Search results for "Monsoon"

showing 10 items of 117 documents

Fluorescent biological aerosol particle measurements at a tropical high-altitude site in southern India during the southwest monsoon season

2016

An ultraviolet aerodynamic particle sizer (UV-APS) was continuously operated for the first time during two seasons to sample the contrasting winds during monsoon and winter to characterize the properties of fluorescent biological aerosol particles (FBAPs), at a high-altitude site in India. Averaged over the entire monsoon campaign (1 June–21 August 2014), the arithmetic mean number and mass concentrations of coarse-mode (> 1 µm) FBAPs were 0.02 cm−3 and 0.24 µg m−3, respectively, which corresponded to  ∼  2 and 6 % of total aerosol loading, respectively. Average FBAP number size distribution exhibited a peak at  ∼  3 µm, which is attributed to the fungal spores, as supported by scanning …

Atmospheric Science010504 meteorology & atmospheric sciencesParticle number010501 environmental sciencesWind directionEffects of high altitude on humansMonsoon01 natural scienceslcsh:QC1-999Aerosollcsh:Chemistrylcsh:QD1-999ClimatologyEnvironmental scienceRelative humidityPrecipitationlcsh:Physics0105 earth and related environmental sciencesArithmetic meanAtmospheric Chemistry and Physics
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In situ observation of new particle formation (NPF) in the tropical tropopause layer of the 2017 Asian monsoon anticyclone – Part 1: Summary of Strat…

2021

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 (UTLS) of the Asian monsoon anticyclone (AMA) over northern India, Nepal, and Bangladesh. More than 100 events of new particle formation (NPF) were observed. In total, more than 2 h of flight time was spent under NPF conditions as indicated by the abundant presence of nucleation-mode aerosols, i.e. with particle diameters dp smaller than 15 nm, which were detected in situ by means of condensation nuclei counting techniques. Mixing ratios of nucleation-mode particles (nnm) of up to ∼ 50 000 mg−…

Atmospheric Science010504 meteorology & atmospheric sciencesPhysicsQC1-999010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesupper troposphere; lower stratosphere; sulfuric-acid; gravity waves; atmospheric particlesAerosolChemistryAltitude13. Climate actionAnticycloneddc:550Environmental scienceEast Asian MonsoonCloud condensation nucleiTropopauseQD1-999StratosphereAir mass0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Quasi-decadal signals of Sahel rainfall and West African monsoon since the mid-twentieth century

2013

[1] Sahel rainfall shows pronounced decadal variability and a negative trend between wet conditions in the 1950s–1960s and dry ones in the 1970s–1980s. Using continuous wavelet transform, the quasi-decadal variability (QDV) of rainfall reveals zonal contrasts. The highest QDV is identified in the 1950s–1960s over western Sahel and in the 1970s–1980s over eastern Sahel. The quasi-decadal atmospheric anomalies have been reconstructed using Fourier transform for the 1950s–1960s and the 1970s–1980s, respectively, and assessed by the composite analysis of the QDV phases for the periods before and after 1968. Over western Sahel, the rainfall QDV in the 1950s–1960s is related to the North Atlantic…

Atmospheric Science010504 meteorology & atmospheric sciencesWavelet coherenceIntertropical Convergence Zone0207 environmental engineering02 engineering and technologySubtropicsMonsoon01 natural sciencesTroposphereSea surface temperatureWest africanGeophysics13. Climate actionSpace and Planetary ScienceClimatologyEarth and Planetary Sciences (miscellaneous)Moisture convergence020701 environmental engineeringGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Atmospheres
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Intercomparison and analyses of the climatology of the West African Monsoon in the West African Monsoon Modeling and Evaluation project (WAMME) first…

2010

International audience; This paper briefly presents the West African Monsoon (WAM) Modeling and Evaluation Project (WAMME) and evaluates WAMME general circulation models' (GCM) performances in simulating variability of WAM precipitation, surface temperature, and major circulation features at seasonal and intraseasonal scales in the first WAMME experiment. The analyses indicate that models with specified sea surface temperature generally have reasonable simulations of the pattern of spatial distribution of WAM seasonal mean precipitation and surface temperature as well as the averaged zonal wind in latitude-height cross-section and low level circulation. But there are large differences among mo…

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes0207 environmental engineeringTropical Easterly JetEmpirical orthogonal functions02 engineering and technologySensible heatOceanographyMonsoon01 natural sciencesMeteorology/ClimatologyLatent heatGeophysics/GeodesyPrecipitation020701 environmental engineering0105 earth and related environmental sciencesAfrican easterly jet[ SDE.MCG ] Environmental Sciences/Global ChangesSea surface temperature[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyEarth SciencesEnvironmental science[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimate Dynamics
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Assessments for the impact of mineral dust on the meningitis incidence in West Africa.

2013

9 pages; International audience; Recently, mineral dust has been suspected to be one of the important environmental risk factor for meningitis epidemics in West Africa. The current study is one of the first which relies on long-term robust aerosol measurements in the Sahel region to investigate the possible impact of mineral dust on meningitis cases (incidence). Sunphotometer measurements, which allow to derive aerosol and humidity parameters, i.e., aerosol optical thickness, Angström coefficient, and precipitable water, are combined with quantitative epidemiological data in Niger and Mali over the 2004-2009 AMMA (African Monsoon Multidisciplinary Analysis) program period. We analyse how th…

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesDry seasonContext (language use)010501 environmental sciencesMineral dustMonsoon01 natural sciencescomplex mixtures[SDV.MHEP.MI]Life Sciences [q-bio]/Human health and pathology/Infectious diseasesDry seasonWest AfricamedicineMeningitis0105 earth and related environmental sciencesGeneral Environmental Science2. Zero hungerPrecipitable waterHumidityDustmedicine.diseaseAerosol[ SDE.MCG ] Environmental Sciences/Global Changes[ SDV.MHEP.MI ] Life Sciences [q-bio]/Human health and pathology/Infectious diseases13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyEnvironmental science[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyMeningitis
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Interannual and decadal SST-forced responses of the West African monsoon

2010

International audience; We review the studies carried out during the African Monsoon Multidisciplinary Analysis (AMMA)-EU on the changes of interannual sea surface temperature (SST)-West African monsoon (WAM) covariability at multidecadal timescales, together with the influence of global warming (GW). The results obtained in the AMMA-EU suggest the importance of the background state, modulated by natural and anthropogenic variability, in the appearance of different interannual modes. The lack of reliability of current coupled models in giving a realistic assessment for WAM in the future is also stated.

Atmospheric Science010504 meteorology & atmospheric sciencesinterannual variabilityMultidisciplinary analysis[SDE.MCG]Environmental Sciences/Global ChangesGlobal warmingrainfall0207 environmental engineeringSST forced responseAfrican Monsoon02 engineering and technologyMonsoon01 natural sciencesSea surface temperatureWest african[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologySahelianEnvironmental science[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology020701 environmental engineeringdecadal variability0105 earth and related environmental sciences
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Fast transport from Southeast Asia boundary layer sources to northern Europe: rapid uplift in typhoons and eastward eddy shedding of the Asian monsoo…

2014

Abstract. Enhanced tropospheric trace gases such as CO, CH4 and H2O and reduced stratospheric O3 were measured in situ in the lowermost stratosphere over northern Europe on 26 September 2012 during the TACTS aircraft campaign. The measurements indicate that these air masses clearly differ from the stratospheric background. The calculation of 40-day backward trajectories with the trajectory module of the CLaMS model shows that these air masses are affected by the Asian monsoon anticyclone. Some air masses originate from the boundary layer in Southeast Asia/West Pacific and are rapidly lifted (1–2 days) within a typhoon up to the outer edge of the Asian monsoon anticyclone. Afterwards, the ai…

Atmospheric ScienceAtmospheric scienceslcsh:QC1-999Trace gasSoutheast asiaTropospherelcsh:ChemistryBoundary layerlcsh:QD1-999AnticycloneClimatologyTyphoonddc:550East Asian MonsoonStratosphereGeologylcsh:Physics
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A Lagrangian Climatology of Tropical Moisture Exports to the Northern Hemispheric Extratropics

2010

Abstract Case studies have shown that heavy precipitation events and rapid cyclogenesis in the extratropics can be fueled by moist and warm tropical air masses. Often the tropical moisture export (TME) occurs through a longitudinally confined region in the subtropics. Here a comprehensive climatological analysis of TME is constructed on the basis of seven-day forward trajectories started daily from the tropical lower troposphere using 6-hourly 40-yr ECMWF Re-Analysis (ERA-40) data from the 23-year period 1979–2001. The objective TME identification procedure retains only those trajectories that reach a water vapor flux of at least 100 g kg−1 m s−1 somewhere north of 35°N. The results show fo…

Atmospheric ScienceClimatologyCyclogenesisNorthern HemisphereTropicsEnvironmental scienceSubtropicsPrecipitationAtmospheric riverMonsoonTeleconnectionJournal of Climate
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Mid-century effects of Climate Change on African monsoon dynamics using the A1B emission scenario

2012

Future climate changes in African regions are model-dependent and there is no consensus regarding Sahelian rainfall by the end of this century. Using 12 atmosphere-ocean global climate models of the third Coupled Model Intercomparison Project (CMIP3) we propose a multi-model (MM) analysis contrasting the 1960–1999 period (20c3m integration) and the 2031–2070 period (A1B emission scenario). The analyses are based on MM response but also on the ‘one model-one vote’ concept to give the same weight to each model. The results show robust signals in the rainfall response, i.e., increasing (decreasing) amounts in central (western) Sahel associated with specific changes in atmospheric dynamics. The…

Atmospheric ScienceCoupled model intercomparison projectEffects of global warmingGeneral Circulation ModelClimatologyEnvironmental scienceClimate changePrecipitationMonsoonAfrican easterly jetEarth rainfall climatologyInternational Journal of Climatology
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Investigation of the mixing layer height derived from ceilometer measurements in the Kathmandu Valley and implications for local air quality

2017

Abstract. In this study 1 year of ceilometer measurements taken in the Kathmandu Valley, Nepal, in the framework of the SusKat project (A Sustainable Atmosphere for the Kathmandu Valley) were analysed to investigate the diurnal variation of the mixing layer height (MLH) and its dependency on the meteorological conditions. In addition, the impact of the MLH on the temporal variation and the magnitude of the measured black carbon concentrations are analysed for each season. Based on the assumption that black carbon aerosols are vertically well mixed within the mixing layer and the finding that the mixing layer varies only little during night time and morning hours, black carbon emission fluxe…

Atmospheric ScienceDaytime010504 meteorology & atmospheric sciencesDiurnal temperature variationSusKat010501 environmental sciencesMonsoonblack carbon01 natural sciencesCeilometerlcsh:QC1-999boundary layer heightlcsh:ChemistryAtmosphereKathmandulcsh:QD1-999Diurnal cycleClimatologyErdsystem-ModellierungOutgoing longwave radiationEnvironmental sciencemeasurementslcsh:Physics0105 earth and related environmental sciencesMorning
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