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TPF-I SWG Report - Exoplanet Exploration Program - NASA

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C HAPTER 2<br />

Figure 2-6. The mid-infrared spectral features on an Earth-like planet change considerably over its<br />

evolution from a CO 2 -rich (epoch 0) to a CO 2 /CH 4 -rich atmosphere (epoch 3) to a present-day atmosphere<br />

(epoch 5). The black lines show a spectral resolution of 25 comparable to the proposed <strong>TPF</strong>-I mission<br />

concept designs. (Kaltenegger et al. 2006)<br />

This would indicate a stronger feature at 6.3 µm. However, this feature is so strong that it is relatively<br />

insensitive to atmospheric water abundance. Models of Earth’s atmosphere indicate that in the extreme<br />

clear-sky case, that the depth of this feature is very similar for water column abundances between 10%<br />

and more than 200% of the Earth’s present water abundance. 1 Methane and nitrous oxide have features<br />

nearly overlapping in the 7-μm region, and additionally both lie in the red wing of the 6.3-μm water band.<br />

The 6.3-μm H 2 O feature could act instead as a “true/false” indicator of the presence of even very small<br />

amounts of water if the atmosphere is an Earth-analog. Additionally the photons emission is very low at<br />

6.3 μm (see section 2.2).The broad rotational band, extending between 12 and 200 μm, has little spectral<br />

structure. That makes it difficult to discriminate its absorption from other factors affecting the planetary<br />

spectrum, such as the temperature of the emitting layer, which could also result in reduced flux in this<br />

1 Victoria Meadows (Caltech), private communication.<br />

22

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