Search results for "TLA"

showing 10 items of 1764 documents

Numerical evidence for thermohaline circulation reversals during the Maastrichtian

2005

[1] The sensitivity of the Maastrichtian thermohaline circulation to the opening/closing of marine communications between the Arctic and North Pacific oceans is investigated through a set of numerical experiments using the model CLIMBER-2 (Earth Model of Intermediate Complexity). We show here that the opening or closing of an Arctic-Pacific marine gateway induces transitions between different equilibrium states of the thermohaline circulation. Sensitivity tests of the inferred modes of thermohaline circulation to atmospheric CO2 level changes have also been explored. An abrupt switch in deep convection from high northern to high southern latitudes, a change consistent with isotopic evidence…

010504 meteorology & atmospheric sciencesNorth Atlantic Deep Water010502 geochemistry & geophysics01 natural sciencesCretaceousLatitudeGeophysicsOceanographyShutdown of thermohaline circulationArctic13. Climate actionGeochemistry and PetrologyClimatologyThermohaline circulationClimate model14. Life underwatergeographic locationsGeologySea level0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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Radiogenic isotopes: new tools help reconstruct paleocean circulation and erosion input

2001

Ocean and atmosphere circulation and continental weathering regimes have undergone great changes over thousands of years as well as tens of millions of years. During the glacial stages of the Pleistocene, ocean circulation was generally more sluggish and deep water circulation in the Atlantic had a shallower flow. At the same time, weathering on the continents was enhanced by glacial erosion, particularly in high northern latitudes, which increased the input of erosional detritus into the ocean. In addition, atmospheric pressure gradients were larger, leading to higher wind speeds and increased supply of aeolian dust to the ocean. Prior to the onset of Northern Hemisphere glaciation and pro…

010504 meteorology & atmospheric sciencesPleistoceneNorth Atlantic Deep WaterOcean currentPhysical oceanography010502 geochemistry & geophysics01 natural sciencesOceanographyShutdown of thermohaline circulation13. Climate actionInterglacialGeneral Earth and Planetary SciencesThermohaline circulationGlacial periodGeology0105 earth and related environmental sciencesEOS
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Hydrological drivers of wetland vegetation community distribution within Everglades National Park, Florida

2010

The influence of hydrological dynamics on vegetation distribution and the structuring of wetland environments is of growing interest as wetlands are modified by human action and the increasing threat from climate change. Hydrological properties have long been considered a driving force in structuring wetland communities. We link hydrological dynamics with vegetation distribution across Everglades National Park (ENP) using two publicly available datasets to study the probability structure of the frequency, duration, and depth of inundation events along with their relationship to vegetation distribution. This study is among the first to show hydrologic structuring of vegetation communities at…

010504 meteorology & atmospheric sciencesRange (biology)Climate changeWetland010501 environmental sciences01 natural sciencesModelsVegetation typeValidationLandscapeTemporal scales0105 earth and related environmental sciencesWater Science and TechnologyHydrologyEverglades Vegetation Hydrology Wetlandsgeographygeography.geographical_feature_categoryVegetationNational parkSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaCommunity structureVegetation15. Life on landEvergladesScale13. Climate actionWetlandsEnvironmental scienceHydrology
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Late Quaternary Variations in the South American Monsoon System as Inferred by Speleothems—New Perspectives using the SISAL Database

2019

Here we present an overview of speleothem δ18O records from South America, most of which are available in the Speleothem Isotopes Synthesis and Analysis (SISAL_v1) database. South American tropical and subtropical speleothem δ18O time series are primarily interpreted to reflect changes in precipitation amount, the amount effect, and consequently history of convection intensity variability of convergence zones such as the Intertropical Convergence Zone (ITCZ) and the South America Monsoon System (SAMS). We investigate past hydroclimate scenarios in South America related to the South American Monsoon System in three different time periods: Late Pleistocene, Holocene, and the last tw…

010504 meteorology & atmospheric sciencesSAMSSpeleothemlcsh:GN281-289SubtropicsSouth American Monsoon System010502 geochemistry & geophysicscomputer.software_genreMonsoon01 natural scienceslcsh:StratigraphyEarth and Planetary Sciences (miscellaneous)PrecipitationSISALHolocenelcsh:QE640-6990105 earth and related environmental sciencesEarth-Surface Processesgeographyquaternarygeography.geographical_feature_categoryDatabasespeleothemsIntertropical Convergence ZoneMUDANÇA CLIMÁTICAlcsh:Human evolutionSouth Atlantic Convergence ZoneQuaternarycomputerGeologyQuaternary
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Using hydrological connectivity to detect transitions and degradation thresholds: Applications to dryland systems

2020

In arid and semi-arid ecosystems, shortage of water can trigger changes in landscapes’ structures and function leading to degradation and desertification. Hydrological connectivity is a useful framework for understanding water redistribution and scaling issues associated with runoff and sediment production, since human and/or natural disturbances alter surface water availability and pathways increasing/decreasing connectivity. In this paper, we illustrate the use of the connectivity framework for several examples of dryland systems that are analysed at a variety of spatial and temporal scales. In doing so, we draw particular attention to the analysis of coevolution of system structures and …

010504 meteorology & atmospheric sciencesWater en Landgebruikmedia_common.quotation_subjectWetlandSemi-arid environments01 natural sciencesSoilBodemSoil Water and Land UseTemporal scales0105 earth and related environmental sciencesEarth-Surface Processesmedia_commongeographygeography.geographical_feature_categoryWIMEKbusiness.industryWater and Land UseEnvironmental resource management04 agricultural and veterinary sciencesVegetation15. Life on landBodemfysica en LandbeheerPE&RCHydrological connectivityAridLandscape evolutionGeoecologyBodem Water en LandgebruikSoil Physics and Land ManagementDesertification040103 agronomy & agricultureLand degradationErosion0401 agriculture forestry and fisheriesEnvironmental scienceLand degradationbusinessSurface runoff
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Holocene climate variability in north-eastern Italy: potential influence of the NAO and solar activity recorded by speleothem data

2012

Abstract. Here we present high-resolution stable isotope and lamina thickness profiles as well as radiocarbon data for the Holocene stalagmite ER 76 from Grotta di Ernesto (north-eastern Italy), which was dated by combined U-series dating and lamina counting. ER 76 grew between 8 ka (thousands of years before 2000 AD) and today, with a hiatus from 2.6 to 0.4 ka. Data from nine meteorological stations in Trentino show a significant influence of the North Atlantic Oscillation (NAO) on winter temperature and precipitation in the cave region. Spectral analysis of the stable isotope signals of ER 76 reveals significant peaks at periods of 110, 60–70, 40–50, 32–37 and around 25 a. Except for the …

010504 meteorology & atmospheric scienceslcsh:Environmental protectionStratigraphySpeleothemStalagmite010502 geochemistry & geophysics01 natural scienceslaw.inventionMediterranean sealcsh:Environmental pollutionCavelawlcsh:TD169-171.814. Life underwaterRadiocarbon datinglcsh:Environmental sciencesHolocene0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryPaleontology13. Climate actionPluvialNorth Atlantic oscillationClimatologylcsh:TD172-193.5GeologyClimate of the Past
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Soil features in rookeries of Antarctic penguins reveal sea to land biotransport of chemical pollutants

2017

© The Author(s).

010504 meteorology & atmospheric scienceslcsh:MedicineSoil Chemistry010501 environmental sciences01 natural sciencesGeographical LocationsSoilOrganic Chemicalslcsh:ScienceSoil MicrobiologyTotal organic carbonRookeryMultidisciplinaryEcologySoil chemistryGenomicsSeabirdsChemistryMedical MicrobiologyVertebratesPhysical SciencesEnvironmental PollutantsSeasonsSoil microbiologyResearch ArticleChemical ElementsPollutantsDeceptionOceans and SeasSoil ScienceAntarctic RegionsMicrobial GenomicsPenguinsMicrobiologyBirdsGeneticsAnimalsEnvironmental ChemistryDominance (ecology)0105 earth and related environmental sciencesPollutantShetlandBehaviorBacterialcsh:REcology and Environmental SciencesOrganismsBiology and Life SciencesSpheniscidaeAmniotesPeople and PlacesSoil waterAntarcticaMetagenomeEnvironmental sciencelcsh:QMicrobiomeMetagenomics
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Climate variability and lake ecosystem responses in western Scandinavia (Norway) during the last Millennium

2017

This paper provides a high-resolution temperature reconstruction for the last Millennium from Lake Atnsjøen, SE Norway (61°52′31″N, 10°10′37″E). The sedimentary record reveals strong influence of the large-scale global climate patterns on the local climate in southern part of Eastern Norway. We reconstructed mean July air temperature using Chironomidae-based transfer function and fossil Chironomidae assemblages. The reconstruction was supported by a selection of climate-sensitive geochemical and paleoecological sedimentary proxies of terrestrial and aquatic origin, including Cladocera, pollen and macrofossils. Presented results revealed that summer temperatures were 1–2 °C warmer than the m…

010506 paleontology010504 meteorology & atmospheric sciencesDrainage basinta1171chironomidsOceanography01 natural sciencesChironomidaeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyLake ecosystemPaleontologyMacrofossilVegetationbiology.organism_classificationCladoceratemperature reconstructionOceanographyProductivity (ecology)North Atlantic oscillationvesikirputLittle Ice Ageta1181Sedimentary rockScandinaviaNorth Atlantic OscillationGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Carbon accumulation rate in a raised bog in Latvia, NE Europe, in relation to climate warming

2018

The carbon accumulation rate (CAR) over the last 180 years was estimated by measuring carbon concentrations in 1-cm layers in a fine-resolution dated and analysed peat sequence in Teiči Bog, Latvia, NE Europe. We used the Granger causality test to examine the temporal (lagged) relationships between the CAR and the historical climate variables. Our results showed that the average CAR was 192 g C m–2 yr–1 during the last 180 years and 169 g C m–2 yr–1 when excluding the acrotelm where decomposition and the stock of carbon are still not in the balance. The Granger causality test showed significant positive temporal associations between the temperature and the CAR, indicating that the temperatu…

010506 paleontology010504 meteorology & atmospheric scienceslcsh:QE1-996.5Global warmingGranger causality test.chemistry.chemical_elementC/N ratio01 natural scienceslcsh:GeologySphagnumchemistryGeneral Earth and Planetary SciencesEnvironmental sciencecarbon accumulation ratepeatlandPhysical geographyCarbonRaised bog0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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North Atlantic Oscillation recorded in carbonate δ18O signature from Lagunillo del Tejo (Spain)

2016

Abstract Oxygen (δ18O) and carbon (δ13C) isotope compositions of authigenic carbonates measured in Lagunillo del Tejo sediment document precipitation variability during the last millennium in the Iberian Range. Modern water samples show that Lagunillo δ18O and δD plot below the Global Meteoric Water Line (GMWL). Sediment samples show a covariant trend between carbonate δ18O and δ13C, indicating that the precipitation/evaporation ratio has largely controlled the isotopic composition of this lake. This covariant trend is used to extract information about past lake level changes. Humid periods occurred around AD 1300–1450, AD 1620–1775 and AD 1950–1980, while the driest periods were concentrat…

010506 paleontology010504 meteorology & atmospheric sciencesδ13CGlobal meteoric water lineδ18OPaleontologySedimentAuthigenicOceanography01 natural scienceschemistry.chemical_compoundOceanographychemistryNorth Atlantic oscillationCarbonatePrecipitationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface Processes
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