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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Climatic changes - Mediterranean Region. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (438 pages)
    Edition: 1st ed.
    ISBN: 9780080460796
    Series Statement: Issn Series ; v.Volume 4
    DDC: 551.691822
    Language: English
    Note: Cover -- Abridged Contents -- Contents -- Preface -- The Mediterranean Climate: An Overview of the Main Characteristics and Issues -- The Mediterranean Region: Climate and Characteristics -- Regional Processes and Links to the Global Climate -- Climate Trends and Change at Regional Scale -- Socio-environmental Aspects -- Acknowledgements -- References -- Mediterranean Climate Variability over the Last Centuries: A Review -- Introduction -- Past Regional Mediterranean Climate Evidence and Extremes -- Evidence from Early Instrumental and Documentary Data -- Iberian Peninsula -- France -- Italy -- Southern Balkans, Greece and Eastern Mediterranean -- Northern Africa -- Ship Logbooks as a New Documentary Proxy for Past Mediterranean Climate -- Evidence from Natural Proxies -- Tree-Ring Information from the Iberian Peninsula and Italy -- Tree-Ring Information from South Eastern Europe and Eastern Mediterranean -- Tree-Ring Information from Northern Africa -- Speleothems -- Corals -- Evidence from Lower Resolution Natural Proxies and New Marine Archives -- Subsurface temperature information in the Mediterranean from borehole data -- Mediterranean sea temperatures and sea-water chemistry derived from Vermetids, non--tropical, and deep-sea corals -- Large-Scale Climate Reconstructions and Importance of Proxy Data for the Mediterranean -- Mediterranean Winter Temperature and Precipitation Variability over the Last 500 Years -- Connection between the Large-Scale Atmospheric Circulation and Mediterranean Winter Climate over the Last Centuries -- Major Atmospheric Circulation Patterns Associated with Mediterranean Winter Climate Anomalies -- Mediterranean Climate Variability since the Mid-Seventeenth Century in Terms of Large-Scale Circulation Dynamics. , Running Correlation Analysis between the Large-Scale Atmospheric Circulation and Mediterranean Winter Climate over the Last Centuries -- Teleconnection Studies with Other Parts of the Northern Hemisphere -- Mediterranean Winter Temperature and Precipitation Reconstructions in Comparison with the ECHO-G and HadCM3 Coupled Models -- Past Climate Variability and its Relations to Volcanism, Solar Activity and GHG Concentrations: Reconstructions and Models -- Conclusions -- Outlook -- Acknowledgements -- References -- Relations between Climate Variability in the Mediterranean Region and the Tropics: ENSO, South Asian and African Monsoons, Hurricanes and Saharan Dust -- Introduction -- ENSO Impact on the Mediterranean Climate -- ENSO and Eastern Mediterranean (EM) Rainfall -- ENSO and the Western Mediterranean Relationship -- ENSO and Extreme Mediterranean Rainfall -- Transient and Stationary Waves Approach -- Possible Coupling Mechanism of ENSO and the Mediterranean -- South Asian Monsoon Variability and the Mediterranean Climate -- Mediterranean Climate and South Asian Rainfall -- African Monsoon Impact on the Climate of the Mediterranean -- Tropical Cyclones' Impact on the Mediterranean Climate -- Tropical Intrusions into the Mediterranean Basin -- Mediterranean Dust Transport from Sahara -- Conclusions and Outlook -- Future Research on ENSO Impact on Mediterranean Climate -- Future Research on South Asian Monsoon Variability and the Mediterranean Climate -- Future Research on African Monsoon Impacts on the Climate of the Mediterranean -- Future Research on Tropical Intrusions into the Mediterranean Basin -- Acknowledgements -- References -- Relations between Variability in the Mediterranean Region and Mid-Latitude Variability -- Introduction -- Mid-Latitude Modes of Atmospheric Variability and their Impact -- The North Atlantic Oscillation Pattern. , The Eastern Atlantic and Eastern Atlantic/Western Russia Patterns -- The Scandinavian and Blocking Patterns -- Other Modes -- Temperature Variability -- Precipitation Variability -- Trends -- Temperature Trends -- Precipitation Trends -- Contributing Factors for Observed Temperature and Precipitation™Trends -- Other Important Forcing Factors -- Tropical and Extratropical SST -- Solar Variability -- Future Outlook -- Acknowledgements -- References -- Changes in the Oceanography of the Mediterranean Sea and their Link to Climate Variability -- Introduction -- The Forcing of the Mediterranean Sea -- Air& -- ndash -- Sea Interaction -- River Outflow -- Exchanges through the Strait of Gibraltar -- The Exchange with the Black Sea -- The Mediterranean Overturning Circulation -- The Modification of the Atlantic Inflow -- Intermediate Water Formation -- Deep Water Formation in the Eastern Mediterranean -- Deep Water Formation in the Western Mediterranean -- Climatic Changes in the Mediterranean Sea Circulation -- Multidecadal Trends in Water Mass Characteristics -- Rapid Changes: The Eastern Mediterranean Transient -- What Caused the EMT? -- mk4004sec16sec16 -- Where did the Deep Water Formation Take Place? -- How Much Deep Water was Produced by the EMT? -- Why did the EMT Happen? -- The Impact of Large-Scale Atmospheric Variability on the Mediterranean Sea -- Sea Level Changes in the Mediterranean Sea -- Extreme Sea Levels -- Changes in the Wind-wave Field -- Outlook and Future Challenges -- Acknowledgements -- References -- The Atlantic and Mediterranean Sea as Connected Systems -- Introduction -- Mediterranean Outflow vs. Mediterranean Internal Variability -- Description of Numerical Model -- Zonal and Meridional Cells -- Mean State and Variability -- Timescales of Mediterranean Thermohaline Circulation -- Decadal Oscillations in the Mediterranean Sea. , The Strait of Gibraltar: A Gate to the Atlantic -- Spreading of Mediterranean Outflow Water in the North Atlantic -- Dynamics of Mediterranean Outflow Water -- mk4005sec11asec11a -- Meddies -- Mediterranean Undercurrent -- Mediterranean Outflow Water and Stability and Variability of™Meridional Overturning Circulation -- Modelling of Mediterranean Outflow Water -- mk4005sec15asec15a -- Simplified Models -- General Circulation Model Studies -- Discussion and Future Challenges -- References -- Cyclones in the Mediterranean Region: Climatology and Effects on the Environment -- Introduction -- & -- ldquo -- Historical& -- rdquo -- Notes -- Mediterranean Cyclones: Data, Methods and Dynamics -- Dynamics of Cyclones in the Mediterranean Region -- Available Sets of Data -- Methodology -- Climatology of Cyclones in the Mediterranean -- Characteristics, Sub-Areas of Cyclogenesis, Seasonality and™Generation™Mechanisms -- The Role of Large-Scale Climate Patterns on the Mediterranean™Cyclones -- Trends -- Weather Patterns and Mediterranean Environment -- Precipitation -- Strong Winds -- Storm Surge -- Wind Waves -- Landslides -- Conclusions -- Outlook -- Acknowledgements -- References -- Regional Atmospheric, Marine Processes and Climate Modelling -- Introduction -- Teleconnection Patterns from the Mediterranean Region -- Mediterranean Thermohaline Circulation and its Sensitivity to Atmospheric Forcing -- Sensitivity of the Mediterranean Thermohaline Circulation to Anthropogenic Global Warming -- Current Status of Mediterranean Regional Climate Modelling -- Atmosphere-Sea Coupled Modelling -- Perspectives and Outlooks -- High-Resolution Mediterranean Climate Modelling Systems -- Development and Validation of Integrated Regional Modelling Systems -- Acknowledgements -- References -- The Mediterranean Climate Change under Global Warming -- Introduction. , Global-Coupled Climate Models -- Regional Climate Scenarios -- Statistical Downscaling -- RCM Simulations -- AGCM Simulations with Variable Resolution -- Impacts on Land Surface and Vegetation -- Future Research -- References -- Subject Index.
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  • 2
    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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  • 3
    Book
    Book
    Geesthacht : GKSS-Forschungszentrum
    Keywords: Report ; Forschungsbericht
    Type of Medium: Book
    Pages: 53 S , graph. Darst
    Series Statement: GKSS 93/E/44
    Language: English
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  • 4
    Type of Medium: Book
    Pages: IV, 88 S , graph. Darst
    Series Statement: Technical report / European Centre for Medium-Range Weather Forecasts 67
    Language: English
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  • 5
    Publication Date: 2021-07-14
    Description: Soreq (Israel) and Corchia (central Italy) Caves are located 2500 km far apart along the Mediterranean winterstormtrack and are ideally suited for investigating past variations of winter rainfall in the Mediterranean region. Analyses of speleothem δ18O records from both caves for the period between ca. 7 to 4 ka BP show some striking similarities for the ca. 6 and 4 ka interval, but lack agreement between ca. 7 to 6 ka BP. Two prominent isotopic excursions, argued to reflect relatively drier conditions, are centred at ca. 5.6 and ca. 5.2 ka. The 5.2 ka event lasts less than a century, whereas the 5.6 ka event extends fromca. 5.7 to 5.4 ka. A period of progressive drying is also apparent fromca. 5 to 4 ka. Another prominent event, reflecting wetter conditions, is recorded in both records at ca. 5.8 ka and seems to last several decades. The 5.6 and 5.2 ka events occurred within a period of higher deposition of haematite-stained grains in cores of the sub-polar North Atlantic, and correlationwith the wind strength proxy record fromHólmsá loess profile in Iceland suggests that rainfall reductionwas related to a reduced vapour advection from Atlantic towards the Mediterranean connected to northward shift in the Westerlies. A comparisonwith Alpine records, including the Spannagel Cave isotope record, suggests that dry events recorded at Soreq and Corchia caves may correspond to wetter (lake high stands) and cooler (glacier expansion) conditions in the Alpine region, indicating complex regional climate re-organization.
    Description: Published
    Description: 130-139
    Description: 5A. Paleoclima e ricerche polari
    Description: JCR Journal
    Keywords: Speleothems ; Oxygen Isotope ; Corhia ; Soreq ; Dry mid-Holocene events ; Mediterranean climate
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2021-05-19
    Description: The Mediterranean is expected to be one of the most prominent and vulnerable climate change “hotspots” of the twenty-first century, and the physical mechanisms underlying this finding are still not clear. Furthermore, complex interactions and feedbacks involving ocean–atmosphere–land–biogeochemical processes play a prominent role in modulating the climate and environment of the Mediterranean region on a range of spatial and temporal scales. Therefore, it is critical to provide robust climate change information for use in vulnerability–impact–adaptation assessment studies considering the Mediterranean as a fully coupled environmental system. The Mediterranean Coordinated Regional Downscaling Experiment (Med-CORDEX) initiative aims at coordinating the Mediterranean climate modeling community toward the development of fully coupled regional climate simulations, improving all relevant components of the system from atmosphere and ocean dynamics to land surface, hydrology, and biogeochemical processes. The primary goals of Med-CORDEX are to improve understanding of past climate variability and trends and to provide more accurate and reliable future projections, assessing in a quantitative and robust way the added value of using high-resolution and coupled regional climate models. The coordination activities and the scientific outcomes of Med-CORDEX can produce an important framework to foster the development of regional Earth system models in several key regions worldwide.
    Description: Published
    Keywords: MED-CORDEX ; Climate changes
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.1187-1208
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  • 7
    Publication Date: 2020-02-12
    Type: info:eu-repo/semantics/bookPart
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  • 8
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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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  • 9
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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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