Search results for "climate"

showing 10 items of 4934 documents

Tropical Atlantic temperature seasonality at the end of the last interglacial

2015

The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice sheets. These perturbations are crucial for a better understanding of future climate change. The seasonal temperature changes of the tropical ocean, however, which play an important role in seasonal climate extremes such as hurricanes, floods and droughts at the present day, are not well known for this period that led into the last glacial. Here we present a monthly resolved snapshot of reconstructed sea surface temperature in the tropical North Atlantic Ocean for 117.7±0.8 kyr ago, using coral Sr/Ca and δ18O records. W…

geographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ18OOcean currentGeneral Physics and AstronomyGeneral ChemistryTropical Atlantic010502 geochemistry & geophysics01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyArticleSea surface temperatureOceanography13. Climate actionInterglacialClimate model14. Life underwaterGlacial periodIce sheetGeology0105 earth and related environmental sciences
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Antarctic erosion history reconstructed by Terre Adélie moraine geochronology

2020

AbstractWe report apatite fission-track and 10Be terrestrial cosmogenic nuclide (TCN) dating of 14 moraine boulders originating from inland Terre Adélie, East Antarctica. These data show cooling of the Proterozoic Terre Adélie craton at < ~120°C between 350 and 300 Ma, suggesting > 4 km temperate glacial erosion during the Late Palaeozoic Ice Age, followed by nearly null Mesozoic erosion and low glacial erosion (< 2 km) in the Cenozoic. Based on glacial flux maps, the origin of the boulders may be located ~400 km upstream. Preliminary TCN (10Be) datings of moraine boulders cluster within the last 30 ka. Cosmogenic ages from the Lacroix Nunatak suggest a main deglaciation after the …

geographyNunatakgeography.geographical_feature_category010504 meteorology & atmospheric sciences[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeology010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontology13. Climate actionMoraine[SDU]Sciences of the Universe [physics]GeochronologyIce ageDeglaciationGlacial periodYounger Dryas[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/GeomorphologyCosmogenic nuclideEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences
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Expected trends and surprises in the Lateglacial and Holocene vegetation history of the Iberian Peninsula and Balearic Islands

2010

18 páginas, 13 figuras.

geographyPalaeobotanygeography.geographical_feature_categoryHoloceneEcologyPaleontologyClimate changePalaeoecologyPlant communityVegetationPaleolíticQuaternaryPeninsulaPaleoecologyGlacial periodIberiaQuaternaryPalaeogeographyEcology Evolution Behavior and SystematicsHoloceneGeology
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A Soil Water Assessment Tool (SWAT) Modeling Approach to Prioritize Soil Conservation Management in River Basin Critical Areas Coupled With Future Cl…

2021

About 44% of the Indian landmass experiences the adverse impact of land degradation. This loss of sediments caused by soil erosion reduces the water quality of local water bodies and decreases agricultural land productivity. Therefore, decision-makers must formulate policies and management practices for sustainable management of basins that are cost-effective and environment friendly. Application of the best management practices (BMPs) to properly manage river basins is difficult and time-consuming. Its implication under various climate change scenarios makes it more complicated but necessary to achieve sustainable development. In this study, the soil and water assessment tool (SWAT) model…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciences0208 environmental biotechnologyDrainage basinClimate change02 engineering and technologyFuture climate01 natural sciences020801 environmental engineeringEnvironmental sciencesSoil waterLand degradationEnvironmental scienceGE1-350Scenario analysisWater qualitySoil conservationWater resource management0105 earth and related environmental sciencesGeneral Environmental ScienceAir, Soil and Water Research
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Stratospheric aerosol-Observations, processes, and impact on climate

2016

Interest in stratospheric aerosol and its role in climate have increased over the last decade due to the observed increase in stratospheric aerosol since 2000 and the potential for changes in the sulfur cycle induced by climate change. This review provides an overview about the advances in stratospheric aerosol research since the last comprehensive assessment of stratospheric aerosol was published in 2006. A crucial development since 2006 is the substantial improvement in the agreement between in situ and space-based inferences of stratospheric aerosol properties during volcanically quiescent periods. Furthermore, new measurement systems and techniques, both in situ and space based, have be…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAir pollutionClimate changeSulfur cyclerespiratory system010502 geochemistry & geophysicsmedicine.disease_causeAtmospheric sciencescomplex mixtures01 natural sciencesAerosolchemistry.chemical_compoundGeophysicschemistryVolcano13. Climate actionAtmospheric chemistryClimatologymedicineEnvironmental scienceClimate model0105 earth and related environmental sciencesCarbonyl sulfideReviews of Geophysics
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Seasonal variability in silicate weathering signatures recorded by Li isotopes in cave drip-waters

2021

Abstract Silicate weathering is a critical process in Earth’s carbon cycle, but the fundamental controls on weathering are poorly understood and its response to future climate change is uncertain. In particular, the potential for changes in seasonality or extreme weather events to control silicate weathering rates or mechanisms has been little studied. Here, we use lithium (Li) isotope measurements in bimonthly sampled drip-waters from two caves in the Yorkshire Dales (U.K.) to assess the response of silicate weathering processes to changes in temperature and hydrology over seasonal timescales. While the caves are contained in limestone bedrock, the drip-water Li isotope signal predominantl…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesBedrockGeochemistryWeathering010502 geochemistry & geophysics01 natural sciencesSilicateCarbon cyclechemistry.chemical_compoundIsotope fractionationchemistry13. Climate actionGeochemistry and PetrologyEnhanced weatheringPrecipitationClimate state0105 earth and related environmental sciencesGeochimica et Cosmochimica Acta
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Improved discrimination of subglacial and periglacial erosion using10Be concentration measurements in subglacial and supraglacial sediment load of th…

2015

Deciphering the complex interplays between climate, uplift and erosion is not straightforward and estimating present-day erosion rates can provide useful insights. Glaciers are thought to be powerful erosional agents, but most published ‘glacial’ erosion rates combine periglacial, subglacial and proglacial erosion processes. Within a glaciated catchment, sediments found in subglacial streams originate either from glacial erosion of substratum or from the rock walls above the glacier that contribute to the supraglacial load. Terrestrial cosmogenic nuclides (TCN) are produced by interactions between cosmic ray particles and element targets at the surface of the Earth, but their concentration …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesBedrockGeography Planning and DevelopmentSedimentGlacier15. Life on land010502 geochemistry & geophysics01 natural sciencesSubglacial stream13. Climate actionEarth and Planetary Sciences (miscellaneous)Subglacial eruptionErosionGlacial periodCosmogenic nuclideGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesEarth Surface Processes and Landforms
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The role of hydrochlorofluorocarbon densifiers in the formation of clathrate hydrates in deep boreholes and subglacial environments

2007

AbstractClear evidence for the formation of mixed clathrate hydrates of air and hydrochlorofluorocarbon densifier (known as HCFC-141b, sometimes also called R-141b) is found by means of synchrotron X-ray diffraction and Raman spectroscopy on a sample recovered from the bottom of the EPICA Dronning Maud Land deep borehole in Antarctica. Subglacial water (SGW) appears to have reacted with the drilling liquid to build a large lump of clathrate hydrate. The hydrate growth may well have been accelerated by the stirring of the SGW–densifier mixture during drilling. Moreover, dissolved air in the SGW appears to have participated in the formation of mixed hydrates of air and HCFC-141b as evidenced …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesClathrate hydrateBoreholeDrillingMineralogy02 engineering and technology021001 nanoscience & nanotechnology01 natural sciencesSink (geography)symbols.namesake13. Climate actionsymbols0210 nano-technologyPetrologyRaman spectroscopyHydrateGeology0105 earth and related environmental sciencesEarth-Surface ProcessesAnnals of Glaciology
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Widespread persistent polar stratospheric ice clouds in the Arctic

2016

Abstract. Despite a general decline in ozone depleting substances in the stratosphere due to the multi-national commitment to substantially reduce the emissions of their precursors, the magnitude of Arctic polar ozone loss has not decreased in recent years. Thus new observations at cold conditions can help to enhance our knowledge of polar stratospheric cloud (PSC) formation and life cycle which is of relevance for Arctic ozone loss. In the unique winter 2015/16, cold and persistent areas with temperatures below the ice frost point Tice developed in the Arctic stratosphere, caused by reduced perturbations of the polar vortex through planetary waves. Due to these extreme conditions, unpreced…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesClimate changeAtmospheric sciences01 natural sciencesArctic ice packArctic geoengineeringArcticPolar vortexClimatologyFrostIce nucleusEnvironmental scienceStratosphere0105 earth and related environmental sciences
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Quantifying the impact of mechanical layering and underthrusting on the dynamics of the modern India-Asia collisional system with 3-D numerical models

2014

The impact of mechanical layering and the strength of the Indian lower crust on the dynamics of the modern India-Asia collisional system are studied using 3-D thermomechanical modeling. The model includes an Indian oceanic domain, Indian continental domain, and an Asian continental domain. Each domain consists of four layers: upper/lower crust, and upper/lower lithospheric mantle. The Tarim and Sichuan Basins are modeled as effectively rigid blocks and the Quetta-Chaman and Sagaing strike-slip faults as vertical weak zones. The geometry, densities, and viscosities are constrained by geophysical data sets (CRUST2.0, gravity, and seismology). Both static (no horizontal movement of model bound…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesContinental collisionCrustGeophysicsFault (geology)010502 geochemistry & geophysicsOverburden pressure01 natural sciencesOverpressureTectonicsGeophysics13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyLithosphereEarth and Planetary Sciences (miscellaneous)LayeringGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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