (2007)
C.S. Moses, Think Tank #5, Dec. 2007
Significance• Reefs fringe ~15% of world’s coastlines• High biodiversity
– >2,000 reef fishes– >800 species of corals
• Roberts, et al., 2002
• ~58% are threatened by human activities• Ginsburg, et al., 1994
• ~30% decline in calcification at 560 atm CO2 – Ωarag ~ 2.29
• Kleypas, et al. (2006)
• Need for ecosystem-based management approaches• Loreau, et al. (2003)
C.S. Moses, Think Tank #5, Dec. 2007
Millennium Global Coral Reef Map
http://imars.usf.edu/corals/maps/reef_count.html
C.S. Moses, Think Tank #5, Dec. 2007
Unit P, R, P/R, and G
Sensor P R E P/R G(g C m-2 d-1) (g C m-2 d-1) (g C m-2 d-1) (g CaCO3 m-2 d-1)
AISA 3.15 3.71 -0.57 0.85 0.04
IKONOS 3.52 4.20 -0.68 0.84 0.15
ASTER 4.05 4.91 -0.86 0.82 0.36
AISA corrected
3.11 3.67 -0.56 0.85 0.07
L7 NFRT total
3.03 3.61 -0.58 0.84 -0.002
Net heterotrophic: -5.74 x 108 kg C yr-1
Net CO2 sink: ~753 tons yr-1
Net Dissolution: 1.68 x 106 kg CaCO3 yr-1
Comparative Estimates
-1
0
1
2
3
4
5
P R E P/R G
g C m
-2 d
-1
IKONOS
AISA corrected
Landsat 7