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  • 1
    Monograph available for loan
    Monograph available for loan
    Princeton : Princeton University Press
    Call number: PIK N 070-96-0360
    Type of Medium: Monograph available for loan
    Pages: 488 S.
    ISBN: 0691032661
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  • 2
    Call number: PIK N 076-95-0274
    In: Texte
    Type of Medium: Monograph available for loan
    Pages: 131 S.
    Series Statement: Texte
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  • 3
    Call number: AWI A13-01-0160 ; AWI A13-04-0017
    Type of Medium: Monograph available for loan
    Pages: XXXV, 565 S. : Ill., graph. Darst.
    ISBN: 0444503382
    Note: Contents: Organizers. - Lecturers. - Seminar Speakers. - Participants. - Préface (French). - Preface (English). - MAIN COURSES. - Course 1. The Observed Climate of the 20th Century / by E.M. Rasmusson, M. Chelliah and C.F. Ropelewski. - 1. Climatology: From statistics to science. - 1.1. The evolution of climate science. - 1.2. Characteristics and limitations of the instrumental data bases. - 1.3. Interannual to interdecadal variability. - 1.4. Modern climate diagnostics. - 2. The atmospheric general circulation. - 2.1. From Hadley to the mid-20th century: Theory underconstrained by Observations. - 2.2. Post-World War II: Resolving the controversies. - 2.3. Quantifying the balance requirements. - 2.3.1. Angular momentum balance. - 2.3.2. Atmospheric energy cycle. - 2.3.3. Planetary heat balance. - 2.3.4. Hydrologic cycle. - 3. The annual cycle. - 3.1. Basic controls. - 3.2. Focus on the tropics. - 3.3. A monsoon system perspective. - 3.4. Focus on the extratropics. - 4. Interannual variability. - 4. 1. Atmospheric teleconnections. - 4.2. The ENSO phenomenon: Early investigations. - 4.3. ENSO cycle time series. - 4.4. ENSO warm episode evolution. - 4.5. ENSO global response. - 4.5.1. Tropical anomalies. - 4.5.2. Extratropical anomalies. - 5. Decadal/interdecadal variability. - 5.1. Focus on the tropical oceans. - 5.1.1. Pacific sector. - 5.1.2. Atlantic sector. - 5.2. Focus on the extratropics. - 5.2.1. Northem Hemisphere wintertime temperatures: relattonship to the SO and the NAO. - 5.2.2. North Atlantic and North Pacific. - 5.3. Continental precipitation variability. - 5.3.1 . Sahel rainfall. - 5.3.2. North American drought. - 5.3.3. Indian rainfall. - 5.4. Concluding remarks. - References. - Course 2. Numerical Modelling of the Earth's Climate / by L. Bengtsson. - 1. A strategic approach to climate modelling. - 1.1. Introduction. - 1.2. Dynamics of climate. - 1.2.1. Phillips' experiment. - 1.2.2. The key scientific issues in 1955. - 1.3. Climate modelling for different time-scales. - 2. Climate modelling. - 2.1. lntroduction. - 2.2. The climate model as a mathematical system. - 2.3. Overall design of an atmospheric climate model. - 2.4. Numerical solution. - 2.5. Physical parameterization. - 2.6. Climate model performance. - 3. An atmospheric model for climate simulation and prediction studies. - 3.1. lntroduction. - 3.2. Horizontal diffusion. - 3.3. Surface fluxes and vertical diffusion. - 3.4. Land surface processes. - 3.5. Gravity wave drag. - 3.6. Cumulus convection. - 3.6.1. Adjustment closure. - 3. 7. Stratiform clouds. - 3.8. Radiation. - 3.8.1. Longwave radiation. - 3.8.2. Shortwave radiation. - 3.8.3. Shortwave cloud optical properties. - 3.8.4. Longwave cloud optical properties. - 3.8.5. Effective radii of cloud droplets and icc crystals. - 3.8.6. Surface albedo. - 3.8.7. Solar zenith angle. - 3.9. Model validation. - 3.9.1. Radiation and clouds. - 3.9.2. The hydrological cycle. - 3.9.3. The large scale extra-tropical circulation. - 4. Climate response to greenhouse gas forcing. - 4.1. Introduction. - 4.2. Climate feedback processes. - 4.3. The Wonderland climate model. - 4.4. Forcing experiments with the Wonderland model. - 4.4.1. Response to 2 X CO2 and 2% solar forcing. - 4.4.2. Response to the horizontal and vertical distribution of the forcing. - 4.5. Forcing experiments with more realistic climate models. - 5. Climate change prediction. - 5 .1. Introduction. - 5.2. Mechanisms behind climate change. - 5.2.1. How can climate change?. - 5.2.2. Changes in the solar radiation. - 5.2.3. Changes in the greenhouse gases. - 5.2.4. Changes in atrnospheric aerosols. - 5.2.5. Internal, natural variations. - 5.3. Coupled models. - 5.4. Coupled model experiments. - 5.4.1. Transient greenhouse gas experiment. - 5.4.2. Changes in the energy cycle. - 5.4.3. The hydrological cycle. - 5.4.4. Temperature changes. - References. - Course 3. Ocean Modelling and the Role of the Ocean in the Climate System / by P. Delecluse and G. Madec. - 1. Physical properties of the ocean. - 1.1. General structure. - 1.2. Why does the ocean move?. - 1.2.1. Radiative forcing. - 1.2.2. Momentum flux. - 1.2.3. Turbulent fluxes. - 1.2.4. Freshwater flux. - 1.3. Mean vertical structure. - 1.3.1. Seasonal cycle of the mixed layer. - 1.3.2. Midlatitude thermocline ventilation. - 1.3.3. Equatorial thermocline. - 1.3.4. Deep convection and sea ice. - 1.4. Turbulence of the ocean. - 2. Equations of motion. - 2.1. The physical equations. - 2.1.1. Basic assumptions (refer to Pedlosky, 1987). - 2.1.2. The Primitive Equations. - 2.1.3. The boundary conditions. - 2.2. Horizontal pressure gradient formulation. - 2.2.1. Pressure formulation. - 2.2.2. Diagnosing the surface pressure gradient. - 2.2.3. Boundary conditions. - 3. Modelling approach. - 3.1. System of coordinates. - 3.2. Model equations. - 3.3. Vertical system of coordinates. - 3.4. Meridian convergence at the pole. - 3.5. Discretization in space. - 3.5.1. Arrangement of variables for the C grid. - 3.5.2. Discrete operators. - 3.5.3. Conservation properties for the dynamics. - 3.5.4. Conservation properties for the thermodynamics. - 3.6. Discretization in time. - 3.7. Robust diagnostic modelling. - 3.8. Aceeleration of convergence. - 3.9. Surface boundary conditions. - 3.10. Subgrid scale parameterisations. - 3.10. 1. Vertical mixing. - 3.10.2. Convection. - 3.10.3. Lateral mixing. - 4. The global coupled system. - 4.1. Ocean-only models. - 4.1.1. Space or time?. - 4.1.2. Oceanic observations. - 4.1.3. Atmospheric forcing. - 4.1.4. Sensitivity to parameterisation. - 4.2. Coupled models. - 4.2.1. General description of the problem. - 4.2.2. Illustration of drift. - 4.2.3. Flux correction. - 4.2.4. Sensitivity. - 5. The equatorial coupled system. - 5.1. Oceanic equatorial waves. - 5.1.1. Vertical eigenvectors. - 5.1.2. Meridional normal modes. - 5.1.3. Inertia-gravity and Rossby waves. - 5.1.4. Mixed Rossby-gravity wave. - 5.1.5. Equatorial Kelvin wave. - 5.2. Equatorial waves and EI Niiio. - 5.3. Response of forced simulations. - 5.4. Coupled models. - 5.5. Prediction. - 5.6. Some new features to study EI Nino. - 5.6.1. Meridional coupling. - 5.6.2. Barrier layer and freshwater flux. - 6. Conclusion. - References. - Course 4. Past Climatic Changes / by J.-C. Duplessy. - 1. Paleoclimatic and Paleoceanographic tools. - 1.1. Introduction. - 1.2. Transfer functions. - 1.2.1. The Imbrie and Kipp (I&K) technique. - 1.2.2. The Modem Analog Technique (MAT). - 1.2.3. Improving or validating transfer functions. - 1.3. Stable isotope ratio variations. - 1.3.1. Oxygen isotope fractionation during the water cycle. - 1.3.2. Oxygen isotope fractionation during carbonate precipitation. - 1.3.3. Isotope fractionation during the carbon cycle. - 1.4. Dating. - 1.4.1. Radiocarbon. - 1.4.2. Uranium series disequilibria. - 1.4.3. Longer time scales. - 2. The climatic record of the Plio-Pleistocene and the evidence for the Astronomical Theory of paleoclimates. - 2.1. Historical introduction. - 2.2. The Astronomical Theory of glaciations. - 2.3. Extension of the climatic record over the last 6 million years. - 2.4. The last climatic cycle. - 2.5. The last glacial maximum. - 2.6. The last climatic optimum. - 3. Rapid variations within the climate system. - 3.1. Introduction. - 3.2. Evidence of rapid climatic change during the deglaciation. - 3.3. Evidence of rapid climatic change during the glaciation. - 3.4. Mechanisms of rapid climatic change under glacial conditions. - 3.5. A case for the Younger Dryas. - 3.6. Evidence of rapid climatic change during the Eemian. - 3.7. Evidence of rapid climatic change during the Holocene. - 3.8. Modeling of abrupt climatic changes and implications for future climates. - References. - Course 5. Paleomyths I Have Known / by T. J. Crowley. - 1. lntroduction. - 2. General Features of past climate change. - 3. Some significant misconceptions about past climate change. - 4. Discussion of the "paleo-paradigms". - 4.1. "Th
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  • 4
    Call number: PIK N 531-01-0416 ; AWI G1-02-0031
    Type of Medium: Monograph available for loan
    Pages: XVI, 416 Seiten , Illustrationen
    ISBN: 0126312605
    Language: English
    Note: Contents: Contributors. - Foreword by Paul J. Crutzen. - Preface by David Schimel. - Introduction. - 1 Uncertainties of Global Biogeochemical Predictions / E. D. Schulze, D. S. S. Schimel. - 1.1 Introduction. - 1.2 The IGBP Transect Approach. - 1.2.1 The Patagonian Transect. - 1.2.2 The Australian Transect. - 1.2.3 The European Transect. - 1.3 Variability in Processes. - 1.4 Biome Approach and Functional Types. - 1.5 New Approaches to Functional Diversity. - 1.6 Conclusions. - References. - 2 Uncertainties of Global Climate Predictions / L. Bengtsson. - 2.1 Introduction. - 2.2 Observational Evidence. - 2.3 Physical Rationale. - 2.3.1 Stochastic Forcing. - 2.3.2 Solar irradiation Changes. - 2.3.3 Volcanic Effects. - 2.3.4 Anthropogenic Effects. - 2.4 Response to Forcing of the Climate System. - 2.5 Results from Climate Change Prediction Experiments. - 2.6 Summary and Conclusions. - References. - 3 Uncertainties in the Atmospheric Chemical System / G. P. Brasseur, E. A. H. Holland. - 3.1 Introduction. - 3.2 Synthetic View of Chemical Processes in the Troposphere. - 3.3 The IMAGES Model. - 3.4 Changes in the Chemical Composition of the Global Troposphere. - 3.5 Concluding Remarks. - References. - 4 Inferring Biogeochemical Sources and Sinks from Atmospheric Concentrations: General Consideration and Applications in Vegetation Canopies / M. Raupach. - 4.1 Introduction. - 4.2 Scalar and Isotopic Molar Balances. - 4.2.1 General Principles. - 4.2.2 Single-Point Eulerian Equations. - 4.2.3 Source Terms for CO2. - 4.2.4 Single-Point Lagrangian Equations. - 4.3 Inverse Methods for Inferring Scalar Sources and Sinks in Canopies. - 4.3.1 General Principles. - 4.3.2 Localized Near Field Theory. - 4.3.3 The Dispersion Matrix. - 4.3.4 Turbulent Velocity Field. - 4.3.5 Solutions for Forward, Inverse and Implicit Problems. - 4.3.6 Field Tests. - 4.4 Inverse Methods and Isotopes in Canopies. - 4.4.1 Path Integrals and Keeling Plots. - 4.4.2 Inverse Lagrangian Analysis of Isotopic Composition. - 4.5 Summary and Conclusions. - Appendix A. - Appendix B. - References. - 5 Biogeophysical Feedbacks and the Dynamics of Climate / M. Claussen. - 5.1 Introduction. - 5.2 Synergisms. - 5.2.1 High Northern Latitudes. - 5.2.2 Subtropics. - 5.3 Multiple Equilibria. - 5.4 Transient Interaction. - 5.5 Perspectives. - References. - 6 Land-Ocean-Atmosphere Interactions and Monsoon Climate Change: A Paleo-Perspective / J. E. Kutzbach, Michael T. Coe, S. P. Harrison and M. T. Coe. - 6.1 Introduction. - 6.2 Response of the Monsoon to Orbital Forcing. - 6.3 Ocean Feedbacks on the Monsoon. - 6.4 Land-Surface Feedbacks on the Monsoon. - 6.5 Synergies between the Land, Ocean and Atmosphere. - 6.6 The Role of Climate Variability. - 6.7 Final Remarks. - References. - 7 Paleobiogeochemistry / I. C. Prentice, D. Raynaud. - 7.1 Introduction. - 7.2 Methane. - 7.3 Carbon Dioxide. - 7.4 Mineral Dust Aerosol. - 7.5 Scientific Challenges Posed by the Ice-Core Records. - 7.5.1 Methane. - 7.5.2 Carbon Dioxide. - 7.5.3 Mineral Dust Aerosol. - 7.6 Towards an Integrated Research Strategy for Palaeobiogeochemistry. - References. - 8 Should Phosphorus Availability Be Constraining Moist Tropical Forest Responses to Increasing CO2 Concentrations / J. Lloyd, M. I. Bird, E. M. Veenendaal and B. Kruijt. - 8.1 Introduction. - 8.2 Phosphorus in the Soils of the Moist Tropics. - 8.2.1 Soil Organic Phosphorus. - 8.2.2 Soil Inorganic Phosphorus. - 8.2.3 Soil Carbon/Phosphorus Interactions. - 8.3 States and Fluxes of Phosphorus in Moist Tropical Forests. - 8.3.1 Inputs and Losses of Phosphorus Through Rainfall, Dry Deposition and Weathering: Losses Via Leaching. - 8.3.2 Internal Phosphorus Flows in Moist Tropical Forests. - 8.3.3 Mechanisms for Enhanced Phosphorus Uptake in Low P Soils. - 8.4 Linking the Phosphorus and Carbon Cycles. - 8.4.1 To What Extent Does Phosphorus Availability Really Limit Moist Tropical Forest Productivity?. - 8.4.2 Tropical Plant Responses to Increases in Atmospheric CO2 Concentrations. - 8.4.3 Using a Simple Model to Examine CO2/Phosphorus Interactions in Tropical Forests. - References. - 9 Trees in Grasslands: Biogeochemical Consequences of Woody Plant Expansion / S. Archer, T. W. Boutton and K. A. Hibbard. - 9.1 Introduction. - 9.2 Woody Plant Encroachment in Grasslands and Savannas. - 9.3 The La Copita Case Study. - 9.3.1 Biogeographical and Historal Context. - 9.3.2 Herbaceous Retrogression and Soil Carbon Losses. - 9.3.3 Woody Plant Encroachment and Ecosystem Biogeochemistry. - 9.4 Degradation: Ecological Versus Socioeconomic. - 9.5 Implications for Ecosystem and Natural Resources Management. - 9.6 Summary. - References. - 10 Biogeochemistry in the Arctic: Patterns, Processes and Controls / S. Jonasson, F.S. Chapin, III and G. R. Shaver. - 10.1 Introduction. - 10.2 Tundra Organic Matter. - 10.2.1 Distribution of Organic Matter. - 10.2.2 Patterns and Controls of Organic Matter Turnover between Ecosystem Types. - 10.3 Tundra Nutrients. - 10.3.1 Nutrient Distribution and Controls of Nutrient Cycling. - 10.3.2 Nutrient Mineralization and Plant Nutrient Uptake. - 10.3.3 Are there Unaccounted Plant Sources of Limiting Nutrients?. - 10.4 Biogeochemical Responses to Experimental Ecosystem Manipulations. - 10.4.1 Applicability of Experimental Manipulations. - 10.4.2 Responses to Water Applications. - 10.4.3 Response to Nutrient Addition and Warming. - 10.4.4 Responses in Ecosystem Carbon Balance. - 10.5 Summary. - References. - 11 Evaporation in the Boreal Zone During Summer - Physics and Vegetation / F. M. Kelliher, I. Lloyd, C. Rebmann, C. Wirth and E. D. Schulze, D. D. Baldocchi. - 11.1 Introduction. - 11.2 Climate and Soil Water. - 11.3 Evaporation Theory. - 11.4 Evaporation During Summer and Rainfall. - 11.5 Forest Evaporation, Tree Life Form and Nitrogen. - 11.6 Conclusions. - References. - 12 Past and Future Forest Response to Rapid Climate Change / M.B. Davis. - 12.1 Introduction. - 12.2 Long-Distance Dispersal. - 12.3 Estimating Jump Distances. - 12.4 Interactions with Resident Vegetation - Constraints on Establishment. - 12.5 Interactions with Resident Vegetation - Competition for Light and Resulting Constraints on Population Growth. - 12.6 Conclusions. - References. - 13 Biogeochemical Models: Implicit vs. Explicit Microbiology / J. Schimel. - 13.1 Introduction. - 13.2 Microbiology in Biogeochemical Models. - 13.3 Dealing with Microbial Diversity in Models. - 13.4 Kinetic Effects of Microbial Population Size. - 13.5 Microbial Recovery from Stress. - 13.6 Conclusions. - References. - 14 The Global Soil Organic Carbon Pool / M. I. Bird, H. Santruckova, J. Lloyd and E. M. Veenendaal. - 14.1 Introduction: the Soil Carbon Pool and Global Change. - 14.2 Factors Affecting the Distribution of Soil Organic Carbon. - 14.3 Global Variations in the SOC Pool. - 14.4 The Limitations of Available Observational SOC Data. - 14.5 A Stratified Sampling Approach. - 14.6 Conclusions: Sandworld and Clayworld. - References. - 15 Plant Compounds and Their Turnover and Stability as Soil Organic Matter / G. Gleixner, C. Czimczik, C. Kramer, B. M. Lühker and M. W. I. Schmidt. - 15.1 Introduction. - 15.2 Pathways of Soil Organic Matter Formation. - 15.2.1 Formation and Decomposition of Biomass. - 15.2.2 The Influence of Environmental Conditions on SOM Formation. - 15.2.3 For
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  • 5
  • 6
    ISSN: 1546-1718
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] The rate and pattern of sequence substitutions in the mitochondrial DNA (mtDNA) control region (CR) is of central importance to studies of human evolution and to forensic identity testing. Here, we report a direct measurement of the intergenerational substitution rate in the human CR. We compared ...
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  • 7
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The organizer of the vertebrate gastrula is an important signalling centre that induces and patterns dorsal axial structures. Although a topic of long-standing interest, the evolutionary origin of the organizer remains unclear. Here we show that the gastrula of the cephalochordate amphioxus ...
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  • 8
    ISSN: 1432-041X
    Keywords: Key words NK2 homeobox ; Cephalochordata ; Lancelet ; Diencephalon ; Endostyle
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract  We characterized an amphioxus NK-2 homeobox gene (AmphiNk2–1), a homologue of vertebrate Nkx2–1, which is involved in the development of the central nervous system and thyroid gland. At the early neurula stage of amphioxus, AmphiNk2–1 expression is first detected medially in the neural plate. By the mid-neurula stage, expression is localized ventrally in the nerve cord and also begins in the endoderm. During the late neurula stage, the ventral neural expression becomes transiently segmented posteriorly and is then down-regulated except in the cerebral vesicle at the anterior end of the central nervous system. Within the cerebral vesicle AmphiNk2–1 is expressed in a broad ventral domain, probably comprising both the floor plate and basal plate regions; this pattern is comparable to Nkx2–1 expression in the mouse diencephalon. In the anterior part of the gut, expression becomes intense in the endostyle (the right wall of the pharynx), which is the presumed homologue of the vertebrate thyroid gland. More posteriorly, there is transitory expression in the midgut and hindgut. In sum, the present results help to support homologies (1) between the amphioxus endostyle and the vertebrate thyroid gland and (2) between the amphioxus cerebral vesicle and the vertebrate diencephalic forebrain.
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  • 9
    ISSN: 1432-041X
    Keywords: Key words Amphioxus ; Actin ; Tissue-specific gene expression ; Chordate evolution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract  The cephalochordate amphioxus is thought to share a common ancestor with vertebrates. To investigate the evolution of developmental mechanisms in chordates, cDNA clones for two amphioxus actin genes, BfCA1 and BfMA1, were isolated. BfCA1 encodes a cytoplasmic actin and is expressed in a variety of tissues during embryogenesis, beginning in the dorsolateral mesendoderm of the mid-gastrula. At the open neural plate stage, BfCA1 transcripts accumulate at the bases of the neuroectodermal cells adjacent the presumptive notochord. The 3’ untranslated region of BfCA1 contains a sequence that is similar to the ”zipcode” sequence of chicken β-cytoplasmic actin gene, which is thought to direct intracellular mRNA localization. BfCA1 is also expressed in the notochord through the early larval stage, in the pharynx and in the somites at the onset of muscle-cell differentiation. BfMA1 is a vertebrate-type muscle actin gene, although the deduced amino acid sequence is fairly divergent. Transcripts first appear in the early neurula in the somites as they begin to differentiate into axial muscle cells and persist into the adult stage. In young adults, transcripts are localized in the Z-discs of the muscle cells. Smooth muscle cells around the gill slits and striated muscle cells in the pterygeal muscle also express BfMA1; however, there is never any detectable expression in the notochord, which is a modified striated muscle. Together with the alkali myosin light chain gene AmphiMLC-alk, the sequence and muscle-specific expression of BfMA1 implies a conserved mechanism of muscle cell differentiation between amphioxus and vertebrates. Evolution of the chordate actin gene family is discussed based on molecular phylogenetic analysis and expression patterns of amphioxus actin genes.
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  • 10
    ISSN: 1432-041X
    Keywords: Key words Mesoderm ; Notochord ; Brachyury ; Amphioxus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract  In amphioxus embryos, the nascent and early mesoderm (including chorda-mesoderm) was visualized by expression of a Brachyury gene (AmBra-2). A band of mesoderm is first detected encircling the earliest (vegetal plate stage) gastrula sub-equatorially. Soon thereafter, the vegetal plate invaginates, resulting in a cap-shaped gastrula with the mesoderm localized at the blastoporal lip and completely encircling the blastopore. As the gastrula stage progresses, DiI (a vital dye) labeling demonstrates that the entire mesoderm is internalized by a slight involution of the epiblast into the hypoblast all around the perimeter of the blastopore. Subsequently, during the early neurula stage, the internalized mesoderm undergoes anterior extension mid-dorsally (as notochord) and dorsolaterally (in paraxial regions where segments will later form). By the late neurula stage, AmBra-2 is no longer transcribed throughout the mesoderm as a whole; instead, expression is detectable only in the posterior mesoderm and in the notochord, but not in paraxial mesoderm where definitive somites have formed.
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