Search results for "Arm"

showing 10 items of 19046 documents

Simulation of nitrous oxide emissions from wheat-cropped soils using CERES

2005

Estimation of nitrous oxide (N2O) emissions from arable soils, in relation to crop fertilization, is essential to devise strategies to mitigate the impact of agriculture on global warming. This paper presents the development and test of a N2O model resulting from the linkage of a dynamic soil-crop simulation model (CERES) with two sub-models of N2O production and reduction in soils. These sub-models (NOE and NGAS) account for both the nitrification and denitrification pathways. The resulting models (CERES–NOE and CERES–NGAS) were tested against experimental data collected on three contrasting wheat-cropped soils representative of the Beauce agricultural region in France. Although the input …

010504 meteorology & atmospheric sciences[SDV]Life Sciences [q-bio]Soil ScienceSoil scienceengineering.materialCERES01 natural sciencesModellingchemistry.chemical_compound[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentAGRONOMIE[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences2. Zero hungerNitrous oxideGlobal warming04 agricultural and veterinary sciencesNitrous oxideCalcisol15. Life on landSoil type[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentGreenhouse gaseschemistry13. Climate actionGreenhouse gasFertilizationSoil water[SDE]Environmental Sciences040103 agronomy & agricultureengineering0401 agriculture forestry and fisheriesEnvironmental scienceFertilizerArable landAgronomy and Crop Science
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Warm season precipitation signal in δ 2 H values of wood lignin methoxyl groups from high elevation larch trees in Switzerland

2017

RATIONALE In this study, we tested stable hydrogen isotope ratios of wood lignin methoxyl groups (δ 2Hmethoxyl values) as a palaeoclimate proxy in dendrochronology. This is a quite new method in the field of dendrochronology and the sample preparation is much simpler than the methods used before to measure δ2H values from wood. METHODS We measured δ 2Hmethoxyl values in high elevation larch trees (Larix decidua Mill.) from Simplon Valley (southern Switzerland). Thirty-seven larch trees were sampled and five individuals analysed for their δ 2Hmethoxyl values at annual (1971-2009) and pentadal resolution (1746-2009). The δ 2Hmethoxyl values were measured as CH3I released upon treatment of the…

010504 meteorology & atmospheric sciencesbiologyHydrogen isotope010401 analytical chemistryOrganic ChemistryXylemPositive correlationbiology.organism_classificationWarm season01 natural sciences0104 chemical sciencesAnalytical Chemistrychemistry.chemical_compoundAnimal sciencechemistryHigh elevationDendrochronologyLigninLarchSpectroscopy0105 earth and related environmental sciencesRapid Communications in Mass Spectrometry
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Worlds apart, drawn together: Bears, penguins and biodiversity in climate change cartoons

2021

This study shows how cartoonists use iconic and stereotypical animals in their works to reflect society’s knowledge about the effects of climate change. Studying 1022 climate change cartoons including depictions of animals, we noticed that there is very little biodiversity depicted in cartoons. Cartoonists generally avoid using animals indigenous to their own countries; this point is especially true regarding the low presence of insects and other invertebrates. This text also encourages cartoonists to adhere to some recommendations to improve climate change communication. These guidelines are (1) using indigenous wildlife, (2) depicting invertebrate wildlife, (3) improving their knowledge …

010504 meteorology & atmospheric sciencesbusiness.industryClimate ChangeCommunication05 social sciencesBiodiversityWildlifeDistribution (economics)Climate change050801 communication & media studiesEnvironmental ethicsBiodiversity01 natural sciencesIndigenous0508 media and communicationsGeographyArts and Humanities (miscellaneous)Effects of global warmingDevelopmental and Educational PsychologyAnimalsbusiness0105 earth and related environmental sciencesPublic Understanding of Science
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Predicted temperature-increase-induced global health burden and its regional variability

2019

An increase in the global health burden of temperature was projected for 459 locations in 28 countries worldwide under four representative concentration pathway scenarios until 2099. We determined that the amount of temperature increase for each 100 ppm increase in global CO2 concentrations is nearly constant, regardless of climate scenarios. The overall average temperature increase during 2010–2099 is largest in Canada (1.16 °C/100 ppm) and Finland (1.14 °C/100 ppm), while it is smallest in Ireland (0.62 °C/100 ppm) and Argentina (0.63 °C/100 ppm). In addition, for each 1 °C temperature increase, the amount of excess mortality is increased largely in tropical countries such as Vietnam (10.…

010504 meteorology & atmospheric sciencesvulnerabilityVulnerabilityHot temperatureprojection010501 environmental sciencesGlobal Health01 natural sciencesGlobal WarmingRegional variationHot TemperatureAnimal scienceElderly populationPhysical Sciences and MathematicsGlobal healthHumansClimate changeProjectionMortalitylcsh:Environmental sciences0105 earth and related environmental sciencesGeneral Environmental Sciencelcsh:GE1-350Excess mortalityTemperatureregional variationPublic Health Global Health Social Medicine and EpidemiologyAtmospheric temperature rangemortality3. Good healthFolkhälsovetenskap global hälsa socialmedicin och epidemiologiclimate changeRegional variationAvaliação do Impacte em Saúde13. Climate actionEnvironmental scienceDeterminantes da Saúde e da DoençaForecasting
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A global palaeoclimatic reconstruction for the Valanginian based on clay mineralogical and geochemical data

2020

International audience; High-resolution clay mineral and δ18Ocarb analyses have been performed on three sections of Valanginian age (Early Cretaceous), from northwestern (~20–30°N) and southern (~53°S) Tethyan realms. The data have been integrated in a large set of published mineralogical (clays), and geochemical (δ18Ocarb, δ18Obivalve, δ18Olenticulina, δ18Obelemnite, and TEX86) data from 17 sections, situated between ~45°N and ~53°S. Based on this data set, we provide new insights into Valanginian climate conditions from a wide range of palaeolatitudes. We highlight climate trends within specific areas and identify main climate belts. In the Proto-North Atlantic realm (~15–17°N) large amou…

010504 meteorology & atmospheric sciencesδ18OGlobal warming[SDU.STU]Sciences of the Universe [physics]/Earth SciencesTEX86Subtropics15. Life on land010502 geochemistry & geophysics01 natural sciencesCretaceousPaleontology13. Climate action[SDU]Sciences of the Universe [physics]General Earth and Planetary SciencesSedimentary rockThermohaline circulationGlobal coolingGeology0105 earth and related environmental sciences
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2500 Years of European Climate Variability and Human Susceptibility

2011

Climate variations influenced the agricultural productivity, health risk, and conflict level of preindustrial societies. Discrimination between environmental and anthropogenic impacts on past civilizations, however, remains difficult because of the paucity of high-resolution paleoclimatic evidence. We present tree ring-based reconstructions of central European summer precipitation and temperature variability over the past 2500 years. Recent warming is unprecedented, but modern hydroclimatic variations may have at times been exceeded in magnitude and duration. Wet and warm summers occurred during periods of Roman and medieval prosperity. Increased climate variability from similar to 250 to 6…

010506 paleontology010504 meteorology & atmospheric sciencesMeteorologyClimate Changemedia_common.quotation_subjectLast MillenniumCollapseClimatic ProcessesClimate changeCivilizationHistory 18th CenturyHistory 21st Century01 natural sciencesTreesHistory 17th CenturyQuercusReconstructionsDendrochronologyHumansAgricultural productivityEpidemicsRoman Warm PeriodSeriesHistory AncientHoloceneHistory 15th Century0105 earth and related environmental sciencesmedia_commonMultidisciplinaryDroughtHoloceneTemperatureRecordsAgricultureHistory 19th CenturyDemiseHistory 20th Century15. Life on landHistory MedievalRoman EmpireEuropeGeographyHistory 16th Century13. Climate actionAfricaSeasonsPhysical geographyProsperityScience
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Large-scale, millennial-length temperature reconstructions from tree-rings

2018

Supported by the German Science Foundation, grants # Inst 247/665-1 FUGG and ES 161/9-1. SSG acknowledges support by the Alexander von Humboldt Foundation, KJA by US National Science Foundation grants AGS-1501856 and NSF AGS-1501834, and JL and LS by the Belmont Forum and JPI-Climate, Collaborative Research Action INTEGRATE. Over the past two decades, the dendroclimate community has produced various annually resolved, warm season temperature reconstructions for the extratropical Northern Hemisphere. Here we compare these tree-ring based reconstructions back to 831 CE and present a set of basic metrics to provide guidance for non-specialists on their interpretation and use. We specifically d…

010506 paleontology010504 meteorology & atmospheric sciencesNDASPlant ScienceWarm season01 natural sciencesG1Extratropical cycloneddc:550Little ice ageBeneficial effectsWarm season temperatures0105 earth and related environmental sciencesNorthern Hemisphereddc:333.7-333.9EcologyNorthern HemisphereG Geography (General)Medieval Warm PeriodCovarianceTree-ring widthMaximum latewood densityTree (data structure)ClimatologyLittle Ice AgeScale (map)Geology
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The history and impacts of farming activities in south Greenland: an insight from lake deposits.

2013

International audience; Agriculture in southern Greenland has a two-phase history: with the Norse, who first settled and farmed the region between 985ad and circa 1450ad, and with the recent reintroduction of sheep farming (1920ad to the present). The agricultural sector in Greenland is expected to grow over the next century as anticipated climate warming extends the length of the growing season and increases productivity. This article presents a synthesis of results from a well-dated 1500-year lake sediment record from Lake Igaliku, south Greenland (61°00′N, 45°26′W, 15m asl) that demonstrates the relative impacts of modern and Norse agricultural activities. Pollen, non-pollen palynomorphs…

010506 paleontology010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory[SDE.MCG]Environmental Sciences/Global ChangesGeography Planning and DevelopmentContext (language use)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryCoprophilous fungi0105 earth and related environmental sciencesEcologybiologyEcologyGlobal warmingSedimentPlant communityδ15N15. Life on landbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesDiatomProductivity (ecology)13. Climate action[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesGeology
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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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Du Néolithique récent à l’âge du Bronze dans le Centre Nord de la France : les étapes de l’évolution chrono-culturelle

2011

Die seit 2001 im Rahmen eines PCR (Programme Collectif Régional) durchgeführte Gemeinschaftsarbeit über das Ende des Neolithikums und den Beginns der Bronzezeit im Zentrum Nordfrankreichs führt heute zu einer neuen Periodisierung der Zeit zwischen 3600 und 1800 v. Chr. in acht Etappen. Obwohl, insbesondere bezüglich der Transition zwischen dem Mittel-und dem Jungneolithikum einerseits und dem Jung-und dem Endneolithikum andererseits, auch weiterhin einige Lücken bestehen, erlaubt dieser präzisere Rahmen die Hauptetappen im Zentrum Nordfrankreichs mit denen der benachbarten Regionen zu synchronisieren, um eine dynamischere Vision der kulturellen Phänomene vorzuschlagen.

010506 paleontology060102 archaeologyCampaniformemedia_common.quotation_subjectNéolithiqueJungneolithikum ; Endneolithikum ; Frühbronzezeit ; Chronologie ; Zentrum Nordfrankreichs06 humanities and the artsArt01 natural sciences[SHS]Humanities and Social SciencesLate Neolithic ; central part of northern France ; Chronology ; Early Bronze Age ; Final NeolithicChronologie 14C AMSAge du BronzeBronze Age[ SHS ] Humanities and Social Sciences0601 history and archaeologyPharmacology (medical)[SHS] Humanities and Social SciencesBronze ancien ; Néolithique récent ; Néolithique final ; chronologie ; Centre Nord de la FranceHumanitiesNord de la FranceComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesmedia_common
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