2005 Annual Science Report
Virtual Planetary Laboratory (JPL/CalTech) Reporting | JUL 2004 – JUN 2005
Characterization of Terrestrial Planets From Disk-Averaged Spectra: Earths Around Other Stars
Project Summary
Continuing work completed in previous years on Earth-like planets around F, G and K stars, this year we submitted a paper to Astrobiology that describes a coupled photochemical-climate model for Earth-like planets around M stars.
Project Progress
Continuing work completed in previous years on Earth-like planets around F, G and K stars, this year we submitted a paper to Astrobiology that describes a coupled photochemical-climate model for Earth-like planets around M stars. For two active M-stars (Eps Eridani and AD Leo) we constructed absolute FUV- to far-IR spectral energy distributions using optical and near-infrared observations. These spectra, and spectral models of 3 quiescent M stars were input to the climate-chemistry model to estimated the thickness of the ozone layer and the abundance of various biomarker gases (CH4, N2O, and CH3Cl). We calculated visible to mid-infrared spectra for the resulting planetary environments. All of the M-star planets modeled exhibited observable ozone layers, with ozone column depths on the two active M-stars within a factor of 2 of Earth’s (Fig. 1), whereas ozone column depths for planets around quiescent M-stars were up to 8 times smaller. Abundances of reduced biomarker gases were higher on the M-star planets than on Earth, given the same assumed surface fluxes, due to the low near-UV flux from the parent stars. CH4, for example, had a predicted concentration of ~500 ppmv on the active M-star planets, compared to 1.7 ppmv for Earth (Fig. 2). Little radiation is emitted from Mstars in the 200-300 nm range and the production of O(1D) and the corresponding abundance of OH radicals in the troposphere of an M-star planet is much lower than on Earth. The result is that both O2 (or O3) and reduced biomarker gases have a higher probability of being simultaneously observed on such planets, if present, (Fig. 3), providing a strong indicator for life.
High-CO2 planetary atmospheres were also simulated using a 1-D photochemical model to address whether O2 and O3 abiotic abundances can be in false positives for life. Complete FUV-far-IR spectra were assembled for six sun-like stars and spectrum of the object with the highest stellar UV flux (EK Dra) was used. A paper with the results is being prepared.
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PROJECT INVESTIGATORS:
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PROJECT MEMBERS:
Rebecca Butler
Co-Investigator
Martin Cohen
Co-Investigator
David Crisp
Co-Investigator
Victoria Meadows
Co-Investigator
John Scalo
Co-Investigator
Giovanna Tinetti
Co-Investigator
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RELATED OBJECTIVES:
Objective 1.2
Indirect and direct astronomical observations of extrasolar habitable planets
Objective 7.2
Biosignatures to be sought in nearby planetary systems