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  • 1
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: M 11.0356
    Description / Table of Contents: Rivers provide the primary link between land and sea. Utilizing the world's largest database, this book presents a detailed analysis and synthesis of the processes affecting fluvial discharge of water, sediment and dissolved solids. The ways in which climatic variation, episodic events, and anthropogenic activities - past, present and future - affect the quantity and quality of river discharge are discussed in the final two chapters. The book contains 26 tables and more than 165 figures - many in full color - including global and regional maps. The book's extensive appendix presents the 1534-river database as a series of 44 tables that provide quantitative data regarding the discharge of water, sediment and dissolved solids. The complete database is also presented within a GIS-based package available online at www.cambridge.org/milliman. River Discharge to the Coastal Ocean provides an invaluable resource for researchers, professionals and graduate students in hydrology, oceanography, geology, geomorphology and environmental policy
    Type of Medium: Monograph available for loan
    Pages: VIII, 384 S. , Ill., graph. Darst., Kt.
    ISBN: 9780521879873
    Classification:
    Sedimentology
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: PIK N 454-07-0073
    In: LOICZ reports & studies
    Type of Medium: Monograph available for loan
    Pages: 125 S. , Ill., graph. Darst.
    Series Statement: LOICZ reports & studies 3
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Call number: SR 90.0002(529-J)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, J-40 S. + 9 pl.
    Series Statement: U.S. Geological Survey professional paper 529-J
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: G 6817/1
    Type of Medium: Monograph available for loan
    Pages: XV, 375 S. : Ill., graph. Darst.
    Series Statement: Recent sedimentary Carbonates 1
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 5
    Call number: AWI G4-02-0054
    In: Coastal Systems and Continental Margins, Vol. 2
    Description / Table of Contents: Greenhouse-induced climate warming increasingly appears to be a reality, and the warming climate could be accompanied by an accelerated sea level rise - as much as 60-100 cm over the next century. What is commonly absent in the discussion of rising sea level, however, is the role played by the subsidence of low-lying coastal areas, which can have a far greater local effect than the eustatic rise of the sea. The combined sea-level rise and land subsidence will almost certainly make the greatest impact on coastal societies in the densely populated regions of southern Asia, but its effects will be felt globally. This volume explores the concepts of sea-level rise and coastal subsidence, both natural and anthropogenically accelerated, in the form of a series of case studies in such diverse locations as Bangkok, Bangladesh, Venice, and the Niger and Mississippi deltas, as well as a discussion of the economic, engineering and policy responses that must be considered if the effects of local sea-level rise are to be mitigated.
    Type of Medium: Monograph available for loan
    Pages: xiv, 369 S. : graph. Darst.
    ISBN: 0792339339
    Series Statement: Coastal Systems and Continental Margins 2
    Language: English
    Note: Table of contents: In Memoriam: J. M. Broadus. - Introduction: Sea-level Rise and Coastal Subsidence - Towards Meaningful Strategies / J. D. Milliman, B. U. Haq. - PART I: PROCESSES AND PROBLEMS. - 1 Global Sea-level Rise: Past and Future / S. C. B. Raper, T. M. L. Wigley, R. A. Warrick. - Observed Changes in Global Mean Sea Level. - Observed Changes in Global Mean Temperature. - The climate model. - Factors contributing to sea-level rise. - Temperature and Sea-Level Rise Results. - Summary and Conclusions. - Appendix: Radiative Forcing. - 2 Land Subsidence in Coastal Lowlands / Saskia Jelgersma. - Introduction. - Geological Setting. - Subsidence in Coastal Lowlands. - Methods to Control or Inhibit Induced Subsidence. - Conclusions. - 3 River-Sediment Inputs to Major Deltas / Robert H. Meade. - Introduction. - Tabulations of Discharge Data for Major Rivers. - Spatial Distributions of Sediment Sources and Sinks. - Temporal Variations in River-Sediment Discharge. - Storage of Sediment in Large River Systems. - Human Influences on River-Sediment Loads. - 4 Coastal Erosion and Rising Sea-Level / E. C. F. Bird. - Introduction. - Submerging Coastlines. - Coastline Changes. - Cliff Erosion. - Beach Erosion. - Erosion on Deltaic Coasts. - Erosion of Coastal Swamps. - Erosion of Developed Coastlines. - Conclusion. - PART II: CASE STUDIES. - 5 Land Subsidence in Bangkok during 1978-1988 / Prinya Nutalaya, R. N. Yong, Thongchai Chumnankit, Somkid Buapeng. - Introduction. - Land Subsidence Prior to 1978. - 1978 to 1988. - Effects of Land Subsidence. - Aquifer Delineation. - Source and Age of Ground Water. - Geotechnical Properties of Soils. - Mathematical Modeling to Predict Subsidence and Recharge Response. - Recommendations. - 6 Coastal Erosion in the Gulf of Thailand / S. Vongvisessomjai, R. Polsi, C. Manotham, D. Srisaengthong, S. Charulukkana. - Introduction. - Oceanographic Conditions. - Coastal Morphology. - Summary. - 7 Nature of Sediment Load in the Ganges-Brahmaputra River Systems in India / V. Subramanian, A. L. Ramanathan. - Introduction. - Description of the Basins. - Sediment and Water Discharge. - Basin Lithology. - Natural (Tectonic) and Human Impact on Sediment Load. - Erosion vs Deposition. - Nature of Sediment Load. - Conclusion. - 8 Subsidence of the Ganges-Brahmaputra Delta of Bangladesh and Associated Drainage, Sedimentation and Salinity Problems / Mahmood Alam. - Introduction. - Geotectonics. - Depositional Sequence. - Subsidence of the Basin and Progradation of the Delta. - Floods and Drainage Problems. - Effects of Recent Engineering Projects. - Salinity. - Sea-Level Rise. - Conclusions. - 9 Tectonic, Eustatic and Isostatic Changes along the Indian Coast / K. R. Subrahmanya. - Introduction. - Quaternary Eustatic Changes. - Holocene Uplift and Subsidence. - Most Recent Sea-Level Changes along the Indian Coast. - Conclusions. - 10 Effect of Sea-Level Rise and Human Activity on the Yangtze Delta, China / Ren Mei-e, J. D. Milliman. - The Yangtze River and its Delta. - Sea-Level Rise and Subsidence. - Impact of a Future Sea-Level Rise and Changes in Landuse and the Yangtze River. - Concluding Statement. - 11 Rising Sea-Level and Subsidence of the Northern Nile Delta: A Case Study / Mahmoud Kh. El-Sayed. - Introduction. - The Nile Delta. - Present-Day Use of the Northern Nile Delta. - Nile Damming and its Effect. - Impact of Climate Changes and Sea-Level Rise on the Nile Delta. - Scenario Based on Present-Day Assumptions and Socio-Economic Conditions in the Northern Nile Delta. - Management of the Northern Nile Delta. - Conclusions. - 12 Land Subsidence and Sea-Level Rise: The Case of the Po Delta Region, Italy / G. Sestini. - Introduction. - Historical Evolution of the NW Adriatic Coast. - Subsidence and its Impact. - Impact of Changes to River Sediment Discharge. - Discussion. - Conclusions. - 13 The Niger Delta and Sea-Level Rise / A. Chidi Ibe. - Introduction. - Tectonic and Sedimentary Evolution. - General Geomorphology. - Coastal Processes. - Erosion Scenario. - Change in Fluvial Sediment/Water Input to the Delta. - Socio-Economic Setting. - Concluding Statements and Suggestions. - 14 Sea-Level Rise and the Stability of Barrier Islands, with special reference to the Wadden Sea / H. Postma. - Post-Glacial Evolution. - Present-Day Conditions. - Future Sea-Level Rise. - Conclusions. - 15 Subsidence, Sea-Level Rise, and Wetland Loss in the Lower Mississippi River Delta / J. T. Wells. - Introduction. - Geological Setting and History. - Sea-Level Rise and Subsidence. - Subdeltas and Wetland Loss. - The Sediment Problem. - Future Mitigation: Artifical Diversions. - PART III: STRATEGIES. - 16 Economizing Human Responses to Subsidence and Rising Sea Level / J. M. Broadus. - Introduction. - Example Assessments for Bangladesh and Egypt. - An Extension of Crude Loss Estimates. - Qualitative Considerations. - Economic Considerations in Human Responses. - Summary. - 17 Man-Made Projects and Relative Sea-Level Rise / J. G. de Ronde. - General Considerations of Impacts. - A Preliminary Study for The Netherlands. - Policy Analysis. - 18 Impact of Sea Level Rise on Flood Control in Bangkok and Vicinity / Sanga Sabhasri, Ksemsan Suwarnarat. - Introduction. - Flood Control Plans. - Impact of Upstream Agricultural Development. - Land Subsidence. - Sedimention due to the Chao Praya River. - Coastal Vulnerability: Hazards and Strategies / B. U. Haq, J. D. Milliman. - Introduction. - Impacts. - of Accelerated Sea-Level Rise on Coastal Areas. - Impacts of Sea-Level Rise. - Adaptive Strategies. - Examples of Action and Consequences of Inaction. - Concluding Statement. - List of Contributors. - Geographic Index.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 5 (1987), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 28 (1981), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Agglutinated deep-sea benthonic foraminifera with tests composed of phillipsite are documented and illustrated from a red clay sequence in a Giant Piston Core from the central North Pacific. Associated with the benthonic foraminifera are phillipsite crystal rosettes and aggregates of phiilipsite crystals. The benthonic foraminifera and phillipsite crystals constitute most of the 〉 38 μm fraction, but have little effect upon the mean size of the red clay sediments.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 24 (1977), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 23 (1976), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The attached foraminifera, Miniacina miniacea, is a major sedimentary component on the outer shelf off central and southern Morocco, particularly in water depths between 95 and 115 m, where concentrations generally exceed 40% of the carbonate fraction. Predominance of this species may be largely a function of the relatively great water depths which preclude optimal growth of other encrusting organisms.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 22 (1975), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Oolitic sediments occur over large portions of the outer continental shelf off northernmost Brazil and southern French Guiana. Carbon-14 dates, stable isotope values and analogies with similar deposits from other areas in the world indicate that the ooids were formed in shallow water (possibly protected hypersaline environments) during low stands of sea level. In contrast to both modern ooids and other relict ooids, however, the Amazon shelf ooids are composed entirely of magnesian calcite (12 mol % MgCO3) and possess radial crystal microstructures.A comparison of water depths and ages of the Amazon ooids with the generally accepted eustatic sea level curve indicates that the Amazon shelf subsided more than 100 m 16-21 thousand years ago. Prior to and subsequent to the subsidence, however, the outer shelf remained relatively stable.
    Type of Medium: Electronic Resource
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