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  • 2020-2024  (2)
  • 2010-2014  (2)
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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Mittelmeerraum. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (593 pages)
    Edition: 1st ed.
    ISBN: 9780123914774
    DDC: 551.691822
    Language: English
    Note: Front Cover -- The Climate of the Mediterranean Region -- Copyright Page -- Contents -- Preface -- Foreword -- List of Contributors -- Introduction: Mediterranean Climate-Background Information -- I.1 Introduction -- I.2 Socioeconomic Characteristics and Main Vulnerabilities -- I.3 The Mediterranean Region -- I.4 Paleoclimate Reconstruction -- I.5 The Climate of the Mediterranean Region in Historical Times -- I.6 Present Seasonal Temperature and Precipitation and Their Trends -- I.7 Rain Spells and Their Characterization -- I.8 Temperature and Precipitation Extremes -- I.8.1 Temperature Extremes -- I.8.2 Precipitation Extremes -- I.9 Water Balance and Mediterranean Sea Circulation -- I.9.1 Water Balance -- I.9.2 Mediterranean Sea Circulation and Water Masses -- I.10 Present Mediterranean Sea Level -- I.11 River Runoff -- I.12 Cyclone and Main Synoptic Patterns -- I.13 Mediterranean Winds -- I.14 Wind-Generated Waves -- I.15 Aerosol Climatology over the Basin -- I.15.1 Variability -- I.15.2 Radiative Impact -- I.15.3 Impact on Precipitation -- I.16 Future Climate -- I.17 Major Open Issues -- I.17.1 Paleoclimate Reconstructions -- I.17.2 Historical Climatology -- I.17.3 Present Trends in Precipitation -- I.17.4 Water Budget -- I.17.5 Sea Level and Circulation -- I.17.6 The Role of Aerosols -- I.17.7 Climate Projections -- I.17.8 Information for Climate-Change Impacts -- I.17.9 Outlook -- Acknowledgments -- References -- Link -- 1 Paleoclimate Variability in the Mediterranean Region -- 1.1 Introduction to Paleoclimatic Reconstruction Methods -- 1.1.1 Reconstruction Approach -- 1.2 The Geological History of the Mediterranean Through the Meso-Cenozoic: From a Global Latitudinal Ocean to an Enclosed Sea -- 1.2.1 Origin of the Mediterranean -- 1.2.2 The Mediterranean and the Paratethys -- 1.2.3 Mediterranean Salinity Crisis. , The History of Mediterranean Desiccation -- The Onset of Gypsum Deposition on the Marginal Basins -- The Sea-Level Drawdown and Salt Precipitation -- The Lago Mare Phase -- 1.2.4 The Pliocene Mediterranean Flooding -- 1.2.5 Mediterranean Climate During the Pliocene -- 1.3 Sensitivity and Variability at Different Climate States -- 1.3.1 Warm Climate Intervals of the Pleistocene: The Case of the Last Interglacial -- 1.3.2 High-Frequency Variations: The Case of MIS 3 -- 1.3.3 Deglaciation(s): The Case of the Last Glacial-Interglacial Transition (LGIT) -- 1.3.4 Holocene Climate -- General North Hemispheric Climate -- The Holocene in the Mediterranean Region -- HO in the Mediterranean Region -- The 8.2 Event in the Mediterranean Region -- 1.4 Outlook -- Acknowledgments -- References -- 2 A Review of 2000 Years of Paleoclimatic Evidence in the Mediterranean -- 2.1 Introduction -- 2.2 Long Instrumental Data Series from the Mediterranean -- 2.3 Ships' Logbooks from the Mediterranean as Quasi-Instrumental Climate Information -- 2.4 Tree-Ring Information from the Mediterranean -- 2.5 Speleothem Information from the Mediterranean -- 2.6 Paleoflood and Storm Records from the Mediterranean -- 2.7 Lake Sediments from the Mediterranean -- 2.7.1 Late-Holocene Climate Records from Eastern Mediterranean Lake Sediments -- 2.7.2 The Western Mediterranean: Late-Holocene Climate Records from Iberian Lakes -- 2.8 Corals and Lower-Resolution Marine Proxies from the Mediterranean -- 2.8.1 Tropical Corals -- 2.8.2 Temperate Corals: Cladocora caespitosa -- 2.8.3 Deep-Water Corals: Desmophyllum dianthus, Lophelia pertusa, Madrepora oculata, Caryophyllia smithii -- 2.8.4 Low-Resolution Marine Proxies -- Sediment Cores -- Vermetids -- 2.9 Borehole Information from the Mediterranean -- 2.10 Vegetation, Land Use, and Fire History in Mediterranean Ecosystems. , 2.10.1 Mediterranean Vegetation Belts and Climate -- 2.10.2 Vegetation Changes and Land Use -- 2.10.3 Fire Activity -- 2.11 Pollen Data: Their Distribution and Possibilities/Challenges for Climate Reconstructions over the Mediterranean -- 2.12 Sea-Level Variations over the Last 2000 Years in the Mediterranean -- 2.13 Paleoclimate Modeling and Data Assimilation for Paleoclimatological Analysis in the Mediterranean -- 2.14 Data Assimilation with Paleo Data -- 2.15 Conclusions and Outlook -- Acknowledgments -- References -- 3 Circulation of the Mediterranean Sea and its Variability -- 3.1 Introduction -- 3.2 Changes in the Thermohaline Circulation of the Mediterranean Sea -- 3.2.1 Large-Scale Circulation Variability -- 3.2.2 Mesoscale Circulation Variability -- 3.2.3 Water-Mass Variability -- The Climatological Characteristics of Water Masses -- Interannual Variability -- Long-Term Changes -- 3.2.4 Changes in Water-Mass Formation -- The Eastern Basin -- The Western Basin -- 3.3 The Forcings of the Mediterranean Sea -- 3.3.1 The Surface Heat and Freshwater Exchanges -- Heat and Freshwater Budgets -- Climatological Mean Air-Sea Flux Fields -- Influence of Large-Scale Modes of Atmospheric Variability -- Regional Modeling/Dynamical Downscaling Perspective -- 3.3.2 The River Runoff -- 3.3.3 The Exchanges Through the Strait of Gibraltar -- 3.3.4 The Exchanges with the Black Sea -- The Region -- Interbasin Coupling and Contrasts -- Water Fluxes -- Strait Dynamics -- Climate Variability -- 3.3.5 The Exchanges Between the Eastern and the Western Mediterranean -- 3.4 Variability in the Heat and Freshwater Characteristics at Interannual to Multidecadal Timescales -- 3.5 Outlook and Future Research Priorities -- Acknowledgments -- References -- 4 Mediterranean Sea-Level Variability and Trends -- 4.1 Introduction. , 4.2 How Do We Observe Sea Levels in the Mediterranean Sea? -- 4.2.1 Tide Gauges -- 4.2.2 Satellite Measurements -- 4.2.3 Comparison Between Tide Gauge and Altimetry Data -- 4.2.4 Measurement of Land Movements -- 4.2.5 Synthesis of Sea-Level Observations into Sea-Level Indexes -- 4.3 Interannual to Interdecadal Mean Sea-Level Changes and Trends -- 4.3.1 Observed Mean Sea-Level Trends -- 4.3.2 The Atmospheric Contribution-Variability and Trends -- 4.3.3 The Steric Contribution-Variability and Trends -- 4.3.4 Mass Changes-Variability and Trends -- 4.3.5 Changes in the Oceanic Circulation -- 4.4 Interannual to Interdecadal Changes in the Seasonal Cycle -- 4.4.1 The Mean Seasonal Cycle -- 4.4.2 Changes in the Mean Seasonal Cycle -- 4.4.3 The Atmospheric Contribution to the Seasonal Cycle -- 4.4.4 The Steric Contribution to the Seasonal Cycle -- 4.4.5 The Mass Contribution to the Seasonal Cycle -- 4.4.6 The Oceanic Circulation and the Local Seasonal Cycle -- 4.5 Changes in Extreme Sea-Level Events -- 4.5.1 Extreme Sea Levels in the Mediterranean -- 4.5.2 Tidal Residuals/Storm Surges -- 4.5.3 Changes in Extreme Storm Surges -- 4.5.4 Meteotsunamis -- 4.6 Open Issues in the Study of Long-Term Sea-Level Variability -- 4.6.1 The Role of the Straits in Determining Long-Term Sea-Level Variability -- 4.6.2 Uncertainties in Estimates of Sea-Level Changes -- 4.6.3 Other Open Issues in Mediterranean Sea-Level Research -- 4.7 Conclusions -- Acknowledgments -- References -- 5 Climate of the Mediterranean: Synoptic Patterns, Temperature, Precipitation, Winds, and Their Extremes -- 5.1 Introduction -- 5.2 Teleconnection Patterns Influencing the MR -- 5.3 Cyclones in the MR and Links to Large-Scale Patterns -- 5.3.1 General Characteristics of Cyclones in the MR -- 5.3.2 Seasonal Variations of Cyclones -- 5.3.3 Genoa Cyclones and Mechanisms of Cyclone Development. , 5.3.4 Cyprus Cyclones and Their Related Rains -- 5.3.5 North African Cyclones -- 5.3.6 Explosive Cyclones in the Mediterranean -- 5.3.7 Links Between Cyclones and Large-Scale Patterns -- 5.3.8 Synoptic Patterns in the EM -- 5.4 Temperature and Temperature Extremes -- 5.4.1 Mean Temperature Trends and Large-Scale Atmospheric Circulation Regimes -- 5.4.2 Extreme Temperature and Large-Scale Atmospheric Circulation -- 5.5 Precipitation Extremes -- 5.6 Wind and Wind Extremes: Wind Storms, Dust Storms, and Storm Surges -- 5.6.1 Extreme Winds and Wind Storms in the Mediterranean -- 5.6.2 Local Winds and Wind Extremes -- 5.6.3 Dust Storms -- 5.6.4 Marine Storms -- 5.6.5 Ocean-Wave Variability -- 5.7 Conclusion -- Acknowledgments -- References -- 6 Large-Scale Atmospheric Circulation Driving Extreme Climate Events in the Mediterranean and its Related Impacts -- 6.1 Introduction -- 6.2 HW Mechanisms and Impacts -- 6.2.1 Atmospheric Circulation and HWs -- Persistent Circulation Anomalies -- Large-Scale Forcing Mechanisms -- Trends in Temperature/Atmospheric Circulation Relationship -- 6.2.2 HWs and Their Impacts in the Eastern and Western Mediterranean -- HWs in the Eastern Mediterranean -- Deadly HWs in the Eastern Mediterranean -- The Western Mediterranean: The 2003 HW Case Study -- 6.3 Mediterranean Droughts and the El Niño-Southern Oscillation -- 6.3.1 Influence of ENSO Extremes on Drought Conditions in the Mediterranean Basin -- 6.4 Mediterranean Water Cycle -- 6.4.1 Characterizing Major External and Internal Moisture Sources Affecting the Mediterranean Basin -- Main Moisture Sources -- 6.4.2 Long-Term Mediterranean Water-Cycle Changes in Observations -- 6.5 The NAO Impact on Renewable Energy and Vegetation Dynamics -- 6.5.1 The Role of Winter NAO in Modulating Cloud Cover and Available Solar Energy in the Western Mediterranean. , 6.5.2 Assessing the Role of NAO and Climate Variability in the Vegetation Dynamics over Iberia-Wheat Production in Portugal: A Case Study.
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  • 2
    Publication Date: 2020-02-12
    Type: info:eu-repo/semantics/bookPart
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  • 3
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-29
    Description: We propose an analytical expression describing the probability of occurrence of tornadoes as a function of selected meteorological variables. Our study is based on the available lists of recorded tornadoes events in the USA and Europe matched with the meteorological conditions provided by the high resolution ERA5 reanalysis data. The statistical validation of the results has been carried out using Bootstrap techniques and Monte Carlo permutation procedures. The considered variables are the convective available potential energy, the vertical wind shear, the storm-relative helicity, and the lifting condensation level. Our analysis suggests that the most suitable representation for the probability of occurrence of tornadoes is a bivariate exponential-like expression as a function of the convective available potential energy and either the wind shear or the storm relative helicity. This expression allows to compute the probability of tornado occurrence using data extracted from operational weather prediction and available climate projections, thus compensating for the lack of resolution needed to explicitly model tornadoes in these simulations. The proposed methodological approach can be used to obtaining formula of increasing accuracy as larger datasets of tornado events will become progressively available in the future.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 4
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-29
    Description: Model simulations of the last glacial maximum (LGM) and RCP8.5 projections suggest that factors responsible for past and future changes in the Mediterranean region are different. The wet LGM conditions were determined mainly by low evaporation, with some increase of precipitation in the western areas, while dry rcp8.5 conditions will be driven by a reduction of precipitation over the whole region. These changes were caused by atmospheric dynamics (changes of mean atmospheric circulation ) in LGM and it will be caused by the atmospheric thermodynamics (reduction of mean moisture content ) in the future rcp8.5. In both cases, the Mediterranean region appears to be more sensitive to climate change than the rest of areas within the same latitudinal range, particularly considering the hydrological cycle, whose characteristics in winter exhibit large changes between these two different climates. These conclusions emerge from the substantial consensus among six PMIP3 and CMIP5 models, simulating LGM, pre-Industrial and rcp8.5 climate conditions.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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