Abstract:We have measured in the laboratory the far ultraviolet (FUV: 125.0-170.0 nm) cascade-induced spectrum of the Lyman-Birge-Hopfield (LBH) band system (a 1 Π g →X 1 Σ þ g ) of N 2 excited by 30-200 eV electrons. The cascading transition begins with two processes: radiative and collision-induced electronic transitions (CIETs) involving two states (a′ 1 Σ − u and w 1 Δ u → a 1 Π g ), which are followed by a cascade induced transition a 1 Π g →X 1 Σ þ g at the single-scattering pressures employed here. Direct excita… Show more
“…The experimental apparatus comprised of a large (0.3 m in length) electrostatic electron gun system and the IUVS OEU housed in a large (1.5 m diameter and 2.35 m length) vacuum chamber referred to as the multi-optical beam instrument (MOBI). This experimental setup has been described in detail previously (Ajello et al, 2017;Kanik et al, 2003;Noren et al, 2001), and an experimental schematic is given in Ajello et al (2017Ajello et al ( , 2020. The experimental procedure is a replication of Ajello et al (2019) wherein an electron beam with an energy resolution of ∼1 eV was passed through static CO gas with a chamber pressure of 1 × 10 −5 Torr (n = 3 × 10 11 cm −3 ) and gas swarm temperature of 300 K. The cylindrical emission glow profile produced about the electron beam was measured up to a radial distance of ∼400 mm, moving upward from the electron beam centered initially at 0 mm, using the IUVS OEU mounted to a vertically moving stage, to fully observe and measure optically allowed and forbidden transitions.…”
Section: Experimental Apparatus and Proceduresmentioning
confidence: 99%
“…Cameron Band Total Emission Cross Sections From Electron Impact of CO From 180 to 280 nm With an Uncertainty of 35% (Ajello et al, 2020) laboratory temperature. The CB volume emission rate in the cylindrical glow about the electron beam falls off a little faster than 1/r due to the exponential factor with lifetime.…”
Section: Tablementioning
confidence: 99%
“…Most of these metastable molecules drift out of the field of view as a result of thermal motion. It was shown in the past for N 2 that it is possible to determine what fraction of the total emission cross section is actually observed (Ajello et al, 2017(Ajello et al, , 2020Kanik et al, 2003) by using a large apparatus with an imaging detector, and a knowledge of the velocity distribution and the effective lifetime of the metastable state.…”
mentioning
confidence: 99%
“…We have started a laboratory aeronomy program at the University of Colorado to study electron impact fluorescence of the CB in the MUV from two parent gases, CO and CO 2 , to match and model the spectra of past, present, and future spacecraft equipped with MUV capabilities to observe the upper atmosphere of Mars and Venus (100-300 km) where both gases are present and abundant (Fox, 2008;Gérard et al, 2019;Krasnopolsky & Feldman, 2002). A thorough understanding of CO CB emissions by the same laboratory technique as performed for the LBH bands (Ajello et al, 2020) from a large chamber will lend greater precision in the spectral analysis of solar system objects. These laboratory measurements of both cross sections and spectra are an important step in allowing forward modeling to determine the excitation rates and volume emission rates in the thermospheres of Mars and Venus (Evans et al, 2015;Gérard et al, 2011Gérard et al, , 2019Hubert et al, 2010;Jain et al, 2015;Stevens et al, 2015).…”
We have analyzed medium‐resolution (full width at half maximum, FWHM = 1.2 nm), Middle UltraViolet (MUV; 180–280 nm) laboratory emission spectra of carbon monoxide (CO) excited by electron impact at 15, 20, 40, 50, and 100 eV under single‐scattering conditions at 300 K. The MUV emission spectra at 100 eV contain the Cameron Bands (CB) CO(a 3Π → X 1Σ+), the fourth positive group (4PG) CO(A 1Π → X 1Σ+), and the first negative group (1NG) CO+(B 2Σ+ → X 2Σ) from direct excitation and cascading‐induced emission of an optically thin CO gas. We have determined vibrational intensities and emission cross sections for these systems, important for modeling UV observations of the atmospheres of Mars and Venus. We have also measured the CB “glow” profile about the electron beam of the long‐lived CO (a 3Π) state and determined its average metastable lifetime of 3 ± 1 ms. Optically allowed cascading from a host of triplet states has been found to be the dominant excitation process contributing to the CB emission cross section at 15 eV, most strongly by the d 3Δ and a' 3Σ+ electronic states. We normalized the CB emission cross section at 15 eV electron impact energy by multilinear regression (MLR) analysis to the blended 15 eV MUV spectrum over the spectral range of 180–280 nm, based on the 4PG emission cross section at 15 eV that we have previously measured (Ajello et al., 2019, https://doi.org/10.1029/2018ja026308). We find the CB total emission cross section at 15 eV to be 7.7 × 10−17 cm2.
“…The experimental apparatus comprised of a large (0.3 m in length) electrostatic electron gun system and the IUVS OEU housed in a large (1.5 m diameter and 2.35 m length) vacuum chamber referred to as the multi-optical beam instrument (MOBI). This experimental setup has been described in detail previously (Ajello et al, 2017;Kanik et al, 2003;Noren et al, 2001), and an experimental schematic is given in Ajello et al (2017Ajello et al ( , 2020. The experimental procedure is a replication of Ajello et al (2019) wherein an electron beam with an energy resolution of ∼1 eV was passed through static CO gas with a chamber pressure of 1 × 10 −5 Torr (n = 3 × 10 11 cm −3 ) and gas swarm temperature of 300 K. The cylindrical emission glow profile produced about the electron beam was measured up to a radial distance of ∼400 mm, moving upward from the electron beam centered initially at 0 mm, using the IUVS OEU mounted to a vertically moving stage, to fully observe and measure optically allowed and forbidden transitions.…”
Section: Experimental Apparatus and Proceduresmentioning
confidence: 99%
“…Cameron Band Total Emission Cross Sections From Electron Impact of CO From 180 to 280 nm With an Uncertainty of 35% (Ajello et al, 2020) laboratory temperature. The CB volume emission rate in the cylindrical glow about the electron beam falls off a little faster than 1/r due to the exponential factor with lifetime.…”
Section: Tablementioning
confidence: 99%
“…Most of these metastable molecules drift out of the field of view as a result of thermal motion. It was shown in the past for N 2 that it is possible to determine what fraction of the total emission cross section is actually observed (Ajello et al, 2017(Ajello et al, , 2020Kanik et al, 2003) by using a large apparatus with an imaging detector, and a knowledge of the velocity distribution and the effective lifetime of the metastable state.…”
mentioning
confidence: 99%
“…We have started a laboratory aeronomy program at the University of Colorado to study electron impact fluorescence of the CB in the MUV from two parent gases, CO and CO 2 , to match and model the spectra of past, present, and future spacecraft equipped with MUV capabilities to observe the upper atmosphere of Mars and Venus (100-300 km) where both gases are present and abundant (Fox, 2008;Gérard et al, 2019;Krasnopolsky & Feldman, 2002). A thorough understanding of CO CB emissions by the same laboratory technique as performed for the LBH bands (Ajello et al, 2020) from a large chamber will lend greater precision in the spectral analysis of solar system objects. These laboratory measurements of both cross sections and spectra are an important step in allowing forward modeling to determine the excitation rates and volume emission rates in the thermospheres of Mars and Venus (Evans et al, 2015;Gérard et al, 2011Gérard et al, , 2019Hubert et al, 2010;Jain et al, 2015;Stevens et al, 2015).…”
We have analyzed medium‐resolution (full width at half maximum, FWHM = 1.2 nm), Middle UltraViolet (MUV; 180–280 nm) laboratory emission spectra of carbon monoxide (CO) excited by electron impact at 15, 20, 40, 50, and 100 eV under single‐scattering conditions at 300 K. The MUV emission spectra at 100 eV contain the Cameron Bands (CB) CO(a 3Π → X 1Σ+), the fourth positive group (4PG) CO(A 1Π → X 1Σ+), and the first negative group (1NG) CO+(B 2Σ+ → X 2Σ) from direct excitation and cascading‐induced emission of an optically thin CO gas. We have determined vibrational intensities and emission cross sections for these systems, important for modeling UV observations of the atmospheres of Mars and Venus. We have also measured the CB “glow” profile about the electron beam of the long‐lived CO (a 3Π) state and determined its average metastable lifetime of 3 ± 1 ms. Optically allowed cascading from a host of triplet states has been found to be the dominant excitation process contributing to the CB emission cross section at 15 eV, most strongly by the d 3Δ and a' 3Σ+ electronic states. We normalized the CB emission cross section at 15 eV electron impact energy by multilinear regression (MLR) analysis to the blended 15 eV MUV spectrum over the spectral range of 180–280 nm, based on the 4PG emission cross section at 15 eV that we have previously measured (Ajello et al., 2019, https://doi.org/10.1029/2018ja026308). We find the CB total emission cross section at 15 eV to be 7.7 × 10−17 cm2.
“…This suggests that the flight spectrum includes contributions from cascade as well as from direct excitation (Eastes, 2000). Direct excitation is the dominant source of emission from the ~1 mm emitting region of the lamp where cascade effects would be negligible (Ajello et al, 2020).…”
The Global-scale Observations of the Limb and Disk (GOLD) is a National Aeronautics and Space Administration mission of opportunity designed to study how the Earth's ionosphere-thermosphere system responds to geomagnetic storms, solar radiation, and upward propagating atmospheric tides and waves. GOLD employs an instrument with two identical ultraviolet spectrographs that make observations of the Earth's thermosphere and ionosphere from a commercial communications satellite owned and operated by Société Européenne des Satellites (SES) and located in geostationary orbit at 47.5°west longitude (near the mouth of the Amazon River). They make images of atomic oxygen 135.6 nm and N 2 Lyman-Birge-Hopfield (LBH) 137-162 nm radiances of the entire disk that is observable from geostationary orbit and on the near-equatorial limb. They also observe occultations of stars to measure molecular oxygen column densities on the limb. Here, we provide an overview of the instrument and compare its prelaunch and early flight measurement performance. Direct comparison of LBH spectra of an electron lamp taken before launch with spectra on orbit provides evidence that both cascade and direct excitation are important sources of thermospheric LBH emission.
Plain Language Summary The Global-scale Observations of the Limb and Disk (GOLD) is aNational Aeronautics and Space Administration mission of opportunity designed to study how the Earth's ionosphere-thermosphere system responds to geomagnetic storms, solar radiation, and upward propagating tides on time scales as short as 30 min. GOLD employs two identical ultraviolet spectrographs that make observations of the Earth's thermosphere and ionosphere from a commercial communications satellite owned and operated by SES and located in geostationary orbit at 47.5°west longitude (near the mouth of the Amazon River). They make images of atomic oxygen 135.6 nm and N 2 LBH radiances of the entire disk that is observable from geostationary orbit and on the near-equatorial limb. They also observe occultations of stars to measure molecular oxygen column densities on the limb. Here we describe the GOLD instrument including its optical system and detector. Its performance was characterized in the lab before launch. We compare measurements of laboratory sources made then to observations of the thermosphere after launch and find good agreement.
As energetic electrons, protons, and photons are deposited into the high-latitude upper atmosphere, their deposited energy begins cascades of energy and interactions that excite and ionize atmospheric oxygen and nitrogen species. This molecular and atomic ionization and dissociation processes result in emissions in the visible, ultraviolet, and extreme-ultraviolet spectra called the aurora. Being able to understand the Earth's aurora provides great insight into physical mechanisms behind the coupling among the magnetosphere, ionosphere, and thermosphere (MIT), and the interactions of this coupled MIT system with the solar wind. Simultaneous global observations of the aurora over the high-latitude region achieved in the past with space-based instruments have proved essential to these efforts. Examples of these instruments include far ultraviolet (FUV) imagers on board spacecraft with highly elliptical near-polar orbits such as the NASA IMAGE and POLAR satellites (Burch et al., 2001;Germany et al., 1998). However, since the deactivation of POLAR in 2008 and loss of contact with IMAGE in 2005, our global observing capabilities of aurora have since been lost. As a result, our space-based coverage of the polar Abstract Far ultraviolet (FUV) imaging of the aurora from space provides great insight into the dynamic coupling of the atmosphere, ionosphere, and magnetosphere on global scales. To gain a quantitative understanding of these coupling processes, the global distribution of auroral energy flux is required, but the inversion of FUV emission to derive precipitating auroral particles' energy flux is not straightforward. Furthermore, the spatial coverage of FUV imaging from Low Earth Orbit (LEO) altitudes is often insufficient to achieve global mapping of this important parameter. This study seeks to fill these gaps left by the current geospace observing system using a combination of data assimilation and machine learning techniques. Specifically, this paper presents a new data-driven modeling approach to create instantaneous, global assimilative mappings of auroral electron total energy flux from Lyman-Birge-Hopfield (LBH) emission data from the Defense Meteorological System Program (DMSP) Special Sensor Ultraviolet Spectrographic Imager (SSUSI). We take a two-step approach; the creation of assimilative maps of LBH emission using optimal interpolation, followed by the conversion to energy flux using a neural network model trained with conjunction observations of in-situ auroral particles and LBH emission from the DMSP Special Sensor J and SSUSI instruments. The paper demonstrates the feasibility of this approach with a model prototype built with DMSP data from 17 February 2014 to 23 February 2014. This study serves as a blueprint for a future comprehensive data-driven model of auroral energy flux that is complementary to traditional inversion techniques to take advantage of FUV imaging from LEO platforms for global assimilative mapping of auroral energy flux.Plain Language Summary When energetic protons and electrons...
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