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  • 1
    Online-Ressource
    Online-Ressource
    Cambridge :Cambridge University Press,
    Schlagwort(e): Mars (Planet)--Atmosphere. ; Electronic books.
    Beschreibung / Inhaltsverzeichnis: Humanity has long been fascinated by the planet Mars. What is the atmosphere like today and why did it change so dramatically over time? In this book students, researchers and non-specialists alike are guided through a detailed description of the atmosphere and climate of this most Earth-like of planetary neighbours.
    Materialart: Online-Ressource
    Seiten: 1 online resource (614 pages)
    Ausgabe: 1st ed.
    ISBN: 9781108180702
    Serie: Cambridge Planetary Science Series ; v.Series Number 18
    DDC: 551.5099923
    Sprache: Englisch
    Anmerkung: Cover -- Half-title -- Series information -- Title page -- Copyright information -- Dedication -- Table of contents -- List of contributors -- General Acknowledgments -- 1 Introduction -- References -- 2 Understanding Mars and Its Atmosphere -- 2.1 In the Beginning -- 2.2 1962-1972: A Decade of Change With the First Wave of Spacecraft Exploration -- 2.3 Viking: the Second Wave of Spacecraft Exploration of Mars -- 2.4 The Third Wave of Spacecraft Exploration of Mars -- 2.5 Mars Atmospheric Phenomena: Where Are We Now? -- 2.5.1 Early Mars -- 2.5.2 Middle Mars -- 2.5.3 Modern Mars: the Present Atmosphere -- 2.6 Basic Parameters and Nomenclature -- 2.6.1 Temperature -- 2.6.2 Clouds -- 2.6.3 Dust Storms and Mars Years -- 2.7 Summary -- ACKNOWLEDGMENTS -- References -- 3 History of Mars Atmosphere Observations -- 3.1 Introduction -- 3.2 Pre-Viking Observations -- 3.3 Viking and Post-Viking Years -- 3.3.1 Viking Orbiters -- 3.3.2 Viking Landers -- 3.3.3 Phobos 2 -- 3.3.4 Hubble Space Telescope -- 3.4 Ground-Based Spectroscopy -- 3.5 Orbiters -- 3.5.1 Mars Global Surveyor -- 3.5.2 Mars Odyssey -- 3.5.3 Mars Express -- 3.5.4 Mars Reconnaissance Orbiter -- 3.5.4.1 Mars Atmosphere and Volatile Evolution -- 3.6 Landers and Rovers -- 3.6.1 Mars Pathfinder -- 3.6.2 Mars Exploration Rovers -- 3.6.3 Phoenix -- 3.6.4 Mars Science Laboratory (MSL) -- 3.6.5 Descent Profiles -- 3.7 Looking to the Future -- References -- 4 Thermal Structure and Composition -- 4.1 Introduction -- 4.2 Thermal Structure -- 4.2.1 Overview of Mars Atmosphere Thermal Structure -- 4.2.2 Available Observations -- 4.2.2.1 Thermal Infrared Sounding -- 4.2.2.2 Radio Occultation Observations -- 4.2.2.3 Stellar Occultation Observations -- 4.2.2.4 Entry Profiles and Aerobraking -- 4.2.2.5 Observations From the Surface of Mars -- 4.2.3 Observed Thermal Structure. , 4.2.3.1 Lower Atmosphere Thermal Structure -- 4.2.3.2 Middle Atmosphere Thermal Structure -- 4.2.3.3 Global Mean and Extreme Temperatures -- 4.2.3.4 Diurnal Variations and Tides -- 4.2.3.5 Inter-Annual Variations -- 4.3 Composition -- 4.3.1 Surface Pressure -- 4.3.2 Nitrogen -- 4.3.3 Argon -- 4.3.4 Oxygen -- 4.3.5 Carbon Monoxide -- 4.3.6 Ozone -- 4.3.7 Hydrogen Peroxide -- 4.3.8 Hydrogen -- 4.3.9 Nitrogen Monoxide -- 4.3.10 Methane -- 4.3.11 Upper Limits of Other Trace Species -- 4.3.12 Isotopic Ratios -- 4.3.12.1 Carbon and Oxygen -- 4.3.12.2 Nitrogen and Noble Gases -- 4.3.12.3 Hydrogen -- 4.4 Reference Atmosphere -- 4.4.1 Standard Mars Atmosphere -- 4.4.2 Mars-GRAM -- 4.4.3 Mars Climate Database -- 4.5 Summary and Future Issues -- Acknowledgments -- References -- 5 Mars Clouds -- 5.1 Introduction -- 5.2 Specific Cloud Morphologies and Occurrences -- 5.3 The Global-Scale Distribution of Mars Water Ice Clouds -- 5.3.1 Aphelion Cloud Belt -- 5.3.2 Polar Hoods -- 5.3.3 High-Altitude Hazes -- 5.3.4 Inter-Annual Variability -- 5.4 Water Ice Clouds in the Lower Boundary Layer: Phoenix LIDAR Observations -- 5.5 Physical and Radiative Properties of Mars Water and CO2 Ice Clouds -- 5.5.1 Cloud Physical Properties -- 5.5.2 Cloud Radiative Properties -- 5.6 Simulating Water Ice Clouds in Mars General Circulation Models -- 5.6.1 Cloud Microphysics -- 5.6.2 Representation of Water Ice Clouds in Mars General Circulation Models -- 5.6.3 Dynamical Control of Global Cloud Structures on Mars -- 5.6.3.1 The Aphelion Cloud Belt -- 5.6.3.2 The Polar Hoods -- 5.6.4 Radiative Effects of Clouds and Thermal Tides -- 5.7 CO2 Ice Clouds in the Mars Atmosphere -- 5.7.1 Observations of CO2 Clouds -- 5.7.2 CO2 Cloud Formation Microphysics -- 5.7.3 Implications of CO2 Clouds for Early Mars Climates -- 5.8 Conclusions -- References. , 6 Radiative Process: Techniques and Applications -- 6.1 Introduction -- 6.2 Radiative Transfer Equation (RTE) -- 6.2.1 A Note on Units and Nomenclature -- 6.2.2 General Scalar Equation -- 6.2.3 Neglect of Polarization -- 6.2.4 Plane-Parallel Approximation -- 6.2.4.1 No (Internal) Source Function Approximation -- 6.2.4.2 Single-Scattering and Purely Absorbing Approximations -- 6.2.4.3 Two-Stream Approximations -- 6.2.4.4 Numerical Solutions -- (a) Discrete Ordinate Method -- (b) Spherical Harmonics Method (SHM) -- (c) Two-Stream Codes -- 6.2.5 Spherical Shell -- 6.2.5.1 Breakdown of Plane-Parallel Geometry -- 6.2.5.2 Numerical Solutions -- (a) Analytical Plus Approximation -- (b) Pseudo-Spherical Approximation -- (c) Spherical Treatment -- 6.2.6 Three-Dimensional (3D) Radiative Transfer -- 6.3 Sources of Atmospheric Absorption and Scattering -- 6.3.1 Atoms and Molecules - Scattering -- 6.3.1.1 Rayleigh Scattering -- 6.3.1.2 Raman Scattering -- 6.3.2 Atoms and Molecules - Absorption -- 6.3.2.1 Ultraviolet Cross-Sections -- (a) CO2 -- (b) O3 -- (c) Other UV Absorbers -- 6.3.2.2 Near-Infrared and Infrared Cross-Sections -- (a) Line-by-Line Technique -- (b) Band Models -- (c) Correlated-k Technique -- (d) Other Techniques -- 6.3.2.3 Clear-Air Molecular Transmittance Illustrations -- 6.3.3 Aerosols -- 6.3.3.1 RTE-Related Definitions -- (a) Ensemble of Identical Particles -- (b) Ensemble of Non-Identical Particles -- (c) Separate Ensembles -- 6.3.3.2 Particle Size Distributions -- 6.3.3.3 Calculation of Single-Particle Scattering Properties -- (a) Separation-of-Variables Method (SVM) -- (b) T-Matrix Method (TMM) -- (c) Finite-Difference Time-Domain Method (FDTDM) -- (d) Geometrical Optics Approximation (GOA) -- 6.3.3.4 The Importance of Non-Spherical Particles -- 6.3.3.5 Dust Aerosols -- (a) Refractive Indices -- (b) Shape -- (c) Size. , (d) Representative Radiative Properties -- 6.3.3.6 H2O Ice Aerosols -- (a) Refractive Indices -- (b) Shape -- (c) Size -- (d) Representative Radiative Properties -- 6.3.3.7 CO2 Ice Aerosols -- (a) Macroscopic Properties -- (b) Representative Radiative Properties -- 6.3.3.8 General Spatial/Temporal Distribution of Aerosols - Databases -- 6.4 Radiative Sources -- 6.4.1 Solar Spectrum -- 6.4.2 Thermal (LTE) and Non-LTE Emission -- 6.4.2.1 Thermal Versus Non-Thermal Emission Versus Airglow -- 6.4.2.2 Non-LTE Radiative Transfer -- (a) Statistical Equilibrium Equation -- (b) Non-LTE Radiative Transfer Equation -- (c) Difficulties and Approximate Solutions -- 6.4.2.3 Non-LTE Data and Modeling of the Martian Atmosphere -- 6.5 Energetic Particles -- 6.6 Applications -- 6.6.1 Global Climate Models (GCMs) -- 6.6.1.1 Aerosol Representation in Models -- 6.6.1.2 Simulated Heating Rates -- 6.6.1.3 Water Ice Clouds -- 6.6.1.4 Radiation Budget -- 6.6.1.5 Archetypical Flux Spectra -- 6.6.2 Remote Sensing and Radiative Transfer -- 6.6.2.1 Retrievals - Temperature Profiles -- 6.6.2.2 Retrievals - Aerosols -- (a) Column-Integrated Optical Depths -- (b) Macrophysical Retrievals -- 6.6.3 Non-Local Thermodynamic Equilibrium -- 6.6.3.1 NLTE Parameterizations for GCMs -- 6.6.3.2 Mesospheric Forcing of Thermal Tides -- 6.6.3.3 NLTE Radiative Damping of Gravity Waves -- 6.6.3.4 Mesospheric Winds From the 10 µm CO2 Bands -- 6.7 Conclusion -- Acknowledgments -- References -- 7 The Martian Planetary Boundary Layer -- 7.1 Introduction -- 7.2 Atmospheric Boundary Layer Physics -- 7.3 Comparison and Roles of Planetary Boundary Layers on Earth and Mars -- 7.3.1 Energy Budget of PBL and Surface -- 7.3.2 Boundary Layer Turbulence -- 7.3.3 Dust Devils and Dust Storms -- 7.3.4 The Influence of the PBL on Martian Weather and Climate -- 7.4 Recent and Current Missions and Observations. , 7.4.1 Surface In Situ Observations -- 7.4.1.1 Viking Landers' Meteorological Instrumentation -- 7.4.1.2 Mars Pathfinder Meteorological Instrumentation -- 7.4.1.3 Phoenix Meteorological Instrumentation -- 7.4.1.4 Mars Science Laboratory, First Results -- 7.4.2 Surface-Based Remote Sensing -- 7.4.2.1 Imaging Instruments -- 7.4.2.2 Mini-TES Instruments on the MERs -- 7.4.2.3 Phoenix LIDAR -- 7.4.3 Orbital Observations -- 7.4.3.1 Radio Occultation -- 7.4.3.2 Other Orbital Measurements -- 7.4.4 Use of Mars Lander Data to Validate Surface Layer Scaling Laws -- 7.5 Modeling the Martian Planetary Boundary Layer -- 7.5.1 Bulk and Mixing Length Parameterized Models of the Martian PBL -- 7.5.1.1 Physics of the Martian PBL as Revealed by First-Order Closure Models -- 7.5.2 TKE Closures for the Martian PBL -- 7.5.3 Large-Eddy Simulations of the Martian PBL -- 7.5.3.1 General Principles -- 7.5.3.2 LES Standard Settings -- 7.5.3.3 First Results -- 7.5.3.4 Recent Efforts and Perspectives -- 7.5.3.5 LES and Hazards for Mission Operations -- 7.6 Discussion and Outstanding Issues -- References -- 8 Mesoscale Meteorology -- 8.1 Introduction -- 8.2 The Definition of the Mesoscale -- 8.2.1 Rossby Radius of Deformation -- 8.2.2 Richardson Number -- 8.2.3 Rossby Number -- 8.2.4 Energy Cascade -- 8.2.5 A Practical Definition -- 8.3 Mesoscale Models -- 8.3.1 Dynamical Cores -- 8.3.2 Physical Parameterizations -- 8.3.3 Initial and Boundary Conditions -- 8.3.4 Grid Nesting -- 8.4 Key Martian Mesoscale Systems -- 8.4.1 Near-Surface Mesoscale Phenomena -- 8.4.1.1 Thermal Circulations Related to Topography -- 8.4.1.2 Circulations Related to Thermal Contrasts -- 8.4.2 Mesoscale Waves -- 8.5 Clouds and Dust -- 8.5.1 Water Ice Clouds -- 8.5.2 Carbon Dioxide Ice Clouds -- 8.5.3 Dust Storms -- 8.6 Aeolian Processes -- 8.7 Mesoscale Model Applications -- References. , 9 The Global Circulation.
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  • 2
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] Observations from the gamma-ray spectrometer instrument suite on the Mars Odyssey spacecraft have been interpreted as indicating the presence of vast reservoirs of near-surface ice in high latitudes of both martian hemispheres. Ice concentrations are estimated to range from 70 per cent at ...
    Materialart: Digitale Medien
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  • 3
    Publikationsdatum: 2023-03-01
    Beschreibung: Long-term, continuous in situ observations of the near-surface atmospheric boundary layer are critical for many weather and climate applications. Although there is a proliferation of surface stations globally, especially in and around populous areas, there are notably fewer tall meteorological towers with multiple instrumented levels. This is particularly true in remote and extreme environments such as the Eastern Antarctic plateau. In the article, we present and analyze 10 years (2010-2019) of data from 6 levels of meteorological instrumentation mounted on a 45-m tower located at Dome C, East Antarctica near the Concordia research station, producing a unique climatology of the near-surface environment. Large seasonal differences are evident in the monthly mean temperature and wind data, depending on the presence or absence of solar surface forcing. Strong vertical temperature gradients (inversions) frequently develop in calm, winter conditions, while vertical convective mixing occurs in the summer leading to near-uniform temperatures along the tower. Seasonal variation in wind speed is much less notable at this location than the temperature variation as the winds are less influenced by the solar cycle; there are no katabatic winds as Dome C is quite flat. Harmonic analysis confirms that most of the energy in the power spectrum is at diurnal, annual and semi-annual scales. Analysis of observational uncertainty and comparison to reanalysis data from ERA-5 indicate that wind speed is particularly difficult to measure at this location.
    Schlagwort(e): Antarctic Plateau; Antartic field data for CALibration and VAlidation of meteorological and climate models and satellite retrievals, Antarctic Coast to Dome C; boundary layer; CALVA; Date/Time local; DOME_C_CALVA; Dome C, Antarctica; meteorology; Profile; Temperature; Tower; Weather station/meteorological observation; wind; Wind monitor, R.M. Young, model 05103; Wind speed; WST
    Materialart: Dataset
    Format: text/tab-separated-values, 911449 data points
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  • 4
    Publikationsdatum: 2023-03-01
    Beschreibung: Long-term, continuous in situ observations of the near-surface atmospheric boundary layer are critical for many weather and climate applications. Although there is a proliferation of surface stations globally, especially in and around populous areas, there are notably fewer tall meteorological towers with multiple instrumented levels. This is particularly true in remote and extreme environments such as the Eastern Antarctic plateau. In the article, we present and analyze 10 years (2010-2019) of data from 6 levels of meteorological instrumentation mounted on a 45-m tower located at Dome C, East Antarctica near the Concordia research station, producing a unique climatology of the near-surface environment. Large seasonal differences are evident in the monthly mean temperature and wind data, depending on the presence or absence of solar surface forcing. Strong vertical temperature gradients (inversions) frequently develop in calm, winter conditions, while vertical convective mixing occurs in the summer leading to near-uniform temperatures along the tower. Seasonal variation in wind speed is much less notable at this location than the temperature variation as the winds are less influenced by the solar cycle; there are no katabatic winds as Dome C is quite flat. Harmonic analysis confirms that most of the energy in the power spectrum is at diurnal, annual and semi-annual scales. Analysis of observational uncertainty and comparison to reanalysis data from ERA-5 indicate that wind speed is particularly difficult to measure at this location.
    Schlagwort(e): Antarctic Plateau; Antartic field data for CALibration and VAlidation of meteorological and climate models and satellite retrievals, Antarctic Coast to Dome C; boundary layer; CALVA; Date/Time local; DOME_C_CALVA; Dome C, Antarctica; meteorology; Profile; Temperature; Temperature, air; Thermometer/Hygrometer, Vaisala, HMP155, PT100 sensor; Tower; Weather station/meteorological observation; wind; WST
    Materialart: Dataset
    Format: text/tab-separated-values, 1199618 data points
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  • 5
    Publikationsdatum: 2021-02-25
    Beschreibung: The detection of methane on Mars has been interpreted as indicating that geochemical or biotic activities could persist on Mars today1. A number of different measurements of methane show evidence of transient, locally elevated methane concentrations and seasonal variations in background methane concentrations2-5. These measurements, however, are difficult to reconcile with our current understanding of the chemistry and physics of the Martian atmosphere6,7, which-given methane's lifetime of several centuries-predicts an even, well mixed distribution of methane1,6,8. Here we report highly sensitive measurements of the atmosphere of Mars in an attempt to detect methane, using the ACS and NOMAD instruments onboard the ESA-Roscosmos ExoMars Trace Gas Orbiter from April to August 2018. We did not detect any methane over a range of latitudes in both hemispheres, obtaining an upper limit for methane of about 0.05 parts per billion by volume, which is 10 to 100 times lower than previously reported positive detections2,4. We suggest that reconciliation between the present findings and the background methane concentrations found in the Gale crater4 would require an unknown process that can rapidly remove or sequester methane from the lower atmosphere before it spreads globally.
    Beschreibung: Published
    Beschreibung: 517–520
    Beschreibung: 6A. Geochimica per l'ambiente e geologia medica
    Beschreibung: JCR Journal
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
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  • 6
    Publikationsdatum: 2020-03-19
    Beschreibung: Global dust storms on Mars are rare1,2 but can affect the Martian atmosphere for several months. They can cause changes in atmospheric dynamics and inflation of the atmosphere3, primarily owing to solar heating of the dust3. In turn, changes in atmospheric dynamics can affect the distribution of atmospheric water vapour, with potential implications for the atmospheric photochemistry and climate on Mars4. Recent observations of the water vapour abundance in the Martian atmosphere during dust storm conditions revealed a high-altitude increase in atmospheric water vapour that was more pronounced at high northern latitudes5,6, as well as a decrease in the water column at low latitudes7,8. Here we present concurrent, high-resolution measurements of dust, water and semiheavy water (HDO) at the onset of a global dust storm, obtained by the NOMAD and ACS instruments onboard the ExoMars Trace Gas Orbiter. We report the vertical distribution of the HDO/H2O ratio (D/H) from the planetary boundary layer up to an altitude of 80 kilometres. Our findings suggest that before the onset of the dust storm, HDO abundances were reduced to levels below detectability at altitudes above 40 kilometres. This decrease in HDO coincided with the presence of water-ice clouds. During the storm, an increase in the abundance of H2O and HDO was observed at altitudes between 40 and 80 kilometres. We propose that these increased abundances may be the result of warmer temperatures during the dust storm causing stronger atmospheric circulation and preventing ice cloud formation, which may confine water vapour to lower altitudes through gravitational fall and subsequent sublimation of ice crystals3. The observed changes in H2O and HDO abundance occurred within a few days during the development of the dust storm, suggesting a fast impact of dust storms on the Martian atmosphere.
    Beschreibung: Published
    Beschreibung: 521–525
    Beschreibung: 6A. Geochimica per l'ambiente e geologia medica
    Beschreibung: JCR Journal
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
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  • 7
    Publikationsdatum: 2022-05-25
    Beschreibung: Recent measurements of methane (CH4) by the Mars Science Laboratory (MSL) now confront us with robust data that demand interpretation. Thus far, the MSL data have revealed a baseline level of CH4 (∼0.4 parts per billion by volume [ppbv]), with seasonal variations, as well as greatly enhanced spikes of CH4 with peak abundances of ∼7 ppbv. What do these CH4 revelations with drastically different abundances and temporal signatures represent in terms of interior geochemical processes, or is martian CH4 a biosignature? Discerning how CH4 generation occurs on Mars may shed light on the potential habitability of Mars. There is no evidence of life on the surface of Mars today, but microbes might reside beneath the surface. In this case, the carbon flux represented by CH4 would serve as a link between a putative subterranean biosphere on Mars and what we can measure above the surface. Alternatively, CH4 records modern geochemical activity. Here we ask the fundamental question: how active is Mars, geochemically and/or biologically? In this article, we examine geological, geochemical, and biogeochemical processes related to our overarching question. The martian atmosphere and surface are an overwhelmingly oxidizing environment, and life requires pairing of electron donors and electron acceptors, that is, redox gradients, as an essential source of energy. Therefore, a fundamental and critical question regarding the possibility of life on Mars is, "Where can we find redox gradients as energy sources for life on Mars?" Hence, regardless of the pathway that generates CH4 on Mars, the presence of CH4, a reduced species in an oxidant-rich environment, suggests the possibility of redox gradients supporting life and habitability on Mars. Recent missions such as ExoMars Trace Gas Orbiter may provide mapping of the global distribution of CH4. To discriminate between abiotic and biotic sources of CH4 on Mars, future studies should use a series of diagnostic geochemical analyses, preferably performed below the ground or at the ground/atmosphere interface, including measurements of CH4 isotopes, methane/ethane ratios, H2 gas concentration, and species such as acetic acid. Advances in the fields of Mars exploration and instrumentation will be driven, augmented, and supported by an improved understanding of atmospheric chemistry and dynamics, deep subsurface biogeochemistry, astrobiology, planetary geology, and geophysics. Future Mars exploration programs will have to expand the integration of complementary areas of expertise to generate synergistic and innovative ideas to realize breakthroughs in advancing our understanding of the potential of life and habitable conditions having existed on Mars. In this spirit, we conducted a set of interdisciplinary workshops. From this series has emerged a vision of technological, theoretical, and methodological innovations to explore the martian subsurface and to enhance spatial tracking of key volatiles, such as CH4.
    Beschreibung: Published
    Beschreibung: 6A. Geochimica per l'ambiente e geologia medica
    Beschreibung: JCR Journal
    Schlagwort(e): Methane, Mars
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
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