Search results for "oceanic"

showing 10 items of 642 documents

Generation of Earth's early continents from a relatively cool Archean mantle

2019

This research has been supported by DFG grant, SPP 1833 Building a Habitable Earth and MAGMA Consolidator Grant (ERC project #71143). Several lines of evidence suggest that the Archean (4.0 2.5 Ga) mantle was hotter than today's potential temperature (TP) of  1350 ° C. However, the magnitude of such difference is poorly constrained, with TP estimation spanning from 1500 ° C to 1600 ° C during the Meso‐Archean (3.2‐2.8 Ga). Such differences have major implications for the interpreted mechanisms of continental crust generation on the early Earth, as their efficacy is highly sensitive to the TP. Here, we integrate petrological modeling with thermomechanical simulations to understand the dynami…

Continental crust010504 meteorology & atmospheric sciencesArchean010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geochemistry and PetrologyOceanic crustGeodynamic modelingPetrology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryGEContinental crustPartial meltingEarly EarthDASEarly EarthCratonGeophysics13. Climate actionIntraplate earthquakeBDCGeologyGE Environmental Sciences
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Initiation of deep convection at marginal instability in an ensemble of mesoscale models: a case-study from COPS

2011

The present study investigates the initiation of precipitating deep convection in an ensemble of convection-resolving mesoscale models. Results of eight different model runs from five non-hydrostatic models are compared for a case of the Convective and Orographically-induced Precipitation Study (COPS). An isolated convective cell initiated east of the Black Forest crest in southwest Germany, although convective available potential energy was only moderate and convective inhibition was high. Measurements revealed that, due to the absence of synoptic forcing, convection was initiated by local processes related to the orography. In particular, the lifting by low-level convergence in the planet…

Convection021110 strategic defence & security studiesAtmospheric ScienceConvective inhibition010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layer0211 other engineering and technologiesMesoscale meteorologyOrography02 engineering and technologyForcing (mathematics)01 natural sciencesConvective available potential energyFree convective layerPhysics::Fluid Dynamics13. Climate actionClimatologyPhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesQuarterly Journal of the Royal Meteorological Society
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Further evidence for CCN aerosol concentrations determining the height of warm rain and ice initiation in convective clouds over the Amazon basin

2017

We have investigated how aerosols affect the height above cloud base of rain and ice hydrometeor initiation and the subsequent vertical evolution of cloud droplet size and number concentrations in growing convective cumulus. For this purpose we used in situ data of hydrometeor size distributions measured with instruments mounted on HALO aircraft during the ACRIDICON–CHUVA campaign over the Amazon during September 2014. The results show that the height of rain initiation by collision and coalescence processes (Dr, in units of meters above cloud base) is linearly correlated with the number concentration of droplets (Nd in cm−3) nucleated at cloud base (Dr ≈ 5 ⋅ Nd). Additional cloud processes…

ConvectionAtmospheric Science010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:ChemistryCloud basecloudrainWolkenphysikAerosolPhysics::Atmospheric and Oceanic Physicsconvection0105 earth and related environmental sciencesEffective radiusCoalescence (physics)15. Life on landlcsh:QC1-999AerosolAmbient airlcsh:QD1-99913. Climate actionEnvironmental scienceHalolcsh:PhysicsAmazon basinAtmospheric Chemistry and Physics
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Impact of deep convection in the tropical tropopause layer in West Africa: in-situ observations and mesoscale modelling

2011

Abstract. We present the analysis of the impact of convection on the composition of the tropical tropopause layer region (TTL) in West-Africa during the AMMA-SCOUT campaign. Geophysica M55 aircraft observations of water vapor, ozone, aerosol and CO2 during August 2006 show perturbed values at altitudes ranging from 14 km to 17 km (above the main convective outflow) and satellite data indicates that air detrainment is likely to have originated from convective cloud east of the flights. Simulations of the BOLAM mesoscale model, nudged with infrared radiance temperatures, are used to estimate the convective impact in the upper troposphere and to assess the fraction of air processed by convecti…

ConvectionAtmospheric Science010504 meteorology & atmospheric sciencesMesoscale meteorologyAtmospheric sciences01 natural sciencesTropospherelcsh:Chemistry010309 optics0103 physical sciencesddc:550Astrophysics::Solar and Stellar AstrophysicsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Convective inhibitionFree convective layerlcsh:QC1-999Jlcsh:QD1-99913. Climate actionClimatologyRadianceOutflowWater vaporGeologylcsh:Physics
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Simulations of convectively-driven density currents in the Atlas region using a regional model: Impacts on dust emission and sensitivity to horizonta…

2009

[1] During the SAMUM field campaign in southern Morocco in May and June 2006 density currents generated by evaporative cooling after convective precipitation were frequently observed at the Sahara side of the Atlas Mountain chain. The associated strong surface cold-air outflow during such events has been observed to lead to dust mobilization in the foothills. Here a regional model system is used to simulate a density current case on 3 June 2006 and the subsequent dust emission. The model studies are performed with different parameterization schemes for convection, and with different horizontal model grid resolutions to examine to which extent the model system can be used for reproducing dus…

ConvectionAtmospheric Science010504 meteorology & atmospheric sciencesMeteorologySoil ScienceAquatic Science010502 geochemistry & geophysicsOceanographyAtmospheric sciences01 natural sciencesGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Physics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyEcologyAtlas (topology)PaleontologyForestryGeophysicsMountain chain13. Climate actionSpace and Planetary ScienceOutflowRegional modelCurrent densityParametrizationGeologyEvaporative cooler
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Observed and Simulated Variability of Droplet Spectral Dispersion in Convective Clouds Over the Amazon

2021

In this study, the variability of the spectral dispersion of droplet size distributions (DSDs) in convective clouds is investigated. Analyses are based on aircraft measurements of growing cumuli near the Amazon basin, and on numerical simulations of an idealized ice‐free cumulus. In cleaner clouds, the relative dispersion ϵ, defined as the ratio of the standard deviation to the mean value of the droplet diameter, is negatively correlated with the ratio of the cloud water content (qc) to the adiabatic liquid water content (qa), while no strong correlation between ϵ and qc/qa is seen in polluted clouds. Bin microphysics numerical simulations suggest that these contrasting behaviors are associ…

ConvectionAtmospheric ScienceAmazon rainforestaerosolcloudsSpectral dispersionMICROFÍSICA DE NUVENSAtmospheric sciencesdroplet spectumStandard deviationGeophysicsddc:551.5Space and Planetary ScienceLiquid water contentEarth and Planetary Sciences (miscellaneous)Environmental sciencedispersionAdiabatic processDroplet sizeWater contentPhysics::Atmospheric and Oceanic Physics
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Tropical–extratropical interactions related to upper-level troughs at low latitudes

2007

Abstract Momentum and kinetic energy fluxes associated with low-latitude transient disturbances at upper-levels play an important role in the general circulation of the atmosphere. They are related to eastward and equatorward propagating, positively tilted wave trains from the extratropics. Theoretical, modelling and observational studies show that this particular kind of tropical–extratropical interaction is most common in regions of mean upper-level westerlies at low latitudes, i.e. over the central and eastern Pacific and Atlantic Oceans during boreal winter and spring. The penetration of an upper-level trough into the Tropics is often associated with enhanced convection and the formatio…

ConvectionAtmospheric ScienceAtmospheric circulationRossby waveGeologyWesterliesJet streamOceanographyAtmospheric sciencesPhysics::GeophysicsAtmospheric convectionClimatologyExtratropical cycloneComputers in Earth SciencesTrough (meteorology)Physics::Atmospheric and Oceanic PhysicsGeologyDynamics of Atmospheres and Oceans
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Numerical sensitivity studies on the impact of aerosol properties and drop freezing modes on the glaciation, microphysics, and dynamics of clouds

2006

[1] Numerical simulations were performed to investigate the effects of drop freezing in immersion and contact modes for a convective situation. For the description of heterogeneous drop freezing, new approaches were used considering the significantly different ice nucleating efficiencies of various ice nuclei. An air parcel model with a sectional two-dimensional description of the cloud microphysics was employed. Sensitivity studies were undertaken by varying the insoluble particle types as well as the soluble fraction of the aerosol particles showing the effects of these parameters on drop freezing and their possible impact on the vertical cloud dynamics. The soluble fraction ɛ decides whe…

ConvectionAtmospheric ScienceMaterials scienceNuclear TheorySoil ScienceMineralogyAquatic ScienceOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Nuclear ExperimentPhysics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyEcologyMicrophysicsDrop (liquid)PaleontologyCloud physicsForestryMechanicsFreezing pointAerosolGeophysicsSpace and Planetary ScienceIce nucleusFreezing-point depressionJournal of Geophysical Research
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Simple kinematic models for the environmental interaction of tropical cyclones in vertical wind shear

2011

A major impediment to the intensity forecast of tropical cyclones (TCs) is believed to be associated with the interaction of TCs with dry environmental air. However, the conditions under which pronounced TC-environment interaction takes place are not well understood. As a step towards improving our understanding of this problem, we analyze here the flow topology of a TC immersed in an environment of vertical wind shear in an idealized, three-dimensional, convection-permitting numerical experiment. A set of distinct streamlines, the so-called manifolds, can be identified under the assumptions of steady and layer-wise horizontal flow. The manifolds are shown to divide the flow around the TC i…

ConvectionAtmospheric ScienceMeteorologyEyeFlow (psychology)InflowMechanicslcsh:QC1-999Vortexlcsh:Chemistrylcsh:QD1-999Wind shearStreamlines streaklines and pathlinesOutflowlcsh:PhysicsPhysics::Atmospheric and Oceanic PhysicsGeologyAtmospheric Chemistry and Physics
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Modeling of biomass smoke injection into the lower stratosphere by a large forest fire (Part I): reference simulation

2006

Abstract. Wildland fires in boreal regions have the potential to initiate deep convection, so-called pyro-convection, due to their release of sensible heat. Under favorable atmospheric conditions, large fires can result in pyro-convection that transports the emissions into the upper troposphere and the lower stratosphere. Here, we present three-dimensional model simulations of the injection of fire emissions into the lower stratosphere by pyro-convection. These model simulations are constrained and evaluated with observations obtained from the Chisholm fire in Alberta, Canada, in 2001. The active tracer high resolution atmospheric model (ATHAM) is initialized with observations obtained by r…

ConvectionAtmospheric SciencePyrocumulonimbus cloudMeteorology010504 meteorology & atmospheric sciences0211 other engineering and technologies02 engineering and technologySensible heatAtmospheric sciences7. Clean energy01 natural scienceslcsh:ChemistryTropospherePhysics::Fluid DynamicsLatent heatCloud baseAstrophysics::Solar and Stellar AstrophysicsStratospherePhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciences040101 forestry[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere021110 strategic defence & security studies04 agricultural and veterinary sciences15. Life on landlcsh:QC1-999lcsh:QD1-99913. Climate action0401 agriculture forestry and fisheriesEnvironmental scienceTropopauselcsh:Physics
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