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  • 1
    Online Resource
    Online Resource
    Leverkusen-Opladen :Verlag Barbara Budrich,
    Keywords: Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (177 pages)
    Edition: 1st ed.
    ISBN: 9783847413851
    Language: German
    Note: Cover -- Klima, Wetter, Mensch -- Inhaltsverzeichnis -- 1. Überblick und Danksagung -- 2. Einleitung: Klimasicht im Wandel der Zeit -- 3. Klima als Zustand und Ressource -- 3.1. Klima als Umwelterfahrung -- 3.2. Klima als naturwissenschaftliches System -- 3.3. Klima als soziales Konstrukt -- 3.4. Gesellschaft und Mensch als klimatisches Konstrukt -- 3.5. Die Wirkungen des Klimas auf den Menschen: Der heutige Erkenntnisstand -- 4. Klima als Risiko und Bedrohung -- 4.1. Ideengeschichte der Klimaänderungen -- 4.2. Natürliche Klimavariabilität -- 4.3. Exkurs: Wem gehört 2025 das Wetter? -- 4.4. Der vom Menschen verursachte Klimawandel -- 4.5. Klimaänderungen als soziales Konstrukt -- 4.6. Das Alltagsverständnis von Klima: Das Vertrauen in die Normalität -- a) Die soziale Wahrnehmung des Klimas -- b) Meinungsumfragen -- c) Soziales Verhalten und Vertrauen -- d) Der Mensch als Zuschauer -- e) Unparteilichkeit -- f) Extreme als Bestätigung der Normalität -- g) Zusammenfassende Bemerkung -- 4.7. Die Geschichte der anthropogenen Klimakatastrophen -- 4.8. Der Einfluss von Klimaveränderungen auf die Gesellschaft -- a) Klimafolgen -- b) Klimapolitik: Der technokratische Ansatz -- c) Klimapolitik: Die Rolle der Perzeptionen -- 5. Zeppelin-Manifest zum Klimaschutz -- 6. Zusammenfassung und Ausblick -- 7. Literaturverzeichnis -- Register.
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Sedimentology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (386 pages)
    Edition: 1st ed.
    ISBN: 9783319498942
    Series Statement: Coastal Research Library ; v.19
    DDC: 551.45709116334
    Language: English
    Note: Intro -- Contents -- Chapter 1: Introduction -- References -- Part I: Concepts and Model Approaches -- Chapter 2: What Determines the Change of Coastlines in the Baltic Sea? -- 2.1 Introduction -- 2.2 Geological Compartments and Coastal Types -- 2.3 The Model -- 2.4 Relative Sea-Level Change and Glacio-Isostatic Adjustment -- 2.5 Coastal Morphogenesis at the Southern and South-Eastern Baltic Sea -- 2.6 Summary and Conclusions -- References -- Chapter 3: The Challenge of Baltic Sea Level Change -- 3.1 Introduction -- 3.2 The Transdisciplinary of Sea-Level Science -- 3.3 The Heterogeneity of Sea-Level Data -- 3.4 The Detection of Acceleration in Long-Term Baltic Sea Level -- 3.5 Outlook -- References -- Chapter 4: Recent Baltic Sea Level Changes Induced by Past and Present Ice Masses -- 4.1 Introduction -- 4.2 Interactions Between Ice, Ocean and Solid Earth -- 4.2.1 The Sea-Level Equation -- 4.2.2 GIA-Induced Mass Signals -- 4.2.3 Mass Signals Due to Recent Cryospheric Changes -- 4.3 Observation of Mass Signal -- 4.3.1 Relative Sea-Level Changes - Tide Gauges -- 4.3.2 Crustal Deformations - GPS -- 4.3.3 Volumetric Sea-Level Changes - Tide Gauges and GPS -- 4.4 Summary -- References -- Chapter 5: Factors and Processes Forming the Polish Southern Baltic Sea Coast on Various Temporal and Spatial Scales -- 5.1 Introduction -- 5.2 General Characteristics of the Southern Baltic Sea Coastline -- 5.3 The Impact of Geological and Tectonic Setting on Coastline Shaping and Evolution (Millennia Scale -- 1-st Order Coastal Syst... -- 5.4 Holocene Transgression in the Southern Baltic Area, Eustatic Sea-Level Fluctuations, and Their Morphodynamic Effects (Cent... -- 5.5 Sea-Level Changes and Morphodynamics on the Decadal Scale (3-rd Order Coastal Systems). , 5.6 Seasonal Changes (Occurring on the Annual Scale) and Short-Term Changes (Weeks, Days) - (4th - 6th Order Coastal Systems) -- 5.7 Extreme Events and Anthropogenic Activities in the Marine Coastal Zone -- 5.8 Summary -- References -- Chapter 6: The Dynamic Equilibrium Shore Model for the Reconstruction and Future Projection of Coastal Morphodynamics -- 6.1 Introduction -- 6.2 Dynamic Equilibrium Shore Model (DESM) -- 6.2.1 Modelling for the Past Reconstruction of Coastal Morphology -- 6.2.2 Quantitative Estimation of Alongshore Sediment Transport Rate -- 6.2.3 First-Order Future Projection of Coastline Recession -- 6.3 Application of the Model at Open Oceanic Coasts -- 6.3.1 Łeba Open Barrier Coast -- 6.3.1.1 Geological Setting -- 6.3.1.2 Model Setting -- Relative Sea-Level Changes -- Alongshore Sediment Transport Capacity -- Recent DEM and Historical Coastline Changes -- 6.3.1.3 Hindcast Scenarios and Future Projection -- 6.3.2 Hel Sandy Spit -- 6.3.2.1 Geological Setting -- 6.3.2.2 Model Setting -- Relative Sea-Level Changes -- Along-Shore Sediment Transport Capacity -- Recent DEM and Historical Coastline Changes -- Hindcast Scenarios and Future Projection -- 6.4 Discussions -- 6.5 Conclusions -- References -- Chapter 7: Modelling of Medium-Term (Decadal) Coastal Foredune Morphodynamics- Historical Hindcast and Future Scenarios of the... -- 7.1 Introduction -- 7.2 Area of Investigation -- 7.3 The Model -- 7.3.1 The Cellular Automata Module -- 7.3.1.1 Aeolian Erosion and Transport -- 7.3.1.2 Avalanche -- 7.3.1.3 Vegetation -- 7.3.2 The Subaqueous Module -- 7.3.2.1 Land-Sea Boundary and Alongshore Sediment Transport -- 7.3.2.2 Cross-Shore Sediment Transport and Beach Profile Change -- 7.4 Model Application -- 7.4.1 Model Set-Up and Historical Hindcast (1951-2012) for the Study Area -- 7.4.2 Model Projection ( 2013-2050AD) -- 7.5 Discussion. , 7.6 Conclusions -- References -- Chapter 8: Constraints of Radiocarbon Dating in Southeastern Baltic Lagoons: Assessing the Vital Effects -- 8.1 Introduction -- 8.2 Geological Setting -- 8.3 Methods -- 8.3.1 Field Observations and Sampling -- 8.3.2 Radiocarbon (14C) Dating Analyses -- 8.3.3 Palaeodosimetric Dating (IR-OSL, ESR) -- 8.3.4 Pollen Analysis -- 8.4 Results -- 8.4.1 Radiocarbon Analysis -- 8.4.2 Palaeodosimetric Dating -- 8.4.3 Pollen Analysis -- 8.5 Discussion -- 8.5.1 Vital Effects -- 8.5.2 Conceptual Model of Chronometric Pathways -- 8.6 Conclusions -- References -- Part II: Regional Studies -- Chapter 9: Late Glacial to Holocene Environmental Changes (with Particular Reference to Salinity) in the Southern Baltic Recon... -- 9.1 Introduction -- 9.2 Study Area -- 9.3 Material and Methods -- 9.3.1 14C Dating -- 9.3.2 Diatom Analysis -- 9.4 Results -- 9.4.1 Lithology -- 9.4.1.1 Core T28 -- 9.4.1.2 Core T15 -- 9.4.2 Diatoms -- 9.4.2.1 Core T28 -- 9.4.2.2 Core T15 -- 9.5 Discussion -- 9.5.1 Palaeoenvironmental Reconstruction -- 9.5.2 Salinity Responses of the Rega Valley -- References -- Chapter 10: Postglacial Evolution of the Odra River Mouth, Poland-Germany -- 10.1 Introduction -- 10.2 Study Area -- 10.3 Methods -- 10.4 Results -- 10.4.1 Seismoacoustics -- 10.4.2 Lithostratigraphy -- 10.4.3 Datings -- 10.5 Discussion -- 10.6 Conclusions -- References -- Chapter 11: Morphodynamic Processes of the Swina Gate Coastal Zone Development (Southern Baltic Sea) -- 11.1 Introduction -- 11.1.1 Geology and Geomorphology Area of the Investigations -- 11.2 Materials and Methods -- 11.3 Results -- 11.3.1 Changes in the Dune Base Line (DBL) Position -- 11.3.2 Changes of the Beach Width (WB) -- 11.3.3 Changes of the Width of the Underwater Longshore Bars Zone (WUBZ) -- 11.3.4 Spatial Correlation Between the DBL, WB and WUBZ. , 11.3.5 Influence of the Coastline Orientation to the DBL, WB and WUBZ Changes -- 11.3.6 Influence of the Beach Width to the DBL, WB and WUBZ Changes -- 11.3.7 Influence of the DBL Elevation to the DBL, WB and WUBZ Changes -- 11.3.8 Influence of the Beach Slope to the DBL, WB and WUBZ Changes -- 11.4 Discussion - Driving Forces Responsible for the Coastal Zone Changes -- 11.4.1 Influence of the Water Level on the DBL, WB and WUBZ Changes -- 11.4.2 Influence of the Storm Surges on the DBL, WB and WUBZ Changes -- 11.4.3 Influence of the Waves Regime on the DBL, WB and WUBZ Changes -- 11.4.4 Influence of the Hydrological Engineering Constructions on the DBL, WB and WUBZ Changes -- 11.4.5 Long-Term Coastline Changes -- 11.5 Summary and Conclusions -- References -- Chapter 12: New Demands on Old Maps - An Approach for Estimating Aspects of Accuracy of Old Maps as Basis for Landscape Develo... -- 12.1 Introduction -- 12.2 Methods -- 12.3 Accuracy of Locations on Maps -- 12.4 Accuracy of Map Content -- 12.5 Digitalisation of Maps -- 12.6 Conclusions -- References -- Chapter 13: Reconstruction of Coastline Changes by the Comparisons of Historical Maps at the Pomeranian Bay, Southern Baltic S... -- 13.1 Introduction -- 13.2 Methodology -- 13.2.1 Geo-Referencing ``Ur-Messtischblatt´´ Maps in 1829AD -- 13.2.2 Accuracy of Coastline Changes -- 13.3 Results -- 13.3.1 Accuracy Quantification -- 13.3.2 Analysis of Coastline Changes -- 13.4 Discussions -- 13.4.1 Map Accuracy -- 13.4.2 Spatial Classification -- 13.4.3 Temporal Change -- 13.5 Conclusions -- References -- Chapter 14: Changes in the Szczecin Lagoon Shoreline as Determined from Selected Seventeenth and Nineteenth Century Maps -- 14.1 Introduction -- 14.2 Area of Study: The Szczecin Lagoon -- 14.3 Indicators of Changes in the Water Level -- 14.4 Research Methods. , 14.4.1 On Surveying in the Thirteenth to Eighteenth Century -- 14.4.2 Source Materials -- 14.4.3 Raster Map Georeferencing -- 14.4.4 Map Components Essential for the Assessment of Changes in the Shoreline and Its Immediate Hinterland -- 14.4.5 Potential Sources of Errors in the Old Map Analysis -- 14.5 Results of Old Map Analyses -- 14.5.1 Study Site: Pomeranian Sandbank -- 14.5.2 Study Site: Wolin Sandbank -- 14.5.3 Study Site: Nowe Warpno Peninsula and Warpno Sandbank -- 14.5.3.1 Stony Area -- 14.5.3.2 Islands on Nowe Warpno Lake -- 14.6 The Image of the Wolin Island on Old Maps -- 14.7 Kamień Lagoon -- 14.8 Summing Up and Discussion -- 14.9 Conclusions -- References -- Chapter 15: Retrieving the Signal of Climate Change from Numerically Simulated Sediment Transport Along the Eastern Baltic Sea... -- 15.1 Introduction -- 15.2 Simulation of the Baltic Sea Wave Fields -- 15.3 Sediment Transport by Waves That Approach Under Large Angles -- 15.4 Spatial Distribution of Sediment Transport Rates on the Eastern Baltic Sea Coast -- 15.5 Spatio-temporal Variations in Sediment Transport Rates -- 15.6 Interannual Variations in the Bulk and Net Transport -- 15.7 Abrupt Turn in the Geostrophic Air-Flow Direction -- 15.8 Patterns of Wave Set-Up Heights Signal Wave Climate Changes -- 15.9 Concluding Remarks -- References -- Chapter 16: Sea-Level Change and Flood Risks at Estonian Coastal Zone -- 16.1 Introduction -- 16.2 Long-Term Relative Sea-Level Changes in the Baltic Sea and in Estonian Coastal Zone -- 16.3 Present Post-glacial Land Uplift and Sea-Level Change in Estonia -- 16.4 Extreme Sea Levels and Floods in the Estonian Coastal Zone -- 16.5 Sea-Level Scenarios for the Twenty-First Century -- 16.6 Urban Areas Exposed to Coastal Flooding -- 16.7 Setting an Estonian National Climate Change Adaptation Policy -- 16.8 Summary -- References.
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  • 3
    Online Resource
    Online Resource
    Berlin, Heidelberg : Springer Berlin / Heidelberg
    Keywords: Electronic books
    Description / Table of Contents: Intro -- Beteiligte -- Inhaltsverzeichnis -- 1 Einleitung und Zusammenfassung -- 1.1 Kurzdarstellung -- 1.2 Methode der Erstellung des Berichtes -- 1.2.1 Wissen, Konsens, Szenarien -- 1.2.2 Prozess -- 1.3 Zusammenfassung -- 1.3.1 Klima der Region - Zustand, bisherige Entwicklung und mögliche Änderungen bis 2100 (▶ Kap. 2) -- 1.3.2 Stadtklima in Hamburg (▶ Kap. 3) -- 1.3.3 Deutsche Bucht mit Tideelbe und Lübecker Bucht (▶ Kap. 4) -- 1.3.4 Aquatische Ökosysteme: Nordsee, Wattenmeer, Elbeästuar und Ostsee (▶ Kap. 5) -- 1.3.5 Terrestrische und semiterrestrische Ökosysteme (▶ Kap. 6) -- 1.3.6 Land- und Forstwirtschaft, Fischerei (▶ Kap. 7) -- 1.3.7 Gesundheit (▶ Kap. 8) -- 1.3.8 Infrastrukturen (Energie- und Wasserversorgung) (▶ Kap. 9) -- 1.3.9 Migration (▶ Kap. 10) -- 1.3.10 Hafen Hamburg, Schifffahrt und Verkehr (▶ Kap. 11) -- 1.3.11 Klimawandel in den Medien (▶ Kap. 12) -- 1.3.12 Wahrnehmung des Klimawandels in der Metropolregion Hamburg (▶ Kap. 13) -- 1.3.13 Lokale Klima-Governance im Mehrebenen-System: formale und informelle Regelungsformen (▶ Kap. 14) -- 1.3.14 Technischer Klimaschutz (▶ Kap. 15) -- 1.3.15 Klimawandel, Nachhaltigkeit und Transformationsgestaltung (▶ Kap. 16) -- I Klima der Region und Einfluss auf Ökosysteme -- 2 Klima der Region - Zustand, bisherige Entwicklung und mögliche Änderungen bis 2100 -- 2.1 Einführung -- 2.2 Klimazustand -- 2.2.1 Wind -- 2.2.2 Lufttemperatur -- 2.2.3 Niederschlag -- 2.2.4 Sonnenscheindauer -- 2.3 Bisherige klimatische Entwicklung in der Region -- 2.3.1 Die atmosphärische Zirkulation -- 2.3.2 Wind -- 2.3.3 Lufttemperatur -- 2.3.4 Niederschlag -- 2.4 Mögliche Änderungen des Klimas im 21. Jahrhundert -- 2.4.1 Einleitung: Klimaprojektionen für das 21. Jahrhundert -- 2.4.2 Projizierte Klimaänderungen in der Metropolregion Hamburg im 21. Jahrhundert -- 2.5 Zusammenfassung und Ausblick -- Literatur.
    Type of Medium: Online Resource
    Pages: 1 online resource (311 pages)
    ISBN: 9783662553794
    Language: German
    Note: Description based on publisher supplied metadata and other sources
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  • 4
    Keywords: Electronic books
    Description / Table of Contents: Intro -- Preface -- Contents -- List of Facsimiles -- 1 Klaus Hasselmann-His Scientific Footprints and Achievements -- 1.1 Overview -- 1.2 The Naturwissenschaftler -- 1.3 The Enabler -- 1.4 The Public Figure -- 1.5 In 1997, A Visitor Told His Perceptions When Visiting the MPI -- 2 Klaus Hasselmann-His Own Account -- 2.1 The 2006 Interview -- 2.2 Supplement 26 June 2021 -- 2.3 Conversation in 2021 About Climate Science Becoming a Political Actor -- 3 The Strands of Klaus Hasselmann's Science -- 3.1 Ocean Wave Theory and Prediction: From Basic Physics to an Integrated Wind and Wave Data Assimilation System -- 3.2 Remote Sensing -- 3.3 Stochastic Climate Model -- 3.4 Reducing the Phase Space: Signal-to-Noise Analysis and Detection and Attribution -- 3.5 Climate and Society -- 3.6 Strategy in Climate Modelling at MPI -- 3.7 Metrons-Particle Physics -- 4 Personal Accounts by Colleagues and Co-workers -- 4.1 Susanne Hasselmann: Klaus-Scientist, Husband, Father, Grandfather, Great-Grandfather -- 4.2 Dirk Olbers: How to Cook an Ostrich Egg -- 4.3 Peter Müller -- 4.4 Jürgen-Willebrand: Kiel-Hamburg Oscillations -- 4.5 Peter Lemke: A Stochastic Decision? -- 4.6 Martin Heimann -- 4.7 Christoph Heinze -- 4.8 Mojib Latif -- 4.9 Hans Graf -- 4.10 Gabriele Hegerl: Der Alte -- 4.11 Jin-Song von Storch -- 4.12 Hans Von Storch -- 4.13 Patrick Heimbach: Interactions with Klaus' Sphere of Influence -- 4.14 Jörg Wolff: The Shortbread Biscuit -- 4.15 Ben Santer: A Road Trip with Klaus -- 4.16 Ulrich Cubasch: How a Postdoc Became an IPCC Convening Lead Author -- 4.17 Achim Stössel: From Seaman to Professor Thanks to Klaus Hasselmann -- 4.18 Robert Sausen: Interactions with Klaus Hasselmann -- 4.19 Dmitry V. Kovalevsky -- 4.20 Carola Kauhs: A Non-Scientific View on Professor Klaus Hasselmann from the Institute's Librarian -- 4.21 Gerbrand Komen.
    Type of Medium: Online Resource
    Pages: 1 online resource (324 pages)
    ISBN: 9783030917166
    Language: English
    Note: Description based on publisher supplied metadata and other sources
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 405 (2000), S. 615-615 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Many people think that the threat of ‘global warming’ arose only towards the end of the twentieth century. But the idea of human (anthropogenic) interference with climate has an important — although often overlooked — historical dimension. Climate change, either natural ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Global change biology 3 (1997), S. 0 
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: The assessment of possible implications of anthropogenic climate change requires the evaluation of results obtained with complex climate models. Here we considered the problem of assessing the impact of climate variability on successional events in a lake (Plußsee) of the temperate region between January and May. We first established a statistical link between large-scale air temperature, at about 1500 m height, and the local temperature, in order to bridge the spatial gap of information obtained from global climate models and local climate which forces processes in the lake. Secondly, the local temperatures were statistically related to biologically induced dynamic features in the lake, derived from Secchi depths readings (as integrated measures). The observed relationships were compared with results from a phyto- and zooplankton population-dynamic model run under different temperature regimes. The local temperatures approximated closely the large-scale temperature. The timing of phyto- and zooplankton maxima (clearwater phase) were negatively related to the temperature. Thus, with a temperature increase both occurred earlier. The intensity of the spring algal maximum was negatively related to its timing, whereas no clear relation between the timing and intensity of the clearwater phase (zooplankton maximum) could be obtained.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    International journal of biometeorology 41 (1997), S. 5-12 
    ISSN: 1432-1254
    Keywords: Key words Plant phenology ; Galanthus nivalis L. ; Climatic effect of plant events ; Statistical downscaling ; Northern Germany
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Notes: Abstract  We have examined the relationship between phenological data and concurrent large-scale meterological data. As phenological data we have chosen the beginning of the flowering of Galanthus nivalis L. (flowering date) in Northern Germany, and as large-scale meteorological data we use monthly mean near-surface air temperatures for January, February and March. By means of canonical correlation analysis (CCA), a strong linear correlation between both sets of variables is identified. Twenty years of observed data are used to build the statistical model. To validate the derived relationship, the flowering date is downscaled from air temperature observations of an independent period. The statistical model is found to reproduce the observed flowering dates well, both in terms of variability as well as amplitude. Air temperature data from a general circulation model of climate change are used to estimate the flowering date in the case of increasing atmospheric carbon dioxide concentration. We found that at a time of doubled CO2 concentration (expected by about 2035) G. nivalis L. in Northern Germany will flower ∼2 weeks and at the time of tripled CO2 concentration (expected by about 2085) ∼4 weeks earlier than presently.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 365 (1993), S. 791-791 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] SIR - In the debate concerning climate change due to increasing emissions of radiatively active gases into the atmosphere, many people are concerned about the possibility of an intensification of extratropical storms. Even though the International Panel on Climate Change1 took a cautious stand in ...
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2018-07-23
    Description: The ECMWF-T21 atmospheric GCM is forced by observed near-global SST from January 1970 to December 1985. Its response in low level winds and surface wind stress over the Pacific Ocean is compared with various observations. The time dependent SST clearly induces a Southern Oscillation (SO) in the model run which is apparent in the time series of all variables considered. The phase of the GCM SO is as observed, but its low frequency variance is too weak and is mainly confined to the western Pacific. Because of the GCM's use as the atmospheric component in a coupled ocean-atmosphere model, the response of an equatorial oceanic primitive equation model to both the modeled and observed wind stress is examined. The ocean model responds to the full observed wind stress forcing in a manner almost identical to that when it is forced by the first two low frequency EOFs of the observations only. These first two EOFs describe a regular eastward propagation of the SO signal from the western Pacific to the central Pacific within about a year. The ocean model's response to the modeled wind stress is too weak and similar to the response when the observed forcing is truncated to the first EOF only. In other words, the observed SO appears as a sequence of propagating patterns but the simulated SO as a standing oscillation. The nature of the deviation of the simulated wind stress from observations is analyzed by means of Model Output Statistics (MOS). It is shown that a MOS-corrected simulated wind stress, if used to force an ocean GCM, leads to a significant enhancement of low frequency SST variance, which is most pronounced in the western Pacific.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2023-08-15
    Description: This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change. The evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future. The BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme.
    Type: Book , NonPeerReviewed
    Format: text
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