Search results for "Ocean current"

showing 10 items of 21 documents

Annually resolved δ13Cshell chronologies of long-lived bivalve mollusks (Arctica islandica) reveal oceanic carbon dynamics in the temperate North Atl…

2011

Abstract The ability of the ocean to absorb carbon dioxide is likely to be adversely affected by recent climate change. However, relatively little is known about the spatiotemporal variability in the oceanic carbon cycle due to the lack of long-term, high-resolution dissolved inorganic carbon isotope ( δ 13 C DIC ) data, especially for the temperate North Atlantic, which is the major oceanic sink for anthropogenic CO 2 . Here, we report shell carbon isotope values ( δ 13 C shell ), a potential proxy for δ 13 C DIC , of old-grown specimens of the long-lived bivalve mollusk, Arctica islandica . This paper presents the first absolutely dated, annually resolved δ 13 C shell record from surface …

010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsOceanography01 natural sciencesCarbon cycleSuess effectSclerochronologySclerochronology14. Life underwaterArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesPolar frontStable carbon isotope ratiobiologyOcean currentOceanic Suess effectPaleontologybiology.organism_classificationDissolved inorganic carbonOceanographyCarbon dioxide13. Climate actionIsotopes of carbon[SDE]Environmental SciencesOceanic carbon cycleGeology
researchProduct

Record-breaking warming and extreme drought in the Amazon rainforest during the course of El Niño 2015–2016

2016

AbstractThe El Niño-Southern Oscillation (ENSO) is the main driver of interannual climate extremes in Amazonia and other tropical regions. The current 2015/2016 EN event was expected to be as strong as the EN of the century in 1997/98, with extreme heat and drought over most of Amazonian rainforests. Here we show that this protracted EN event, combined with the regional warming trend, was associated with unprecedented warming and a larger extent of extreme drought in Amazonia compared to the earlier strong EN events in 1982/83 and 1997/98. Typical EN-like drought conditions were observed only in eastern Amazonia, whilst in western Amazonia there was an unusual wetting. We attribute this wet…

010504 meteorology & atmospheric sciencesAmazonian0208 environmental biotechnologyClimate change02 engineering and technologyRainforest01 natural sciencesArticle//purl.org/pe-repo/ocde/ford#1.05.00 [http]Environmental impactEcosystem0105 earth and related environmental sciences//purl.org/pe-repo/ocde/ford#1.05.09 [http]MultidisciplinaryAmazon rainforestOcean currentTropics020801 environmental engineeringGeography//purl.org/pe-repo/ocde/ford#1.05.10 [http][SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyAbrupt climate changeENSOClimate-change impacts
researchProduct

HF radar for wind waves measurements in the Malta-Sicily Channel

2018

Abstract The CALYPSO HF radar network is a permanent and fully operational observing system currently composed of four CODAR SeaSonde stations. The system is providing real-time hourly maps of sea surface currents and waves data in the Malta-Sicily Channel. The present work aims to compare significant wave height measurements by HF Radar to wave data from numerical models and satellite altimeter. This is the first time that this set of wave data are analysed since the four HF radars were installed between 2012 and 2015. Results suggest that CODAR HF Radar wave data are a reliable source of wave information even in the case of extreme events, providing an avenue to improve and complete the o…

010504 meteorology & atmospheric sciencesHF radar010505 oceanographyWave modelApplied MathematicsInstrumentationOcean currentMalta-Sicily ChannelWave parameterCondensed Matter Physics01 natural sciencesSatellite altimeterlaw.inventionWave modellawWind waveSatellite altimeterElectrical and Electronic EngineeringRadarSignificant wave heightInstrumentationGeology0105 earth and related environmental sciencesRemote sensingCommunication channelMeasurement
researchProduct

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
researchProduct

Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the co…

2013

11 pages; International audience; The Neodymium(Nd) isotope composition of fish remains has beenwidely used to track past changes in oceanic circulation. Although the number of published Nd isotope data for the Cretaceous has markedly increased in the last years, no consensus has been reached on the structure of the oceanic circulation and its evolution during the Late Cretaceous. Yet this period is characterised bymajor geodynamical and climatic changes andmarked by the disappearance of global oceanic anoxic events inwhich changes in oceanic circulation modesmay have played a significant role. In this study we present the first record of Nd isotopic composition of fish remains from contine…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousIsotopic signaturePaleontologyContinental marginJapanGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryoceanic circulation14. Life underwater[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesRadiogenic nuclide[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySeafloor spreadingCretaceous[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPeriod (geology)Seawaterneodymium isotopesGeology
researchProduct

Detailed record of the mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion in two hemipelagic sections (France and Switzerland): A plate …

2007

14 pages; International audience; The Oxfordian (Late Jurassic) was a time of widespread change in Jurassic marine (carbonate) sedimentation patterns. A marked positive excursion in δ13C is dated as Middle Oxfordian in age. In this study we investigate if changes in carbonate sedimentation coincided with altered carbon cycling and climate. We use C-isotope records as a proxy for the evolution of the carbon cycle and compare δ13C-trends with the evolution of sedimentation in a segment of the opening Tethys seaway. One of the studied sections is located in the Subalpine basin of France (Trescléoux and Oze), the other in the Swiss Jura mountains (Liesberg). Carbon-isotope stratigraphy of carbo…

010506 paleontologyClimate[SDE.MCG]Environmental Sciences/Global ChangesCarbon stable isotopes010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeCarbon cycleOxfordianchemistry.chemical_compoundPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterTethysEcology Evolution Behavior and SystematicsSea level[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbon[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGlobal warmingExcursionPaleontologyCarbon cycle[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryPlate tectonics[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryPalaeo-oceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
researchProduct

Regional coherency of boreal forest growth defines Arctic driftwood provenancing

2016

Arctic driftwood represents a unique proxy archive at the interface of marine and terrestrial environments. Combined wood anatomical and dendrochronological analyses have been used to detect the origin of driftwood and may allow past timber floating activities, as well as past sea ice and ocean current dynamics to be reconstructed. However, the success of driftwood provenancing studies depends on the length, number, and quality of circumpolar boreal reference chronologies. Here, we introduce a Eurasian-wide high-latitude network of 286 ring width chronologies from the International Tree Ring Data Bank (ITRDB) and 160 additional sites comprising the three main boreal conifers Pinus, Larix, a…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEcologybiologyEcologyTaigaOcean currentPlant ScienceCircumpolar starDriftwoodbiology.organism_classification01 natural sciencesBorealArcticSea icePhysical geographyLarchGeology0105 earth and related environmental sciencesDendrochronologia
researchProduct

Persistent link between Caribbean precipitation and Atlantic Ocean circulation during the Last Glacial revealed by a speleothem record from Puerto Ri…

2020

The sensitivity of tropical Atlantic precipitation patterns to the mean position of the Intertropical Convergence Zone (ITCZ) at different time scales is well‐known. However, recent research suggests a more complex behavior of the northern hemispheric tropical rain belt related to the ITCZ in the western tropical Atlantic. Here we present a precisely dated speleothem multi‐proxy record from a well‐monitored cave in Puerto Rico, covering the period between 46.2 and 15.3 ka. The stable isotope and trace element records document a pronounced response of regional rainfall to abrupt climatic excursions in the North Atlantic across the Last Glacial such as Heinrich stadials and Dansgaard/Oeschger…

551.7Atmospheric Sciencegeographygeography.geographical_feature_categoryStable isotope ratio550.28Last GlacialspeleothemsOcean currentPaleontologySpeleothemstable isotopesprecipitation reconstructionOceanographyOceanographyHeinrich stadialsPrecipitationGlacial periodGeologyDansgaard/Oeschger cycles
researchProduct

Freshening of the Alaska Coastal Current recorded by coralline algal Ba/Ca ratios

2011

Arctic Ocean freshening can exert a controlling influence on global climate, triggering strong feedbacks on ocean‐atmospheric processes and affecting the global cycling of the world’s oceans. Glacier‐fed ocean currents such as the Alaska Coastal Current are important sources of freshwater for the Bering Sea shelf, and may also influence the Arctic Ocean freshwater budget. Instrumental data indicate a multiyear freshening episode of the Alaska Coastal Current in the early 21st century. It is uncertain whether this freshening is part of natural multidecadal climate variability or a unique feature of anthropogenically induced warming. In order to answer this, a better understanding of past var…

Atmospheric Science010504 meteorology & atmospheric sciencesTemperature salinity diagramsSoil ScienceAquatic Science010502 geochemistry & geophysicsOceanography01 natural sciencesGeochemistry and PetrologySclerochronologyEarth and Planetary Sciences (miscellaneous)14. Life underwaterGlacial periodPrecipitation0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyEcologybiologyOcean currentPaleontologyCoralline algaeForestrybiology.organism_classificationGeophysicsOceanographyArctic13. Climate actionSpace and Planetary ScienceGeologyPacific decadal oscillationJournal of Geophysical Research
researchProduct

Long-term changes of precipitation in Latvia

2010

This study investigated long-term variability and trends in Latvia's annual, seasonal, monthly and daily precipitation using data from 10 meteorological stations for the period 1925–2006 and from station Riga University for the period 1850–2006. The obtained results indicate that during the 20th century a significant increase in precipitation has occurred in the cold season while the warm period showed a decreasing tendency. The annual precipitation totals showed a slight decrease, at half of the studied stations, due to opposite tendencies in cold season and warm season. The long-term trend in the annual precipitation in Riga (from 1850) was positive with large interannual and interdecadal…

Hydrology (agriculture)North Atlantic oscillationClimatologyOcean currentEnvironmental scienceClimate changePrecipitationCold periodWinter seasonWarm seasonWater Science and TechnologyHydrology Research
researchProduct