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  • 1
    Digitale Medien
    Digitale Medien
    Amsterdam : Elsevier
    Solid State Communications 22 (1977), S. 251-255 
    ISSN: 0038-1098
    Quelle: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Thema: Physik
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Digitale Medien
    Digitale Medien
    Amsterdam : Elsevier
    Physica B+C 90 (1977), S. 154-178 
    ISSN: 0378-4363
    Quelle: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Thema: Physik
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2019-07-17
    Beschreibung: Water vapour (H2O) is one of the operationally retrieved key species of the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) instrument aboard the Environmental Satellite (ENVISAT) which was launched into its sun-synchronous orbit on 1 March 2002 and operated until April 2012. Within the MIPAS validation activities, independent observations from balloons, aircraft, satellites, and ground-based stations have been compared to European Space Agency (ESA) version 4.61 operational H2O data comprising the time period from July 2002 until March 2004 where MIPAS measured with full spectral resolution. No significant bias in the MIPAS H2O data is seen in the lower stratosphere (above the hygropause) between about 15 and 30 km. Differences of H2O quantities observed by MIPAS and the validation instruments are mostly well within the combined total errors in this altitude region. In the upper stratosphere (above about 30 km), a tendency towards a small positive bias (up to about 10%) is present in the MIPAS data when compared to its balloon-borne counterpart MIPAS-B, to the satellite instruments HALOE (Halogen Occultation Experiment) and ACE-FTS (Atmospheric Chemistry Experiment, Fourier Transform Spectrometer), and to the millimeter-wave airborne sensor AMSOS (Airborne Microwave Stratospheric Observing System). In the mesosphere the situation is unclear due to the occurrence of different biases when comparing HALOE and ACE-FTS data. Pronounced deviations between MIPAS and the correlative instruments occur in the lowermost stratosphere and upper troposphere, a region where retrievals of H2O are most challenging. Altogether it can be concluded that MIPAS H2O profiles yield valuable information on the vertical distribution of H2O in the stratosphere with an overall accuracy of about 10 to 30% and a precision of typically 5 to 15% – well within the predicted error budget, showing that these global and continuous data are very valuable for scientific studies. However, in the region around the tropopause retrieved MIPAS H2O profiles are less reliable, suffering from a number of obstacles such as retrieval boundary and cloud effects, sharp vertical discontinuities, and frequent horizontal gradients in both temperature and H2O volume mixing ratio (VMR). Some profiles are characterized by retrieval instabilities.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2019-07-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2019-03-26
    Beschreibung: Volcanoes are an important source of aerosols to the troposphere. Within minutes after emission, volcanic plume aerosol catalyses conversion of co-emitted HBr, HCl into highly reactive halogens (e.g. BrO, OClO) through chemical cycles that cause substantial ozone depletion in the dispersing downwind plume. This study quantifies the sub-to-supramicron primary volcanic aerosol emission (0.2–5 lm diameter) and its role in this process. An in-situ ground-based study at Mt Etna (Italy) during passive degassing co-deployed an optical particle counter and Multi-Gas SO2 sensors at high time resolution (0.1 Hz) enabling to characterise the aerosol number, size-distribution and emission flux. A tri-modal volcanic aerosol size distribution was found, to which lognormal distributions are fitted. Total particle volume correlates to SO2 (as a plume tracer). The measured particle volume:SO2 ratio equates to a sulfate:SO2 ratio of 1–2% at the observed meteorological conditions (40% Relative Humidity). A particle mass flux of 0.7 kg s 1 is calculated for the measured Mt Etna SO2 flux of 1950 tonnes/day. A numerical plume atmospheric chemistry model is used to simulate the role of the hygroscopic primary aerosol surface area and its humidity dependence on volcanic plume BrO and OClO chemistry. As well as predicting volcanic BrO formation and O3 depletion, the model achieves OClO/SO2 in broad quantitative agreement with recently reported Mt Etna observations, with a predicted maximum a few minutes downwind. In addition to humidity – that enhances aerosols surface area for halogen cycling – background ozone is predicted to be an important control on OClO/SO2. Dependence of BrO/SO2 on ambient humidity is rather low near-to-source but increases further downwind. The model plume chemistry also exhibits strong across-plume spatial variations between plume edge and centre.
    Beschreibung: Published
    Beschreibung: 74-93
    Beschreibung: 4V. Processi pre-eruttivi
    Beschreibung: 5V. Processi eruttivi e post-eruttivi
    Beschreibung: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Beschreibung: JCR Journal
    Schlagwort(e): 04.08. Volcanology
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2016-11-29
    Beschreibung: Author(s): S. Lepoutre, L. Fouché, A. Boissé, G. Berthet, G. Salomon, A. Aspect, and T. Bourdel We report on the production of K 39 matter-wave bright solitons, i.e., one-dimensional matter waves that propagate without dispersion thanks to attractive interactions. The volume of the soliton is studied as a function of the scattering length through three-body losses, revealing peak densities as h… [Phys. Rev. A 94, 053626] Published Mon Nov 28, 2016
    Schlagwort(e): Matter waves and collective properties of cold atoms and molecules
    Print ISSN: 1050-2947
    Digitale ISSN: 1094-1622
    Thema: Physik
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2023-09-12
    Beschreibung: The Hunga Tonga eruption on January 14〈sup〉th〈/sup〉 and 15〈sup〉th〈/sup〉 2022 injected water, a variety of gases and aerosols into the Upper Troposphere and Lower Stratosphere up to altitude of ~50 km. Space-borne observations show that the eruption had the strongest impact on the stratospheric Aerosol Optical Depth since the Pinatubo eruption in 1991. We performed two measurement campaigns using weather balloons with the Light Optical Aerosol Counter (LOAC, version 1.5) within the fresh (~1 week post eruption, on Reunion island 21°S) and aged (~8 months post eruption, in South Africa 24°S) stratospheric Hunga Tonga plume. Within this talk, I will present aerosol size distribution and typology information based on LOAC in situ measurements, in the context of collocated ground-based aerosol lidar profiles recorded at OPAR (Observatoire de Physique de l'Atmosphère à La Réunion) and global space-borne observations. Plume peak altitudes have decreased by 2-3 km between the two in situ measurement campaigns. LOAC observations point to exclusively small aerosol particles (〈1 µm in diameter) within the fresh stratospheric plume (22-23 km altitude) and a significant increase in particle size for the aged, descended plume (~20 km altitude). This points to freshly nucleated aerosol particles within the fresh plume and growing particles (e.g. coagulation processes) within the aged plume. While satellite observations only identify sulfate particles, LOAC typology information show indications of a small absorbing component for particles 〈 0.5 µm, which potentially points to small fractured sulfur coated ash particles.
    Sprache: Englisch
    Materialart: info:eu-repo/semantics/conferenceObject
    Standort Signatur Einschränkungen Verfügbarkeit
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