Search results for "Cold front"

showing 4 items of 4 documents

Analysis of a severe pollution episode in Valencia (Spain) and its effect on ground level particulate matter

2013

Abstract This study analyzes the atmospheric particles concentration at ground level during a severe pollution event that took place in Valencia (Spain) from 7 to 12 February 2011. The episode was related to a subtropical anticyclone system that affected the Iberian Peninsula and western Europe. The dominant anticyclone imposed an extended low gradient pressure system and a low mixing layer height in the region that caused the accumulation of pollutants over the western Mediterranean. Moreover, the stagnant conditions led to the formation of the local sea breeze, accompanied by an increase of relative humidity and the decrease of ambient temperature. Our study is mainly focused on the analy…

Fluid Flow and Transfer ProcessesPollutionMediterranean climateAtmospheric ScienceEnvironmental EngineeringbiologyMeteorologyMechanical Engineeringmedia_common.quotation_subjectParticulatesAtmospheric sciencesAethalometerbiology.organism_classificationPollutionCold frontSea breezeAnticycloneEnvironmental scienceValenciamedia_commonJournal of Aerosol Science
researchProduct

The 1-way on-line coupled atmospheric chemistry model system MECO(n) – Part 3: Meteorological evaluation of the on-line coupled system

2012

Abstract. Three detailed meteorological case studies are conducted with the global and regional atmospheric chemistry model system ECHAM5/MESSy(→COSMO/MESSy)n, shortly named MECO(n), in order to assess the general performance of the on-line coupling of the regional model COSMO to the global model ECHAM5. The cases are characterised by intense weather systems in Central Europe: an intense cold frontal passage in March 2010, a convective frontal event in July 2007, and the high impact winter storm "Kyrill" in January 2007. Simulations are performed with the new on-line-coupled model system and compared to classical, off-line COSMO hindcast simulations driven by ECMWF analyses. Precipitation o…

Convectionmodel evaluationnestingMeteorology010504 meteorology & atmospheric sciencesatmospheric model0207 environmental engineering0211 other engineering and technologies02 engineering and technologyprecipitation01 natural sciencesMESSyHindcastPrecipitationmeteorology020701 environmental engineeringLine (formation)0105 earth and related environmental sciences021110 strategic defence & security studiesglobal modelregional modelCOSMOlcsh:QE1-996.5Stormlcsh:GeologyCold front13. Climate actionAtmospheric chemistryClimatologyEnvironmental sciencemodel couplingDynamik der AtmosphäreLead time
researchProduct

Orographic Effects and Evaporative Cooling along a Subtropical Cold Front: The Case of the Spectacular Saharan Dust Outbreak of March 2004

2012

Abstract On 2 March 2004 a marked upper-level trough and an associated surface cold front penetrated into the Sahara. High winds along and behind this frontal system led to an extraordinary, large-scale, and long-lived dust outbreak, accompanied by significant precipitation over parts of Algeria, Tunisia, and Libya. This paper uses sensitivity simulations with the limited-area model developed by the Consortium for Small-Scale Modeling (COSMO) together with analysis data and surface observations to test several hypotheses on the dynamics of this case proposed in previous work. It is demonstrated that air over central Algeria is cooled by evaporation of frontal precipitation, substantially en…

Atmospheric ScienceLeading edgeCold frontMountain chainClimatologyEnvironmental scienceSubtropicsMineral dustAtmospheric sciencesTrough (meteorology)Evaporative coolerOrographic liftMonthly Weather Review
researchProduct

Blast waves from violent explosive activity at Yasur Volcano, Vanuatu

2013

[1] Infrasonic and seismic waveforms were collected during violent strombolian activity at Yasur Volcano (Vanuatu). Averaging ~3000 seismic events showed stable waveforms, evidencing a low-frequency (0.1–0.3 Hz) signal preceding ~5–6 s the explosion. Infrasonic waveforms were mostly asymmetric with a sharp compressive (5–106 Pa) onset, followed by a small long-lasting rarefaction phase. Regardless of the pressure amplitude, the ratio between the positive and negative phases was constant. These waveform characteristics closely resembled blast waves. Infrared imagery showed an apparent cold spherical front ~20 m thick, which moved between 342 and 405 m/s before the explosive hot gas/fragments…

010504 meteorology & atmospheric sciencesExplosive materialFront (oceanography)RarefactionGeophysics010502 geochemistry & geophysics01 natural sciencesStrombolian eruptionsymbols.namesakeGeophysicsCold frontMach number13. Climate actionsymbolsGeneral Earth and Planetary SciencesSupersonic speedGeologyBlast waveSeismology0105 earth and related environmental sciencesGeophysical Research Letters
researchProduct