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CO - Summer School Alpbach 2012

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Orbiting Carbon Observatory (O<strong>CO</strong>)<br />

O 2 A-band <strong>CO</strong> 2 1.61μm <strong>CO</strong> 2 2.06 μm<br />

Clouds/Aerosols,<br />

Surface Pressure<br />

Glint Spot<br />

Ground Track<br />

Local Nadir<br />

Column <strong>CO</strong> 2<br />

Clouds/Aerosols,<br />

H 2 O,<br />

Temperature<br />

Space-based X <strong>CO</strong>2 measurements<br />

with precisions of 1–2 ppm (0.3–<br />

0.5%) on regional scales will:<br />

• Resolve pole to pole X <strong>CO</strong>2<br />

gradients on regional scales<br />

• Resolve the X <strong>CO</strong>2 seasonal cycle<br />

in the Northern Hemisphere<br />

• Improve constraints on <strong>CO</strong> 2 fluxes<br />

(sources and sinks) compared to<br />

the current knowledge<br />

– Reduce regional scale flux<br />

uncertainties from >2000 gC m -2<br />

yr -1 to < 200 gC m -2 yr -1<br />

– Reduce continental scale flux<br />

uncertainties below 30 gC m -2 yr -<br />

1<br />

Launch in Feb 2009 failed<br />

Reflight Feb 2013 („O<strong>CO</strong>-2“, carbon copy of O<strong>CO</strong>) 50

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