Search results for "Wave"

showing 10 items of 6009 documents

On the Angola low interannual variability and its role in modulating ENSO effects in southern Africa

2019

Abstract The Angola low is a summertime low pressure system that affects the convergence of low-level moisture fluxes into southern Africa. Interannual variations of the Angola low reduce the seasonal prediction skills for this region that arise from coupled atmosphere–ocean variability. Despite its importance, the interannual dynamics of the Angola low, and its relationship with El Niño–Southern Oscillation (ENSO) and other coupled modes of variability, are still poorly understood, mostly because of the scarcity of atmospheric data and short-term duration of atmospheric reanalyses in the region. To bypass this issue, we use a long-term (3500 year) run from a 50-km-resolution global coupled…

Atmospheric Science010504 meteorology & atmospheric sciencesMoistureTeleconnection010502 geochemistry & geophysics01 natural sciencesStationary waveLow-pressure areaStationary wavesSeasonal forecastingInterannual variabilityEl Niño Southern Oscillation[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionTeleconnectionsClimatologySeasonal forecastingAfricaEnvironmental scienceENSO0105 earth and related environmental sciencesTeleconnection
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2017

Abstract. Microphysical and radiation measurements were collected with the novel AIRcraft TOwed Sensor Shuttle (AIRTOSS) – Learjet tandem platform. The platform is a combination of an instrumented Learjet 35A research aircraft and an aerodynamic bird, which is detached from and retracted back to the aircraft during flight via a steel wire with a length of 4000 m. Both platforms are equipped with radiative, cloud microphysical, trace gas, and meteorological instruments. The purpose of the development of this tandem set-up is to study the inhomogeneity of cirrus as well as other stratiform clouds. Sophisticated numerical flow simulations were conducted in order to optimally integrate an axial…

Atmospheric Science010504 meteorology & atmospheric sciencesParticle number010505 oceanographyIrradianceAtmospheric sciences01 natural sciencesTrace gasWavelengthMiddle latitudesRadiative transferEnvironmental scienceOutflowCirrus0105 earth and related environmental sciencesRemote sensingAtmospheric Measurement Techniques
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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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Aviation Contrail Cirrus and Radiative Forcing Over Europe During 6 Months of COVID‐19

2021

Abstract The COVID‐19 pandemic led to a 72% reduction of air traffic over Europe in March–August 2020 compared to 2019. Modeled contrail cover declined similarly, and computed mean instantaneous radiative contrail forcing dropped regionally by up to 0.7 W m−2. Here, model predictions of cirrus optical thickness and the top‐of‐atmosphere outgoing longwave and reflected shortwave irradiances are tested by comparison to Meteosat‐SEVIRI‐derived data. The agreement between observations and modeled data is slightly better when modeled contrail cirrus contributions are included. The spatial distributions and diurnal cycles of the differences in these data between 2019 and 2020 are partially caused…

Atmospheric Science010504 meteorology & atmospheric sciencesPollution: Urban Regional and GlobalcirrusForcing (mathematics)Atmospheric Composition and Structure010502 geochemistry & geophysicsAtmospheric sciencesBiogeosciences01 natural sciencesOceanography: Biological and ChemicalCloud/Radiation InteractionRadiative transferWolkenphysikInstitut für Physik der AtmosphäreMarine PollutioncontrailOceanography: GeneralGeophysicsPollution: Urban and RegionalAtmospheric ProcessesCirrusClouds and AerosolssatelliteMegacities and Urban Environmentcontrail aircraft climate observation model traffic Meteosat CoCiPRadiation: Transmission and ScatteringAtmospherePaleoceanographyEvolution of the EarthCOVID‐19Research LetterGlobal ChangeBiosphere/Atmosphere InteractionsUrban Systems0105 earth and related environmental sciencesEvolution of the AtmosphereAerosolsradiative forcingVerkehrsmeteorologieAtmosphereLongwaveAtmosphärische SpurenstoffeRadiative forcingAerosols and ParticlesNumerical weather predictionTectonophysicsaviationGeneral Earth and Planetary SciencesEnvironmental scienceShortwaveNatural HazardsGeophysical Research Letters
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A Phase Locking Perspective on Rossby Wave Amplification and Atmospheric Blocking Downstream of Recurving Western North Pacific Tropical Cyclones

2019

Abstract The extratropical transition (ET) of tropical cyclones (TCs) can significantly influence the evolution of the midlatitude flow. However, the interaction between recurving TCs and upstream upper-level troughs features a large and partly unexplained case-to-case variability. In this study, a synoptic, feature-based climatology of TC–trough interactions is constructed to discriminate recurving TCs that interact with decelerating and accelerating troughs. Upper-level troughs reducing their eastward propagation speed during the interaction with recurving TCs exhibit phase locking with lower-level temperature anomalies and are linked to pronounced downstream Rossby wave amplification. Co…

Atmospheric Science010504 meteorology & atmospheric sciencesPotential vorticityMiddle latitudesClimatologyRossby waveExtratropical cycloneTropical cyclone010502 geochemistry & geophysics01 natural sciencesPhase lockingGeology0105 earth and related environmental sciencesMonthly Weather Review
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Mountain waves modulate the water vapor distribution in the UTLS

2017

Abstract. The water vapor distribution in the upper troposphere–lower stratosphere (UTLS) region has a strong impact on the atmospheric radiation budget. Transport and mixing processes on different scales mainly determine the water vapor concentration in the UTLS. Here, we investigate the effect of mountain waves on the vertical transport and mixing of water vapor. For this purpose we analyze measurements of water vapor and meteorological parameters recorded by the DLR Falcon and NSF/NCAR Gulfstream V research aircraft taken during the Deep Propagating Gravity Wave Experiment (DEEPWAVE) in New Zealand. By combining different methods, we develop a new approach to quantify location, direction…

Atmospheric Science010504 meteorology & atmospheric sciencesTransportmountain wavesAtmospheric sciences01 natural sciences010305 fluids & plasmaslcsh:ChemistryTroposphere0103 physical sciencesUTLSGravity waveWolkenphysikDropsondeStratosphere0105 earth and related environmental sciencesVerkehrsmeteorologieRadiative forcinglcsh:QC1-999water vapourWavelengthlcsh:QD1-999ClimatologyEnvironmental scienceTropopauselcsh:PhysicsWater vapor
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Dynamics of Rossby Wave Packets in a Quantitative Potential Vorticity–Potential Temperature Framework

2016

Abstract Rossby wave packets (RWPs) have been associated with increased atmospheric predictability but also with the growth and propagation of forecast uncertainty. To address the important question of under which conditions RWPs imply high and low predictability, a potential vorticity–potential temperature (PV–θ) framework is introduced to diagnose RWP dynamics. Finite-amplitude RWPs along the midlatitude waveguide are considered and are represented by the synoptic-scale, wavelike undulations of the tropopause. The evolution of RWPs is examined by the amplitude evolution of the individual troughs and ridges. Troughs and ridges are identified as PV anomalies on θ levels intersecting the mid…

Atmospheric Science010504 meteorology & atmospheric sciencesWave packet0208 environmental biotechnologyDiabaticRossby wave02 engineering and technologyGeophysicsAtmospheric sciences01 natural sciences020801 environmental engineeringAmplitudePotential vorticityPotential temperatureTropopausePredictabilityGeology0105 earth and related environmental sciencesJournal of the Atmospheric Sciences
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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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Regionalizing Rainfall at Very High Resolution over La Réunion Island: A Case Study for Tropical Cyclone Ando

2016

AbstractEnsemble simulations of Tropical Cyclone (TC) Ando (31 December 2000–9 January 2001) are performed over the southwest Indian Ocean using the nonhydrostatic WRF Model. Nested domains centered over the island of La Réunion allow for the simulation of local rainfall amounts associated with TC Ando at very high resolution (680-m grid spacing). The model is forced by and nudged toward ERA-Interim during the first (1–6) day(s) of the TC’s life cycle. The nudging ends at various dates to constrain either the whole life cycle or only parts of it.As expected, results show weakened member dispersion, as the relaxation lasts longer, with more members producing similar cyclone tracks and intens…

Atmospheric Science010504 meteorology & atmospheric sciences[ SDU.STU.ME ] Sciences of the Universe [physics]/Earth Sciences/MeteorologyRegional modelsTerrain[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology010502 geochemistry & geophysics01 natural sciencesWind speed[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionTropical cyclonesClimatologyWeather Research and Forecasting ModelCyclonePrecipitation[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyTropical cycloneDispersion (water waves)Tropical cyclone rainfall forecastingIndian OceanGeology0105 earth and related environmental sciencesMonthly Weather Review
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Observed versus simulated mountain waves over Scandinavia – improvement of vertical winds, energy and momentum fluxes by enhanced model resolut…

2017

Abstract. Two mountain wave events, which occurred over northern Scandinavia in December 2013 are analysed by means of airborne observations and global and mesoscale numerical simulations with horizontal mesh sizes of 16, 7.2, 2.4 and 0.8 km. During both events westerly cross-mountain flow induced upward-propagating mountain waves with different wave characteristics due to differing atmospheric background conditions. While wave breaking occurred at altitudes between 25 and 30 km during the first event due to weak stratospheric winds, waves propagated to altitudes above 30 km and interfacial waves formed in the troposphere at a stratospheric intrusion layer during the second event. Global an…

Atmospheric Science010504 meteorology & atmospheric sciencesairborne observationsFlow (psychology)Mesoscale meteorologygravity waves010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPhysics::GeophysicsTropospherelcsh:ChemistryGW-LCYCLE IPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesMomentum (technical analysis)Institut für Physik der AtmosphäreLidarTurbulent diffusionVerkehrsmeteorologieBreaking wavelcsh:QC1-999WavelengthAmplitudenumerical modelinglcsh:QD1-999Geologylcsh:PhysicsAtmospheric Chemistry and Physics
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