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  • Wissenschaftspark Albert Einstein  (3)
  • SB Eisenhüttenstadt  (1)
  • SB Guben
  • Stadtmuseum Berlin
  • 2000-2004  (4)
Type of Medium
Language
Region
Year
Keywords
  • 1
    UID:
    gbv_352556080
    Format: 240 S , Ill., graph. Darst
    Edition: 1. ed.
    ISBN: 0805067817 , 0805075127
    Note: Includes bibliographical references (p. [215]-226) and index
    Language: English
    Keywords: Astrobiologie
    Author information: Ward, Peter D. 1949-
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  • 2
    UID:
    kobvindex_VBRD-i38994106100380
    Format: 380 Seiten
    Edition: 1. Auflage
    ISBN: 3899410610
    Series Statement: Mira Taschenbuch 25050 * New York Times Bestseller Autoren : Historical * The Well Pleasured ; 2
    Uniform Title: A well favored gentleman
    Content: Über Lady Alanna gibt es jede Menge Gerüchte und niemand weiß, wo sie sich aufhält. Immerhin ist sie die Herrin von Fionnaway Manor. Ian Fairchild möchte, dass das Herrenhaus ihm gehört, aber dazu müsste er Lady Alanna heiraten. Als diese ihr Versteckspiel aufgibt und wieder ihren rechtmäßigen Platz einnimmt, steht Ian eine Menge Überredungsarbeit bevor, wenn er wirklich will, dass sie seine Frau wird. Denn die bezaubernde junge Frau hat auch noch jede Menge Verstand und ist nicht so leicht zu überlisten.
    Note: Aus dem Amerikanischen übersetzt
    Language: German
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  • 3
    Book
    Book
    New York, NY : Freeman
    UID:
    kobvindex_GFZ67651
    Format: xxi, 465 S. , zahlr. Ill., graph. Darst., Kt. , 28 cm
    ISBN: 0716737418
    Note: MAB0014.001: M 02.0062 , MAB0014.002: AWI A3-02-0023 , MAB0014.003: PIK N 456-02-0005 , Contents: Preface. - PART 1 FRAMEWORK OF CLIMATE SCIENCE. - 1 Overview of Climate Science. - Climate and Climate Change. - 1-1 Geologic Time. - 1-2 How This Book Is Organized. - Development of Climate Science. - 1-3 How Scientists Study Climate Change. - Overview of the Climate System. - 1-4 Components of the Climate System. - 1-5 Climate Forcing. - 1-6 Climate System Responses. - 1-7 Time Scales of Forcing versus Response. - 1-8 Response Rates and Interactions Within the Climate System. - 1-9 Feedbacks in the Climate System. - Tools Of Climate Science: Temperature Scales. - 2 Earth's Climate System Today. - Heating Earth. - 2-1 Incoming Solar Radiation. - 2-2 Receipt and Storage of Solar Heat. - 2-3 Heat Transformation. - Heat Transfer in Earth's Atmosphere. - 2-4 Overcoming Stable Layering in the Atmosphere. - 2-5 Tropical-Subtropical Atmospheric Circulation. - 2-6 Atmospheric Circulation at Middle and High Latitudes. - Heat Transfer in Earth's Oceans. - 2-7 The Surface Ocean. - 2-8 Deep-Ocean Circulation. - Ice on Earth. - 2-9 Sea Ice. - 2-10 Glacial Ice. - Earth's Biosphere. - 2-11 Response of the Biosphere to the Physical Climate System. - 2-12 Effects of the Biosphere on the Climate System. - Looking Deeper into Climate Science: The Structure of Earth's Atmosphere. - Climate Interactions and Feedbacks: Albedo/Temperature. - Climate Interactions and Feedbacks: Water in the Climate System. - Climate Interactions and Feedbacks: Water Vapor. - Looking Deeper into Climate Science: The Conolis Effect. - Climate Interactions and Feedbacks: Vegetation-Climate Feedbacks. - 3 Climate Archives, Oata, and Models. - Climate Archives. - 3-1 Types of Archives. - 3-2 Dating Climate Records. - 3-3 Climate Resolution. - Climate Data. - 3-4 Biotic Data. - 3-5 Geological and Geochemical Data. - Climate Models. - 3-6 Physical Climate Models. - 3-7 Geochemical (Mass Balance) Models. - PART II TECTONIC-SCALE CLIMATE CHANGE. - 4 CO2 and Long-term Climate. - Greenhouse Worlds. - The Faint Young Sun Paradox. - Carbon Exchanges between Rocks and the Atmosphere. - 4-1 Volcanic Input of Carbon from Rocks to the Atmosphere. - 4-2 Chemical Weathering Removal of CO2 from the Atmosphere. - Climate Factors That Control Chemical Weathering. - Chemical Weathering: Earth's Thermostat?. - Is Life the Ultimate Control on Earth's Thermostat?. - 4-3 The Gaia Hypothesis. - Climate Debate: A Snowball Earth?. - Looking Deeper into Climate Science: The Organic Carbon Subcycle. - 5 Plate Tectonics and Climate. - Plate Tectonics. - 5-1 Structure and Composition of Tectonic Plates. - 5-2 Evidence of Past Plate Motions. - The Polar Position Hypothesis. - 5-3 Glaciations and Continental Positions since 500 Myr Ago. - Modeling Climate on the Supercontinent Pangaea. - 5-4 Input to the Model Simulation of Pangaean Climate. - 5-5 Output from the Model Simulation of Pangaean Climate. - Tectonic Control of CO2 Input: The BLAG Spreading Rate Hypothesis. - 5-6 Control of CO2 Input by Seafloor Spreading. - 5-7 Initial Evaluation of the BLAG Spreading Rate Hypothesis. - Tectonic Control of CO2 Removal: The Uplift Weathering Hypothesis. - 5-8 Rock Exposure and Chemical Weathering. - 5-3 Uplift and Chemical Weathering. - What Controls Chemical Weathering?. - 5-10 Weathering: Climate Forcing and Feedback. - Looking Deeper into Climate Science: Brief Glatiation 430 Myr Ago. - 6 Greenhouse Earth. - What Explains Greenhouse Warmth 100 Myr Ago?. - 6-1 Model Simulations of a Greenhouse World. - 6-2 What Explains the Data-Model Mismatch?. - Sea Level Changes and Climate. - 6-3 Causes of Tectonic-Scale Changes in Sea Level. - 6-4 Effect of Sea Level Changes on Climate. - Asteroid Impacts. - Climate Interactions and Feedbacks: The Effect of CO2 on Climate. - Looking Deeper into Climate Science: Calculating Changes in Sea Level. - 7 Back into the Icehouse: The Last 55 Million years. - Global Climate Change Since 55 Myr Ago. - 7-1 Evidence from Ice and Vegetation. - 7-2 Oxygen Isotope Data. - Why Did Global Climate Cool over the Last 55 Myr?. - 7-3 Evaluating the BLAG Spreading Rate Hypothesis. - 7-4 Evaluating the Uplift Weathering Hypothesis. - 7-5 Evaluating the Ocean Heat Transport Hypothesis. - 7-6 Causes of Brief Tectonic-Scale Climate Change. - Understanding and Predicting Tectonic Climate Change. - Tools Of Climate Science: Oxtygen Isotope Ratios (δ18O). - Climate Debate: The Timing of Uplift in Western North America. - Looking Deeper into Climate Science: Is 87Sr/86Sr an Index of Chemical Weathering?. - PART III ORBITAL-SCALE CLIMATE CHANGE. - 8 Astronomical Control of Solar Radiation. - Earth's Orbit Today. - 8-1 Earth's Tilted Axis of Rotation and the Seasons. - 8-2 Earth's Eccentric Orbit: Changes in the Distance Between Earth and Sun. - Long-Term Changes in Earth's Orbit. - 8-3 Changes in Earth's Axial Tilt Through Time. - 8-4 Changes in Earth's Eccentric Orbit Through Time. - 8-5 Precession of Solstices and Equinoxes around Earth's Orbit. - Changes in Insolation Received on Earth. - 8-6 Insolation Changes by Month and Season. - 8-7 Insolation Changes According to Caloric Season. - Looking for Orbital-Scale Changes in Climate Records. - 8-8 Time Series Analysis. - 8-9 Aliasing of Climate Records. - 8-10 Tectonic-Scale Changes in Earth's Orbit. - Tools Of Climate Science: Cycles and Modulation. - Looking Deeper into Climate Science: Earth's Precession as a Sine Wave. - 9 Insolation Control of Monsoons. - Monsoon Circulations. - 9-1 Orbital-Scale Control of Summer Monsoons. - Evidence of Orbital-Scale Changes in Summer Monsoons. - 3-2 "Stinky Muds" in the Mediterranean. - 9-3 Freshwater Diatoms in the Tropical Atlantic. - 9-4 Upwelling in the Equatorial Atlantic. - Refinements of the Orbital Monsoon Hypothesis. - 9-5 Lag of Monsoons Behind Summer Insolation. - 9-6 Clipped Monsoon Responses and Monsoon Harmonics. - Monsoon Forcing Earlier in Earth's History. - 8-7 Monsoons on Pangaea 200 Myr Ago. - 9-8 Joint Tectonic and Orbital Control of Monsoons. - 10 Insolation Control of Ice Sheets. - What Controls the Size of Ice Sheets?. - 10-1 Orbital-Scale Control of Ice Sheets. - The Milankovitch Theory. - Modeling the Behavior of Ice Sheets. - 10-2 Insolation Control of Ice Sheet Size. - 10-3 Ice Sheet Lags behind Summer Insolation Forcing. - 10-4 Delayed Bedrock Response Beneath Ice Sheets. - 10-5 Full Cycle of Ice Growth and Decay. - 10-6 Ice Slipping and Calving. - Northern Hemisphere Ice Sheet History. - 10-7 Conceptual Model: Evolution of Ice Sheet Cycles. - 10-8 Evidence from δ18O: How Ice Sheets Actually Evolved. - 10-9 Confirming Ice Volume Changes: Coral Reefs and Sea Level. - 10-10 Using Astronomical and δ18O Signals as a Chronometer. - Looking Deeper into Climate Science: Ice Volume Response to Insolation. - Climate Debate: Antarctic Deglaciation 3 Myr Ago?. - Looking Deeper into Climate Science: Sea Level on Uplifting Islands. - 11 Orbital-Scale Changes in Carbon Dioxide and Methane. - Ice Cores. - 11-1 Drilling and Dating Ice Cores. - 11-2 Trapping Gases in the Ice. - Orbital-Scale Changes in Methane. - Orbital-Scale Changes in CO2. - 11-3 Physical Oceanographic Explanations of CO2 Changes. - 11-4 Orbital-Scale Carbon Reservoirs. - 11-5 Tracking Carbon through the Climate System. - 11-6 Can δ13C Evidence Detect Glacial Changes in Carbon Reservoirs?. - 11-7 Pumping of Carbon into the Deep Ocean during Glaciations. - 11-8 Changes in the Circulation of Deep Water during Glaciations. - Tools Of Climate Science: Carbon Isotope Ratios (δ13C). - Climate Debate: Do Winds Fertilize the Glacial Ocean?. - 12 Orbital-Scale Interactions in the Climate System. - Orbital-Scale Forcing and Response Revisited. - Ice-Driven Climate Responses. - 12-1 Ice-Driven Responses in High Northern Latitudes. - 12-2 Orbital Cycles in Regions Remote fro
    Language: English
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  • 4
    UID:
    kobvindex_GFZ89758
    Format: xii, 352 S. , 26 cm
    ISBN: 0231127391
    Series Statement: MARGINS theoretical and experimental earth science series
    Content: Traditionally, investigations of the rheology and deformation of the lithosphere (the rigid or mechanically strong outer layer of the Earth, which contains the crust and the uppermost part of the mantle) have taken place at one scale in the laboratory and at an entirely different scale in the field. Laboratory experiments are generally restricted to centimeter-sized samples and day- or year-length times, while geological processes occur over tens to hundreds of kilometers and millions of years. The application of laboratory results to geological systems necessitates extensive extrapolation in both temporal and spatial scales, as well as a detailed understanding of the dominant physical mechanisms. The development of an understanding of large-scale processes requires an integrated approach.
    Note: MAB0014.001: M 04.0414 , MAB0014.002: M 04.0514 , MAB0036: m , Includes bibliographical references and index
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