Search results for "Climate"

showing 10 items of 4934 documents

The transport history of two Saharan dust events archived in an Alpine ice core

2005

Mineral dust from the Saharan desert can be transported across the Mediterranean towards the Alpine region several times a year. When coinciding with snowfall, the dust can be deposited on Alpine glaciers and then appears as yellow or red layers in ice cores. Two such significant dust events were identified in an ice core drilled at the high-accumulation site Piz Zupó in the Swiss Alps (46°22' N, 9°55' E, 3850 m a.s.l.). From stable oxygen isotopes and major ion concentrations, the events were approximately dated as October and March 2000. In order to link the dust record in the ice core to the meteorological situation that led to the dust events, a novel methodology based on b…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereGlacierMineral dustSnowAtmospheric sciences010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenlcsh:QC1-999Aerosollcsh:ChemistryDeposition (aerosol physics)Ice corelcsh:QD1-99913. Climate actionPaleoclimatologyGeologylcsh:Physics0105 earth and related environmental sciences
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A theoretical study of the wet removal of atmospheric pollutants. Part I: the redistribution of aerosol particles captured through nucleation and imp…

1985

Abstract A theoretical model is formulated which allows the processes that control the wet deposition of atmospheric pollutants to be included in cloud dynamic models. The model considers the condensation process and the collision-coalescence process which, coupled together, control the fate of atmospheric aerosol particles removed by clouds and precipitation through nucleation scavenging and impaction scavenging. The model was tested by substituting a simple parcel model for the dynamic framework. In this form the model was used to determine the time evolution of the aerosol particle mass scavenged by drops as well as the aerosol particle mass left unactivated in air as “drop-interstitial”…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmospherePollutionAtmospheric ScienceMeteorologyAerosol impactionmedia_common.quotation_subjectAir pollutionNucleationrespiratory systemmedicine.disease_causeAtmospheric sciencescomplex mixturesAerosolDistribution function13. Climate actionmedicineEnvironmental scienceRedistribution (chemistry)ScavengingComputingMilieux_MISCELLANEOUSPhysics::Atmospheric and Oceanic Physicsmedia_common
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In-Situ observation of New Particle Formation in the upper troposphere/lower stratosphere of the Asian Monsoon Anticyclone

2020

Abstract. During the monsoon season of the year 2017 the airborne StratoClim mission took place in Kathmandu, Nepal with eight mission flights of the M-55 Geophysica in the upper troposphere/lower stratosphere (UT/LS) of the Asian Monsoon Anticyclone (AMA) over northern India, Nepal and Bangladesh. More than hundred events of New Particle Formation (NPF) were observed. In total, more than two hours of flight time were spent under NPF conditions as indicated by the abundant presence of ultrafine aerosols, i.e. with particle diameters dp smaller than 15 nm, which were in-situ detected by means of condensation nuclei counting techniques. Mixing ratios of ultrafine particles (nuf) of up to ~ 50…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereTroposphere13. Climate actionAnticycloneClimatologyddc:550East Asian MonsoonEnvironmental scienceParticle (ecology)MonsoonStratosphere
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A numerical study of tropical cross-tropopause transport by convective overshoots

2007

Abstract. Observations obtained during the Tropical Convection, Cirrus and Nitrogen Oxides (TROCCINOX) golden day have revealed the presence of ice particles up to 410 K (18.2 km) 2 km above the local tropopause. The case was investigated using a three-dimensional quadruply nested non-hydrostatic simulation and Meteosat Second Generation (MSG) observations. The simulation reproduced the measurements along the flight track fairly well. A reasonable agreement with MSG observations was also achieved: the 10.8-μm brightness temperature (BT) minimum of 187 K was reproduced (a value 6 K colder than the environmental cold-point temperature) as was the positive BT difference between the 6.2- and 10…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Mass fluxConvectionAtmospheric Science010504 meteorology & atmospheric sciences010501 environmental sciencesAtmospheric sciences01 natural scienceslcsh:QC1-999lcsh:ChemistryFlight tracklcsh:QD1-99913. Climate actionBrightness temperatureClimatologyTRACEREnvironmental scienceCirrusTropopauselcsh:PhysicsWater vapor0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Magma-derived gas influx and water-rock interactions in the volcanic aquifer of Mt. Vesuvius, Italy

2002

We report in this paper a systematic investigation of the chemical and isotopic composition of groundwaters flowing in the volcanic aquifer of Mt. Vesuvius during its current phase of dormancy, including the first data on dissolved helium isotope composition and tritium content. The relevant results on dissolved He and C presented in this paper reveal that an extensive interaction between rising magmatic volatiles and groundwaters currently takes place at Vesuvius.Vesuvius groundwaters are dilute (mean TDS ∼ 2800 mg/L) hypothermal fluids ( mean T = 17.7°C) with a prevalent alkaline-bicarbonate composition. Calcium-bicarbonate groundwaters normally occur on the surrounding Campanian Plain, l…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistryAquifer010502 geochemistry & geophysics01 natural sciencesGeochemistryVolcano13. Climate actionGeochemistry and PetrologyMagmaWater chemistry[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesPetrology
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Isotope geochemistry of Pantelleria volcanic fluids, Sicily Channel rift: a mantle volatile end-member for volcanism in southern Europe

2000

Chemical and isotopic ratio (He, C, H and O) analysis of hydrothermal manifestations on Pantelleria island, the southernmost active volcano in Italy, provides us with the first data upon mantle degassing through the Sicily Channel rift zone, south of the African–European collision plate boundary. We find that Pantelleria fluids contain a CO2–He-rich gas component of mantle magmatic derivation which, at shallow depth, variably interacts with a main thermal (∼100°C) aquifer of mixed marine–meteoric water. The measured 3He/4He ratios and δ13C of both the free gases (4.5–7.3 Ra and −5.8 to −4.2‰, respectively) and dissolved helium and carbon in waters (1.0–6.3 Ra and −7.1 to −0.9‰), together wi…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categoryRift010504 meteorology & atmospheric sciencesSubductionGeochemistry010502 geochemistry & geophysics01 natural sciencesMantle (geology)Plate tectonicsGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyIsotope geochemistryEarth and Planetary Sciences (miscellaneous)CalderaRift zone[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences
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Small-scale mixing processes enhancing troposphere-to-stratosphere transport by pyro-cumulonimbus storms

2007

Abstract. Deep convection induced by large forest fires is an efficient mechanism for transport of aerosol particles and trace gases into the upper troposphere and lower stratosphere (UT/LS). For many pyro-cumulonimbus clouds (pyroCbs) as well as other cases of severe convection without fire forcing, radiometric observations of cloud tops in the thermal infrared (IR) reveal characteristic structures, featuring a region of relatively high brightness temperatures (warm center) surrounded by a U-shaped region of low brightness temperatures. We performed a numerical simulation of a specific case study of pyroCb using a non-hydrostatic cloud resolving model with a two-moment cloud microphysics p…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospherelcsh:Chemistry010504 meteorology & atmospheric scienceslcsh:QD1-99913. Climate action[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmosphere010501 environmental sciences15. Life on land01 natural scienceslcsh:Physicslcsh:QC1-9990105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Intraseasonal descriptors and rainfall extremes in austral summer over South Africa : Observations and Meso-scale modelling

2022

Rainfall extremes are of major and increasing importance in semi-arid countries and their variability has strong implications for water resource and climate impacts on the local societies and environment. Here, we examine intraseasonal descriptors (ISDs) and wet extremes in austral summer rainfall (November−February) over South Africa (SA). Using daily observations from 225 rain gauges and ERA5 reanalysis between 1979 and 2015, we propose a novel typology of wet extreme events based on their spatial fraction, thus differentiating large- and small-scale extremes. Long-term variability of both types of extreme rainfall events is then extensively discussed in the context of ISDs. Following the…

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyIintraseasonal descriptorsRainfall variabilityDescripteurs intraseonauxRegional climate modelingModélisation du climat régionalVariabilité des précipitations
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Climats tropicaux d'aujourd'hui à demain : variabilité et changements

2008

Present and future tropical climates : their climate variability and their climate changes The oriffttality of tropical climates is re-examined under the light of climate variability and climate change, both present and future . The interannual variability of rainfall is on average larger in the tropics than in the extra-tropics, but it is also spatially more contrasted. Human communities have often responded to this constraint through efficient coping strategies. The regions showing the most variable climate do not necessarily have lower population densities, an indication that in the long run variability is not decisive. However, the recent demographic growth of these regions is often low…

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SHS.GEO] Humanities and Social Sciences/Geographyrainfall ; seasonal prediction ; climate inpacts. ; climatic hazards ; climate change ; Tropics ; interannual variability[SHS.GEO]Humanities and Social Sciences/Geography[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyComputingMilieux_MISCELLANEOUSaléas climatiques ; variabilité interannuelle ; impacts climatiques. ; prévision saisonnière ; précipitations ; tropicalité ; changements climatiques[ SHS.GEO ] Humanities and Social Sciences/Geography
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Impacts sur le climat régional induits par l'immersion d'une zone aride : cas de Chott Jérid (sud de la Tunisie).

2017

This work aims to show the possible impacts on the regional climate that could be caused by the partial immersion ofChott Jérid located in the south of Tunisia. Climate simulations have been carried out using the Weather Research andForecasting (WRF) model to compare the present climate of the Chott area simulated over the period 1991-2011 under realconditions of land use to the climate simulated in the fictional presence of a vast artificial waterbody (or lake). Comparisonsshowed that the lake would have a particularly moderating effect on average air temperatures. The sensible heat flux wouldincrease substantially during the winter and decrease during the summer, while latent heat and moi…

[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatologyregional climateWRFimpacts climatiques régionauxChott Jérid[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatologylac artificielartificial lake
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