0000000000203950

AUTHOR

Harald Sodemann

showing 7 related works from this author

Lagrangian matches between observations from aircraft, lidar and radar in a warm conveyor belt crossing orography

2021

Warm conveyor belts (WCBs) are important airstreams in extratropical cyclones, often leading to the formation of intense precipitation and the amplification of upper-level ridges. This study presents a case study that involves aircraft, lidar and radar observations in a WCB ascending from western Europe towards the Baltic Sea during the Hydrological Cycle in the Mediterranean Experiment (HyMeX) and T-NAWDEX-Falcon in October 2012, a preparatory campaign for the THORPEX North Atlantic Waveguide and Downstream Impact Experiment (T-NAWDEX). Trajectories were used to link different observations along the WCB, that is, to establish so-called Lagrangian matches between observations. To this aim, …

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Lagrangian matches between observations from aircraft, lidar and radar in an orographic warm conveyor belt

2020

Warm conveyor belts (WCBs) are important airstreams in extratropical cyclones, often leading to the formation of intense precipitation and the amplification of upper-level ridges. This study presents a case study that involves aircraft, lidar and radar observations in a WCB ascending from western Europe towards the Baltic Sea during the Hydrological Cycle in the Mediterranean Experiment (HyMeX) and T-NAWDEX-Falcon in October 2012, a preparatory campaign for the THORPEX North Atlantic Waveguide and Downstream Impact Experiment (T-NAWDEX). Trajectories were used to link different observations along the WCB, that is, to establish so-called Lagrangian matches between observations. To this aim, …

warm conveyor beltLidar010504 meteorology & atmospheric sciencesAtmosphärische SpurenstoffeOrographyInflowtracer01 natural sciencesFalconTroposphereobservationsClimatologyExtratropical cycloneOutflowPrecipitationWater cycleWolkenphysikGeology0105 earth and related environmental sciencesOrographic lift
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Advances in understanding mineral dust and boundary layer processes over the Sahara from Fennec aircraft observations

2015

Abstract. The Fennec climate programme aims to improve understanding of the Saharan climate system through a synergy of observations and modelling. We present a description of the Fennec airborne observations during 2011 and 2012 over the remote Sahara (Mauritania and Mali) and the advances in the understanding of mineral dust and boundary layer processes they have provided. Aircraft instrumentation aboard the UK FAAM BAe146 and French SAFIRE (Service des Avions Français Instrumentés pour la Recherche en Environnement) Falcon 20 is described, with specific focus on instrumentation specially developed for and relevant to Saharan meteorology and dust. Flight locations, aims and associated met…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layerCONVECTIVE SYSTEMEnvironmental Sciences & EcologyAEROSOL OPTICAL-PROPERTIESMineral dust010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesCOARSE MODElcsh:ChemistryHaboobDust storm0201 Astronomical and Space SciencesMeteorology & Atmospheric SciencesSatellite imagerySOUTHERN MOROCCO0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]GBScience & TechnologyHEAT LOWAIRBORNE OBSERVATIONSRETRIEVAL PRODUCTSOzone depletionlcsh:QC1-999PARTICLE-SIZEAERONETBoundary layerlcsh:QD1-99913. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPhysical SciencesWEST-AFRICAN MONSOONEnvironmental science0401 Atmospheric SciencesNORTH-ATLANTIC OCEANLife Sciences & Biomedicinelcsh:PhysicsEnvironmental SciencesAtmospheric Chemistry and Physics
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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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Sources of water vapour contributing to the Elbe flood in August 2002-A tagging study in a mesoscale model

2009

In this study we investigate the contribution of various moisture sources to the Elbe flood that occurred in Central Europe during August 2002. An 8-day simulation with the mesoscale numerical weather prediction model CHRM, including newly implemented water vapour tracers, has been performed. According to the simulation, rather than drawing moisture from one single dominant source region, water vapour from widely separated moisture sources contributed to the extreme precipitation in the most affected area, notably at distinct, subsequent periods of time, and each in significant amounts. These moisture sources include the Atlantic and Mediterranean ocean areas inside the model domain, evapot…

Atmospheric ScienceMoistureMeteorologyAdvectionEvapotranspirationMesoscale meteorologyCycloneEnvironmental scienceMoisture advectionPrecipitationAtmospheric sciencesNumerical weather predictionQuarterly Journal of the Royal Meteorological Society
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Interannual variability of Greenland winter precipitation sources: Lagrangian moisture diagnostic and North Atlantic Oscillation influence

2008

[1] We present a new Lagrangian diagnostic for identifying the sources of water vapor for precipitation. Unlike previous studies, the method allows for a quantitative demarcation of evaporative moisture sources. This is achieved by taking into account the temporal sequence of evaporation into and precipitation from an air parcel during transport, as well as information on its proximity to the boundary layer. The moisture source region diagnostic was applied to trace the origin of water vapor for winter precipitation over the Greenland ice sheet for 30 selected months with pronounced positive, negative, and neutral North Atlantic Oscillation (NAO) index, using the European Centre for Medium-…

Atmospheric ScienceAtlantic hurricaneEcologybiologyMoistureAdvectionPaleontologySoil ScienceGreenland ice sheetForestryAquatic ScienceOceanographybiology.organism_classificationGeophysicsIce coreSpace and Planetary ScienceGeochemistry and PetrologyNorth Atlantic oscillationClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceGroenlandiaPrecipitationEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Interannual variability of Greenland winter precipitation sources: 2. Effects of North Atlantic Oscillation variability on stable isotopes in precipi…

2008

[1] A new Lagrangian moisture source diagnostic is applied to identify the atmospheric conditions relevant for the fractionation of stable water isotopes during evaporation over the ocean and subsequent transport to Greenland. Northern Hemisphere winter months with positive and negative North Atlantic Oscillation (NAO) index are studied on the basis of ERA-40 reanalysis data. Diagnosed moisture transport conditions are supplied to a Rayleigh-type isotope fractionation model to derive estimates for the isotopic composition of stable isotopes in winter precipitation on the Greenland plateau for the two NAO phases. Because of changes in atmospheric circulation, moisture source locations for pr…

Atmospheric Science010504 meteorology & atmospheric sciencesδ18O0207 environmental engineeringSoil ScienceGreenland ice sheet02 engineering and technologyAquatic ScienceOceanography01 natural sciencesIsotope fractionationIce coreGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)020701 environmental engineering[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereEcologyStable isotope ratioNorthern HemispherePaleontologyForestrySea surface temperatureGeophysics13. Climate actionSpace and Planetary ScienceNorth Atlantic oscillationClimatologyEnvironmental science
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