Ashwin Braude
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View article: Optical constants of laboratory-generated analogs of the red chromophores in Jupiter’s atmosphere
Optical constants of laboratory-generated analogs of the red chromophores in Jupiter’s atmosphere Open
The identity of the coloring agent, or chromophore, in Jupiter’s atmosphere that causes the planet’s striking red clouds and storms is an area of active research. Despite being studied for more than 50 years across multiple observational m…
View article: Sulfur allotropes and sulfur hydrides on the Venus cloud chemistry
Sulfur allotropes and sulfur hydrides on the Venus cloud chemistry Open
. IntroductionThe cloud layer of Venus between 47 and 70 km is home to a vivid sulfur chemistry and microphysics, with SO2 as the major gas species and condensed phase composed of H2SO4 and H2O. This cloud layer has been extensively observ…
View article: Joint Observations of Mesospheric Aerosols on Mars from MAVEN/IUVS and MRO/MCS
Joint Observations of Mesospheric Aerosols on Mars from MAVEN/IUVS and MRO/MCS Open
JOINT OBSERVATIONS OF MESOSPHERIC AEROSOLS ON MARS FROM MAVEN/IUVS AND MRO/MCS Ashwin S. Braude1, Marek Slipski1, Sumedha Gupta2, Nicholas M. Schneider2, Armin Kleinböhl1, Franck Montmessin3, Sonal Jain2, Roger V. Yelle4 and Justin Deighan…
View article: Modelling the Effect of the Sulphur Cycle on Episodic Climactic Changes on Early Mars
Modelling the Effect of the Sulphur Cycle on Episodic Climactic Changes on Early Mars Open
Introduction: Although Mars is now a cold, dry planet, the geological record shows that, early in its history, Mars not only went through episodes of wet-dry cycling [1], in which Mars could maintain liquid water on its surface for s…
View article: Seasonal, Latitudinal, and Longitudinal Trends in Nighttime Ozone Vertical Structure on Mars From MAVEN/IUVS Stellar Occultations
Seasonal, Latitudinal, and Longitudinal Trends in Nighttime Ozone Vertical Structure on Mars From MAVEN/IUVS Stellar Occultations Open
Stellar occultation measurements conducted by the Mars Atmosphere and Volatile and EvolutioN/Imaging UltraViolet Spectrograph instrument were able to make vertically resolved measurements of ozone density in the middle atmosphere of Mars t…
View article: Pyrocast: a Machine Learning Pipeline to Forecast Pyrocumulonimbus (PyroCb) Clouds
Pyrocast: a Machine Learning Pipeline to Forecast Pyrocumulonimbus (PyroCb) Clouds Open
Pyrocumulonimbus (pyroCb) clouds are storm clouds generated by extreme wildfires. PyroCbs are associated with unpredictable, and therefore dangerous, wildfire spread. They can also inject smoke particles and trace gases into the upper trop…
View article: Identifying the Causes of Pyrocumulonimbus (PyroCb)
Identifying the Causes of Pyrocumulonimbus (PyroCb) Open
A first causal discovery analysis from observational data of pyroCb (storm clouds generated from extreme wildfires) is presented. Invariant Causal Prediction was used to develop tools to understand the causal drivers of pyroCb formation. T…
View article: Measurements of HDO and the D/H ratio in the Martian atmosphere from ACS MIR
Measurements of HDO and the D/H ratio in the Martian atmosphere from ACS MIR Open
<p><strong>Abstract</strong></p> <p>Measuring vertical variations in the deuterium to hydrogen ratio with altitude is essential in understanding the processes that lead to the escape of water vapour from the M…
View article: Modeling the Martian HDO cycle with a Global Climate Model during the &#8220;dusty&#8221; season
Modeling the Martian HDO cycle with a Global Climate Model during the “dusty” season Open
<p><strong>Abstract</strong></p> <p>The D/H ratio measured in the Martian atmosphere gives an estimation of the planet’s water escape rate. We present here a global circulation model including the wa…
View article: Upper limits on volcanic gases in the Martian atmosphere from the ACS MIR instrument
Upper limits on volcanic gases in the Martian atmosphere from the ACS MIR instrument Open
<p><strong>Abstract</strong></p> <p>The geological record provides convincing evidence for very recent volcanic activity on Mars (e.g. Horvath et al. 2021, Icarus 365, 114499). In this talk we present the resu…
View article: A Four-Year Search of Methane on Mars with ACS onboard ExoMars TGO
A Four-Year Search of Methane on Mars with ACS onboard ExoMars TGO Open
<p><strong>Summary</strong></p> <p>The mid-infrared channel of the Atmospheric Chemistry Suite (ACS) [1] onboard ESA’s Trace Gas Orbiter (TGO) has performed a sensitive search of methane in the Marti…
View article: Monitoring of Martian water ice clouds over one Martian Year with TGO/ACS-MIR
Monitoring of Martian water ice clouds over one Martian Year with TGO/ACS-MIR Open
<p>The Atmospheric Chemistry Suite (ACS) MIR channel onboard the ESA-Roscosmos Trace Gas Orbiter (TGO) (Korablev et al., 2018, 2019) probes the Martian atmosphere in the 2.3 – 4.2 µm spectral range using t…
View article: Isotopic Composition of CO<sub>2</sub> in the Atmosphere of Mars: Fractionation by Diffusive Separation Observed by the ExoMars Trace Gas Orbiter
Isotopic Composition of CO<sub>2</sub> in the Atmosphere of Mars: Fractionation by Diffusive Separation Observed by the ExoMars Trace Gas Orbiter Open
Isotopic ratios in atmospheric CO 2 are shaped by various processes throughout Mars' history, and can help understand what the atmosphere of early Mars was like to sustain liquid water on its surface. In this study, we monitor the O and C …
View article: No detection of SO2, H2S, or OCS in the atmosphere of Mars from the first two Martian years of observations from TGO/ACS
No detection of SO2, H2S, or OCS in the atmosphere of Mars from the first two Martian years of observations from TGO/ACS Open
The detection of sulphur species in the Martian atmosphere would be a strong indicator of volcanic outgassing from the surface of Mars. We wish to establish the presence of SO2, H2S, or OCS in the Martian atmosphere or determine upper limi…
View article: No detection of SO<sub>2</sub>, H<sub>2</sub>S, or OCS in the atmosphere of Mars from the first two Martian years of observations from TGO/ACS
No detection of SO<sub>2</sub>, H<sub>2</sub>S, or OCS in the atmosphere of Mars from the first two Martian years of observations from TGO/ACS Open
Context. The detection of sulphur species in the Martian atmosphere would be a strong indicator of volcanic outgassing from the surface of Mars. Aims. We wish to establish the presence of SO 2 , H 2 S, or OCS in the Martian atmosphere or d…
View article: The RISOTTO radiative transfer and retrieval pipeline for the analysis of occultation spectra
The RISOTTO radiative transfer and retrieval pipeline for the analysis of occultation spectra Open
International audience
View article: Comparison of the HDO cycle in the LMD Mars GCM with ACS/TGO observations
Comparison of the HDO cycle in the LMD Mars GCM with ACS/TGO observations Open
HDO and the D/H ratio are important in order to understand Mars past and present climate, in particular regarding the evolution through ages of the Martian water cycle. We present simulations of the HDO cycle with the LMD Mars GCM and…
View article: A stringent upper limit of 20 pptv for methane on Mars and constraints on its dispersion outside Gale crater
A stringent upper limit of 20 pptv for methane on Mars and constraints on its dispersion outside Gale crater Open
Context. Reports on the detection of methane in the Martian atmosphere have motivated numerous studies aiming to confirm or explain its presence on a planet where it might imply a biogenic or more likely a geophysical origin. Aims. Our int…
View article: Upper limits for phosphine (PH<sub>3</sub>) in the atmosphere of Mars
Upper limits for phosphine (PH<sub>3</sub>) in the atmosphere of Mars Open
Phosphine (PH 3 ) is proposed to be a possible biomarker in planetary atmospheres and has been claimed to have been observed in the atmosphere of Venus, sparking interest in the habitability of Venus’s atmosphere. Observations of another b…
View article: Color and aerosol changes in Jupiter after a North Temperate Belt disturbance
Color and aerosol changes in Jupiter after a North Temperate Belt disturbance Open
View article: Colour and tropospheric cloud structure of Jupiter from MUSE/VLT: Retrieving a universal chromophore
Colour and tropospheric cloud structure of Jupiter from MUSE/VLT: Retrieving a universal chromophore Open
View article: Latitudinal variation in the abundance of methane (CH4) above the clouds in Neptune's atmosphere from VLT/MUSE Narrow Field Mode Observations
Latitudinal variation in the abundance of methane (CH4) above the clouds in Neptune's atmosphere from VLT/MUSE Narrow Field Mode Observations Open
View article: Colour and cloud structure in the atmospheres of the giant planets
Colour and cloud structure in the atmospheres of the giant planets Open
For decades, the origin of colour-carrying compounds ('chromophores') in Jupiter and Saturn's atmospheres has remained elusive. Changes in colour are often associated with cyclical meteorological events ('upheavals') on Jupiter. Multiple d…
View article: Analysis of gaseous ammonia (NH3) absorption in the visible spectrum of Jupiter
Analysis of gaseous ammonia (NH3) absorption in the visible spectrum of Jupiter Open