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  • 1
    Call number: PIK N 071-97-0047 ; PIK N 071-97-0169
    In: IPCC Technical Paper
    Type of Medium: Monograph available for loan
    Pages: 51 S.
    ISBN: 9291691011
    Series Statement: IPCC Technical Paper
    Language: English
    Location: A 18 - must be ordered
    Location: A 18 - must be ordered
    Branch Library: PIK Library
    Branch Library: PIK Library
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  • 2
    Call number: PIK N 071-97-0170
    In: IPCC Technical Paper
    Type of Medium: Monograph available for loan
    Pages: 48 p.
    ISBN: 929169102x
    Series Statement: IPCC Technical Paper
    Language: English
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 98.0091 ; PIK N 455-97-0197
    Type of Medium: Monograph available for loan
    Pages: XI, 230 S.
    ISBN: 3540618449
    Uniform Title: Global warming
    Classification:
    Meteorology and Climatology
    Language: German
    Location: Upper compact magazine
    Location: A 18 - must be ordered
    Branch Library: GFZ Library
    Branch Library: PIK Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: AWI A5-98-0026
    Description / Table of Contents: Dr Houghton has revised the acclaimed first edition of The Physics of Atmospheres in order to bring this important textbook completely up-to-date. Several factors have led to vigorous growth in the atmospheric sciences, particularly the availability of powerful computers for detailed modelling, the investigation of the atmospheres of other planets, and techniques of remote sensing. The author describes the physical processes governing the structure and circulation of the atmosphere. Simple physical models are constructed by applying the principles of classical thermodynamics, radiative transfer and fluid mechanics, together with analytic and numerical techniques. These models are applied to real planetary atmospheres. This new edition is essential for undergraduates or graduate students studying atmospheric physics, climatology or meteorology, as well as planetary scientists with an interest in atmospheres.
    Type of Medium: Monograph available for loan
    Pages: XIV, 271 S. , Ill., graph. Darst
    Edition: 2nd ed., reprint.
    ISBN: 0521339561
    Language: English
    Note: Contents: Preface to first edition. - Preface to second edition. - Acknowledgements. - 1 Some basic ideas. - 1.1 Planetary atmospheres. - 1.2 Equilibrium temperatures. - 1.3 Hydrostatic equation. - 1.4 Adiabatic lapse rate. - 1.5 Sandström's theorem. - Problems. - 2 A radiative equilibrium model. - 2.1 Black-body radiation. - 2.2 Absorption and emission. - 2.3 Radiative equilibrium in a grey atmosphere. - 2.4 Radiative time constants. - 2.5 The greenhouse effect. - Problems. - 3 Thermodynamics. - 3.1 Entropy of dry air. - 3.2 Vertical motion of saturated air. - 3.3 The tephigram. - 3.4 Total potential energy of an air column. - 3.5 Available potential energy. - 3.6 Zonal and eddy energy. - Problems. - 4 More complex radiation transfer. - 4.1 Solar radiation: its modification by scattering. - 4.2 Absorption of solar radiation by ozone. - 4.3 Absorption by single lines. - 4.4 Transmission of an atmospheric path. - 4.5 The integral equation of transfer. - 4.6 Integration over frequency. - 4.7 Heating rate due to radiative processes. - 4.8 Cooling by carbon dioxide emission from upper stratosphere and lower mesosphere. - 4.9 Bandmodels. - 4.10 Continuum absorption. - 4.11 Global radiation budget. - Problems. - 5 The middle and upper atmospheres. - 5.1 Temperature structure. - 5.2 Diffusive separation. - 5.3 The escape of hydrogen. - 5.4 The energy balance of the thermosphere. - 5.5 Photochemical processes. - 5.6 Breakdown of thermodynamic equilibrium. - Problems. - 6 Clouds. - 6.1 Cloud formation. - 6.2 The growth of cloud particles. - 6.3 The radiative properties of clouds. - 6.4 Radiative transfer in clouds. - Problems. - 7 Dynamics. - 7.1 Total and partial derivatives. - 7.2 Equations of motion. - 7.3 The geostrophic approximation. - 7.4 Cyclostrophic motion. - 7.5 Surfaces of constant pressure. - 7.6 The thermal wind equation. - 7.7 The equation of continuity. - Problems. - 8 Atmospberic waves. - 8.1 Introduction. - 8.2 Sound waves. - 8.3 Gravity waves. - 8.4 Rossby waves. - 8.5 The vorticity equation. - 8.6 Three dimensional Rossby-type waves. - Problems. - 9 Turbulence. - 9.1 The Reynolds number. - 9.2 Reynolds stresses. - 9.3 Ekman's solution. - 9.4 The mixing-length hypothesis. - 9.5 Ekman pumping. - 9.6 The spectrum of atmospheric turbulence. - Problems. - 10 The general circulation. - 10.1 Labaratory experiments. - 10.2 A symmetric circulation. - 10.3 Inertial Instability. - 10.4 Barotropic instability. - 10.5 Baroclinic instability. - 10.6 Sloping convection. - 10.7 Energy transport. - 10.8 Transport of angular momentum. - 10.9 The general circulation of the middle atmosphere. - Problems. - 11 Numerical modelling. - 11.1 A barotropic model. - 11.2 Baroclinic models. - 11.3 Primitive equation models. - 11.4 Inclusion of orography. - 11.5 Convection. - 11.6 Moist processes. - 11.7 Radiation transfer. - 11.8 Inclusion of clouds. - 11.9 Sub grid scale processes. - 11.10 Transfer across the surface. - 11.11 Forecasting models. - 11.12 Other models. - Problems. - 12 Global observation. - 12.1 What Observations are required?. - 12.2 ConventionaJ observations. - 12.3 Remote sounding from satellites. - 12.4 Remote sounding of atmospheric temperature. - 12.5 Remote measurements of composition. - 12.6 Other remote sounding observations. - 12.7 Observations from remote platforms. - 12.8 Achieving global coverage. - Problems. - 13 Atmospheric predictability and climatic change. - 13.1 Short-term predictability. - 13.2 Variations of climate. - 13.3 Atmospheric feedback processes. - 13.4 Different kinds of predictability. - 13.5 Jupiter's Great Red Spot. - 13.6 The challenge of climate research. - Problems. - Appendices. - 1 Some useful physical constants and data on dry air. - 2 Properties of water vapour. - 3 Atmospheric composition. - 4 Relation of geopotential to geometric height. - 5 Model atmospheres (0-105 km). - 6 Mean reference atmosphere (110- 500 km). - 7 The Planck function. - 8 Solar radiation. - 9 Absorption of solar radiation by oxygen and ozone. - 10 Spectral band information. - Bibliography. - References to works cited in the text. - Answers to problems and hints to their solution. - Index.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 5
    Call number: PIK N 071-99-0123
    Type of Medium: Monograph available for loan
    Pages: 347 p.
    ISBN: 0521559626
    Language: English
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 6
    ISSN: 1520-4804
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1520-4804
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1365-2958
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: Degradation of protocatechuate in Pseudomonas putida is accomplished by the products of the pca genes (pcaH,G, pcaBDC, pcaI, J and pcaF ). In P. putida, all these genes (with the exception of pcaH,G ) are activated by the regulatory protein PcaR, in association with the pathway intermediate β-ketoadipate. Having previously cloned and characterized the pcaR locus, we have overexpressed and purified the PcaR protein to homogeneity. The purified PcaR protein was shown to form a homodimer in solution and to bind specifically to its own promoter, as well as to the promoter regions of pcaI, J and pcaF. Subsequent footprint analyses demonstrated that the binding of PcaR to its own promoter occurs within a footprint that extends from the −20 to the +4 position. In contrast, PcaR appeared to interact with the inducible pcaI, J promoter as a dimer of dimers; binding in tandem within a dual footprint encompassing both the ‘−35′ and the ‘−10’ regions of the promoter sequence. The similarities and differences between the two binding patterns correlate well with the very different effects that PcaR has upon transcription at each of the promoter sequences. The interactions at the pcaI, J promoter are reminiscent of those exhibited by the MerR family of regulatory proteins. However, as PcaR bears very little primary sequence homology to any of the regulatory proteins within this family, the results presented here reveal the possible existence of a new series of functionally related transcriptional inducers.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 386 (1997), S. 345-345 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Laboratory Earth: The Planetary Gamble We Can't Afford To Lose by Stephen Schneider Basic Books: 1997. Pp.174. $20. Weidenfeld & Nicholson£11.99 Humans have rarely anticipated environmental pollution; action and pollution control have generally followed on from ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 383 (1996), S. 572-572 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] SIR á€" John Maddox questions the validity of the 'consensus' sometimes associated with the conclusions of the Intergovernmental Panel on Climate Change (IPCC) (Nature 383, 17; 1996). As he points out, the nature of the scientific process, which is built on debate, argument and ...
    Type of Medium: Electronic Resource
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