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  • 1
    Keywords: Earth. ; Electronic books.
    Description / Table of Contents: The authors of this book are experts on the subject of extrasolar planets. By presenting an updated perspective of our planet as seen from outer space, they provide a guide for the remote detection of life on other planets and planets beyond the solar system.
    Type of Medium: Online Resource
    Pages: 1 online resource (429 pages)
    Edition: 1st ed.
    ISBN: 9781441916846
    Series Statement: Astronomy and Astrophysics Library
    Language: English
    Note: The Earth as a Distant Planet -- Preface -- 1 Observing the Earth -- 1.1 The Exploration of Our Planet -- 1.2 First Observations of Our Planet from the Air -- 1.2.1 Early Balloon Pictures -- 1.2.2 The Space Research -- 1.2.2.1 The First Attempts -- 1.2.2.2 The Manned Flights -- 1.2.2.3 The Earth Observatory -- 1.2.2.4 Infrared Images -- 1.3 The Earth-Moon System -- 1.4 The Solar System -- 1.4.1 General Characteristics -- 1.4.2 A View from the Edge -- 1.4.3 Our Environment -- 1.4.3.1 Nearby Stars -- 1.4.3.2 The Gaseous and Dusty Neighbourhood -- 1.4.3.3 The Galaxy -- References -- 2 The Earth in Time -- 2.1 The Earth at the Present Time -- 2.1.1 The Interior -- 2.1.1.1 Inner Core -- 2.1.1.2 Outer Core -- 2.1.1.3 Mantle -- 2.1.1.4 Lithosphere -- 2.1.1.5 Energy Budget -- 2.1.2 Plate Tectonics -- 2.1.3 The Atmosphere -- 2.1.4 Energy Balance of the Atmosphere -- 2.1.4.1 Albedo -- 2.1.4.2 The Planet's Mean Temperature -- 2.1.4.3 Greenhouse Gases -- 2.1.4.4 2D Models -- 2.2 The Precambrian Era (4,500-4,550 Ma BP) -- 2.2.1 The Formation of the Earth: The Hadean Era -- 2.2.1.1 The Moon and the Earth Rotation -- 2.2.1.2 Late Heavy Bombardment -- 2.2.1.3 The Early Crust and Mantle -- 2.2.1.4 The Young and Faint Sun -- 2.2.2 The Archaean and Proterozoic Times -- 2.2.2.1 The Origin and Development of Life -- 2.2.2.2 The Carbon Dioxide Cycle -- 2.2.2.3 Sea-Floor Spreading and Continental Growth -- 2.2.2.4 Greenhouse Gases and Paleoclimate -- 2.2.2.5 Oxygen, Ozone and Ultraviolet Radiation -- 2.2.2.6 The Snowball Earth -- 2.3 The Phanerozoic Era -- 2.3.1 The Drift, Breakup and Assembly of the Continents -- 2.3.2 Supereruptions and Hot Spots -- 2.3.3 The Connection Temperature-Greenhouse Gases -- 2.3.4 Temporal Variations of the Magnetic Field -- 2.3.5 Mass Extinctions in the Fossil Record -- 2.3.5.1 Historical Introduction. , 2.3.5.2 Biological Extinctions During the Phanerozoic Era -- 2.3.5.3 The K/T Extinction -- 2.4 The Quaternary -- 2.4.1 The Ice Ages -- 2.4.2 The Present Warming: The Anthropocene -- 2.5 The Future of Earth -- 2.5.1 The End of Life -- 2.5.2 The End of the Earth -- References -- 3 The Pale Blue Dot -- 3.1 Globally Integrated Observations of the Earth -- 3.1.1 Earth Orbiting Satellites -- 3.1.2 Observations from Long-range Spacecrafts -- 3.1.3 An Indirect View of the Earth: Earthshine -- 3.2 The Earth's Photometric Variability in Reflected Light -- 3.2.1 Observational Data -- 3.2.2 Reflectance Models -- 3.2.3 The Earth's Light Curves -- 3.2.4 The Rotational Period -- 3.2.5 Cloudiness and Apparent Rotation -- 3.2.6 Glint Scattering -- 3.3 Earth's Infrared Photometry -- 3.4 Spectroscopy of Planet Earth -- 3.4.1 The Visible Spectrum -- 3.4.2 The Infrared Spectrum -- 3.4.3 The Earth's Transmission Spectrum -- 3.5 Polarimetry of Planet Earth -- 3.5.1 Linear Polarization -- 3.5.2 Circular Polarization -- References -- 4 The Outer Layers of the Earth -- 4.1 Temperature Profile and the Energy Balance -- 4.2 Stratosphere: The Ozone Layer -- 4.2.1 Natural Processes of Ozone Formation and Destruction -- 4.2.1.1 Ozone Formation -- 4.2.1.2 Ozone Destruction -- 4.2.1.3 Ozone Transport -- 4.3 Mesosphere -- 4.4 The Thermosphere -- 4.5 The Exosphere: Geocorona -- 4.6 Airglow -- 4.6.1 Nightglow -- 4.6.2 Dayglow -- 4.6.3 Twilight Airglow -- 4.7 The Ionosphere -- 4.7.1 General Structure -- 4.7.2 Ionosphere Indicators -- 4.7.3 Lightnings -- 4.8 The Magnetosphere -- 4.8.1 Description -- 4.8.2 Radiation Belts -- 4.8.3 Aurorae -- 4.9 Radio Emission of the Earth and Other Planets -- 4.10 The Earth in X-Rays -- 4.11 The Earth's Gamma Ray Emission -- 4.12 The Outer Layers of the Early Earth -- References -- 5 Biosignatures and the Search for Life on Earth. , 5.1 The Physical Concept of Life -- 5.2 Astrobiology: New Perspectives for an Old Question -- 5.3 Requirements for Life -- 5.3.1 Biogenic Elements -- 5.3.2 A Solvent: Water -- 5.3.3 Energy Source -- 5.3.3.1 Solar Radiation: Photosynthesis -- 5.3.3.2 Chemical Energy -- 5.4 Biosignatures on Present Earth -- 5.4.1 Spectral Biosignatures in the Atmosphere -- 5.4.1.1 Atmospheric Carbon dioxide, Water Vapour and Ozone: The Triple Fingerprint -- 5.4.1.2 Other Atmospheric Biosignatures -- 5.4.2 Chlorophyll and Other Spectral Biosignatures of the Planetary Surface: The Red Edge -- 5.4.3 Chirality and Polarization as Biosignatures -- 5.5 Biosignatures on Early-Earth -- 5.6 Life in the Universe -- 5.6.1 Circumstellar Habitable Zone -- 5.6.1.1 Stellar Constraints -- 5.6.1.2 M Stars and Tidal Locking -- 5.6.1.3 Planetary Constraints -- 5.6.1.4 The Continuously Habitable Zone -- 5.6.2 Additional Constraints for Habitability -- 5.6.2.1 Short-term Stellar Variability -- 5.6.2.2 Ultraviolet and Ionizing Radiation -- 5.6.3 Galactic Habitable Zone -- 5.7 Signatures of Technological Civilizations -- 5.7.1 Night Lights -- 5.7.2 Spectral Features -- 5.7.3 Artificial Radioemission -- 5.7.4 Nuclear Explosions -- 5.7.5 Extraterrestrial Pulses -- References -- 6 Detecting Extrasolar Earth-like Planets -- 6.1 First Attempts to Discover Exoplanets -- 6.2 The Mass Limit: From Brown Dwarfs to Giant Planets -- 6.2.1 The Brown Dwarf Desert -- 6.3 The Detection of Earth-like Planets: A Complex Problem -- 6.3.1 Brightness Ratio -- 6.3.2 Angular Distance -- 6.4 Methods for the Detection of Exoplanets -- 6.4.1 Indirect Detection of Exoplanets -- 6.4.1.1 Astrometry -- 6.4.1.2 Radial Velocity -- 6.4.1.3 Pulsar Timing -- 6.4.1.4 Microlensing Events -- 6.4.1.5 Transits -- 6.4.1.6 Differential Spectro-photometry During Transits -- 6.4.1.7 Miscellaneous Indirect Detection Methods. , 6.4.2 Direct Observations of Exoplanets -- 6.4.2.1 Coronagraphy -- 6.4.2.2 Nulling Interferometry -- 6.4.2.3 Polarimetry -- 6.5 The Next 20 Years -- References -- 7 The Worlds Out There -- 7.1 Definition of a Planet -- 7.2 Our Solar System -- 7.2.1 General Facts -- 7.2.2 Chemical Abundances in the Solar System -- 7.2.3 Giant Planets -- 7.2.4 Terrestrial Planets -- 7.2.5 Dwarf Planets and Other Minor Bodies -- 7.2.5.1 Asteroid Belt -- 7.2.5.2 Kuiper Belt -- 7.2.5.3 Oort Cloud -- 7.3 Planetary Atmospheres -- 7.4 Statistical Properties of the Extrasolar Giant Planets -- 7.4.1 Mass Distribution -- 7.4.2 Hot Jupiters -- 7.4.3 Eccentric Planets -- 7.4.4 Role of the Metallicity -- 7.4.5 Stellar Masses -- 7.5 Types of Terrestrial Planets -- 7.5.1 Rocky Planets -- 7.5.2 Super-Earths -- 7.5.2.1 Internal Structure -- 7.5.2.2 Surface Appearance and Habitability -- 7.5.3 Carbon-Oxygen Ratio: The Carbon Planets -- 7.5.4 Super-Mercuries -- 7.5.5 Planets Around Pulsars in Metal-Poor Environments -- 7.5.6 Terrestrial Planets Around Giant Planets:The Rocky Moons -- 7.5.7 Free-Floating Planets -- 7.6 Characterization of Exoplanets -- 7.6.1 Mass-Radius Relationships -- 7.6.2 Atmospheres of Exoplanets -- 7.6.2.1 HD 189733b -- 7.6.2.2 HD 209458b -- 7.6.2.3 Terrestrial Planets -- 7.6.3 Radio Emission of Exoplanets -- 7.7 Terraformed Planets -- 7.8 Expect the Unexpected -- References -- 8 Extrasolar Planetary Systems -- 8.1 The Origin of the Solar System: Early Attempts -- 8.1.1 Nebular Theory -- 8.1.2 Catastrophic Theories -- 8.2 Formation of Planetary Systems -- 8.2.1 Stellar Formation -- 8.2.2 The Early Accretion Phase -- 8.2.3 The Protoplanetary and Debris Disks -- 8.2.4 Formation of Giant Planets -- 8.2.5 Formation of Terrestrial Planets -- 8.3 Planetary Orbits -- 8.3.1 Basic Orbital Elements -- 8.3.2 Keplerian Orbits -- 8.3.3 Harmony and Chaos. , 8.3.3.1 Historical Background -- 8.3.4 Relevant Parameters of Dynamical Stability -- 8.3.4.1 Uncertainty -- 8.3.5 Resonances in Planetary Systems -- 8.3.5.1 Laplace Resonances -- 8.3.5.2 Kirkwood Gaps -- 8.3.5.3 Spin-Orbit Resonance -- 8.3.6 Lagrangian Points -- 8.4 The Dynamically Habitable Zone -- 8.5 Architecture of Planetary Systems -- 8.5.1 Systems with Hot Jupiters: The Planetary Migration -- 8.5.1.1 Planetesimal-driven Migration -- 8.5.1.2 Planet-Planet Scattering -- 8.5.1.3 The LHB Event and the Nice Model -- 8.5.1.4 Interaction with a Distant Companion Star -- 8.5.1.5 Gas Disk Migration -- 8.5.1.6 Stopping the Migration -- 8.5.1.7 Survival of Terrestrial Planets -- 8.5.2 Binary Systems -- 8.5.3 Multiple Planetary Systems -- 8.5.3.1 Gliese 581 -- 8.5.3.2 Gliese 876 -- 8.5.3.3 Upsilon Andromeda (HD 9826) -- 8.5.3.4 55 Cancri (HD 75732) -- 8.5.3.5 47 UMa (HD 95128) -- 8.5.3.6 HD 69830 -- 8.5.3.7 HD160691 ( Arae) -- 8.5.3.8 HD 40307 -- 8.6 Violence and Harmony -- References -- 9 Is Our Environment Special? -- 9.1 Is the Sun Anomalous? -- 9.1.1 Singularity -- 9.1.2 Mass -- 9.1.3 Location -- 9.1.4 Age -- 9.1.5 Chemical Composition: Metallicity -- 9.1.6 Magnetic Activity -- 9.1.7 Solar Analogs -- 9.2 Is the Solar System Unique? -- 9.2.1 Nature vs. Nurture -- 9.2.1.1 Formation -- 9.2.1.2 Stellar Encounters -- 9.2.1.3 Gravitational Interactions: LHB Events -- 9.2.1.4 Mercury: The Achilles Heel -- 9.2.2 Debris Disks -- 9.2.3 The Energetic Environment -- 9.2.4 Solar System Analogs -- 9.3 Is the Earth Something Special? -- 9.3.1 Habitability -- 9.3.2 Variations of Orbital Parameters -- 9.3.3 Presence of a Large Satellite -- 9.4 The Ultimate Factor: Life -- References -- Index.
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  • 2
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 87 (2000), S. 8201-8203 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: High dose nitrogen implantations have been performed at an energy of 30 keV. After high temperature annealing, 1200 °C, a buried layer composed mostly of silicon nitride is formed leaving an overlayer with a high fraction of crystalline silicon. The lattice constant of the overlayer and the region below the SiNx are reduced in 0.13% and 0.089%, respectively. The substitutional N seems to be responsible for this reduction. © 2000 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 91 (2002), S. 6209-6211 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Boron, nitrogen, and carbon ions were co-implanted in silicon wafers, and subsequently annealed. Infrared spectra show the formation of BN-rich buried layers. The presence of a band at 1375 cm−1 characteristic of boron nitride in a hexagonal configuration has been observed. Traces of the cubic phase formation were detected in some cases. Implanted samples exhibit a broad emission band about 550 nm. © 2002 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 70 (1999), S. 384-386 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: Local plasma emissivity of TJ-II plasmas will be determined using pyroelectric detectors. For tomographic reconstructions three fan-like arrays, 20 channels each, will be installed at the top, side, and bottom ports of the same sector. The designed compact in-vessel systems will use folding support structures to introduce the arrays through small diameter flanges and translation and rotary drives to position them at their measuring sites. Special individual "honeycomb-like" collimators (transparency of around 50% and spatial resolution of about 2 cm at the plasma center) have been designed to optimize the signal level and to act as a microwave filter. In the first stage, radial profiles of plasma emissivity will be obtained with a single detector, on the basis of frozen plasma parameters during a few ms. This detector is equipped with a rotary slit that scans the whole plasma cross section from 10–20 times per shot. To perform power balances, global plasma emission is monitored with three pyroelectric detectors. Collimators are movable slits that enable probing either the full plasma cross section or narrow central chords; when fully closed they protect detectors during wall conditioning and permit background noise characterization. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: The set of diagnostics that are being installed in TJ–II are meant to cover the full photon energy range expected in TJ–II during the electron cyclotron resonance heating phase. The obtained information will be used to evaluate the energy contained in the superthermal electron populations and its possible relevance in the global power balance as well as for standard electron temperature estimations. Two NaI(Tl) detectors located at the equatorial plane of the machine will be used to analyze the highest energy photons (over 50 keV). One Si(Li) and a planar Ge detector will be used to obtain the emission spectra between 1 and 100 keV. Tomographic reconstruction of plasma emissivity (up to 10 keV) will be carried out using four p-n silicon photodiodes arrays of 16 detectors, located at the same poloidal section. An additional camera will be used to detect toroidal asymmetries. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 66 (1995), S. 1056-1060 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: For research into space plasma turbulence, we have developed a number of space-flight instruments for making in situ measurements of plasma wave activity. One of these instruments, the NRL downconverter, is used to measure plasma waves in the 2- to 20-MHz frequency range by downconverting a 100-kHz band of frequencies to the baseband. Input frequency tuning is controlled by an imbedded microcomputer, and can be programmed to scan in any desired frequency pattern. The in-phase and quadrature receiver outputs, each having a 50-kHz bandwidth, are processed externally by digital signal processors (DSP). The receiver achieves 35 dB of sideband rejection using a hybrid quadrature mixer design, which incorporates an analog front end with digital signal processing. This design yields 15 dB of improved sideband rejection over more conventional analog techniques. The microcomputer control, DSP processing, and modular design contribute to the flexibility of the receiver, which has allowed the system to be used on a number of different missions. © 1995 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 67 (1996), S. 3751-3754 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: We have developed a digital signal processor (DSP) system to extend the capabilities of a variety of scientific instruments used to make in situ ionospheric plasma measurements from sounding rockets and spacecraft. The DSP system is extremely flexible due to the use of a field programmable gate array, sigma-delta analog-to-digital converters, and a highly integrated single-chip DSP. Using virtually identical circuitry, we have operated DSP systems processing data from low-frequency electric field detectors, Langmuir probes, and several radio-frequency receivers on several sounding rockets and spacecraft with different digital telemetry interfaces. The DSP system provides three major improvements to our instruments: (1) reduced telemetry bandwidth (data) requirements, (2) improved signal-to-noise ratio, and (3) digital antialiasing filtering. We describe our DSP system and show three examples of how we have implemented it with our instruments. Similar systems should be of interest to researchers in many fields of research.
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Contact dermatitis 32 (1995), S. 0 
    ISSN: 1600-0536
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Anatomia, histologia, embryologia 22 (1993), S. 0 
    ISSN: 1439-0264
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Mathematical models describing the histomorphometric growth of ruminant stomach during prenatal lifeOne hundred forty four ovine embryos and feti were used in an investigation to determine mathematical models describing the histomorphometric growth of tissues and compartments of the ruminant stomach. The results indicate that during prenatal life the diameter of the gastric chambers increase more slowly than the length. The tissue layers of the gastric walls, particularly the muscular tunic of all compartments demonstrated a uniform tendency toward more rapid development than the compartment walls proper.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 667 (1992), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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