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1. Martian atmospheric disturbances from orbital images and surface pressure at Jezero Crater, Mars, during Martian Year 36

Author

Sánchez-Lavega, A., Larsen, E., del Río-Gaztelurrrutia, T., Hernández-Bernal, J., Ordóñez-Etxebarría, I., Hueso, R., Tanguy, B., Lemmon, M., Juarez, M. de la Torre, Martínez, G. M., Munguira, A., Rodríguez-Manfredi, J. A., Harri, A. -M., Pla-García, J., Toledo, D., and Newman, C.

Subjects
Astrophysics - Earth and Planetary Astrophysics
Abstract

We present a study of atmospheric disturbances at Jezero Crater, Mars, using ground-based measurements of surface pressure by the Perseverance rover in combination with orbital images from the Mars Express and Mars Reconnaissance Orbiter missions. The study starts at Ls $\sim$ 13.3{\deg} in MY36 (March 6th, 2021) and extends up to Ls $\sim$ 30.3{\deg} in MY37 (February 28th, 2023). We focus on the characterization of the major atmospheric phenomena at synoptic and planetary-scales. These are the thermal tides (measured up to the sixth component), long-period pressure oscillations (periods > 1 sol), the Aphelion Cloud Belt, and the occasional development of regional dust storms over Jezero. We present the seasonal evolution of the amplitudes and phases of the thermal tides and their relation with the atmospheric dust content (optical depth). Three regional dust storms and one polar storm extending over Jezero produced an increase in the diurnal and semidiurnal amplitudes but resulted in inverse responses in their phases. We show that the primary regular wave activity is due to baroclinic disturbances with periods of 2-4 sols and amplitudes $\sim$ 1-15 Pa increasing with dust content, in good agreement with theoretical predictions by model calculations. The spacecraft images show a number of arc-shaped, spiral and irregular cyclonic vortices, traced by dust and clouds at the edge of the North Polar Cap, that could be behind some of the pressure oscillations measured at Jezero.

Published
2025
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2. Mars 2020 Perseverance rover studies of the Martian atmosphere over Jezero from pressure measurements

Author

Sánchez-Lavega, A., del Rio-Gaztelurrutia, T., Hueso, R., Juárez, M. de la Torre, Martínez, G. M., Harri, A. -M., Genzer, M., Hieta, M., Polkko, J., Rodríguez-Manfredi, J. A., Lemmon, M. T., Pla-García, J., Toledo, D., Vicente-Retortillo, A., Viúdez-Moreiras, Daniel, Munguira, A., Tamppari, L. K., Newman, C., Gómez-Elvira, J., Guzewich, S., Bertrand, T., Apéstigue, V., Arruego, I., Wolff, M., Banfield, D., Jaakonaho, I., and Mäkinen, T.

Subjects
Astrophysics - Earth and Planetary Astrophysics
Abstract

The pressure sensors on Mars rover Perseverance measure the pressure field in the Jezero crater on regular hourly basis starting in sol 15 after landing. The present study extends up to sol 460 encompassing the range of solar longitudes from Ls 13{\deg} - 241{\deg} (Martian Year (MY) 36). The data show the changing daily pressure cycle, the sol-to-sol seasonal evolution of the mean pressure field driven by the CO2 sublimation and deposition cycle at the poles, the characterization of up to six components of the atmospheric tides and their relationship to dust content in the atmosphere. They also show the presence of wave disturbances with periods 2-5 sols, exploring their baroclinic nature, short period oscillations (mainly at night-time) in the range 8-24 minutes that we interpret as internal gravity waves, transient pressure drops with duration 1-150 s produced by vortices, and rapid turbulent fluctuations. We also analyze the effects on pressure measurements produced by a regional dust storm over Jezero at Ls 155{\deg}.

Published
2024
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3. Denoising Atmospheric Temperature Measurements Taken by the Mars Science Laboratory on the Martian Surface

Author

Zurita-Zurita, S., Escribano, Francisco J., Sáez-Landete, J., and Rodríguez-Manfredi, J. A.

Subjects
Electrical Engineering and Systems Science - Signal Processing, Astrophysics - Earth and Planetary Astrophysics, Computer Science - Information Retrieval, Physics - Data Analysis, Statistics and Probability
Abstract

In the present article we analyze data from two temperature sensors of the Mars Science Laboratory, which has been active in Mars since August 2012. Temperature measurements received from the rover are noisy and must be processed and validated before being delivered to the scientific community. Currently, a simple Moving Average (MA) filter is used to perform signal denoising. The application of this basic method relies on the assumption that the noise is stationary and statistically independent from the underlying structure of the signal, an arguable assumption in this kind of harsh environment. In this paper, we analyze the application of two alternative methods to process the temperature sensor measurements: the Discrete Wavelet Transform (DWT) and the Hilbert-Huang Transform (HHT). We consider two different datasets, one belonging to the current Martian measurement campaigns, and the other to the Thermal Vacuum Tests. The processing of these datasets allows to separate the random noise from the interference created by other systems. The experiments show that the MA filter may provide useful results under given circumstances. However, the proposed methods allow a better fitting for all the realistic scenarios, while providing the possibility to identify and analyze other interesting signal features and artifacts that could be later studied and classified. The large amount of data to be processed makes computational efficiency an important requirement in this mission. Considering the computational cost and the filtering performance, we propose the method based on DWT as more suitable for this application., Comment: 10 pages, 7 figures, accepted for publication at IEEE Transactions on Instrumentation and Measurement

Published
2020
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4. In situ recording of Mars soundscape

Author

Maurice, S., Chide, B., Murdoch, N., Lorenz, R. D., Mimoun, D., Wiens, R. C., Stott, A., Jacob, X., Bertrand, T., Montmessin, F., Lanza, N. L., Alvarez-Llamas, C., Angel, S. M., Aung, M., Balaram, J., Beyssac, O., Cousin, A., Delory, G., Forni, O., Fouchet, T., Gasnault, O., Grip, H., Hecht, M., Hoffman, J., Laserna, J., Lasue, J., Maki, J., McClean, J., Meslin, P.-Y., Le Mouélic, S., Munguira, A., Newman, C. E., Rodríguez Manfredi, J. A., Moros, J., Ollila, A., Pilleri, P., Schröder, S., de la Torre Juárez, M., Tzanetos, T., Stack, K. M., Farley, K., and Williford, K.

Published
2022
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5. Author Correction: In situ recording of Mars soundscape

Author

Maurice, S., Chide, B., Murdoch, N., Lorenz, R. D., Mimoun, D., Wiens, R. C., Stott, A., Jacob, X., Bertrand, T., Montmessin, F., Lanza, N. L., Alvarez-Llamas, C., Angel, S. M., Aung, M., Balaram, J., Beyssac, O., Cousin, A., Delory, G., Forni, O., Fouchet, T., Gasnault, O., Grip, H., Hecht, M., Hoffman, J., Laserna, J., Lasue, J., Maki, J., McClean, J., Meslin, P.-Y., Le Mouélic, S., Munguira, A., Newman, C. E., Rodríguez Manfredi, J. A., Moros, J., Ollila, A., Pilleri, P., Schröder, S., de la Torre Juárez, M., Tzanetos, T., Stack, K. M., Farley, K., and Williford, K.

Published
2022
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6. One Martian Year of Near‐Surface Temperatures at Jezero From MEDA Measurements on Mars2020/Perseverance.

Author

Munguira, A., Hueso, R., Sánchez‐Lavega, A., Toledo, D., de la Torre Juárez, M., Vicente‐Retortillo, A., Martínez, G. M., Bertrand, T., del Rio‐Gaztelurrutia, T., Sebastián, E., Lemmon, M., Pla‐García, J., and Rodríguez‐Manfredi, J. A.

Subjects
CONVECTIVE boundary layer (Meteorology), MARTIAN surface, ATMOSPHERIC temperature, CLIMATE change models, ATMOSPHERIC models
Abstract

Measurements of ground and near surface atmospheric temperatures at Jezero obtained during 700 sols by the Mars Environmental Dynamics Analyzer (MEDA) characterize the thermal behavior of the near surface Martian atmosphere during a full Martian Year. The seasonal evolution of MEDA measurements is compared with predictions from the Mars Climate Database and the solar irradiance at the surface. Thermal tides observed in the daily cycle of temperatures follow a seasonal cycle with additional variations greater than 2 K on time‐scales of tens of sols. We also observe sol‐to‐sol variations of about 1 K in mean daily air temperatures in autumn and winter with periodicities of 4–7 sols that might be related to baroclinic disturbances that are frequent in those seasons at high latitudes. We examine the evolution of the vertical thermal gradient and temperature fluctuations without finding a seasonal response to irradiance and dust load. We find that the convective boundary layer becomes isothermal and collapses 1 hr before sunset except during northern hemisphere winter, when the collapse occurs closer to sunset, implying a longer duration of the daytime convective instability. Around this period, the rover was located in the delta front in a location of complex topography where we observed stronger thermal gradients and intense daytime air temperature fluctuations. We also find in this place a nighttime event of gravity waves on near‐surface air temperatures, with amplitudes of 2 K and periods of 10 min. These waves possibly propagate downward through a near isothermal stable layer. Plain Language Summary: The Perseverance rover on Mars is carrying a meteorological station that among other measurements obtains air temperatures at three heights near the surface as well as ground temperatures. We analyze seasonal and local changes in temperatures measured over one Martian year (687 Earth days) in which Perseverance moved several kilometers across Jezero crater, comparing in situ observations with the output from a Global Climate Model of the atmosphere of Mars. Our results show that the diurnal cycle of temperatures is modulated by the solar irradiance on the surface, the amount of dust in the atmosphere, local dynamics and large‐scale weather systems. The temperature difference between the ground and the atmosphere greatly determines the meteorology in the lower atmosphere. Neither this temperature difference, nor temperature fluctuations, which during daytime are a proxy of atmospheric convection driven by the heating of the surface, show seasonal variations in line with the seasonal solar irradiance or dust load. Instead, the rover path toward a more complex topography led to the highest surface‐to‐air temperature difference during the northern hemisphere winter, despite the solar irradiance being minimum at that time. Close to this complex topography, the meteorological station recorded oscillations in near‐surface temperature related to gravity waves. Key Points: Seasonal variations in irradiance at Mars' surface drive observed daily mean near‐surface air temperatures with some differences from modelsThermal tides and long‐period traveling waves present a clear seasonal cycle with autumn and winter seasons more prone to variabilityAir temperatures underwent non‐seasonal changes near Jezero's delta, with strong daytime convection and nighttime gravity waves [ABSTRACT FROM AUTHOR]

Published
2024
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7. Cyborg Systems as Platforms for Computer-Vision Algorithm-Development for Astrobiology

Author

McGuire, Patrick C., Rodriguez-Manfredi, J. A., Sebastian-Martinez, E., Gomez-Elvira, J., Diaz-Martinez, E., Ormo, J., Neuffer, K., Giaquinta, A., Camps-Martinez, F., Lepinette-Malvitte, A., Perez-Mercader, J., Ritter, H., Oesker, M., Ontrup, J., and Walter, J.

Subjects
Computer Science - Computer Vision and Pattern Recognition, Astrophysics, Computer Science - Artificial Intelligence, I.4.0, I.4.6, I.4.8, I.4.9, I.5.4, I.5.5, J.2, I.2.5, I.2.10
Abstract

Employing the allegorical imagery from the film "The Matrix", we motivate and discuss our `Cyborg Astrobiologist' research program. In this research program, we are using a wearable computer and video camcorder in order to test and train a computer-vision system to be a field-geologist and field-astrobiologist., Comment: Updated biblio info

Published
2004

8. Nocturnal Turbulence at Jezero Crater as Determined From MEDA Measurements and Modeling

Author

Pla‐García, Jorge, primary, Munguira, A., additional, Rafkin, S., additional, Newman, C., additional, Bertrand, T., additional, Martínez, G., additional, Hueso, R., additional, Sánchez‐Lavega, A., additional, del Río Gaztelurrutia, T., additional, Stott, A., additional, Murdoch, N., additional, de la Torre Juárez, M., additional, Lemmon, M., additional, Chide, B., additional, Viúdez‐Moreiras, D., additional, Savijarvi, H., additional, Richardson, M., additional, Marín, M., additional, Sebastian, E., additional, Lepinette‐Malvitte, A., additional, Mora, L., additional, and Rodríguez‐Manfredi, J. A., additional

Published
2023
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9. The Diverse Meteorology of Jezero Crater over the First 250 Sols of Perseverance on Mars

Author

Universidad de Sevilla. Departamento de Electrónica y Electromagnetismo, Ministerio de Economía y Competitividad (MINECO). España, Ministerio de Ciencia, Innovación y Universidades (MICINN). España, Ministerio de Ciencia e Innovación (MICIN). España, Spanish State Research Agency (AEI), Gobierno Vasco, European Research Council (ERC), National Aeronautics and Space Administration, Rodríguez Manfredi, J. A., Torre Juárez, M. de la, Sánchez Lavega, A., Hueso, R., Martínez, G., Lemmon, M. T., Newman, C. E., Munguira, A., Hieta, M., Tamppari, L. K., Espejo Meana, Servando Carlos, Zurita, S., Universidad de Sevilla. Departamento de Electrónica y Electromagnetismo, Ministerio de Economía y Competitividad (MINECO). España, Ministerio de Ciencia, Innovación y Universidades (MICINN). España, Ministerio de Ciencia e Innovación (MICIN). España, Spanish State Research Agency (AEI), Gobierno Vasco, European Research Council (ERC), National Aeronautics and Space Administration, Rodríguez Manfredi, J. A., Torre Juárez, M. de la, Sánchez Lavega, A., Hueso, R., Martínez, G., Lemmon, M. T., Newman, C. E., Munguira, A., Hieta, M., Tamppari, L. K., Espejo Meana, Servando Carlos, and Zurita, S.

Abstract

NASA’s Perseverance rover’s Mars Environmental Dynamics Analyzer is collecting data at Jezero crater, characterizing the physical processes in the lowest layer of the Martian atmosphere. Here we present measurements from the instrument’s first 250 sols of operation, revealing a spatially and temporally variable meteorology at Jezero. We find that temperature measurements at four heights capture the response of the atmospheric surface layer to multiple phenomena. We observe the transition from a stable night-time thermal inversion to a daytime, highly turbulent convective regime, with large vertical thermal gradients. Measurement of multiple daily optical depths suggests aerosol concentrations are higher in the morning than in the afternoon. Measured wind patterns are driven mainly by local topography, with a small contribution from regional winds. Daily and seasonal variability of relative humidity shows a complex hydrologic cycle. These observations suggest that changes in some local surface properties, such as surface albedo and thermal inertia, play an influential role. On a larger scale, surface pressure measurements show typical signatures of gravity waves and baroclinic eddies in a part of the seasonal cycle previously characterized as low wave activity. These observations, both combined and simultaneous, unveil the diversity of processes driving change on today’s Martian surface at Jezero crater.

Published
2023

10. Dust Lifting Through Surface Albedo Changes at Jezero Crater, Mars

Author

Vicente‐Retortillo, A., primary, Martínez, G.M., additional, Lemmon, M. T., additional, Hueso, R., additional, Johnson, J. R, additional, Sullivan, R., additional, Newman, C. E., additional, Sebastián, E., additional, Toledo, D., additional, Apéstigue, V., additional, Arruego, I., additional, Munguira, A., additional, Sánchez‐Lavega, A., additional, Murdoch, N., additional, Gillier, M., additional, Stott, A., additional, Mora‐Sotomayor, L., additional, Bertrand, T., additional, Tamppari, L. K., additional, Juárez, M. de la Torre, additional, and Rodríguez‐Manfredi, J.‐A., additional

Published
2023
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11. Convective Vortices and Dust Devils Detected and Characterized by Mars 2020

Author

Hueso, R., primary, Newman, C. E., additional, del Río‐Gaztelurrutia, T., additional, Munguira, A., additional, Sánchez‐Lavega, A., additional, Toledo, D., additional, Apéstigue, V., additional, Arruego, I., additional, Vicente‐Retortillo, A., additional, Martínez, G., additional, Lemmon, M., additional, Lorenz, R., additional, Richardson, M., additional, Viudez‐Moreiras, D., additional, de la Torre‐Juarez, M., additional, Rodríguez‐Manfredi, J. A., additional, Tamppari, L. K., additional, Murdoch, N., additional, Navarro‐López, S., additional, Gómez‐Elvira, J., additional, Baker, M., additional, Pla‐García, J., additional, Harri, A. M., additional, Hieta, M., additional, Genzer, M., additional, Polkko, J., additional, Jaakonaho, I., additional, Makinen, T., additional, Stott, A., additional, Mimoun, D., additional, Chide, B., additional, Sebastian, E., additional, Banfield, D., additional, and Lepinette‐Malvite, A., additional

Published
2023
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12. Surface Energy Budget, Albedo, and Thermal Inertia at Jezero Crater, Mars, as Observed From the Mars 2020 MEDA Instrument

Author

Martínez, G. M., primary, Sebastián, E., additional, Vicente‐Retortillo, A., additional, Smith, M. D., additional, Johnson, J. R., additional, Fischer, E., additional, Savijärvi, H., additional, Toledo, D., additional, Hueso, R., additional, Mora‐Sotomayor, L., additional, Gillespie, H., additional, Munguira, A., additional, Sánchez‐Lavega, A., additional, Lemmon, M. T., additional, Gómez, F., additional, Polkko, J., additional, Mandon, L., additional, Apéstigue, V., additional, Arruego, I., additional, Ramos, M., additional, Conrad, P., additional, Newman, C. E., additional, Torre‐Juarez, M. de la, additional, Jordan, F., additional, Tamppari, L. K., additional, McConnochie, T. H., additional, Harri, A.‐M., additional, Genzer, M., additional, Hieta, M., additional, Zorzano, M.‐P., additional, Siegler, M., additional, Prieto, O., additional, Molina, A., additional, and Rodríguez‐Manfredi, J. A., additional

Published
2023
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13. Near Surface Atmospheric Temperatures at Jezero from Mars 2020 MEDA measurements

Author

Munguira, A., primary, Hueso, R., additional, Sánchez‐Lavega, A., additional, Torre‐Juarez, M. de la, additional, Martínez, G., additional, Newman, C. E., additional, Sebastian, E., additional, Lepinette, A., additional, Vicente‐Retortillo, A., additional, Chide, B., additional, Lemmon, M. T., additional, Bertrand, T., additional, Lorenz, R., additional, Banfield, D., additional, Gómez‐Elvira, J., additional, Martín‐Soler, J., additional, Navarro, S., additional, Pla‐García, J., additional, Rodríguez‐Manfredi, J. A., additional, Romeral, J., additional, Smith, M. D., additional, and Torres, J., additional

Published
2023
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14. Mars 2020 Perseverance Rover Studies of the Martian Atmosphere Over Jezero From Pressure Measurements

Author

Sánchez‐Lavega, A., primary, del Rio‐Gaztelurrutia, T., additional, Hueso, R., additional, Juárez, M. de la Torre, additional, Martínez, G. M., additional, Harri, A.‐M., additional, Genzer, M., additional, Hieta, M., additional, Polkko, J., additional, Rodríguez‐Manfredi, J. A., additional, Lemmon, M. T., additional, Pla‐García, J., additional, Toledo, D., additional, Vicente‐Retortillo, A., additional, Viúdez‐Moreiras, D., additional, Munguira, A., additional, Tamppari, L. K., additional, Newman, C., additional, Gómez‐Elvira, J., additional, Guzewich, S., additional, Bertrand, T., additional, Apéstigue, V., additional, Arruego, I., additional, Wolff, M., additional, Banfield, D., additional, Jaakonaho, I., additional, and Mäkinen, T., additional

Published
2023
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15. Winds at the Mars 2020 Landing Site: 1. Near‐Surface Wind Patterns at Jezero Crater

Author

Viúdez‐Moreiras, D., primary, Lemmon, M., additional, Newman, C. E., additional, Guzewich, S., additional, Mischna, M., additional, Gómez‐Elvira, J., additional, Herkenhoff, K., additional, Sánchez‐Lavega, A., additional, de la Torre, M., additional, Rodríguez‐Manfredi, J. A., additional, Lorenz, R. D., additional, Pla‐García, J., additional, Hueso, R., additional, Richardson, M., additional, Tamppari, L., additional, Smith, M., additional, Apéstigue, V., additional, Toledo, D., additional, and Bell, J., additional

Published
2022
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16. Winds at the Mars 2020 Landing Site. 2. Wind Variability and Turbulence

Author

Viúdez‐Moreiras, D., primary, de la Torre, M., additional, Gómez‐Elvira, J., additional, Lorenz, R. D., additional, Apéstigue, V., additional, Guzewich, S., additional, Mischna, M., additional, Sullivan, R., additional, Herkenhoff, K., additional, Toledo, D., additional, Lemmon, M., additional, Smith, M., additional, Newman, C. E., additional, Sánchez‐Lavega, A., additional, Rodríguez‐Manfredi, J. A., additional, Richardson, M., additional, Hueso, R., additional, Harri, A. M., additional, Tamppari, L., additional, Arruego, I., additional, and Bell, J., additional

Published
2022
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18. Diurnal Cycle of Rapid Air Temperature Fluctuations at Jezero Crater: Probability Distributions, Exponential Tails, Scaling, and Intermittency.

Author

de la Torre Juárez, M., Chavez, A., Tamppari, L. K., Munguira, A., Martínez, G., Hueso, R., Chide, B., Murdoch, N., Stott, A. E., Navarro, S., Sánchez‐Lavega, A., Orton, G. S., Viúdez‐Moreiras, D., Banfield, D. J., and Rodríguez‐Manfredi, J. A.

Subjects
ATMOSPHERIC temperature, DISTRIBUTION (Probability theory), MARTIAN atmosphere, MARTIAN surface, STOCHASTIC processes
Abstract

We study the diurnal cycle of rapid thermal fluctuations observed by the Mars Environmental Dynamics Analyzer, onboard the Perseverance rover at Jezero Crater, as a function of local time and season. In this context, rapid refers to periods between 15 min and half a second. Some insight is also provided into wind fluctuations that are the base for most of the existing theories on turbulent flows. The results expand the observations from previous Mars missions, namely Viking, Mars Pathfinder, and Phoenix, and they add to our knowledge of near‐surface fluctuations on Mars. (a) Probability distribution functions of the fluctuations are determined and found to have exponential tails. This means that models that represent the interaction within the environment and with the surface as a stochastic forcing need to account for the sudden events responsible for the exponential tails. (b) Power density spectra are calculated and show several dynamical regimes with different slopes associated to forcing, an intermediate regime, and a higher frequency regime. All change with time of the day. The results imply that the fastest regime is not a universal scenario for the temperature fluctuations near the surface. (c) The scale dependence of the fluctuations confirms the existence of intermittent outbursts associated to the slower fluctuations, possibly associated to the larger scale structures, and explains why the spectral density slopes do not follow Kolmogorov's law. Understanding the role of larger scale structures would help refine scaling theories of the near‐surface Martian atmosphere and its interactions with the surface. Plain Language Summary: The Martian atmosphere is mostly driven by solar radiative forcing that also controls how it interacts with the surface. Atmospheric phenomena respond within seconds to years, but models can only resolve limited ranges of these time scales. This work explores how temperature fluctuates at time scales faster than what models typically resolve, and how this variability affects phenomena at the time scales that they resolve. The statistical properties of rapid environmental changes, or fluctuations, caused by solar forcing help us understand how the lowest atmosphere and surface evolve and interact. Theories that have been tested on Earth predicting how energy transfers or dissipates between the fast and slow dynamical regimes are explored here searching for rules that relate both regimes on another world. This work finds that fluctuations of air temperature and horizontal winds near the Martian surface do not follow probability distributions typical of normal random processes. The energy transfer rate is not consistent at scales faster than 10 s with a unique, or universal, rule relating fast to slow fluctuations. Finally, it suggests that this lack of universality is caused by intermittent disruptions through sudden large coherent structures, like convective vortices and waves, that influence how temperature dissipates. Key Points: Probability Distribution functions for temperature fluctuations at Jezero Crater on the time scale of seconds have exponential tailsPower density spectra of temperature fluctuations find at least two dynamical regimes that evolve differently with time of the daySudden outbursts, likely associated to coherent structures, disrupt intermittently the rate of temperature dissipation to the smaller scales [ABSTRACT FROM AUTHOR]

Published
2023
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19. REMS: The Environmental Sensor Suite for the Mars Science Laboratory Rover

Author

Gómez-Elvira, J., Armiens, C., Castañer, L., Domínguez, M., Genzer, M., Gómez, F., Haberle, R., Harri, A.-M., Jiménez, V., Kahanpää, H., Kowalski, L., Lepinette, A., Martín, J., Martínez-Frías, J., McEwan, I., Mora, L., Moreno, J., Navarro, S., de Pablo, M. A., Peinado, V., Peña, A., Polkko, J., Ramos, M., Renno, N. O., Ricart, J., Richardson, M., Rodríguez-Manfredi, J., Romeral, J., Sebastián, E., Serrano, J., de la Torre Juárez, M., Torres, J., Torrero, F., Urquí, R., Vázquez, L., Velasco, T., Verdasca, J., Zorzano, M.-P., and Martín-Torres, J.

Published
2012
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20. REMS: The Environmental Sensor Suite for the Mars Science Laboratory Rover

Author

Gómez-Elvira, J., primary, Armiens, C., additional, Castañer, L., additional, Domínguez, M., additional, Genzer, M., additional, Gómez, F., additional, Haberle, R., additional, Harri, A.-M., additional, Jiménez, V., additional, Kahanpää, H., additional, Kowalski, L., additional, Lepinette, A., additional, Martín, J., additional, Martínez-Frías, J., additional, McEwan, I., additional, Mora, L., additional, Moreno, J., additional, Navarro, S., additional, de Pablo, M. A., additional, Peinado, V., additional, Peña, A., additional, Polkko, J., additional, Ramos, M., additional, Renno, N. O., additional, Ricart, J., additional, Richardson, M., additional, Rodríguez-Manfredi, J., additional, Romeral, J., additional, Sebastián, E., additional, Serrano, J., additional, de la Torre Juárez, M., additional, Torres, J., additional, Torrero, F., additional, Urquí, R., additional, Vázquez, L., additional, Velasco, T., additional, Verdasca, J., additional, Zorzano, M.-P., additional, and Martín-Torres, J., additional

Published
2012
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21. Meteorological Predictions for Mars 2020 Perseverance Rover Landing Site at Jezero Crater

Author

Pla García, Jorge, Rafkin, S. C. R., Martínez, G. M., Retortillo, Vicente Á., Newman, C. E., Rodríguez Manfredi, J. A., Gómez, F., Molina, A., Viúdez Moreiras, D., Harri, Ari Matti, and Spanish Ministry of Economy and Competiveness (MINECO), ESP2016-79612-C3-1-R. S.R.

Subjects
Atmosphere, Mars 2020, Mars, Perseverance
Abstract

The Mars Regional Atmospheric Modeling System (MRAMS) and a nested simulation of the Mars Weather Research and Forecasting model (MarsWRF) are used to predict the local meteorological conditions at the Mars 2020 Perseverance rover landing site inside Jezero crater (Mars). These predictions are complemented with the COmplutense and MIchigan MArs Radiative Transfer model (COMIMART) and with the local Single Column Model (SCM) to further refine predictions of radiative forcing and the water cycle respectively. The primary objective is to facilitate interpretation of the meteorological measurements to be obtained by the Mars Environmental Dynamics Analyzer (MEDA) aboard the rover, but also to provide predictions of the meteorological phenomena and seasonal changes that might impact operations, from both a risk perspective and from the perspective of being better prepared to make certain measurements. A full diurnal cycle at four different seasons (L-s 0 degrees, 90 degrees, 180 degrees, and 270 degrees) is investigated. Air and ground temperatures, pressure, wind speed and direction, surface radiative fluxes and moisture data are modeled. The good agreement between observations and modeling in prior works [Pla-Garcia et al. in Icarus 280:103-113, 2016; Newman et al. in Icarus 291:203-231, 2017; Vicente-Retortillo et al. in Sci. Rep. 8(1):1-8, 2018; Savijarvi et al. in Icarus, 2020] provides confidence in utilizing these models results to predict the meteorological environment at Mars 2020 Perseverance rover landing site inside Jezero crater. The data returned by MEDA will determine the extent to which this confidence was justified. With funding from the Spanish government through the "María de Maeztu Unit of Excellence" accreditation (MDM-2017-0737); This research has been partially supported by the Spanish Ministry of Economy and Competiveness (MINECO), under project ESP2016-79612-C3-1-R. S.R. supported this work on his own time in the absence of funding. Germán Martinez wishes to acknowledge USRA contract number 1638782. MTJ’s work was carried out at the Jet Propulsion Laboratory/California Institute of Technology. MTJ and CEN acknowledge support from NASA’s STMD and GCD directorates through the M2020 project. A.M. is funded by the Project “MarsFirstWater”, European Research Council, Consolidator Grant no. 818602. In addition, we wish to express our gratitude to the MEDA instrument team members to supporting this investigation Peer review

Published
2020

22. Preliminary interpretation of the REMS pressure data from the first 100 sols of the MSL mission

Author

Haberle, R. M., Gómez-Elvira, J., de la Torre Juárez, M., Harri, A.-M., Hollingsworth, J. L., Kahanpää, H., Kahre, M. A., Lemmon, M., Martín-Torres, F. J., Mischna, M., Moores, J. E., Newman, C., Rafkin, S. C. R., Rennó, N., Richardson, M. I., Rodríguez-Manfredi, J. A., Vasavada, A. R., Zorzano-Mier, M.-P. and REMS/MSL Science Teams, and DLR Collaborator (MSL Science Team), Reitz G.

Subjects
Curiosity rover, Mars, MSL mission, Gale Crater
Published
2014

23. Zoé

Author

Cuesta Crespo, L., Ruiz Zelmanovitch, B., Vaquerizo Gallego, J. A., Montesinos Comino, B., Cuevas Manrubia, S., Gómez Gómez, F., Martín Torres, J., Martín Soler, J., Gómez Elvira Rodríguez, J., Cernicharo, J., Mas Hesse, J. M., Parro García, V., Amils, R., and Rodríguez Manfredi, J. A.

Subjects
Centro de Astrobiología, Vida en otros mundos, Astrobiology, Planetas y atmósfera
Abstract

Depósito Legal: NIPO: 078-11-003-6 NIPO en línea: 078-11-004-1 La pregunta “¿Hay vida en otros lugares del Universo?” tenía, hasta hace poco, únicamente implicaciones filosóficas. Pero, actualmente se está empezando a abordar desde otros campos de la Ciencia. Precisamente, la Astrobiología aglutina todos los esfuerzos dirigidos a encontrar su respuesta, tratando de entender cómo son los procesos por los que una nube de polvo interestelar llega a transformarse en un sistema planetario en el que alguno de sus cuerpos se desarrolla de tal forma que aparecen microorganismos que lo pueblan y evolucionan. El reto de la Astrobiología es fabuloso y, embarcarse en esa misión, es realmente una aventura: la “aventura de la vida”. “La divulgación es una obligación que tiene la comunidad científica y tecnológica con la sociedad”: ésta es una frase que, desgraciadamente, todavía no ha calado lo suficiente en nuestra comunidad. Quizás el problema esté en nuestra formación: nadie nos ha enseñado a hacerlo y muchos no sabemos cómo se hace, pero nuestra obligación es intentarlo, porque es realmente una obligación para con la sociedad. No cabe duda de que la divulgación en Astrobiología es muy atractiva para el gran público por el interés del tema que aborda y porque su multidisciplinariedad atrae a “curiosos” de muchas áreas. Desde su creación, de la mano de Juan Pérez-Mercader, el Centro de Astrobiología (CSIC-INTA) ha considerado la divulgación como una de sus actividades básicas: esta revista es un intento más en esa dirección. Con ella, no sólo se quiere informar a la sociedad de sus actividades más relevantes, sino que pretende ser un “imán” para atraer hacia la ciencia y la tecnología a todo aquel que sienta curiosidad y quiera satisfacerla. D. Jaime Denís Zambrana – Director General del Instituto Nacional de Técnica Aeroespacial (INTA) Ministerio de Defensa- Secretaría General Técnica. Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y Consejo Superior de Investigaciones Científicas Peerreview

Published
2011

24. Molecular preservation in halite- and perchlorate-rich hypersaline subsurface deposits in the Salar Grande basin (Atacama Desert, Chile): Implications for the search for molecular biomarkers on Mars

Author

Fernández-Remolar, D. C., primary, Chong-Díaz, G., additional, Ruíz-Bermejo, M., additional, Harir, M., additional, Schmitt-Kopplin, P., additional, Tziotis, D., additional, Gómez-Ortíz, D., additional, García-Villadangos, M., additional, Martín-Redondo, M. P., additional, Gómez, F., additional, Rodríguez-Manfredi, J. A., additional, Moreno-Paz, M., additional, De Diego-Castilla, G., additional, Echeverría, A., additional, Urtuvia, V. N., additional, Blanco, Y., additional, Rivas, L., additional, Izawa, M. R. M., additional, Banerjee, N. R., additional, Demergasso, C., additional, and Parro, V., additional

Published
2013
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25. Diurnal Cycle of Rapid Air Temperature Fluctuations at Jezero Crater: Probability Distributions, Exponential Tails, Scaling, and Intermittency

Author

Torre Juárez, M., Chavez, A., Tamppari, L. K., Munguira, A., Martínez, G., Hueso, R., Chide, B., Murdoch, N., Stott, A. E., Navarro, S., Sánchez‐Lavega, A., Orton, G. S., Viúdez‐Moreiras, D., Banfield, D. J., and Rodríguez‐Manfredi, J. A.

Abstract

We study the diurnal cycle of rapid thermal fluctuations observed by the Mars Environmental Dynamics Analyzer, onboard the Perseverance rover at Jezero Crater, as a function of local time and season. In this context, rapid refers to periods between 15 min and half a second. Some insight is also provided into wind fluctuations that are the base for most of the existing theories on turbulent flows. The results expand the observations from previous Mars missions, namely Viking, Mars Pathfinder, and Phoenix, and they add to our knowledge of near‐surface fluctuations on Mars. (a) Probability distribution functions of the fluctuations are determined and found to have exponential tails. This means that models that represent the interaction within the environment and with the surface as a stochastic forcing need to account for the sudden events responsible for the exponential tails. (b) Power density spectra are calculated and show several dynamical regimes with different slopes associated to forcing, an intermediate regime, and a higher frequency regime. All change with time of the day. The results imply that the fastest regime is not a universal scenario for the temperature fluctuations near the surface. (c) The scale dependence of the fluctuations confirms the existence of intermittent outbursts associated to the slower fluctuations, possibly associated to the larger scale structures, and explains why the spectral density slopes do not follow Kolmogorov's law. Understanding the role of larger scale structures would help refine scaling theories of the near‐surface Martian atmosphere and its interactions with the surface. The Martian atmosphere is mostly driven by solar radiative forcing that also controls how it interacts with the surface. Atmospheric phenomena respond within seconds to years, but models can only resolve limited ranges of these time scales. This work explores how temperature fluctuates at time scales faster than what models typically resolve, and how this variability affects phenomena at the time scales that they resolve. The statistical properties of rapid environmental changes, or fluctuations, caused by solar forcing help us understand how the lowest atmosphere and surface evolve and interact. Theories that have been tested on Earth predicting how energy transfers or dissipates between the fast and slow dynamical regimes are explored here searching for rules that relate both regimes on another world. This work finds that fluctuations of air temperature and horizontal winds near the Martian surface do not follow probability distributions typical of normal random processes. The energy transfer rate is not consistent at scales faster than 10 s with a unique, or universal, rule relating fast to slow fluctuations. Finally, it suggests that this lack of universality is caused by intermittent disruptions through sudden large coherent structures, like convective vortices and waves, that influence how temperature dissipates. Probability Distribution functions for temperature fluctuations at Jezero Crater on the time scale of seconds have exponential tailsPower density spectra of temperature fluctuations find at least two dynamical regimes that evolve differently with time of the daySudden outbursts, likely associated to coherent structures, disrupt intermittently the rate of temperature dissipation to the smaller scales Probability Distribution functions for temperature fluctuations at Jezero Crater on the time scale of seconds have exponential tails Power density spectra of temperature fluctuations find at least two dynamical regimes that evolve differently with time of the day Sudden outbursts, likely associated to coherent structures, disrupt intermittently the rate of temperature dissipation to the smaller scales

Published
2023
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26. Astrobiological Field Campaign to a Volcanosedimentary Mars Analogue Methane Producing Subsurface Protected Ecosystem: Imuruk Lake (Alaska)

Author

Gómez, F., primary, Prieto-Ballesteros, O., additional, Fernández-Remolar, D., additional, Rodríguez-Manfredi, J. A., additional, Fernández-Sampedro, M., additional, Postigo Cacho, M., additional, Torres Redondo, J., additional, Rodríguez, N., additional, Gómez-Elvira, J., additional, and Amils, R., additional

Published
2011
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27. Initial results from the InSight mission on Mars

Author

Sharon Kedar, Don Banfield, Scott M. McLennan, Nicholas Schmerr, Justin N. Maki, Gareth S. Collins, John Clinton, Anna Mittelholz, Paul Morgan, Mélanie Drilleau, Sabine Stanley, Chloé Michaut, Nicholas A Teanby, Daniele Antonangeli, Jeroen Tromp, W. Bruce Banerdt, James B. Garvin, Mark A. Wieczorek, Jerzy Grygorczuk, Suzanne E. Smrekar, Catherine L. Johnson, Aymeric Spiga, Peter Chi, Brigitte Knapmeyer-Endrun, Raphaël F. Garcia, Claire E. Newman, Seiichi Nagihara, Matthias Grott, W. Thomas Pike, Philippe Lognonné, Véronique Dehant, Ana-Catalina Plesa, Matthew Fillingim, Domenico Giardini, Taichi Kawamura, Mark T. Lemmon, Antoine Mocquet, Naomi Murdoch, Ebru Bozdag, David Mimoun, Ludovic Margerin, Matthew P. Golombek, Jessica C. E. Irving, Troy L. Hudson, Sami W. Asmar, Günter Kargl, Martin Knapmeyer, Mark P. Panning, Francis Nimmo, Scott D. King, John A. Grant, Sebastien Rodriguez, Martin van Driel, Nicholas H. Warner, Nils Mueller, José Antonio Rodríguez-Manfredi, Christopher T. Russell, Caroline Beghein, Clément Perrin, Ulrich R. Christensen, William M. Folkner, Renee Weber, Neil Bowles, Ingrid Daubar, Simon Stähler, Tilman Spohn, Eléanore Stutzmann, Ralph D. Lorenz, Matthew A. Siegler, Institut Supérieur de l'Aéronautique et de l'Espace - ISAE-SUPAERO (FRANCE), Jet Propulsion Laboratory (JPL), California Institute of Technology (CALTECH)-NASA, Cornell Center for Astrophysics and Planetary Science (CCAPS), Cornell University, Institute of Geophysics [ETH Zürich], Department of Earth Sciences [ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich), Department of Earth, Ocean and Atmospheric Sciences [Vancouver] (EOAS), University of British Columbia (UBC), Département de géophysique spatiale et planétaire (DGSP (UMR_7096)), Université Paris Diderot - Paris 7 (UPD7)-IPG PARIS-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), DLR Institut für Planetenforschung, Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Department of Atmospheric, Oceanic and Planetary Physics [Oxford] (AOPP), University of Oxford [Oxford], Department of Geosciences [Princeton], Princeton University, Max Planck Institute for Solar System Research (MPS), Max-Planck-Gesellschaft, Swiss Seismological Service [ETH Zurich] (SED), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich)-Department of Earth Sciences [ETH Zürich] (D-ERDW), Department of Earth Science and Engineering [Imperial College London], Imperial College London, Department of Earth, Environmental and Planetary Sciences [Providence], Brown University, Royal Observatory of Belgium [Brussels], Space Sciences Laboratory [Berkeley] (SSL), University of California [Berkeley], University of California-University of California, Département Electronique, Optronique et Signal (DEOS), Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Institute of Remote Sensing and Geographic Information System (IRSGIS), School of Earth and Space Sciences [Beijing], Peking University [Beijing]-Peking University [Beijing], Austrian Academy of Sciences (OeAW), Graphics and Vision Research Laboratory (Graphics Lab), University of Otago [Dunedin, Nouvelle-Zélande], Deutsches Zentrum für Luft- und Raumfahrt (DLR), Space Science Institute [Boulder] (SSI), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Department of Geosciences, Stony Brook University [SUNY] (SBU), State University of New York (SUNY)-State University of New York (SUNY), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), AstraZeneca, Aeolis Research, Department of Earth and Planetary Sciences [Santa Cruz], University of California [Santa Cruz] (UCSC), Department of Geological Sciences, University of Florida [Gainesville], Centro de Astrobiologia [Madrid] (CAB), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Spain] (CSIC), Department of Earth, Planetary and Space Sciences [Los Angeles] (EPSS), University of California [Los Angeles] (UCLA), The Open University [Milton Keynes] (OU), Morton K. Blaustein Department of Earth and Planetary Sciences [Baltimore], Johns Hopkins University (JHU), School of Earth Sciences [Bristol], University of Bristol [Bristol], Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich), University of Southern California (USC), Joseph Louis LAGRANGE (LAGRANGE), Université Nice Sophia Antipolis (... - 2019) (UNS), COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Observatoire de la Côte d'Azur, COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS), Cornell University [New York], Department of Earth Sciences [Swiss Federal Institute of Technology - ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), Department of Earth, Ocean and Atmospheric Sciences [Vancouver] (UBC EOAS), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)-Department of Earth Sciences [Swiss Federal Institute of Technology - ETH Zürich] (D-ERDW), Royal Observatory of Belgium [Brussels] (ROB), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Southwest Research Institute [Boulder] (SwRI), Astrophysique Interprétation Modélisation (AIM (UMR_7158 / UMR_E_9005 / UM_112)), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), University of California, Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), NASA-California Institute of Technology (CALTECH), Institut de recherche pour le développement [IRD] : UR206-Muséum national d'Histoire naturelle (MNHN)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Muséum national d'Histoire naturelle (MNHN)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Centre National de la Recherche Scientifique (CNRS), University of Oxford, Max-Planck-Institut für Sonnensystemforschung = Max Planck Institute for Solar System Research (MPS), University of California [Berkeley] (UC Berkeley), University of California (UC)-University of California (UC), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), University of California [Santa Cruz] (UC Santa Cruz), Astrophysique Interprétation Modélisation (AIM (UMR7158 / UMR_E_9005 / UM_112)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), University of California (UC), Unidad de Excelencia Científica María de Maeztu Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, MDM-2017-0737, Tromp, J. [0000-0002-2742-8299], Rodríguez, S. [0000-0003-1219-0641], Lognonné, P. [0000-0002-1014-920X], Perrin, C. [0000-0002-7200-5682], Murdoch, N. [0000-0002-9701-4075], Knapmeyer, M. [0000-0003-0319-2514], Rodríguez Manfredi, J. A. [0000-0003-0461-9815], Spiga, A. [0000-0002-6776-6268], Panning, M. P. [0000-0002-2041-3190], García, R. [0000-0003-1460-6663], Johnson, C. [0000-0001-6084-0149], Stutzmann, E. [0000-0002-4348-7475], Knapmeyer-Endrun, B. [0000-0003-3309-6785], Schmerr, N. [0000-0002-3256-1262], Irving, J. C. E. [0000-0002-0866-8246], Morgan, P. [0000-0001-8714-4178], Mueller, N. [0000-0001-9229-8921], Pike, W. [0000-0002-7660-6231], Kawamura, T. [0000-0001-5246-5561], Clinton, J. [0000-0001-8626-2703], Agence Nationale de la Recherche (ANR), Swiss National Science Foundation (SNSF), Agence Nationale de la Recherche (ANR), ANR-10LABX-0023 ANR-11-IDEX-0005-0, Swiss National Science Foundation (SNSF- ANR project), 157133, ETH Research grant, ETH-06 17-02, Lunar and Planetary Institute, 2250, UCL - SST/ELI/ELIC - Earth & Climate, Science and Technology Facilities Council (STFC), and Science & Technology Facilities Council

Subjects
Seismometer, 010504 meteorology & atmospheric sciences, [PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], [SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], Mars, 010502 geochemistry & geophysics, 01 natural sciences, Atmosphere, [SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology, Impact crater, Autre, Planet, Inner planets, InSight Mars Geophysik, Meteorology & Atmospheric Sciences, Seismology, ComputingMilieux_MISCELLANEOUS, 0105 earth and related environmental sciences, Atmospheric dynamics, Geomorphology, Moment magnitude scale, Mars InSight, Geomagnetism, Mars Exploration Program, Geophysics, [SDU]Sciences of the Universe [physics], 13. Climate action, Intraplate earthquake, General Earth and Planetary Sciences, Timekeeping on Mars, [SDU.OTHER]Sciences of the Universe [physics]/Other, InSight mission, Geology
Abstract

Banerdt, William B. et al., NASA’s InSight (Interior exploration using Seismic Investigations, Geodesy and Heat Transport) mission landed in Elysium Planitia on Mars on 26 November 2018. It aims to determine the interior structure, composition and thermal state of Mars, as well as constrain present-day seismicity and impact cratering rates. Such information is key to understanding the differentiation and subsequent thermal evolution of Mars, and thus the forces that shape the planet’s surface geology and volatile processes. Here we report an overview of the first ten months of geophysical observations by InSight. As of 30 September 2019, 174 seismic events have been recorded by the lander’s seismometer, including over 20 events of moment magnitude M = 3–4. The detections thus far are consistent with tectonic origins, with no impact-induced seismicity yet observed, and indicate a seismically active planet. An assessment of these detections suggests that the frequency of global seismic events below approximately M = 3 is similar to that of terrestrial intraplate seismic activity, but there are fewer larger quakes; no quakes exceeding M = 4 have been observed. The lander’s other instruments—two cameras, atmospheric pressure, temperature and wind sensors, a magnetometer and a radiometer—have yielded much more than the intended supporting data for seismometer noise characterization: magnetic field measurements indicate a local magnetic field that is ten-times stronger than orbital estimates and meteorological measurements reveal a more dynamic atmosphere than expected, hosting baroclinic and gravity waves and convective vortices. With the mission due to last for an entire Martian year or longer, these results will be built on by further measurements by the InSight lander., With funding from the Spanish government through the "María de Maeztu Unit of Excellence" accreditation (MDM-2017-0737)

Published
2020
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28. Radiometric and angular calibration tests for the MEDA-TIRS radiometer onboard NASA's Mars 2020 mission

Author

José Antonio Rodríguez Manfredi, Miguel Ramos, Frank Haenschke, Eduardo Sebastián, Ricardo Ferrandiz, Maite Fernandez, German Martinez, Fernández Sampedro, M. [0000-0003-1932-7591], Rodríguez Manfredi, J. A. [0000-0003-0461-9815], Instituto Nacional de Tecnica Aeroespacial (INTA), Unidad de Excelencia Científica María de Maeztu Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, USRA, 1638782, Unidad de Excelencia Científica María de Maeztu Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, MDM-2017-0737, Agencia Estatal de Investigación (AEI), and Ministerio de Economía y Competitividad (MINECO)

Subjects
Systematic error, Radiometric and angular calibration, Calibration (statistics), Mars, 02 engineering and technology, 01 natural sciences, chemistry.chemical_compound, 0202 electrical engineering, electronic engineering, information engineering, Electrical and Electronic Engineering, Instrumentation, Calibration accuracy, Remote sensing, Martian, Thermal infrared, Radiometer, Spacecraft instrumentation, IR radiometer, Applied Mathematics, 020208 electrical & electronic engineering, 010401 analytical chemistry, Astrophysics::Instrumentation and Methods for Astrophysics, Mars Exploration Program, Condensed Matter Physics, 0104 chemical sciences, chemistry, Physics::Space Physics, Environmental science, Radiometric dating, Astrophysics::Earth and Planetary Astrophysics, MEDA
Abstract

This article describes a comprehensive testing method for the radiometric and angular calibration of the Thermal InfraRed Sensor (TIRS) onboard NASA's Mars 2020 mission. First, details of the TIRS opto-mechanical design, construction aspects of the IR detectors, and an update of the mathematical model used for the calculation of sensor internal IR fluxes are provided. Then, a set of sequential calibration tests to identify the radiometer model parameters are defined. The test setups are described, highlighting their limitations and restrictions based on differences between simulated and actual Martian environmental conditions. Finally, the uncertainty sources and potential systematic errors associated with the calibration tests are quantified and compared with the radiometer scientific requirements established by the Mars 2020 science team., With funding from the Spanish government through the "María de Maeztu Unit of Excellence" accreditation (MDM-2017-0737)

Published
2020

29. The atmosphere of Mars as observed by InSight

Author

Justin N. Maki, A. Jacob, Stephen R. Lewis, Nicholas A Teanby, Mercedes Marin-Jimenez, Anna Mittelholz, Constantinos Charalambous, Sara Navarro, M. M. Baker, Mark T. Lemmon, Tristram Warren, Javier Gómez-Elvira, Alexander E. Stott, Matthew P. Golombek, Antoine Lucas, Jorge Pla-Garcia, J. Torres, Eric Beucler, Balthasar Kenda, Aymeric Spiga, Rudolf Widmer-Schnidrig, Philippe Lognonné, Veronique Ansan, V. Peinado, Özgür Karatekin, William T. Pike, Nils Mueller, Savas Ceylan, K. Hurst, Daniel Viúdez-Moreiras, Christopher T. Russell, Antonio Molina, Sebastien Rodriguez, Clément Perrin, Naomi Murdoch, David Mimoun, Claire E. Newman, Ralph D. Lorenz, L. Martire, Luis Mora-Sotomayor, Simon Stähler, Tilman Spohn, Lucie Rolland, Stephen Sackett, Ingrid Daubar, Raphaël F. Garcia, W. Bruce Banerdt, Catherine L. Johnson, Domenico Giardini, Brian Carcich, Don Banfield, Suzanne E. Smrekar, John Clinton, François Forget, Ehouarn Millour, Taichi Kawamura, J. A. Rodríguez-Manfredi, Bart Van Hove, A. Lepinette, Anni Määttänen, J. B. McClean, Cornell Center for Astrophysics and Planetary Science (CCAPS), Cornell University, Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris), Aeolis Research, Space Science Institute [Boulder] (SSI), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Centro de Astrobiologia [Madrid] (CAB), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Spain] (CSIC), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS), Institut Universitaire de France (IUF), Ministère de l'Education nationale, de l’Enseignement supérieur et de la Recherche (M.E.N.E.S.R.), Royal Observatory of Belgium [Brussels], School of Earth Sciences [Bristol], University of Bristol [Bristol], Jet Propulsion Laboratory (JPL), California Institute of Technology (CALTECH)-NASA, DLR Institut für Planetenforschung, Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR), Department of Electrical and Electronic Engineering [London] (DEEE), Imperial College London, Department of Earth, Ocean and Atmospheric Sciences [Vancouver] (EOAS), University of British Columbia (UBC), IMPEC - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Sorbonne Université (SU), School of Physical Sciences [Milton Keynes], The Open University [Milton Keynes] (OU), Swiss Seismological Service [ETH Zurich] (SED), Institute of Geophysics [ETH Zürich], Department of Earth Sciences [ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich)-Department of Earth Sciences [ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (ETH Zürich), Department of Physics [Oxford], University of Oxford [Oxford], Department of Earth, Environmental and Planetary Sciences [Providence], Brown University, Géoazur (GEOAZUR 7329), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Université Côte d'Azur (UCA), Universität Stuttgart [Stuttgart], Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), Morton K. Blaustein Department of Earth and Planetary Sciences [Baltimore], Johns Hopkins University (JHU), Center for Earth and Planetary Studies [Washington] (CEPS), Smithsonian National Air and Space Museum, Smithsonian Institution-Smithsonian Institution, Department of Earth, Planetary and Space Sciences [Los Angeles] (EPSS), University of California [Los Angeles] (UCLA), University of California-University of California, Département Electronique, Optronique et Signal (DEOS), Cornell University [New York], École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), Centre National de la Recherche Scientifique (CNRS)-Université de La Réunion (UR)-Université Paris Diderot - Paris 7 (UPD7)-IPG PARIS-Institut national des sciences de l'Univers (INSU - CNRS), Royal Observatory of Belgium [Brussels] (ROB), NASA-California Institute of Technology (CALTECH), Department of Earth, Ocean and Atmospheric Sciences [Vancouver] (UBC EOAS), PLANETO - LATMOS, Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Faculty of Science, Technology, Engineering and Mathematics [Milton Keynes], The Open University [Milton Keynes] (OU)-The Open University [Milton Keynes] (OU), Department of Earth Sciences [Swiss Federal Institute of Technology - ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)-Department of Earth Sciences [Swiss Federal Institute of Technology - ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud]), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut Supérieur de l'Aéronautique et de l'Espace - ISAE-SUPAERO (FRANCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA), Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), University of Oxford, University of California (UC)-University of California (UC), ANR-14-CE36-0012,SEISMARS,Seismology on Mars(2014), ANR-19-CE31-0008,MAGIS,MArs Geophysical InSight(2019), Unidad de Excelencia Científica María de Maeztu Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, MDM-2017-0737, Määttänen, A. [0000-0002-7326-8492], Martire, L. [0000-0002-9402-6150], Rodríguez Manfredi, J. A. [0000-0003-0461-9815], Lognonné, P. [0000-0002-1014-920X], Rodríguez, S. [0000-0003-1219-0641], Spiga, A. [0000-0002-6776-6268], Perrin, C. [0000-0002-7200-5682], Molina, A. [0000-0002-5038-2022], García, R. [0000-0003-1460-6663], Murdoch, N. [0000-0002-9701-4075], Lorenz, R. [0000-0001-8528-4644], Mittelholz, A. [0000-0002-5603-7334], Kawamura, T. [0000-0001-5246-5561], Widmer Schnidrig, R. [0000-0001-9698-2739], McClean, J. [0000-0002-7863-0120], Mueller, N. [0000-0001-9229-8921], Lewis, S. [0000-0001-7237-6494], Teanby, N. [0000-0003-3108-5775], Warren, T. [0000-0003-3877-0046], Milliour, E. [0000-0003-4808-9203], Lemmon, M. [0000-0002-4504-5136], Clinton, J. [0000-0001-8626-2703], Ceylan, S. [0000-0002-6552-6850], Banfield, D. [0000-0003-2664-0164], Agence Nationale de la Recherche (ANR), and Consejo Superior de Investigaciones Científicas [Spain] (CSIC)-Instituto Nacional de Técnica Aeroespacial (INTA)

Subjects
Martian, 010504 meteorology & atmospheric sciences, Atmosphere, Mars, Mars Exploration Program, Atmosphere of Mars, 010502 geochemistry & geophysics, Mars Atmosphere, 01 natural sciences, Wind speed, Astrobiology, Autre, 13. Climate action, Dust storm, [SDU]Sciences of the Universe [physics], General Earth and Planetary Sciences, Environmental science, Aeolian processes, [SDU.OTHER]Sciences of the Universe [physics]/Other, Meteorologie, InSight mission, Dust devil, 0105 earth and related environmental sciences, InSight
Abstract

Banfield, D. et al., The atmosphere of Mars is thin, although rich in dust aerosols, and covers a dry surface. As such, Mars provides an opportunity to expand our knowledge of atmospheres beyond that attainable from the atmosphere of the Earth. The InSight (Interior Exploration using Seismic Investigations, Geodesy and Heat Transport) lander is measuring Mars’s atmosphere with unprecedented continuity, accuracy and sampling frequency. Here we show that InSight unveils new atmospheric phenomena at Mars, especially in the higher-frequency range, and extends our understanding of Mars’s meteorology at all scales. InSight is uniquely sensitive to large-scale and regional weather and obtained detailed in situ coverage of a regional dust storm on Mars. Images have enabled high-altitude wind speeds to be measured and revealed airglow—faint emissions produced by photochemical reactions—in the middle atmosphere. InSight observations show a paradox of aeolian science on Mars: despite having the largest recorded Martian vortex activity and dust-devil tracks close to the lander, no visible dust devils have been seen. Meteorological measurements have produced a catalogue of atmospheric gravity waves, which included bores (soliton-like waves). From these measurements, we have discovered Martian infrasound and unexpected similarities between atmospheric turbulence on Earth and Mars. We suggest that the observations of Mars’s atmosphere by InSight will be key for prediction capabilities and future exploration., With funding from the Spanish government through the "María de Maeztu Unit of Excellence" accreditation (MDM-2017-0737); Centro de Desarrollo Tecnológico e Industrial (CDTI), Ministerio de Economía y Competitividad and the Instituto Nacional de Técnica Aeroespacial (INTA).

Published
2020
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