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  • 2015-2019  (88)
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  • 1
    Schlagwort(e): Forschungsbericht ; Mittlere Atmosphäre ; Meer ; Spurengas ; Aerosol
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (31 Seiten, 1,92 MB) , Illustrationen, Diagramme
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMBF 01LG1217A-B. - Verbund-Nummer 01140205 , Weitere Autoren dem Berichtsblatt entnommen. - Weitere durchführende Institution ist laut Berichtsblatt: KIT - Karlsruher Institut für Technologie , Sprache der Zusammenfassung: Deutsch, Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Fiehn, Alina; Quack, Birgit; Hepach, Helmke; Fuhlbrügge, Steffen; Tegtmeier, Susann; Toohey, Matthew; Atlas, Elliot L; Krüger, Kirstin (2017): Delivery of halogenated very short-lived substances from the west Indian Ocean to the stratosphere during the Asian summer monsoon. Atmospheric Chemistry and Physics, 17(11), 6723-6741, https://doi.org/10.5194/acp-17-6723-2017
    Publikationsdatum: 2023-01-13
    Beschreibung: During two cruises wiht RV Sonne, SO234-2 from 8 to 19 July 2014 (Durban, South Africa to Port Louis, Mauritius) and SO235 from 23 July to 7 August 2014 (Port Louis, Mauritius to Malé, Maldives), within the SPACES (Science Partnerships for the Assessment of Complex Earth System Processes) and OASIS (Organic very short-lived Substances and their air sea exchange from the Indian Ocean to the Stratosphere) research projects, surface water samples were sampled from a continuous running pump in the hydrographic shaft of RV Sonne at a depth of 5 m. Deep water samples were taken from a Niskin-bottle rosette sampler. The samples were then analyzed for halogenated compounds using a purge and trap system onboard, which was attached to a gas chromatograph with an electron capture detector for surface water samples and a GC/MS Agilent 5975 for the deep water samples. An analytical reproducibility of 10% was determined from measuring duplicate water samples, detection limit was 0.2 pmol /L. Calibration was performed with several dilutions of a mixed-compound standard prepared in methanol.
    Materialart: Dataset
    Format: application/zip, 97 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Hepach, Helmke; Quack, Birgit; Tegtmeier, Susann; Engel, Anja; Bracher, Astrid; Fuhlbrügge, Steffen; Galgani, Luisa; Atlas, Elliot L; Lampel, Johannes; Frieß, Udo; Krüger, Kirstin (2016): Biogenic halocarbons from the Peruvian upwelling region as tropospheric halogen source. Atmospheric Chemistry and Physics, 16(18), 12219-12237, https://doi.org/10.5194/acp-16-12219-2016
    Publikationsdatum: 2024-02-01
    Beschreibung: Halocarbons, halogenated short-chained hydrocarbons, are produced naturally in the oceans by biological and chemical processes. They are emitted from surface seawater into the atmosphere, where they take part in numerous chemical processes such as ozone destruction and the oxidation of mercury and dimethyl sulfide. Here we present oceanic and atmospheric halocarbon data for the Peruvian upwelling obtained during the M91 cruise onboard the research vessel Meteor in December 2012. Surface waters during the cruise were characterized by moderate concentrations of bromoform (CHBr3) and dibromomethane (CH2Br2) correlating with diatom biomass derived from marker pigment concentrations, which suggests this phytoplankton group as likely source. Concentrations measured for the iodinated compounds methyl iodide (CH3I) of up to 35.4 pmol L-1, chloroiodomethane (CH2ClI) of up to 58.1 pmol L-1 and diiodomethane (CH2I2) of up to 32.4 pmol L-1 in water samples were much higher than previously reported for the tropical Atlantic upwelling systems. Iodocarbons also correlated with the diatom biomass and even more significantly with dissolved organic matter (DOM) components measured in the surface water. Our results suggest a biological source of these compounds as significant driving factor for the observed large iodocarbon concentrations. Elevated atmospheric mixing ratios of CH3I (up to 3.2 ppt), CH2ClI (up to 2.5 ppt) and CH2I2 (3.3 ppt) above the upwelling were correlated with seawater concentrations and high sea-to-air fluxes. The enhanced iodocarbon production in the Peruvian upwelling contributed significantly to tropospheric iodine levels.
    Schlagwort(e): SOPRAN; Surface Ocean Processes in the Anthropocene
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-02-01
    Schlagwort(e): Bromoiodomethane; Chloroiodomethane; CT; DATE/TIME; DEPTH, water; Dibromochloromethane; Dibromomethane; Diiodomethane; Iodomethane; LATITUDE; LONGITUDE; M91; M91-track; Meteor (1986); SOPRAN; South Pacific Ocean; Surface Ocean Processes in the Anthropocene; Tetrachloromethane; Tribromomethane; Trichloroethane; Trichloromethane; Underway cruise track measurements
    Materialart: Dataset
    Format: text/tab-separated-values, 658 data points
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  • 5
    Publikationsdatum: 2024-02-01
    Schlagwort(e): Bottle number; Bromoiodomethane; Chloroiodomethane; CTD/Rosette; CTD-033; CTD-035; CTD-036; CTD-038; CTD-039; CTD-041; CTD-043; CTD-046; CTD-048; CTD-049; CTD-051; CTD-052; CTD-055; CTD-058; CTD-059; CTD-060; CTD-061; CTD-064; CTD-065; CTD-074; CTD-075; CTD-080; CTD-083; CTD-087; CTD-088; CTD-089; CTD-090; CTD-092; CTD-093; CTD-094; CTD-095; CTD-096; CTD-097; CTD-RO; DATE/TIME; DEPTH, water; Dibromochloromethane; Dibromomethane; Diiodomethane; Event label; Iodomethane; Latitude of event; Longitude of event; M91; M91_1736-1; M91_1737-1; M91_1737-3; M91_1739-1; M91_1739-3; M91_1741-1; M91_1743-1; M91_1746-1; M91_1748-1; M91_1749-1; M91_1751-1; M91_1751-3; M91_1752-8; M91_1754-1; M91_1755-2; M91_1755-4; M91_1756-1; M91_1759-1; M91_1760-1; M91_1766-1; M91_1766-3; M91_1769-1; M91_1771-1; M91_1774-1; M91_1774-3; M91_1775-1; M91_1775-3; M91_1776-3; M91_1777-1; M91_1777-12; M91_1777-4; M91_1777-7; M91_1778-1; Meteor (1986); Optional event label; Sample code/label; SOPRAN; South Pacific Ocean; Surface Ocean Processes in the Anthropocene; Tetrachloromethane; Tribromomethane; Trichloroethane; Trichloromethane
    Materialart: Dataset
    Format: text/tab-separated-values, 1919 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2024-04-02
    Schlagwort(e): 19-Butanoyloxyfucoxanthin; 19-Hexanoyloxyfucoxanthin; Alloxanthin; alpha-Carotene, beta,epsilon-Carotene; Antheraxanthin; Astaxanthin; beta-Carotene, beta,beta-Carotene; Chlorophyll a; Chlorophyll b; Chlorophyll c1+c2; Chlorophyll c3; CT; CTD/Rosette; CTD-002; CTD-003; CTD-010; CTD-013; CTD-017; CTD-019; CTD-021; CTD-024; CTD-026; CTD-028; CTD-030; CTD-034; CTD-035; CTD-036; CTD-039; CTD-041; CTD-043; CTD-044; CTD-045; CTD-046; CTD-047; CTD-048; CTD-049; CTD-050; CTD-052; CTD-055; CTD-058; CTD-060; CTD-061; CTD-064; CTD-065; CTD-067; CTD-068; CTD-071; CTD-073; CTD-075; CTD-080; CTD-082; CTD-083; CTD-088; CTD-090; CTD-094; CTD-095; CTD-096; CTD-097; CTD-RO; DATE/TIME; DEPTH, water; Diadinoxanthin; Diatoxanthin; Dinoxanthin; Divinyl chlorophyll a; Divinyl chlorophyll b; Event label; Fucoxanthin; Gear; High Performance Liquid Chromatography (HPLC); LATITUDE; LONGITUDE; Lutein; M91; M91_1713-1; M91_1713-3; M91_1719-1; M91_1721-3; M91_1724-3; M91_1725-3; M91_1727-1; M91_1729-1; M91_1731-1; M91_1733-1; M91_1733-13; M91_1736-3; M91_1737-1; M91_1737-3; M91_1739-3; M91_1741-1; M91_1743-1; M91_1744-1; M91_1745-1; M91_1746-1; M91_1747-1; M91_1748-1; M91_1749-1; M91_1750-1; M91_1751-3; M91_1752-8; M91_1754-1; M91_1755-4; M91_1756-1; M91_1759-1; M91_1760-1; M91_1762-2; M91_1763-1; M91_1764-8; M91_1765-1; M91_1766-3; M91_1769-1; M91_1770-4; M91_1771-1; M91_1774-3; M91_1775-3; M91_1777-12; M91_1777-4; M91_1777-7; M91_1778-1; M91-track; Meteor (1986); Mg-2,4-divinyl pheoporphyrin a5 monomethyl ester; Neoxanthin; Peridinin; Phaeophorbide a; Pheophytin a; Pheophytin b; Pyropheophorbide a; Pyropheophytin a; Sample code/label; South Pacific Ocean; Underway cruise track measurements; Violaxanthin; Zeaxanthin
    Materialart: Dataset
    Format: text/tab-separated-values, 7378 data points
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  • 7
    Publikationsdatum: 2020-02-06
    Beschreibung: Reanalysis data sets are widely used to understand atmospheric processes and past variability, and are often used to stand in as "observations" for comparisons with climate model output. Because of the central role of water vapor (WV) and ozone (O3) in climate change, it is important to understand how accurately and consistently these species are represented in existing global reanalyses. In this paper, we present the results of WV and O3 intercomparisons that have been performed as part of the SPARC (Stratosphere–troposphere Processes and their Role in Climate) Reanalysis Intercomparison Project (S-RIP). The comparisons cover a range of timescales and evaluate both inter-reanalysis and observation-reanalysis differences. We also provide a systematic documentation of the treatment of WV and O3 in current reanalyses to aid future research and guide the interpretation of differences amongst reanalysis fields. The assimilation of total column ozone (TCO) observations in newer reanalyses results in realistic representations of TCO in reanalyses except when data coverage is lacking, such as during polar night. The vertical distribution of ozone is also relatively well represented in the stratosphere in reanalyses, particularly given the relatively weak constraints on ozone vertical structure provided by most assimilated observations and the simplistic representations of ozone photochemical processes in most of the reanalysis forecast models. However, significant biases in the vertical distribution of ozone are found in the upper troposphere and lower stratosphere in all reanalyses. In contrast to O3, reanalysis estimates of stratospheric WV are not directly constrained by assimilated data. Observations of atmospheric humidity are typically used only in the troposphere, below a specified vertical level at or near the tropopause. The fidelity of reanalysis stratospheric WV products is therefore mainly dependent on the reanalyses' representation of the physical drivers that influence stratospheric WV, such as temperatures in the tropical tropopause layer, methane oxidation, and the stratospheric overturning circulation. The lack of assimilated observations and known deficiencies in the representation of stratospheric transport in reanalyses result in much poorer agreement amongst observational and reanalysis estimates of stratospheric WV. Hence, stratospheric WV products from the current generation of reanalyses should generally not be used in scientific studies.
    Materialart: Article , PeerReviewed
    Format: text
    Format: text
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  • 8
    Publikationsdatum: 2020-10-20
    Beschreibung: A quality assessment of the CFC-11 (CCl3F), CFC-12 (CCl2F2), HF, and SF6 products from limb-viewing satellite instruments is provided by means of a detailed intercomparison. The climatologies in the form of monthly zonal mean time series are obtained from HALOE, MIPAS, ACE-FTS, and HIRDLS within the time period 1991–2010. The intercomparisons focus on the mean biases of the monthly and annual zonal mean fields and aim to identify their vertical, latitudinal and temporal structure. The CFC evaluations (based on MIPAS, ACE-FTS and HIRDLS) reveal that the uncertainty in our knowledge of the atmospheric CFC-11 and CFC-12 mean state, as given by satellite data sets, is smallest in the tropics and mid-latitudes at altitudes below 50 and 20 hPa, respectively, with a 1σ multi-instrument spread of up to ±5 %. For HF, the situation is reversed. The two available data sets (HALOE and ACE-FTS) agree well above 100 hPa, with a spread in this region of ±5 to ±10 %, while at altitudes below 100 hPa the HF annual mean state is less well known, with a spread ±30 % and larger. The atmospheric SF6 annual mean states derived from two satellite data sets (MIPAS and ACE-FTS) show only very small differences with a spread of less than ±5 % and often below ±2.5 %. While the overall agreement among the climatological data sets is very good for large parts of the upper troposphere and lower stratosphere (CFCs, SF6) or middle stratosphere (HF), individual discrepancies have been identified. Pronounced deviations between the instrument climatologies exist for particular atmospheric regions which differ from gas to gas. Notable features are differently shaped isopleths in the subtropics, deviations in the vertical gradients in the lower stratosphere and in the meridional gradients in the upper troposphere, and inconsistencies in the seasonal cycle. Additionally, long-term drifts between the instruments have been identified for the CFC-11 and CFC-12 time series. The evaluations as a whole provide guidance on what data sets are the most reliable for applications such as studies of atmospheric transport and variability, model–measurement comparisons and detection of long-term trends. The data sets will be publicly available from the SPARC Data Centre and through PANGAEA (doi:10.1594/PANGAEA.849223).
    Materialart: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
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  • 9
    Publikationsdatum: 2019-02-01
    Beschreibung: The first concerted multi-model intercomparison of halogenated very short-lived substances (VSLS) has been performed, within the framework of the ongoing Atmospheric Tracer Transport Model Intercomparison Project (TransCom). Eleven global models or model variants participated, simulating the major natural bromine VSLS, bromoform (CHBr3) and dibromomethane (CH2Br2), over a 20-year period (1993-2012). The overarching goal of TransCom-VSLS was to provide a reconciled model estimate of the stratospheric source gas injection (SGI) of bromine from these gases, to constrain the current measurement-derived range, and to investigate inter-model differences due to emissions and transport processes.Models ran with standardised idealised chemistry, to isolate differences due to transport, and we investigated the sensitivity of results to a range of VSLS emission inventories. Models were tested in their ability to reproduce the observed seasonal and spatial distribution of VSLS at the surface, using measurements from NOAA’s long-term global monitoring network, and in the tropical troposphere, using recent aircraft measurements - including high altitude observations from the NASA Global Hawk platform. The models generally capture the seasonal cycle of surface CHBr3 and CH2Br2 well, with a strong model-measurement correlation (r ≥ 0.7) and a low sensitivity to the choice of emission inventory, at most sites. In a given model, the absolute model-measurement agreement is highly sensitive to the choice of emissions and inter-model differences are also apparent, even when using the same inventory, highlighting the challenges faced in evaluating such inventories at the global scale. Across the ensemble, most consistency is found within the tropics where most of the models (8 out of 11) achieve optimal agreement to surface CHBr3 observations using the lowest of the three CHBr3 emission inventories tested (similarly, 8 out of 11 models for CH2 Br2). In general, the models are able to reproduce well observations of CHBr3 and CH2 Br2 obtained in the tropical tropopause layer (TTL) at various locations throughout the Pacific. Zonal variability in VSLS loading in the TTL is generally consistent among models, with CHBr3 (and to a lesser extent CH2 Br2) most elevated over the tropical West Pacific during boreal winter. The models also indicate the Asian Monsoon during boreal summer to be an important pathway for VSLS reaching the stratosphere, though the strength of this signal varies considerably among models. We derive an ensemble climatological mean estimate of the stratospheric bromine SGI from CHBr3 and CH2 Br2 of 2.0 (1.2-2.5) ppt, ≫ 57% larger than the best estimate from the most recent World Meteorological Organization (WMO) Ozone Assessment Report. We find no evidence for a long-term, transport-driven trend in the stratospheric SGI of bromine over the simulation period. However, transport-driven inter-annual variability in the annual mean bromine SGI is of the order of a ±5%, with SGI exhibiting a strong positive correlation with ENSO in the East Pacific.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Publikationsdatum: 2019-09-23
    Beschreibung: Halocarbons are produced naturally in the oceans by biological and chemical processes. They are emitted from surface seawater into the atmosphere, where they take part in numerous chemical processes such as ozone destruction and the oxidation of mercury and dimethyl sulfide. Here we present oceanic and atmospheric halocarbon data for the Peruvian upwelling zone obtained during the M91 cruise onboard the research vessel METEOR in December 2012. Surface waters during the cruise were characterized by moderate concentrations of bromoform (CHBr3) and dibromomethane (CH2Br2) correlating with diatom biomass derived from marker pigment concentrations, which suggests this phytoplankton group is a likely source. Concentrations measured for the iodinated compounds methyl iodide (CH3I) of up to 35.4 pmol L−1, chloroiodomethane (CH2ClI) of up to 58.1 pmol L−1 and diiodomethane (CH2I2) of up to 32.4 pmol L−1 in water samples were much higher than previously reported for the tropical Atlantic upwelling systems. Iodocarbons also correlated with the diatom biomass and even more significantly with dissolved organic matter (DOM) components measured in the surface water. Our results suggest a biological source of these compounds as a significant driving factor for the observed large iodocarbon concentrations. Elevated atmospheric mixing ratios of CH3I (up to 3.2 ppt), CH2ClI (up to 2.5 ppt) and CH2I2 (3.3 ppt) above the upwelling were correlated with seawater concentrations and high sea-to-air fluxes. During the first part of the cruise, the enhanced iodocarbon production in the Peruvian upwelling contributed significantly to tropospheric iodine levels, while this contribution was considerably smaller during the second part.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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