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  • 1
    Monograph available for loan
    Monograph available for loan
    San Diego [u.a.] : Academic Press
    Associated volumes
    Call number: AWI A5-99-0315
    In: International Geophysics Series, Vol. 65
    Type of Medium: Monograph available for loan
    Pages: XVII, 469 S.
    ISBN: 0121995704
    Series Statement: International Geophysics Series 65
    Language: English
    Note: Contents: Preface. - Acknowledgements. - Publisher's Credits. - Part I Basic Concepts. - Chapter 1 Composition, Structure, and State. - 1.1 Composition of the Atmosphere. - 1.2 Composition of the Ocean. - 1.3 Pressure. - 1.4 Density. - 1.5 Temperature. - 1.6 Kinetic-Molecular Model of the Ideal Gas. - 1.7 Equation of State for Air. - 1.8 Equation of State for Seawater. - 1.9 Compressibility and Expansion Coefficients. - 1.10 Hydrostatic Equilibrium. - Notes. - Problems. - Chapter 2 First and Second Laws of Thermodynamics. - 2.1 Work. - 2.2 Heat. - 2.3 First Law. - 2.4 Applications of the First Law to Ideal Gases. - 2.5 Entropy. - 2.6 Second Law. - 2.7 Equilibrium and the Combined First and Second Laws. - 2.8 Calculation of Thermodynamic Relations. - 2.9 Heat Capacity. - 2.10 Dry Adiabatic Processes in the Atmosphere. - 2.11 Adiabatic Processes in the Ocean. - Notes. - Problems. - Chapter 3 Transfer Processes. - 3.1 Time-dependent Thermodynamics. - 3.2 Radiant Energy. - 3.3 Radiative Transfer. - 3.4 Diffusive Transfer Processes. - 3.5 Turbulence and Turbulent Transport. - 3.6 Time-dependent Equations for the Ocean and Atmosphere. - Notes. - Problems. - Chapter 4 Thermodynamics of Water. - 4.1 Molecular Structure and Properties of Water. - 4.2 Thermodynamic Degrees of Freedom. - 4.3 Phase Equilibria. - 4.4 Atmospheric Humidity Variables. - 4.5 Colligative Properties of Water Solutions. - 4.6 Simple Eutectics. - Notes. - Problems. - Chapter 5 Nucleation and Diffusional Growth. - 5.1 Surface Tension. - 5.2 Nucleation of the Liquid Phase. - 5.3 Nucleation of the Ice Phase. - 5.4 Diffusional Growth of Cloud Drops. - 5.5 Ice Crystal Morphology and Growth. - 5.6 Formation of the Initial Sea Ice Cover. - 5.7 Formation of Sea Ice Transition and Columnar Zones. - Notes. - Problems. - Part II Applications. - Chapter 6 Moist Thermodynamic Processes in the Atmosphere. - 6.1 Combined First and Second Laws. - 6.2 Isobaric Cooling. - 6.3 Cooling and Moistening by Evaporation of Water. - 6.4 Saturation by Adiabatic, Isobaric Mixing. - 6.5 Saturated Adiabatic Cooling. - 6.6 The Ice Phase. - 6.7 Conserved Moist Thermodynamic Variables. - 6.8 Aerological Diagrams. - Notes. - Problems. - Chapter 7 Static Stability of the Atmosphere and Ocean. - 7.1 Stability Criteria. - 7.2 Stability of a Saturated Atmosphere. - 7.3 Processes Producing Changes in Stability. - Notes. - Problems. - Chapter 8 Cloud Characteristics and Processes. - 8.1 Cloud Classification and Characteristics. - 8.2 Precipitation Processes. - 8.3 Radiative Transfer in a Cloudy Atmosphere. - 8.4 Fogs, Stratus Clouds, and Stratocumulus Clouds. - 8.5 Cumuliform Clouds. - 8.6 Parameterization of Cloud Microphysical Processes. - Notes. - Problems. - Chapter 9 Ocean Surface Exchanges of Heat and Freshwater. -
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 115 (1977), S. 1463-1491 
    ISSN: 1420-9136
    Keywords: Monsoon evolution ; monsoon structure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary An attempt is made to identify the basic structure of the planetary scale monsoon and to define and describe the various mechanisms effecting or producing that structure and its variation on a variety of time scales. Both observational and theoretical descriptions are used to define the monsoon system or to point towards problems that require clarification. The basic mean summer and winter monsoon regimes are described and a discussion presented on their degree of dependence on the distributions of orography, the form and distribution of land and ocean and the state of the interactive oceans adjacent to the major land masses. It is suggested that orography plays a critical role in determining the state of the mean summer and winter circulations behaving principally as an elevated heat source in summer and a mechanical perturber of the mean flow in winter. The spatial variation of sea-surface temperature and the distribution of land are shown to be theprimum mobile of the mean seasonal monsoon. Various modes and time scales of the variable monsoon are defined. It is shown that the principal time scale variation or phasing of theinterseasonal transition is determined by the different response times of the oceans and land areas to variable solar heating. The reaction of the ocean is a strong function of latitude because of its ability to be heated by solar radiation and mixed mechanically by the atmosphere. The return heating distribution imposed on the atmosphere by the ocean strongly effects the circulation. The inclusion of a hydrology cycle adds a further time scale to the monsoon system allowing much more rapid variations to be superimposed on the modulations caused by radiative and sensible heating effects. The inclusion of clouds introduces a furtherintra-seasonal time-scale into the monsoon circulation causing ‘break-like’ variations of the precipitation pattern and circulation fields during the late summer. Finally, a brief discussion is given on the various forms of interhemispheric interaction. It is suggested that contrary to earlier theoretical speculation, the equatorial latitudes may be considerably more ‘porous’ to mid-latitude disturbances than hitherto anticipated.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 401 (1999), S. 356-360 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Climate variability in the Indian Ocean region seems to be, in some aspects, independent of forcing by external phenomena such as the El Niño/Southern Oscillation. But the extent to which, and how, internal coupled ocean–atmosphere dynamics determine the state of the Indian Ocean ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 248 (1974), S. 212-213 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] To obtain a Eulerian data set, thfc Lagrangian data required transformation. As no general analytical transformation exists2, the Eulerian information was obtained by computing daily averages of all the measured Lagrangian quantities in each area of 10 latitude by 20 longitude. The resulting ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 56 (1995), S. 1-1 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 390 (1997), S. 562-564 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] If events run true to form, the present El Niño is approaching a climax — which is why, acknowledging a Christmas connection, the phenomenon was so named. Predicting these events and their consequences is a daunting task, but there is progress to ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Climatic change 6 (1984), S. 377-390 
    ISSN: 1573-1480
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The pervasive opinion on the relationship between the state of the climate and the increasing concentration of CO2 is that a general global warming will occur with social, economical and environmental corollaries that may be adverse. However, there exist a number of dissenting arguments that call for a much smaller increase in global temperature or even an induced global cooling. Furthermore, the positive biological effects of a greater atmospheric CO2 loading are emphasized. The difference of opinion is highlighted in two recent publications: CO 2, Friend or Foe by Sherwood Idso and Carbon Dioxide: A Second Assessment by the National Academy of Science CO2/Climate Review Committee. Using the two publications as focal points, some personal remarks are made regarding the controversy and the relative merits of the scientific arguments.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2016-09-01
    Print ISSN: 0002-1962
    Electronic ISSN: 1435-0645
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Wiley
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  • 9
    Publication Date: 1981-08-01
    Print ISSN: 0036-8733
    Electronic ISSN: 1946-7087
    Topics: Biology , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 10
    Publication Date: 2018-01-22
    Print ISSN: 0894-8755
    Electronic ISSN: 1520-0442
    Topics: Geography , Geosciences , Physics
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