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  • 1
    Monograph available for loan
    Monograph available for loan
    Sausalito, Calif. : Univ. Science Books
    Call number: AWI A13-06-0025
    Type of Medium: Monograph available for loan
    Pages: XIII, 353 S. , Ill., graph. Darst. , 26 cm
    Edition: 2. ed.
    ISBN: 1891389351
    Note: Contents: Preface. - 1 Introduction and Historical Development. - 2 Physical Description of the Climate System. - 2.1 Atmosphere. - 2.1 .1 Atmospheric composition. - 2.1.2 Temperature profiles. - 2.1.3 Energy balances. - 2.1.4 Average surface temperature patterns. - 2.1.5 Large-scale hemispheric circulation patterns: Three-cell structure. - 2.1.6 Land/sea breezes and monsoons. - 2.2 Oceans. - 2.2.1 Seawater composition. - 2.2.2 Ocean temperatures. - 2.2.3 Ocean circulation. - 2.3 Sea Ice. - 2.3.1 Global sea ice distributions. - 2.3.2 Sea ice formation and growth. - 2.3.3 Sea ice ablation. - 2.3.4 Sea ice composition and properties. - 2.3.5 Sea ice topography. - 2.3.6 Sea ice concentration and velocity. - 2.4 Atmosphere/Ocean/lce Interconnections. - 2.4.1 Impacts of the atmosphere. - 2.4.2 Impacts of the ocean. - 2.4.3 An example of atmosphere/ocean interconnections: The El Nino/Southern Oscillation. - 2.4.4 North Atlantic Oscillation (NAO). - 2.4.5 Impacts of the ice. - 3 Basic Model Equations. - 3.1 Fundamental Equations. - 3.1.1 Conservation of momentum. - 3.1.2 Conservation of mass. - 3.1.3 First law of thermodynamics. - 3.1.4 Equation of state. - 3.2 Summary of the Basic Predictive Equations for the Atmosphere. - 3.3 Vertical Coordinate Systems. - 3.4 Atmospheric and Ocean Dynamics. - 3.4.1 Vorticity and divergence equations. - 3.4.2 Baroclinic models. - 3.5 Early General Atmospheric Circulation Model of the Atmosphere. - 3.6 Radiative and Cloud Processes. - 3.6.1 Radiation: Basic principles. - 3.6.2 Radiation: Physical laws. - 3.6.3 Solar radiation. - 3.6.4 Radiation: Effect of aerosols. - 3.6.5 Net heating/cooling rates. - 3.6.6 Moisture and precipitation. - 3.6.7 Clouds. - 3.6.8 Cumulus parameterization, general theory. - 3.6.9 Convective adjustment parameterization. - 3.6.10 More refined schemes for cumulus convection. - 3.7 Surface Processes. - 3.7.1 Boundary fluxes at the Earth's surface. - 3.7.2 Computation of surface temperature and hydrology. - 3.8 Ocean Models. - 3.8.1 Ocean model fundamentals. - 3.8.2 Parameterization of ocean eddies. - 3.8.3 Generalized coordinate systems for ocean modeling. - 3.8.4 lsopycnal ocean model. - 3.9 Sea Ice Models. - 3.9.1 lce thermodynamics. - 3.9.2 Ice dynamics. - 3.10 River Transport. - 4 Basic Methods of Solving Model Equations. - 4.1 Finite Differences. - 4.2 Finite Differencing in Two Dimensions. - 4.3 Spectral Method. - 4.3.1 Vibrating string example. - 4.3.2 Gibbs phenomenon. - 4.3.3 More general considerations of Fourier series and integrals. - 4.4 Spherical Representation. - 4.5 Spectral Transform Technique. - 4.6 Vertical Representation. - 4.7 Lagrangian and Semi-Lagrangian Methods. - 4.8 Spectral Element Method. - 5 Examples of Simulations of Present-Day Climate. - 5.1 Simulations of the Atmosphere. - 5.2 Simulations of the Ocean. - 5.3 Simulations of Sea Ice. - 5.4 Coupled Atmosphere, Land / Vegetation, Ocean, and Sea Ice Simulations. - 5.5 El Nino Simulations. - 5.6 Regional Climate Modeling. - 5.7 Modeling Groups. - 6 Climate Sensitivity Experiments. - 6.1 Sample Early Paleoclimate Simulations. - 6.2 Sample Later Paleoclimate Simulations. - 6.3 Sample Simulation of the Last Millennium. - 6.4 Sample Early Simulations of the El Nino/ Southern Oscillation. - 6.5 Sample Later Simulation of the El Nino/ Southern Oscillation. - 6.6 Research on the Climatic Effects of Increasing Greenhouse Gases and Aerosols. - 6.7 Sample Early Climate Model Simulations of the Effects of Greenhouse Gases. - 6.8 Later Simulations of the Effects of Greenhouse Gases, Aerosols, and Other Climate Forcings. - 6.9 Climate Modeling with the Carbon Cycle. - 6.10 Possible Climatic Effects Due to Nuclear War. - 6.11 Overview of Climate Sensitivity Studies. - 7 Outlook for Future Developments. - 7.1 Climate Model Evolution and Status. - 7.2 Issues Involved in Coupling. - 7.3 Continuing Needs. - 7.4 Two Further Potential Uses of Climate Models. - 7.5 National Research Council Assessment. - 7.6 Concluding Remarks. - APPENDIX A Vector Calculus. - A.1 Vector Operations in a Cartesian Coordinate System. - A.1.1 Vector addition and subtraction. - A.1.2 Vector multiplication. - A.1.3 Vector differentiation. - A.1.4 Gradient (del) operator. - A.2 Vector Operations in Generalized and Spherical Coordinates. - A.3 Vectors on a Rotating Sphere. - APPENDIX B Legendre Polynomials and Gaussian Quadrature. - APPENDIX C Derivation of Energy Equations. - APPENDIX D Unit Abbreviations. - APPENDIX E Physical Constants in Système International (SI) Units, and Typical Surface Albedos. - APPENDIX F Conversions and Prefixes. - APPENDIX G Greek Alphabet. - APPENDIX H Acronyms. - APPENDIX I Aerosols. - APPENDIX J Solar Radiation, Including Effects of Aerosols. - APPENDIX K Internet Sites for Climate Modeling and Climate Data. - APPENDIX L Computer Architectures Used in Climate Modeling: Definition of Terms. - Bibliography. - Index. - About the Authors.
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Mill Valley, Cal. : Univ. Science Books
    Call number: AWI A13-92-0295
    Description / Table of Contents: Contents: Preface. - 1 Introduction and Historical Development. - 2 Physical Description of the Climate System. - Atmosphere . - Atmospheric composition. - Temperature profiles. - Energy balances. - Average surface temperature patterns. - Large-scale hemispheric circulation patterns: three-cell structure. - Land/sea breezes and monsoons. - Oceans. - Seawater composition. - Ocean temperatures. - Ocean circulation. - Sea Ice. - Global sea ice distributions. - Sea ice formation and growth. - Sea ice ablation. - Sea ice composition and properties. - Sea ice topography. - Sea ice concentration and velocity. - Atrnosphere/Ocean/Ice Interconnections. - Impacts of the atmosphere. - Impacts of the ocean. - An example of atmosphere/ocean interconnections: the El Niño/Southern Oscillation. - Impacts of the ice. - 3 Basic Model Equations. - Fundamental Equations. - Conservation of momentum. - Conservation of mass. - First law of thermodynamics. - Equation of state. - Summary of Basic Predictive Equations for the Atmosphere. - Vertical Coordinate Systems. - Atmospheric and Ocean Dynamics. - Vorticity and divergence equations. - Rossby wave equation. - Baroclinic models. - Early General Circulation Model of the Atmosphere. - Radiative and Cloud Processes. - Radiation: basic principles. - Radiation: physical laws. - Solar radiation. - Net heating/cooling rates. - Clouds. - Precipitation and cloud processes. - Convective adjustment parameterization. - More refined schemes for cumulus convection. - Surface Processes. - Boundary fluxes at the earth's surface. - Computation of surface temperature and hydrology. - Ocean Models. - Quasi-geostrophic Ocean Circulation Model. - Sea Ice Models. - Ice thermodynamics. - Ice dynamics. - 4 Basic Methods of Solving Model Equations. - Finite Differences. - Finite Differencing in Two Dimensions. - Spectral Method. - More general considerations of Fourier series and integrals. - Spherical Representation. - Spectral Transform Technique. - Vertical Representation. - 5 Examples of Simulations of Present-Day Climate. - Simulations of the Atmosphere. - Zonal mean temperature. - Zonal mean wind. - Meridional mean wind. - Zonal mean vertical velocity. - Geographical distribution of surface air temperature. - Geographical distribution of sea level pressure. - Geographical distribution of the 300 mb zonal component of the wind. - Geographical distribution of precipitation. - Intermodel comparisons. - Simulations of the Ocean. - Ocean circulation. - Ocean heat transport. - Surface heights and temperatures. - Quasi-geostrophic results. - Simulations of Sea Ice. - Sea ice thickness and vertical temperature profiles. - Geographical distribution of sea ice thickness and concentration. - Geographical distribution of sea ice velocities. - Weddell polynya. - Impact of ice dynamics on sea ice simulations. - Sea ice modeling successes and failures. - Coupled Atmosphere, Ocean, Sea Ice Simulations. - Modeling Groups. - 6 Climate Sensitivity Experiments. - Paleoclimate Simulations. - Simulations of El Niño/Southern Oscillation. - Climatic Effects of Carbon Dioxide. - Possible Climatic Effects Due to Nuclear War. - Overview of Climate Sensitivity Studies. - 7 Outlook for Future Developments. - APPENDIX A Vector Calculus. - APPENDIX B Legendre Polynomials and Gaussian Quadrature. - APPENDIX C Derivation of Energy Equations. - APPENDIX D Finite Difference Barotropic Forecast Model. - APPENDIX E Spectral Transform Technique. - APPENDIX F Finite Difference Shallow Water Wave Equation Model. - APPENDIX G Atmospheric General Circulation Model Equations. - APPENDIX H Unit Abbreviations. - APPENDIX I Physical Constants in International Systemof Units (SI). - APPENDIX J Conversions. - APPENDIX K Greek Alphabet . - APPENDIX L Acronyms. - References. - Index.
    Description / Table of Contents: An introduction to three-dimensional climate modeling by Warren M. Washington and Claire L. Parkinson provides a guide to the development and use of computer models of the earth's climate. The book describes the basic theory of climate simulation, including the fundamental equations and relevant numerical techniques for simulating the atmosphere, oceans, and sea ice. Results for a variety of past, present and future climates are shown and compared with observations.
    Type of Medium: Monograph available for loan
    Pages: XIV, 422 S. : Ill., graph. Darst., Kt.
    ISBN: 0935702520
    Branch Library: AWI Library
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  • 3
    Call number: AWI A4-95-0153 ; AWI G7-84-0296(2)
    In: NASA SP
    Type of Medium: Monograph available for loan
    Pages: XVI, 296 S.
    Series Statement: NASA SP 489
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 4
    Call number: AWI G7-84-0296(1)
    In: NASA SP
    Type of Medium: Monograph available for loan
    Pages: 296 S.
    Series Statement: NASA SP 459
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 4 (1989), S. 39-44 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Multiyear averaging in studies seeking long-term trends can be risky and misleading. It is shown here that a change of 1 year in the starting point of the averaging done in generating a multiyear-average sequence can make a dramatic difference in the appearance of the sequence, even including whether the apparent trend is upward or downward. An example is given in which the same time series, when grouped to 3-year averages by starting in turn at the first, second, and third points of the series, yields one 3-year-average sequence that is monotonically increasing, a second 3-year-average sequence that is monotonically decreasing, and a third 3-year-average sequence that has constant values. Furthermore, it is proven in general that such series can be created for n-year averages for any integer n 〉 2, and can be extended to exceed any desired length. Finally, historical sea-ice data from Iceland are used to illustrate with a long-term climate data set the misrepresentation of climate statistics which can occur through selective multiyear averaging.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Climate dynamics 3 (1988), S. 85-91 
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The effect of orbitally induced insolation changes on Antarctic sea-ice cover are examined by means of a dynamic-thermodynamic seaice model. Results are compared with modified CLIMAP 18 000 B.P. sea-ice reconstructions. Calculations suggest that changes in insolation receipt had only a minor influence on Pleistocene sea-ice distributions. The small response can be explained by a number of factors: albedo effects reduce the insolation perturbation at the surface; some of the shortwave radiation entering the ocean contributes to bottom ablation rather than lateral melting; the radiation perturbation at the upper surface of the ice must go to warming the surface to the melting point before melting ensues; and, finally, the relatively high heat capacity of open water dampens the surface temperature response to altered seasonal insolation perturbations.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Variations in production rates of warm North Atlantic Deep Water (NADW) have been proposed as a mechanism for linking climate fluctuations in the northern and southern hemispheres during the Pleistocene. We have tested this hypothesis by examining the sensitivity of a thermodynamic/dynamic model for Antarctic sea ice to changes in vertical ocean heat flux and comparing the simulations with modified CLIMAP sea-ice maps for 18 000 B.P. Results suggest that changes in NADW production rates, and the consequent changes in the vertical ocean heat flux in the Antarctic, can only account for about 20%–30% of the overall variance in Antarctic sea-ice extent. This conclusion has been validated against an independent geological data set involving a time series of sea-surface temperatures from the subantarctic. The latter comparison suggests that, although the overall influence of NADW is relatively minor, the linkage may be much more significant at the 41 000-year obliquity period. Despite some limitations in the models and geological data, we conclude that NADW variations may have played only a modest role in causing late Pleistocene climate change in the high latitudes of the southern hemisphere. Our conclusion is consistent with calculations by Manabe and Broccoli (1985) suggesting that atmospheric CO2 changes may be more important for linking the two hemispheres.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    GeoJournal 18 (1989), S. 9-20 
    ISSN: 1572-9893
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography
    Notes: Abstract In spite of the importance of sea ice to polar climates, sea ice/climate studies have been limited in the past due to the lack of consistent, long-term, global sea ice records. Satellite passive microwave technology, available since the early 1970s, now provides the potential of generating the desired long-term data sets. With passive microwave data, global sea ice distributions can be mapped on a routine basis every few days, to a spatial resolution on the order of 30 km. The sea ice records generated so far from such satellite data have already been used in many scientific investigations, helping to quantify global sea ice distributions and their seasonal and interannual variations, and to illuminate possible ice/ocean and ice/atmosphere interactions. The results to date augur well for the possibilities once the satellite passive microwave record is long enough to form a true climatic data base.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 2 (1979), S. 149-162 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A large scale numerical time-dependent model of sea ice that takes into account the heat fluxes in and out of the ice, the seasonal occurrence of snow, and ice motions has been used in an experiment to determine the response of the Arctic Ocean ice pack to a warming of the atmosphere. The degree of warming specified is that expected for a doubling of atmospheric carbon dioxide with its associated greenhouse effect, a condition that could occur before the middle of the next century. The results of three 5-year simulations with a warmer atmosphere and varied boundary conditions were: (1) that in the face of a 5 K surface atmospheric temperature increase the ice pack disappeared completely in August and September but reformed in the central Arctic Ocean in mid fall; (2) that the simulations were moderately dependent on assumptions concerning cloud cover; and (3) that even when atmospheric temperature increases of 6–9 K were combined with an order-of-magnitude increase in the upward heat flux from the ocean, the ice still reappeared in winter. It should be noted that a year-round ice-free Arctic Ocean has apparently not existed for a million years or more.
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  • 10
    Publication Date: 2019-07-01
    Description: Following over 3 decades of gradual but uneven increases in sea ice coverage, the yearly average Antarctic sea ice extents reached a record high of 12.8 × 106 km2 in 2014, followed by a decline so precipitous that they reached their lowest value in the 40-y 1979–2018 satellite multichannel passive-microwave record, 10.7 × 106 km2, in 2017. In contrast, it took the Arctic sea ice cover a full 3 decades to register a loss that great in yearly average ice extents. Still, when considering the 40-y record as a whole, the Antarctic sea ice continues to have a positive overall trend in yearly average ice extents, although at 11,300 ± 5,300 km2⋅y−1, this trend is only 50% of the trend for 1979–2014, before the precipitous decline. Four of the 5 sectors into which the Antarctic sea ice cover is divided all also have 40-y positive trends that are well reduced from their 2014–2017 values. The one anomalous sector in this regard, the Bellingshausen/Amundsen Seas, has a 40-y negative trend, with the yearly average ice extents decreasing overall in the first 3 decades, reaching a minimum in 2007, and exhibiting an overall upward trend since 2007 (i.e., reflecting a reversal in the opposite direction from the other 4 sectors and the Antarctic sea ice cover as a whole).
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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