Search Results - "Trompet, L."

Explanation for the Increase in High-Altitude Water on Mars Observed by NOMAD During the 2018 Global Dust Storm by Neary, L., Daerden, F., Aoki, S., Whiteway, J., Clancy, R. T., Smith, M., Viscardy, S., Erwin, J.T., Thomas, I. R., Villanueva, G., Liuzzi, G., Crismani, M., Wolff, M., Lewis, S. R., Holmes, J. A., Patel, M. R., Giuranna, M., Depiesse, C., Piccialli, A., Robert, S., Trompet, L., Willame, Y., Ristic, B., Vandaele, A. C.

“…The Nadir and Occultation for MArs Discovery (NOMAD) instrument on board ExoMars Trace Gas Orbiter measured a large increase in water vapor at altitudes in the…”
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Strong Localized Pumping of Water Vapor to High Altitudes on Mars During the Perihelion Season by Brines, A., López‐Valverde, M. A., Funke, B., González‐Galindo, F., Aoki, S., Villanueva, G. L., Holmes, J. A., Belyaev, D. A., Liuzzi, G., Thomas, I. R., Erwin, J. T., Grabowski, U., Forget, F., Lopez‐Moreno, J. J., Rodriguez‐Gomez, J., Daerden, F., Trompet, L., Ristic, B., Patel, M. R., Bellucci, G., Vandaele, A. C.

“…Here we present water vapor vertical profiles observed with the ExoMars Trace Gas Orbiter/Nadir and Occultation for MArs Discovery instrument during the…”
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SOIR/VEx observations of water vapor at the terminator in the Venus mesosphere by Chamberlain, S., Mahieux, A., Robert, S., Piccialli, A., Trompet, L., Vandaele, A.C., Wilquet, V.

“…The Solar Occultation in the InfraRed (SOIR) instrument onboard Venus Express sounded the Venus mesosphere and lower thermosphere using solar occultation…”
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Water Vapor Vertical Profiles on Mars in Dust Storms Observed by TGO/NOMAD by Aoki, S, Vandaele, A C, Daerden, F, Villanueva, G L, Liuzzi, G, Thomas, I R, Erwin, J T, Trompet, L, Robert, S, Neary, L, Viscardy, S, Clancy, R T, Smith, M D, Lopez-Valverde, M A, Hill, B, Ristic, B, Patel, M R, Bellucci, G, Lopez-Moreno, J J

“…It has been suggested that dust storms efficiently transport water vapor from the near‐surface to the middle atmosphere on Mars. Knowledge of the water vapor…”
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Impact of gradients at the martian terminator on the retrieval of ozone from SPICAM/MEx by Piccialli, A., Vandaele, A.C., Trompet, L., Neary, L., Viscardy, S., Erwin, J.T., Määttänen, A., Daerden, F., Willame, Y., Robert, S., Aoki, S., Wilquet, V., Lefèvre, F., Montmessin, F.

“…Rapid variations of pressure, temperature and illumination at the day–night terminator have the potential to cause asymmetries in the abundance distribution of…”
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Global Vertical Distribution of Water Vapor on Mars: Results From 3.5 Years of ExoMars‐TGO/NOMAD Science Operations by Aoki, S., Vandaele, A. C., Daerden, F., Villanueva, G. L., Liuzzi, G., Clancy, R. T., Lopez‐Valverde, M. A., Brines, A., Thomas, I. R., Trompet, L., Erwin, J. T., Neary, L., Robert, S., Piccialli, A., Holmes, J. A., Patel, M. R., Yoshida, N., Whiteway, J., Smith, M. D., Ristic, B., Bellucci, G., Lopez‐Moreno, J. J., Fedorova, A. A.

“…We present water vapor vertical distributions on Mars retrieved from 3.5 years of solar occultation measurements by Nadir and Occultation for Mars Discovery…”
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Explaining NOMAD D/H Observations by Cloud‐Induced Fractionation of Water Vapor on Mars by Daerden, F., Neary, L., Villanueva, G., Liuzzi, G., Aoki, S., Clancy, R. T., Whiteway, J. A., Sandor, B. J., Smith, M. D., Wolff, M. J., Pankine, A., Khayat, A., Novak, R., Cantor, B., Crismani, M., Mumma, M. J., Viscardy, S., Erwin, J., Depiesse, C., Mahieux, A., Piccialli, A., Robert, S., Trompet, L., Willame, Y., Neefs, E., Thomas, I. R., Ristic, B., Vandaele, A. C.

“…The vertical profiles of water vapor and its semi‐heavy hydrogen isotope HDO provided by instruments on ExoMars Trace Gas Orbiter constitute a unique new data…”
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A Global and Seasonal Perspective of Martian Water Vapor From ExoMars/NOMAD by Crismani, M. M. J., Villanueva, G. L., Liuzzi, G., Smith, M. D., Knutsen, E. W., Daerden, F., Neary, L., Mumma, M. J., Aoki, S., Trompet, L., Thomas, I. R., Ristic, B., Bellucci, G., Piccialli, A., Robert, S., Mahieux, A., Lopez Moreno, J.‐J., Sindoni, G., Giuranna, M., Patel, M. R., Vandaele, A. C.

“…Slightly less than a Martian Year of nominal science (March 2018–January 2020) with the ExoMars Trace Gas Orbiter has furthered the ongoing investigation of…”
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Martian Ozone Observed by TGO/NOMAD‐UVIS Solar Occultation: An Inter‐Comparison of Three Retrieval Methods by Piccialli, A., Vandaele, A. C., Willame, Y., Määttänen, A., Trompet, L., Erwin, J. T., Daerden, F., Neary, L., Aoki, S., Viscardy, S., Thomas, I. R., Depiesse, C., Ristic, B., Mason, J. P., Patel, M. R., Wolff, M. J., Khayat, A. S. J., Bellucci, G., Lopez‐Moreno, J.‐J.

“…The NOMAD‐UVIS instrument on board the ExoMars Trace Gas Orbiter has been investigating the Martian atmosphere with the occultation technique since April 2018…”
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Optical and radiometric models of the NOMAD instrument part II: the infrared channels - SO and LNO by Thomas, I R, Vandaele, A C, Robert, S, Neefs, E, Drummond, R, Daerden, F, Delanoye, S, Ristic, B, Berkenbosch, S, Clairquin, R, Maes, J, Bonnewijn, S, Depiesse, C, Mahieux, A, Trompet, L, Neary, L, Willame, Y, Wilque, V, Nevejans, D, Aballea, L, Moelans, W, De Vos, L, Lesschaeve, S, Van Vooren, N, Lopez-Moreno, J-J, Patel, M R, Bellucci, G

“…NOMAD is a suite of three spectrometers that will be launched in 2016 as part of the joint ESA-Roscosmos ExoMars Trace Gas Orbiter mission. The instrument…”
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Carbon monoxide observed in Venus’ atmosphere with SOIR/VEx by Vandaele, A.C., Mahieux, A., Chamberlain, S., Ristic, B., Robert, S., Thomas, I.R., Trompet, L., Wilquet, V., Bertaux, J.L.

“…•Carbon monoxide profiles observed by SOIR from 65 to 150km.•Above 105km, higher CO at Equator than at Poles, reverse below.•No long-term trend observed, but…”
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Contribution from SOIR/VEX to the updated Venus International Reference Atmosphere (VIRA) by Vandaele, A.C., Chamberlain, S., Mahieux, A., Ristic, B., Robert, S., Thomas, I., Trompet, L., Wilquet, V., Belyaev, D., Fedorova, A., Korablev, O., Bertaux, J.L.

“…•SOIR improves next generation VIRA by providing high-resolution vertical profiles.•The SOIR data set covers CO2, CO, HCl, HF, H20, SO2, aerosol and…”
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Carbon Dioxide Retrievals From NOMAD‐SO on ESA's ExoMars Trace Gas Orbiter and Temperature Profiles Retrievals With the Hydrostatic Equilibrium Equation: 1. Description of the Method by Trompet, L., Vandaele, A. C., Thomas, I., Aoki, S., Daerden, F., Erwin, J., Flimon, Z., Mahieux, A., Neary, L., Robert, S., Villanueva, G., Liuzzi, G., López‐Valverde, M. A., Brines, A., Bellucci, G., López‐Moreno, J. J., Patel, M. R.

“…The Solar Occultation (SO) channel of the Nadir and Occultation for Mars Discovery (NOMAD) instrument has been scanning the Martian atmosphere for almost…”
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Water Vapor Vertical Distribution on Mars During Perihelion Season of MY 34 and MY 35 With ExoMars‐TGO/NOMAD Observations by Brines, A., López‐Valverde, M. A., Stolzenbach, A., Modak, A., Funke, B., Galindo, F. G., Aoki, S., Villanueva, G. L., Liuzzi, G., Thomas, I. R., Erwin, J. T., Grabowski, U., Forget, F., Lopez‐Moreno, J. J., Rodriguez‐Gomez, J., Daerden, F., Trompet, L., Ristic, B., Patel, M. R., Bellucci, G., Vandaele, A. C.

“…The water vapor in the Martian atmosphere plays a significant role in the planet's climate, being crucial in most of the chemical and radiative transfer…”
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Description, accessibility and usage of SOIR/Venus Express atmospheric profiles of Venus distributed in VESPA (Virtual European Solar and Planetary Access) by Trompet, L., Geunes, Y., Ooms, T., Mahieux, A., Wilquet, V., Chamberlain, S., Robert, S., Thomas, I.R., Erard, S., Cecconi, B., Le Sidaner, P., Vandaele, A.C.

“…Venus Express SOIR profiles of pressure, temperature and number densities of different constituents of the mesosphere and lower thermosphere of Venus are the…”
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Carbon Dioxide Retrievals From NOMAD‐SO on ESA's ExoMars Trace Gas Orbiter and Temperature Profile Retrievals With the Hydrostatic Equilibrium Equation: 2. Temperature Variabilities in the Mesosphere at Mars Terminator by Trompet, L., Vandaele, A. C., Thomas, I., Aoki, S., Daerden, F., Erwin, J., Flimon, Z., Mahieux, A., Neary, L., Robert, S., Villanueva, G., Liuzzi, G., López‐Valverde, M. A., Brines, A., Bellucci, G., Lopez‐Moreno, J. J., Patel, M. R.

“…The Solar Occultation (SO) channel of the Nadir and Occultation for Mars Discovery (NOMAD) instrument scans the Martian atmosphere since 21 April 2018. In this…”
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Depletion of 13C in CO in the Atmosphere of Mars Suggested by ExoMars-TGO/NOMAD Observations by Aoki, S., Shiobara, K., Yoshida, N., Trompet, L., Yoshida, T., Terada, N., Nakagawa, H., Liuzzi, G., Vandaele, A. C., Thomas, I. R., Villanueva, G. L., Lopez-Valverde, M. A., Brines, A., Patel, M. R., Faggi, S., Daerden, F., Erwin, J. T., Ristic, B., Bellucci, G., Lopez-Moreno, J. J., Kurokawa, H., Ueno, Y.

“…The atmosphere of Mars is mainly composed by carbon dioxide (CO _2 ). It has been predicted that photodissociation of CO _2 depletes ^13 C in carbon monoxide…”
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Virtual European Solar & Planetary Access (VESPA): A Planetary Science Virtual Observatory Cornerstone by Erard, S., Cecconi, B., Le Sidaner, P., Chauvin, C., Rossi, A. P., Minin, M., Capria, T., Ivanovski, S., Schmitt, B., Génot, V., André, N., Marmo, C., Vandaele, A. C., Trompet, L., Scherf, M., Hueso, R., Määttänen, A., Carry, B., Achilleos, N., Soucek, J., Pisa, D., Benson, K., Fernique, P., Millour, E.

“…The Europlanet-2020 programme, which ended on Aug 31 st , 2019, included an activity called VESPA (Virtual European Solar and Planetary Access), which focused…”
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The SOIR/Venus Express species concentration and temperature database: CO2, CO, H2O, HDO, H35Cl, H37Cl, HF individual and mean profiles by Mahieux, A., Robert, S., Piccialli, A., Trompet, L., Vandaele, A.C.

“…This work is an update of the SOIR mean and individual profiles of CO2, CO, H2O, HDO, H35Cl, H37Cl, HF, and the temperature measured at the Venus terminator…”
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Update on SO2, detection of OCS, CS, CS2, and SO3, and upper limits of H2S and HOCl in the Venus mesosphere using SOIR on board Venus Express by Mahieux, A., Robert, S., Mills, F.P., Jessup, K.L., Trompet, L., Aoki, S., Piccialli, A., Peralta, J., Vandaele, A.C.

“…We report on the update of SO2 and first detections of SO3, CS, and CS2, and detection of OCS above the cloud deck using the SOIR instrument on-board Venus…”
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