Detecting and Constraining N Abundances in Planetary Atmospheres Using Collisional Pairs
arXiv:1507.07945 · doi:10.1088/0004-637X/810/1/57
Abstract
Characterizing the bulk atmosphere of a terrestrial planet is important for determining surface pressure and potential habitability. Molecular nitrogen (N) constitutes the largest fraction of Earths atmosphere and is likely to be a major constituent of many terrestrial exoplanet atmospheres. Due to its lack of significant absorption features, N is extremely difficult to remotely detect. However, N produces an N-N collisional pair, (N), which is spectrally active. Here we report the detection of (N) in Earths disk-integrated spectrum. By comparing spectra from NASAs EPOXI mission to synthetic spectra from the NASA Astrobiology Institutes Virtual Planetary Laboratory three-dimensional spectral Earth model, we find that (N) absorption produces a ~35 decrease in flux at 4.15 m. Quantifying N could provide a means of determining bulk atmospheric composition for terrestrial exoplanets and could rule out abiotic O generation, which is possible in rarefied atmospheres. To explore the potential effects of (N) in exoplanet spectra, we used radiative transfer models to generate synthetic emission and transit transmission spectra of self-consistent N-CO-HO atmospheres, and analytic N-H and N-H-CO atmospheres. We show that (N) absorption in the wings of the 4.3 m CO band is strongly dependent on N partial pressures above 0.5 bar and can significantly widen this band in thick N atmospheres. The (N) transit transmission signal is up to 10 ppm for an Earth-size planet with an N-dominated atmosphere orbiting within the HZ of an M5V star and could be substantially larger for planets with significant H mixing ratios.
Accepted for publication in The Astrophysical Journal. 46 pages, 12 figures, 3 tables
References in corpus (11)
- Extreme Water Loss and Abiotic O Buildup On Planets Throughout the Habitable Zones of M Dwarfs
- Atmospheric Retrieval for Super-Earths: Uniquely Constraining the Atmospheric Composition with Transmission Spectroscopy
- Water Vapour Absorption in the Clear Atmosphere of an exo-Neptune
- The Atmospheric Signatures of Super-Earths: How to Distinguish Between Hydrogen-Rich and Hydrogen-Poor Atmospheres
- Nitrogen Isotopic Composition and Density of the Archean Atmosphere
- The Nitrogen Budget of Earth
- Abiotic Ozone and Oxygen in Atmospheres Similar to Prebiotic Earth
- Detection of Ocean Glint and Ozone Absorption Using LCROSS Earth Observations
- The Effects of Refraction on Transit Transmission Spectroscopy: Application to Earth-like Exoplanets
- The Transit Spectra of Earth and Jupiter
- NuSTAR J163433-4738.7: A Fast X-ray Transient in the Galactic Plane
Cited by in corpus (53)
- Exoplanet Biosignatures: A Review of Remotely Detectable Signs of Life
- Characterizing transiting exoplanet atmospheres with JWST
- Exoplanet Biosignatures: Understanding Oxygen as a Biosignature in the Context of Its Environment
- The Habitability of Planets Orbiting M-dwarf Stars
- Exoplanet Biosignatures: A Framework for Their Assessment
- Abiotic O Levels on Planets around F, G, K, and M Stars: Possible False Positives for Life?
- Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life
- Evolved Climates and Observational Discriminants for the TRAPPIST-1 Planetary System
- The Habitability of Proxima Centauri b: II: Environmental States and Observational Discriminants
- On detecting biospheres from chemical thermodynamic disequilibrium in planetary atmospheres
- Identifying Planetary Biosignature Impostors: Spectral Features of CO and O4 Resulting from Abiotic O2/O3 Production
- Redox evolution via gravitational differentiation on low mass planets: implications for abiotic oxygen, water loss and habitability
- False negatives for remote life detection on ocean-bearing planets: Lessons from the early Earth
- Atmospheric characterization of terrestrial exoplanets in the mid-infrared: biosignatures, habitability & diversity
- Large Interferometer For Exoplanets (LIFE): III. Spectral resolution, wavelength range and sensitivity requirements based on atmospheric retrieval analyses of an exo-Earth
- Oceanographic Considerations for Exoplanet Life Detection
- Atmospheric Seasonality as an Exoplanet Biosignature
- Dim Prospects for Transmission Spectra of Ocean Earths Around M Stars
- Detectability of Molecular Signatures on TRAPPIST-1e through Transmission Spectroscopy Simulated for Future Space-Based Observatories
- The White Dwarf Opportunity: Robust Detections of Molecules in Earth-like Exoplanet Atmospheres with the James Webb Space Telescope
- Oxygen False Positives on Habitable Zone Planets Around Sun-Like Stars
- Observing Isotopologue Bands in Terrestrial Exoplanet Atmospheres with the James Webb Space Telescope---Implications for Identifying Past Atmospheric and Ocean Loss
- The K Dwarf Advantage for Biosignatures on Directly Imaged Exoplanets
- Is the Pale Blue Dot unique? Optimized photometric bands for identifying Earth-like exoplanets
- Differentiating Modern and Prebiotic Earth Scenarios for TRAPPIST-1e: High-resolution Transmission Spectra and Predictions for JWST
- The First Habitable Zone Earth-sized Planet from TESS. III: Climate States and Characterization Prospects for TOI-700 d
- The Transit Transmission Spectrum of a Cold Gas Giant Planet
- Simulated Phase-dependent Spectra of Terrestrial Aquaplanets in M Dwarf Systems
- Life as the Only Reason for the Existence of N2-O2-Dominated Atmospheres
- Evaluating the Plausible Range of N2O Biosignatures on Exo-Earths: An Integrated Biogeochemical, Photochemical, and Spectral Modeling Approach
- Synergies between Venus & Exoplanetary Observations
- Analytic Scattering and Refraction Models for Exoplanet Transit Spectra
- The Detectability and Constraints of Biosignature Gases in the Near & Mid-Infrared from Transit Transmission Spectroscopy
- How does Background Air Pressure Influence the Inner Edge of the Habitable Zone for Tidally Locked Planets in a 3D View?
- Alternative Methylated Biosignatures I: Methyl Bromide, A Capstone Biosignature
- Earthshine as an Illumination Source at the Moon
- Stellar Activity Effects on Moist Habitable Terrestrial Atmospheres Around M dwarfs
- Raman Scattering by Molecular Hydrogen and Nitrogen in Exoplanetary Atmospheres
- Earth as an Exoplanet. II. Earth's Time-variable Thermal Emission and Its Atmospheric Seasonality of Bioindicators
- Hierarchical Bayesian Atmospheric Retrieval Modeling for Population Studies of Exoplanet Atmospheres: A Case Study on the Habitable Zone
- MIRECLE: Science Yield for a Mid-IR Explorer-Class Mission to Study Non-Transiting Rocky Planets Orbiting the Nearest M-Stars Using Planetary Infrared Excess
- Constraining Background N2 Inventories on Directly Imaged Terrestrial Exoplanets to Rule Out O2 False Positives
- Earth as an Exoplanet. III. Using Empirical Thermal Emission Spectra as an Input for Atmospheric Retrieval of an Earth-twin Exoplanet
- The origin of Earth's mantle nitrogen: primordial or early biogeochemical cycling?
- Earth: Atmospheric Evolution of a Habitable Planet
- Pursuing Truth: Improving Retrievals on Mid-Infrared Exo-Earth Spectra with Physically Motivated Water Abundance Profiles and Cloud Models
- TRAPPIST-1h as an Exo-Titan. I. The Role of Assumptions about Atmospheric Parameters in Understanding an Exoplanet Atmosphere
- Influence of Biomass Emissions upon Habitability, Biosignatures and Detectability in Earth-like Atmospheres
- Exoplanet Analog Observations of Earth from Galileo Disk-integrated Photometry
- Observability of ultraviolet N I lines in the atmosphere of transiting Earth-like planets
- Near the Runaway: The Climate and Habitability of Teegarden's Star b
- L 98-59: a Benchmark System of Small Planets for Future Atmospheric Characterization
- Piercing through the Haze: Characterizing Titan-like terrestrial exoplanets with JWST