Search results for "Clima"

showing 10 items of 6069 documents

Impact of climate, soil properties and grassland cover on soil water repellency

2021

Abstract Numerous soil water repellency (SWR) studies have investigated the possible causes of this temporal phenomenon, yet there remains a lack of knowledge on the order of importance of the main driving forces of SWR in the context of changing environmental conditions under grassland ecosystems. To study the separate and combined effects of soil texture, climate, and grassland cover type on inducing or altering SWR, four sites from different climatic and soil regions were selected: Ciavolo (CI, IT), Csolyospalos (CSP, HU), Pwllpeiran (PW, UK), Sekule (SE, SK). The investigated parameters were the extent (determined by repellency indices RI, RIc and RIm) and persistence (determined by wat…

geographygeography.geographical_feature_categoryHydrophobic soilSoil textureSorptivitySoil ScienceSoil properties Soil water repellency Grass Length of dry periods Climate factors04 agricultural and veterinary sciences010501 environmental sciences01 natural sciencesSink (geography)GrasslandAgronomyHydraulic conductivitySoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil fertility0105 earth and related environmental sciences
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Tunable diode laser measurements of hydrothermal/volcanic CO<sub>2</sub> and implications for the global CO<sub&am…

2014

Abstract. Quantifying the CO2 flux sustained by low-temperature fumarolic fields in hydrothermal/volcanic environments has remained a challenge, to date. Here, we explored the potential of a commercial infrared tunable laser unit for quantifying such fumarolic volcanic/hydrothermal CO2 fluxes. Our field tests were conducted between April 2013 and March 2014 at Nea Kameni (Santorini, Greece), Hekla and Krýsuvík (Iceland) and Vulcano (Aeolian Islands, Italy). At these sites, the tunable laser was used to measure the path-integrated CO2 mixing ratios along cross sections of the fumaroles' atmospheric plumes. By using a tomographic post-processing routine, we then obtained, for each manifestati…

geographygeography.geographical_feature_categoryInfraredStratigraphyPaleontologySoil ScienceMineralogyGeologyGeophysicsHydrothermal circulationFumaroleGeophysicsVolcanoImpact crater13. Climate actionGeochemistry and PetrologyContour lineAeolian processesTunable laserGeologyEarth-Surface ProcessesSolid Earth
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Minor and trace elements in olivines as probes into early igneous and mantle melting processes

2013

Abstract The trace element composition of olivine is a rapidly growing research area that has several applications of great potential. Mantle olivines can be distinguished from volcanic olivines by lower concentrations of Ca (

geographygeography.geographical_feature_categoryOlivine010504 meteorology & atmospheric sciencesContinental crustMantle metasomatismGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Igneous rockGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyOceanic crustEarth and Planetary Sciences (miscellaneous)Trace element compositionengineeringGeology0105 earth and related environmental sciences
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Changes in vegetation spring dates in the second half of the twentieth century

2011

This study aims at estimating trends in spring phenology from vegetation index and air temperature at 2 m height. To this end, we have developed a methodology to infer spring phenological dates from Global Inventory Modeling and Mapping Studies GIMMS Normalized Difference Vegetation Index NDVI time-series, which are then extrapolated to the period 1948–2006 with the help of Reanalysis data, using its 2 m height air temperature parameter. First, yearly NDVI is fitted to a double-logistic function for the whole extent of the GIMMS database 1981–2003. This fitting procedure allows us to describe, on a yearly basis, the NDVI evolution for each pixel through the estimation of six parameters whic…

geographygeography.geographical_feature_categoryPhenologyAir temperatureClimatologySpring (hydrology)Temperate climateRange (statistics)General Earth and Planetary SciencesClimate changeEnvironmental scienceVegetationNormalized Difference Vegetation IndexInternational Journal of Remote Sensing
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Palaeogeographical relationships between Alpine and Jura glaciers during the two last Pleistocene glaciations

1992

Abstract Two main moraine complexes are usually defined in the northwestern Alpine piedmont: the External Moraine Complex (EMC) dated to the penultimate glaciation (“Riss” sensu lato) and the Internal Moraine Complex (IMC) dated to the last glaciation (“Wurm”). Until recently the prevalent concept was that these two complexes had been built by glaciers originating in the central Alpine zone. This paper presents a new palaeogeographical diagram, based on mapping and petrographical studies of these two moraine complexes, and especially on the relationships between Alpine and Jura tills. We reach the following conclusions. 1. (1) The Jura glaciers were independent of the Alpine glaciers during…

geographygeography.geographical_feature_categoryPleistocenePaleontologyAlpine climateGlacierOceanographyPaleontologyMoraineGlacial periodGeomorphologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Recent Change—Terrestrial Cryosphere

2015

This chapter compiles and assesses information on recent and current change within the terrestrial cryosphere of the Baltic Sea drainage basin. Findings are based on long-term observations. Snow cover extent (SCE), duration and amount have shown a widespread decrease although there is large interannual and regional variation. Few data are available on changes in snow structural properties. There is no evidence for a recent change in the frequency or severity of snow-related extreme events. There has been a decrease in glacier coverage in Sweden and glacier ice thickness in inland Scandinavia. The European permafrost is warming, and there has been a northward retreat of the southern boundary…

geographygeography.geographical_feature_categoryRegional variationClimatologyDrainage basinCryosphereGlacierPhysical geographyPermafrostSnowSnow coverIce thickness
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Ash resuspension related to the 2011–2012 Cordón Caulle eruption, Chile, in a rural community of Patagonia, Argentina

2017

Abstract The 2011–2012 Cordon Caulle eruption emitted about 1 km3 of rhyodacitic tephra. Dominant westerly winds in the region caused most of the primary tephra to deposit in neighboring Argentina. In addition to the impact of widespread dispersal and fallout of primary tephra during the eruption, Argentina was also significantly affected by remobilization of the primary ash even several years after the climactic phase of the eruption. In this mixed methods study, we combine aspects of natural and social sciences to characterize the ash resuspension events associated with the 2011–2012 Cordon Caulle deposits and assess the impacts on the Argentinian farming community of Ingeniero Jacobacci …

geographygeography.geographical_feature_categorySeasonal distribution010504 meteorology & atmospheric sciencesRural communitySteppeWesterlies010502 geochemistry & geophysics01 natural sciencesDeposition (geology)GeophysicsVolcano13. Climate actionGeochemistry and Petrologyddc:550Biological dispersalPhysical geographyTephraGeomorphologyGeology0105 earth and related environmental sciences
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Trace elements mobility in soils from the active hydrothermal area of Nisyros (Greece)

2014

Nisyros Island, Greece, is a stratovolcano known for its intense hydrothermal activity. On June 2013, during a multidisciplinary field campaign, soil samples were collected in the caldera area to determinate the main mineralogical paragenesis and to investigate the distribution of trace elements concentrations and the possible relationship to the contribution of deep originated fluids. Soil samples were analysed with XRD and for the chemical composition of their leachable (deionized water) and near total (microwave digestion) fraction both for major and trace elements. All data were compared to a local background soil. The results allow to divide the samples in 2 groups: Lakki Plain and Ste…

geographygeography.geographical_feature_categorySoil testvolatile elementslcsh:QC801-809Trace elementtrace elements Greece hydrothermal emissions biomonitoringMineralogyvolcanoeslcsh:QC851-999Hydrothermal circulationSettore GEO/08 - Geochimica E Vulcanologialcsh:Geophysics. Cosmic physicsGeophysicsVolcanoSoil waterCalderalcsh:Meteorology. ClimatologyVolatilesChemical compositionfumarolic gasesGeology
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A continuous high-resolution dust record for the reconstruction of wind systems in central Europe (Eifel, Western Germany) over the past 133 ka

2009

[1] The last glacial cycle in Central Europe is dominated by processes of aeolian dust transport and accumulation. These dust deposits are preserved in soils and lake sediments and provide detailed information about the climate variability during cold and dry periods. Especially the transitions from warm into cold periods are characterized by turbulent climate conditions. The main problems of terrestrial paleoclimate reconstructions are the completeness of the core material and a sampling resolution. To detect single dust storms we use a particle detection method, which allows high resolution, sub-annual analyses of sediment structures in undisturbed samples. The ELSA (Eifel Laminated Sedim…

geographygeography.geographical_feature_categoryStack (geology)SedimentStormGeophysicsOceanographyDust stormPaleoclimatologyPeriod (geology)General Earth and Planetary SciencesAeolian processesGlacial periodPhysical geographyGeologyGeophysical Research Letters
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Control of Seasonality and Interannual to Centennial Climate Variability in the Caribbean During the Holocene—Combining Coral Records, Stalagmite Rec…

2014

This study aimed at quantifying the amplitudes of seasonality and interannual to centennial climate variability in the Caribbean region throughout the Holocene, by using marine (shallow-water corals) and terrestrial (speleothems) climate archives, and climate model simulations (COSMOS). Sea-surface temperature (SST) variability on interdecadal to multidecadal timescales was more pronounced during the mid-Holocene compared to the late Holocene. The amplitude of the SST annual cycle was within the present-day range throughout most of the last 6,000 years. Exceptions include slightly increased SST seasonality at 6,200 years ago, which can be attributed mainly to insolation forcing on orbital t…

geographygeography.geographical_feature_categoryStalagmiteTropical AtlanticSeasonalityAnnual cyclemedicine.diseaseOceanographyClimatologyAtlantic multidecadal oscillationPaleoclimatologymedicineClimate modelHolocene
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