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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Environmental sciences. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (373 pages)
    Edition: 1st ed.
    ISBN: 9783319190426
    Series Statement: Advances in Global Change Research Series ; v.55
    DDC: 363.73874
    Language: English
    Note: Intro -- Preface -- Acknowledgements -- Contents -- List of Boxes -- 1 Introduction -- 2 The Basis: Past Climate Observations and Methods -- 2.1 Observations of Weather and Climate -- 2.2 Historical Climate Observations -- 2.2.1 Documentary and Early Instrumental Data -- 2.2.2 From National Weather Services to a Global Observing System -- 2.3 Upper-Air and Satellite Observations -- 2.4 Data Dissemination in the Course of Time -- 2.5 Uncertainties in Climatic Data -- 2.5.1 Uncertainties and Errors in Measurement Series -- 2.5.2 Inhomogeneities and Homogenisation -- 2.5.3 The Chain of Uncertainties -- 2.6 Data Products and Dynamical-Statistical Methods -- 2.6.1 Spatial Information and Geostatistical Methods -- 2.6.2 Data Assimilation and Reanalyses -- 2.7 Climate Models -- 2.7.1 Characteristics of Climate Models -- 2.7.2 Types of Climate Models and Experiments -- 2.7.3 Downscaling, Nudging, and Other Techniques -- 2.8 Palaeoclimate Information and Techniques -- 2.8.1 Climate Proxies -- 2.8.2 Problems Arising When Working with Proxies -- 2.8.3 Calibration and Modelling of Proxies -- 2.8.4 Climate Reconstructions -- 2.8.5 Data Assimilation in Palaeoclimatology -- 2.9 Datasets Used in This Book -- 2.9.1 Overview -- 2.9.2 Observations and Reanalyses -- 2.9.3 Model Simulations -- 2.9.4 Reconstructions and Offline Assimilation -- 2.9.5 Conclusions -- 3 The Machinery: Mechanisms Behind Climatic Changes -- 3.1 Basic Climate Physics: The Mean State -- 3.1.1 Energy Budget and Heat Transport -- 3.1.1.1 Global-Mean Fluxes -- 3.1.1.2 Spatial View of Heat Transport -- 3.1.2 The General Circulation of the Atmosphere -- 3.1.2.1 The Zonally Symmetric Circulation -- 3.1.2.2 The Zonally Asymmetric Circulation -- 3.1.2.3 The Weather Scale -- 3.1.2.4 Energy Transport -- 3.1.3 Stratospheric Circulation -- 3.1.3.1 Demarcation and Zonal-Mean Circulation. , 3.1.3.2 The Quasi-Biennial Oscillation (QBO) -- 3.1.3.3 Meridional Circulation and Wave-Mean Flow Interaction -- 3.1.3.4 Sudden Stratospheric Warmings and Downward Propagation -- 3.1.4 The Ocean, Air-Sea and Land-Sea Interactions -- 3.1.4.1 Ocean-Atmosphere Interaction -- 3.1.4.2 Ocean Currents -- 3.1.4.3 Land-Sea Interaction -- 3.1.4.4 Monsoon -- 3.1.4.5 Sea Ice and Snow Cover -- 3.2 Expressions and Mechanisms of Climate Variability -- 3.2.1 Statistical and Physical Perspectives of Climate Variability -- 3.2.2 Overview of Circulation Variability Modes -- 3.2.3 The North Atlantic Oscillation (NAO) -- 3.2.4 Variability Modes in the Pacific and the Southern Hemisphere -- 3.2.4.1 The Pacific-North American Pattern -- 3.2.4.2 The Pacific-South American Pattern and the Southern Annular Mode -- 3.2.5 Extratropical Circulation Variability Modes and the Stratosphere -- 3.2.6 Tropical Variability Modes: El Niño-Southern Oscillation (ENSO) -- 3.2.6.1 The ENSO Phenomenon -- 3.2.6.2 ENSO Mechanisms -- 3.2.6.3 ENSO Variability and ``Flavours'' of ENSO -- 3.2.6.4 ENSO Teleconnections -- 3.2.7 Variability Modes in the Atlantic and Indian Ocean -- 3.2.8 Decadal Climate Variability Modes -- 3.3 Forced Climatic Changes -- 3.3.1 Volcanic Effects -- 3.3.1.1 Direct (Radiative) Effects -- 3.3.1.2 Indirect Dynamical Effects -- 3.3.1.3 Aerosol Size -- 3.3.1.4 Quantification of Past Volcanic Forcing -- 3.3.2 Solar Influences -- 3.3.2.1 Changes in Solar Activity -- 3.3.2.2 Observed Solar Effects -- 3.3.2.3 Possible Mechanisms -- 3.3.2.4 Beyond the Sunspot Cycle -- 3.3.2.5 Time Series of Solar Forcing -- 3.3.3 Well-Mixed Greenhouse Gases -- 3.3.3.1 Mechanism -- 3.3.3.2 Impacts on Future Climate -- 3.3.3.3 Effects of Greenhouse Gases on Past Climate -- 3.3.3.4 Changes in Greenhouse Gas Concentrations Since 1600 -- 3.3.4 Tropospheric Aerosols and Reactive Trace Gases. , 3.3.4.1 Properties of Aerosols -- 3.3.4.2 Sources and Spatial Distribution of Aerosols -- 3.3.4.3 Impacts on Climate -- 3.3.4.4 Tropospheric Trace Gases -- 3.3.5 Land Surface -- 3.3.5.1 Mechanisms -- 3.3.5.2 Climate Impacts and Development of Land Cover Since 1600 -- 3.4 Coupling Between Systems and Feedback Mechanisms -- 3.4.1 Interaction Within the Machinery -- 3.4.2 Feedbacks Involving Water Vapour and Clouds -- 3.4.3 Feedbacks Involving Freezing Water: Arctic Amplification and the Cryosphere -- 3.4.4 Water as a Reactant: The Role of the Hydroxyl Radical -- 3.4.5 Feedbacks Involving Evaporating Water: Land Surface Feedbacks -- 4 Climatic Changes Since 1700 -- 4.1 Climatic Changes of the Past Centuries: An Overview -- 4.1.1 The Last Millennium -- 4.1.2 An Overview of Climatic Changes Since 1700: Brükner's View -- 4.1.3 Climatic Changes Since 1700 in Climate Reconstructions -- 4.1.3.1 Global and Northern Hemisphere Temperature Changes -- 4.1.3.2 Continental Temperature Reconstructions -- 4.1.3.3 Precipitation and Drought Reconstructions -- 4.1.3.4 Sea-Surface Temperature Reconstructions -- 4.1.3.5 Regional Climate: Central Europe and the European Alps -- 4.1.4 Climatic Changes in CCC400 and EKF400 -- 4.1.4.1 Global, Hemisphere and Continental Scales -- 4.1.4.2 Changes in the Zonal-Mean Circulation -- 4.1.4.3 Changes in Regional Circulation Indices -- 4.1.4.4 Changes in Extremes -- 4.1.5 Drivers of Global Climate Since 1600 -- 4.2 The Period from 1700 to 1890: The Little Ice Age -- 4.2.1 Climate of the 18th and 19th Centuries -- 4.2.1.1 Mean Climate of the 1700-1890 Period -- 4.2.1.2 Triggers of the Little Ice Age -- 4.2.2 The Maunder Minimum: A Compelling Case for Solar Forcing? -- 4.2.2.1 The Late Maunder Minimum: Rock Bottom of the Little Ice Age Climate -- 4.2.2.2 The Late Maunder Minimum in EKF400. , 4.2.3 The 1790s: Temporary Warmth and Strong Tropical Circulation -- 4.2.3.1 The Summers of 1800-1804 in Switzerland -- 4.2.3.2 Warming in Europe -- 4.2.3.3 Regional or Global? -- 4.2.3.4 Causes of the 1790s Warmth -- 4.2.4 Tambora Eruption, Dalton Minimum, and the Year Without a Summer of 1816 -- 4.2.4.1 Anatomy of the Year Without a Summer -- 4.2.4.2 Causes -- 4.2.4.3 The Year Without a Summer of 1816 in EKF400 and Early Instrumental Data -- 4.2.4.4 The Mistery Continues -- 4.2.5 The Maximum State of Alpine Glaciers in the 1850s -- 4.2.5.1 A 19th Century View of Glacier Changes -- 4.2.5.2 Causes of the 1850s Glacier Advance -- 4.2.5.3 Climate and Glacier Growth Assessed from HISTALP Data -- 4.2.5.4 Retreat -- 4.2.6 Global Droughts During 1876-1878 and El Niño -- 4.2.6.1 The 1877/1878 Drought in EKF400, CCC400, and 20CR -- 4.2.7 Frequent Flooding in the Central European Alps: 1830-1880s -- 4.2.7.1 The 1868 Flood in 20CR and Instrumental Data -- 4.2.8 The Broad Lines: The Little Ice Age -- 4.3 The Period from 1890 to 1945: Out of the Cold -- 4.3.1 Global Drivers and Global Changes -- 4.3.1.1 Changes in Circulation Indices -- 4.3.2 The Warming of the European Arctic from the 1910s to the 1940s -- 4.3.2.1 Mechanisms of the Early 20th Century Arctic Warming -- 4.3.2.2 The Early 20th Century Arctic Warming in CCC400, 20CR, and REC1 -- 4.3.3 The ``Dust Bowl'' Droughts of the 1930s -- 4.3.3.1 Development and Causes of the Dust Bowl -- 4.3.3.2 The Dust Bowl in CCC400, 20CR, Reconstruction and Upper-Level Data -- 4.3.3.3 Puzzle Solved? -- 4.3.4 Global Climate Anomalies During the 1939-1942 El Niño -- 4.3.4.1 The 1940-1942 Climate Anomaly in REC1, CCC400, and HISTOZ -- 4.3.4.2 Wider Effects of El Niño -- 4.3.5 The Broad Lines: Out of the Cold -- 4.4 The Period from 1945 to 1985: Delusive Stability -- 4.4.1 Global Drivers and Global Changes. , 4.4.2 Changes in Atmospheric Constituents -- 4.4.2.1 Tropospheric Aerosols -- 4.4.2.2 Ozone, Methane and Earth's Changing Oxidation Capacity -- 4.4.2.3 A Thickening Ozone Layer? -- 4.4.3 European Summers of 1945-1949 -- 4.4.3.1 Causes and Mechanisms -- 4.4.3.2 The Droughts in CCC400, 20CR, and REC2 -- 4.4.3.3 The 1947 Heatwaves -- 4.4.4 Sahel Pluvial and Drought -- 4.4.4.1 Causes and Mechanisms of the Drought -- 4.4.4.2 The Sahel Pluvial and Droughts in CCC400, REC2, and ECHAM-HAM Nudged Simulations -- 4.4.5 The Climate Shift of 1976/1977 -- 4.4.6 The Broad Lines: Delusive Stability -- 4.5 The Period Since 1985: Accelerated and Slowed Warming -- 4.5.1 Global Drivers and Global Changes -- 4.5.1.1 Global Warming and More -- 4.5.1.2 Greenhouse Gases and Global Brightening -- 4.5.2 The Ozone Hole -- 4.5.2.1 Ozone Depletion and the Ozone Hole in the CASTRO Simulations -- 4.5.2.2 Effect of the Ozone Hole on Climate -- 4.5.2.3 The Southern Annular Mode -- 4.5.3 Eruption of Pinatubo -- 4.5.3.1 Stratospheric Ozone and Temperatures -- 4.5.3.2 Effects on the Energy Budget and the Water Cycle -- 4.5.3.3 Effects on the Biosphere -- 4.5.3.4 Small Eruptions -- 4.5.4 Warm European Winters, Increased Storminess and Positive NAO in the 1990s -- 4.5.4.1 Winter Storms -- 4.5.4.2 Forced NAO? -- 4.5.5 The El Niño of 1997/1998, Forest Fires and the Atmospheric Brown Cloud -- 4.5.5.1 Forest Fires -- 4.5.5.2 The Atmospheric Brown Cloud -- 4.5.6 Droughts in Australia and the Northern Subtropics -- 4.5.6.1 Subtropical Drought 1998-2004 -- 4.5.6.2 The Millenium Drought in Australia -- 4.5.7 Megaheatwaves -- 4.5.7.1 Record-Breaking Heatwaves in the NCEP/NCAR Reanalysis -- 4.5.7.2 Changes in Heatwaves -- 4.5.8 Recent Arctic Warming -- 4.5.8.1 Record Sea Ice Loss -- 4.5.8.2 Vertical Structure of Temperature and Moisture Changes. , 4.5.8.3 Links with the Extratropics and Atmospheric Circulation.
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  • 2
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Climatic changes -- History -- 20th century -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (374 pages)
    Edition: 1st ed.
    ISBN: 9781402067662
    Series Statement: Advances in Global Change Research Series ; v.33
    DDC: 551.6
    Language: English
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  • 3
    Online Resource
    Online Resource
    Cham : Springer
    Keywords: Climatology ; Environment ; Environment ; Climatology ; Anthropozän ; Klimaschwankung ; Paläoklima ; Holozän ; Kleine Eiszeit ; Klimaänderung ; Paläoklimatologie ; Anthropozän ; Klimaschwankung ; Paläoklima ; Holozän ; Kleine Eiszeit ; Klimaänderung ; Paläoklimatologie
    Description / Table of Contents: 1. Introduction -- 2. The Basis: Past Climate Observations and Methods -- 3. The Machinery: Mechanisms behind Climate Changes -- 4. Climate Changes since 1700 -- 5. Conclusions -- References.
    Type of Medium: Online Resource
    Pages: Online-Ressource (XV, 360 p. 217 illus., 178 illus. in color, online resource)
    Edition: 1st ed. 2015
    ISBN: 9783319190426
    Series Statement: Advances in Global Change Research 55
    Language: English
    Note: Description based upon print version of record , 1. Introduction2. The Basis: Past Climate Observations and Methods -- 3. The Machinery: Mechanisms behind Climate Changes -- 4. Climate Changes since 1700 -- 5. Conclusions -- References.
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  • 4
    Keywords: Klimatologie ; Historische Klimatologie ; Humboldt, Alexander von 1769-1859 ; Klimatologie ; Geschichte ; Humboldt, Alexander von 1769-1859 ; Klimatologie ; Geschichte
    Type of Medium: Book
    Pages: 239 Seiten , Illustrationen, Diagramme, Karten , 23.5 cm x 19.5 cm
    Edition: 1. Auflage
    ISBN: 9783258083247 , 325808324X
    Series Statement: Haupt Natur
    DDC: 551.5092
    RVK:
    RVK:
    Language: German
    Note: Literaturverzeichnis: Seite 221-227
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 448 (2007), S. 992-992 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Sir 'Atmospheric brown clouds', resulting from the burning of fossil fuels and biomass, have recently been reported to have a large effect on climate by altering the atmosphere's absorption of solar radiation (V. Ramanathan et al. Nature 448, ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Journal of atmospheric chemistry 31 (1998), S. 299-319 
    ISSN: 1573-0662
    Keywords: surface ozone ; total ozone ; UV-B radiation ; radiation model ; ozone photolysis ; photochemistry
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Record high near-surface ozone concentrations at two elevated sites (Chaumont, 1140 m asl, and Rigi, 1030 m asl) in Switzerland were observed simultaneously with extremely low total ozone during a fair weather period in mid-February 1993. An analysis of ozone, temperature, humidity, and wind profiles suggests that the surface ozone peaks were most possibly generated within the region in a layer between about 1000 and 1500 m asl. Mean diurnal cycles of ozone concentration during the period shows a strong increase from late morning to late afternoon at Chaumont and at the same time a decrease at the high alpine site Jungfraujoch (3580 m asl). The different diurnal ozone cycles can both be explained photochemically by taking into account the large difference in NOx concentrations (about two orders of magnitude) between the sites. Photochemical processes are also indicated by the diurnal cycles of NO2 and NO concentration. As a strong photochemical activity is not expected in mid-February at 47°N, we hypothesize that the extremely low total ozone played a role. Total ozone controls the amount of UV-B radiation reaching the troposphere and thus influences photochemical processes. Using a radiation model, we calculated an increase in ozone photolysis at Chaumont and Jungfraujoch of 73% and 83%, respectively, on the day with the lowest total ozone (243 DU) compared to average February conditions (335 DU). It is suggested that total ozone changes have the potential to stimulate photochemistry sufficiently to produce the observed surface ozone peaks at Chaumont and Rigi of 61 and 64 ppbv, respectively. A fog layer just below Chaumont during these days probably also influenced photochemistry, but on a smaller spatial scale. Our empirical results on the influence of changing UV radiation on tropospheric photochemistry are in close agreement with model studies of other groups. Although this case study represents unique conditions, a distinct anticorrelation between near-surface ozone at Chaumont and total ozone also appears in other years (1992–1997) when selecting fair weather days in mid-February. However, other influences cannot be excluded. The selected days provide evidence of a significant photochemical source of ozone in the mid-latitude lower troposphere in late winter.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2019-03-29
    Description: This report outlines the structure of and summarizes the recommendations made at the 5th International Conference on Reanalysis (ICR5)1, attended by 259 participants from 37 countries, in Rome (Italy), on 13-17 November 2017. It first summarizes the conference structure. Then, the key recommendations of ICR5 are given for the five main conference topics: production; observations (data rescue and preparation); data assimilation methods; quality assurance of reanalysis; and applications in science, services, and policymaking. Lastly, five high-level recommendations are proposed to managing agencies on how best to advance the field of reanalyses, which serves tens of thousands of users, via enhanced research, development, and operations.
    Description: Published
    Description: ES139-ES144
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2017-06-06
    Description: Eurasian fall snow cover changes have been suggested as a driver for changes in the Arctic Oscillation and might provide a link between sea-ice decline in the Arctic during summer and atmospheric circulation in the following winter. However, the mechanism connecting snow cover in Eurasia to sea-ice decline in autumn is still under debate. Our analysis is based on snow observations from 820 Russian land stations, moisture transport using a Lagrangian approach derived from meteorological re-analyses. We show that declining sea-ice in the Barents and Kara Seas (BKS) acts as moisture source for the enhanced Western Siberian snow depth as a result of changed tropospheric moisture transport. Transient disturbances enter the continent from the BKS region related to anomalies in the planetary wave pattern and move southward along the Ural mountains where they merge into the extension of the Mediterranean storm track.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 9
    Publication Date: 2013-10-26
    Print ISSN: 0941-2948
    Electronic ISSN: 1610-1227
    Topics: Geography , Physics
    Published by Schweizerbart
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  • 10
    Publication Date: 2013-10-13
    Print ISSN: 0940-5550
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Philosophy
    Published by oekom
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