Search results for "Cir"

showing 10 items of 6404 documents

Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption

2021

Climatic warming from the last glacial maximum to the current interglacial period was punctuated by a similar to 1300 years long cold period, commonly referred to as the Younger Dryas (YD). Several hypotheses have been proposed for the mechanism triggering the abrupt inception of the YD, including freshwater forcing, an extra-terrestrial impact, and aerosols from volcanic eruptions. Here, we use synchronised sulphate and sulphur records from both Greenland and Antarctic ice cores to reconstruct volcanic forcing between 13,200-12,800 a BPGICC05 (years before 1950 CE on the Greenland Ice Core Chronology 2005; GICC05). This continuous reconstruction of stratospheric sulphur injections highligh…

010506 paleontologyArcheologyYounger Dryas010504 meteorology & atmospheric sciences530 PhysicsCIRCULATIONIce cores; Laacher See eruption; Sulphate; Volcanic radiative forcing; Younger DryasSULFURForcing (mathematics)01 natural sciencesVolcanic radiative forcingANTARCTIC ICE-CORESOCEANIce coreCHRONOLOGYYounger Dryas550 Earth sciences & geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeologyLast Glacial MaximumRECORDWAIS DIVIDESulphateRadiative forcingGREENLANDLaacher See eruptionVolcano13. Climate actionIce coresClimatologySYNCHRONIZATIONInterglacialClimate modelSULFATEGeologyQuaternary Science Reviews
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Causes and consequences of past and projected Scandinavian summer temperatures, 500-2100 AD

2011

Tree rings dominate millennium-long temperature reconstructions and many records originate from Scandinavia, an area for which the relative roles of external forcing and internal variation on climatic changes are, however, not yet fully understood. Here we compile 1,179 series of maximum latewood density measurements from 25 conifer sites in northern Scandinavia, establish a suite of 36 subset chronologies, and analyse their climate signal. A new reconstruction for the 1483–2006 period correlates at 0.80 with June–August temperatures back to 1860. Summer cooling during the early 17th century and peak warming in the 1930s translate into a decadal amplitude of 2.9°C, which agrees with existin…

010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciencesAtmospheric circulationClimate ChangeClimate changelcsh:MedicineForcing (mathematics)Scandinavian and Nordic Countries01 natural sciencesAtmospheric CirculationBiospherePaleoclimatologyEnvironmental GeographyAtmospheric DynamicsPaleoclimatologylcsh:Science0105 earth and related environmental sciencesClimatologySeries (stratigraphy)MultidisciplinaryGeographyAtmospherelcsh:RTemperature/dk/atira/pure/core/subjects/geography15. Life on landSea surface temperatureGeographyPhysical Geography13. Climate actionClimate RecordClimatologyPeriod (geology)Earth SciencesClimate modellcsh:QSeasonsEnvironmental SciencesResearch ArticleClimate ModelingPLOS One
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Hydrothermalism in the Tyrrhenian Sea: Inorganic and microbial sulfur cycling as revealed by geochemical and multiple sulfur isotope data

2011

15 pages; International audience; The Palinuro volcanic complex and the Panarea hydrothermal field, both located in the Tyrrhenian Sea (Italy), are associated with island arc magmatism and characterized by polymetallic sulfide mineralization. Dissolved sulfide concentrations, pH, and Eh measured in porewaters at both sites reveal a variable hydrothermal influence on porewater chemistry. Multiple sulfur isotopic measurements for disseminated sulfides (CRS: chromium reducible sulfur) extracted from sediments at Palinuro yielded a broad range in δ34S range between −29.8 and +10.2‰ and Δ33S values between+0.015 and+0.134‰. In contrast, sediments at Panarea exhibit a much smaller range in δ34SCR…

010506 paleontologySulfide[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrychemistry.chemical_elementDisproportionationengineering.material010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationchemistry.chemical_compoundδ34S[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMassive sulfide complexGeochemistry and PetrologyHydrothermalism14. Life underwaterMultiple sulfur isotopesSulfate0105 earth and related environmental scienceschemistry.chemical_classificationgeographygeography.geographical_feature_categorySulfur cyclingGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySulfur[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryVolcano13. Climate actionengineeringPyriteGeologyChemical Geology
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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
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Modelling circulation in an ice-covered lake

2010

In deep ice-covered lakes with temperatures below 4 °C the heat flux from the bottom sediment results in a horizontal density gradient and a consequent flow along the bottom slope. Measurements in Lake Paajarvi, Finland, show a stable temperature field where a heat gain through the bottom and a heat loss through the ice nearly balance each other. The circulation is thermal with low velocities (less than 1.5 cm s -1 ). We used the 3D hydrodynamic Princeton Ocean Model as a tool to simulate the water circulation and the temperature distribution under the ice. The model forcing was based on field temperature measurements. The model simulations suggest that in midwinter the velocity field of th…

0106 biological sciences010504 meteorology & atmospheric sciences010604 marine biology & hydrobiologyFlow (psychology)lcsh:QE1-996.5SedimentForcing (mathematics)Atmospheric sciences01 natural sciencesPrinceton Ocean ModelCurrent (stream)lcsh:GeologyCirculation (fluid dynamics)Heat fluxhydrodynamic modelling13. Climate actionAnticycloneClimatologyGeneral Earth and Planetary Sciences14. Life underwaterLake Pääjärvi.Geologycurrents0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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Summarizing the state of the terrestrial biosphere in few dimensions

2020

Abstract. In times of global change, we must closely monitor the state of the planet in order to understand the full complexity of these changes. In fact, each of the Earth's subsystems – i.e., the biosphere, atmosphere, hydrosphere, and cryosphere – can be analyzed from a multitude of data streams. However, since it is very hard to jointly interpret multiple monitoring data streams in parallel, one often aims for some summarizing indicator. Climate indices, for example, summarize the state of atmospheric circulation in a region. Although such approaches are also used in other fields of science, they are rarely used to describe land surface dynamics. Here, we propose a robust method to crea…

0106 biological sciences010504 meteorology & atmospheric sciencesAtmospheric circulationlcsh:Life0207 environmental engineering02 engineering and technology010603 evolutionary biology01 natural scienceslcsh:QH540-549.5Cryosphere020701 environmental engineeringEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesData stream mininglcsh:QE1-996.5BiosphereGlobal change15. Life on landAlbedolcsh:Geologylcsh:QH501-531Arctic13. Climate actionClimatologyEnvironmental sciencelcsh:EcologyHydrosphere
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Deciphering carbon sources of mussel shell carbonate under experimental ocean acidification and warming.

2018

Abstract Ocean acidification and warming is widely reported to affect the ability of marine bivalves to calcify, but little is known about the underlying mechanisms. In particular, the response of their calcifying fluid carbonate chemistry to changing seawater carbonate chemistry remains poorly understood. The present study deciphers sources of the dissolved inorganic carbon (DIC) in the calcifying fluid of the blue mussel (Mytilus edulis) reared at two pH (8.1 and 7.7) and temperature (16 and 22 °C) levels for five weeks. Stable carbon isotopic ratios of seawater DIC, mussel soft tissues and shells were measured to determine the relative contribution of seawater DIC and metabolically gener…

0106 biological sciences010504 meteorology & atmospheric sciencesMytilus edulisOceans and SeasCarbonateschemistry.chemical_elementAquatic ScienceOceanography01 natural scienceschemistry.chemical_compoundCalcification Physiologichemic and lymphatic diseasesDissolved organic carbonAnimalsSeawater0105 earth and related environmental sciencesCarbon IsotopesChemistry010604 marine biology & hydrobiologyOcean acidificationGeneral MedicineMusselHydrogen-Ion ConcentrationPollutionIsotopes of carbonEnvironmental chemistryCarbonateSeawaterCarbonBlue musselcirculatory and respiratory physiologyMarine environmental research
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Warming in the Agulhas Current system since the 1980's

2009

International audience; Since the 1980's, the sea surface temperature of the Agulhas Current system has increased significantly. The warming is due to an augmentation of its transport in response to an increase in wind stress curl in the South Indian Ocean at relevant latitudes. This causes an increase in the fluxes of salt and heat into the Atlantic Ocean and in the transfer of energy from the ocean to the atmosphere. Therefore, the changes we are witnessing in the region could have far reaching consequences on top of the regional impacts on ecosystem and climate. The increase in wind stress curl is consistent with a poleward shift of westerly wind in the Southern Hemisphere reported by ot…

0106 biological sciences010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010604 marine biology & hydrobiologyClimate changeAgulhas current01 natural sciencesLatitudeAtmosphereSea surface temperature[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyGeneral Earth and Planetary SciencesThermohaline circulationEcosystem[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologySouthern HemisphereGeology0105 earth and related environmental sciences
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Diverse growth trends and climate responses across Eurasia’s boreal forest

2016

The area covered by boreal forests accounts for similar to 16% of the global and 22% of the Northern Hemisphere landmass. Changes in the productivity and functioning of this circumpolar biome not o ...

0106 biological sciences010504 meteorology & atmospheric sciencesbiologyRenewable Energy Sustainability and the EnvironmentEcologyGlobal warmingBiomeTaigaPublic Health Environmental and Occupational HealthScots pineNorthern HemisphereCircumpolar star500 Sciencebiology.organism_classification010603 evolutionary biology01 natural sciencesLatitudeGeographyProductivity (ecology)Climatology550 Earth sciences & geology550 Earth sciences & geology0105 earth and related environmental sciencesGeneral Environmental ScienceEnvironmental Research Letters
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Melatonin in the seasonal response of the aphid Acyrthosiphon pisum.

2018

Aphids display life cycles largely determined by the photoperiod. During the warm long-day seasons, most aphid species reproduce by viviparous parthenogenesis. The shortening of the photoperiod in autumn induces a switch to sexual reproduction. Males and sexual females mate to produce overwintering resistant eggs. In addition to this full life cycle (holocycle), there are anholocyclic lineages that do not respond to changes in photoperiod and reproduce continuously by parthenogenesis. The molecular or hormonal events that trigger the seasonal response (i.e., induction of the sexual phenotypes) are still unknown. Although circadian synthesis of melatonin is known to play a key role in verteb…

0106 biological sciences0301 basic medicineCentral Nervous SystemMaleendocrine systemAANATPhotoperiodCircadian clockZoology01 natural sciencesArylalkylamine N-AcetyltransferaseGeneral Biochemistry Genetics and Molecular BiologyMelatonin03 medical and health sciencesmedicineAnimalsCircadian rhythmEcology Evolution Behavior and SystematicsMelatoninphotoperiodismAphidbiologyfood and beveragesbiology.organism_classificationAcyrthosiphon pisumSexual reproduction010602 entomology030104 developmental biologyInsect ScienceAphidsFemaleSeasonsAgronomy and Crop Sciencehormones hormone substitutes and hormone antagonistsmedicine.drugInsect scienceReferences
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