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  • 1
    Beschreibung / Inhaltsverzeichnis: Die wissenschaftliche Flugzeugmesskampagne MELTEX (Einfluss von Schmelztümpeln auf Energie- und Impulsflüsse zwischen Atmosphäre und Meereis) war ein gemeinsames Projekt des Alfred-Wegener-Instituts für Polar- und Meeresforschung (AWI), des Instituts für Atmosphärenphysik (IPA) der Universität Mainz und von Environment Canada (EC). Sie stellt einen Beitrag zum EU-Projekt DAMOCLES und zum internationalen Polarjahr 2007/2008 dar. Schmelztümpel an der Oberfläche arktischen Meereises bilden sich gewöhnlich von Ende Mai bis Ende August. Sie haben einen starken Einfluss auf den Energieaustausch zwischen Atmosphäre, Meereis und Ozean. Der bedeutendste Effekt ist die Erhöhung der Absorption von Solarstrahlung auf Grund ihrer erheblich niedrigeren Albedo gegenüber der des umgebenden Schnees/Eises. Das Ziel des Projektes MELTEX ist eine Verbesserung des quantitativen Verständnisses des Einflusses von Schmelztümpeln auf Strahlungs-, Wärme-, Feuchte- sowie Impulsflüsse über arktischem Meereis. Insbesondere in der Phase der Schmelzsaison, in der Schmelztümpel anfangen, sich zu bilden, wird die zeitliche Entwicklung des Schmelztümpelbedeckungsgrades und der Albedo in Meereis- und Klimamodellen nur sehr grob erfasst. Deshalb fand die Kampagne im Spätfrühling/Frühsommer statt. Vom 09.Mai bis 08.Juni 2008 operierten wir in der kanadischen Arktis, hauptsächlich über der südlichen Beaufort See mit Inuvik als Basis für POLAR 5. Für einen Messflug über rauhem mehrjährigen Eis nördlich von Ellesmere Island wurde POLAR 5 vom 22.bis 24.Mai 2008 nach Eureka überführt. Insgesamt wurden 12 Messflüge durchgeführt.
    Materialart: Online-Ressource
    Seiten: Online-Ressource
    Serie: Berichte zur Polar- und Meeresforschung 593
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2018-08-13
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
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  • 3
    Publikationsdatum: 2019-06-17
    Beschreibung: Clouds play an important role in Arctic amplification. This term represents the recently observed enhanced warming of the Arctic relative to the global increase of near-surface air temperature. However, there are still important knowledge gaps regarding the interplay between Arctic clouds and aerosol particles, and surface properties, as well as turbulent and radiative fluxes that inhibit accurate model simulations of clouds in the Arctic climate system. In an attempt to resolve this so-called Arctic cloud puzzle, two comprehensive and closely coordinated field studies were conducted: the Arctic Cloud Observations Using Airborne Measurements during Polar Day (ACLOUD) aircraft campaign and the Physical Feedbacks of Arctic Boundary Layer, Sea Ice, Cloud and Aerosol (PASCAL) ice breaker expedition. Both observational studies were performed in the framework of the German Arctic Amplification: Climate Relevant Atmospheric and Surface Processes, and Feedback Mechanisms (AC)3 project. They took place in the vicinity of Svalbard, Norway, in May and June 2017. ACLOUD and PASCAL explored four pieces of the Arctic cloud puzzle: cloud properties, aerosol impact on clouds, atmospheric radiation, and turbulent dynamical processes. The two instrumented Polar 5 and Polar 6 aircraft; the icebreaker Research Vessel (R/V) Polarstern; an ice floe camp including an instrumented tethered balloon; and the permanent ground-based measurement station at Ny-Ålesund, Svalbard, were employed to observe Arctic low- and mid-level mixed-phase clouds and to investigate related atmospheric and surface processes. The Polar 5 aircraft served as a remote sensing observatory examining the clouds from above by downward-looking sensors; the Polar 6 aircraft operated as a flying in situ measurement laboratory sampling inside and below the clouds. Most of the collocated Polar 5/6 flights were conducted either above the R/V Polarstern or over the Ny-Ålesund station, both of which monitored the clouds from below using similar but upward-looking remote sensing techniques as the Polar 5 aircraft. Several of the flights were carried out underneath collocated satellite tracks. The paper motivates the scientific objectives of the ACLOUD/PASCAL observations and describes the measured quantities, retrieved parameters, and the applied complementary instrumentation. Furthermore, it discusses selected measurement results and poses critical research questions to be answered in future papers analyzing the data from the two field campaigns.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
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  • 4
    Publikationsdatum: 2020-11-16
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
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  • 5
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    Alfred Wegener Institute for Polar and Marine Research
    In:  EPIC3Berichte zur Polar- und Meeresforschung = Reports on polar and marine research, Bremerhaven, Alfred Wegener Institute for Polar and Marine Research, 754, 99 p., ISSN: 1866-3192
    Publikationsdatum: 2021-07-05
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: "Berichte zur Polar- und Meeresforschung" , notRev
    Format: application/pdf
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  • 6
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    Copernicus Publications on behalf of the European Geosciences Union.
    In:  EPIC3Atmos. Chem. Phys.,, Copernicus Publications on behalf of the European Geosciences Union., 20, pp. 8139-8156
    Publikationsdatum: 2020-10-12
    Beschreibung: The magnitude of solar radiative effects (cooling or warming) of black carbon (BC) particles embedded in the Arctic atmosphere and surface snow layer was explored on the basis of case studies. For this purpose, combined at- mospheric and snow radiative transfer simulations were per- formed for cloudless and cloudy conditions on the basis of BC mass concentrations measured in pristine early summer and more polluted early spring conditions. The area of inter- est is the remote sea-ice-covered Arctic Ocean in the vicin- ity of Spitsbergen, northern Greenland, and northern Alaska typically not affected by local pollution. To account for the radiative interactions between the black-carbon-containing snow surface layer and the atmosphere, an atmospheric and snow radiative transfer model were coupled iteratively. For pristine summer conditions (no atmospheric BC, minimum solar zenith angles of 55◦) and a representative BC particle mass concentration of 5 ng g−1 in the surface snow layer, a positive daily mean solar radiative forcing of +0.2Wm−2 was calculated for the surface radiative budget. A higher load of atmospheric BC representing early springtime conditions results in a slightly negative mean radiative forcing at the surface of about −0.05 W m−2, even when the low BC mass concentration measured in the pristine early summer condi- tions was embedded in the surface snow layer. The total net surface radiative forcing combining the effects of BC em- bedded in the atmosphere and in the snow layer strongly de- pends on the snow optical properties (snow specific surface area and snow density). For the conditions over the Arctic Ocean analyzed in the simulations, it was found that the at- mospheric heating rate by water vapor or clouds is 1 to 2 or-ders of magnitude larger than that by atmospheric BC. Sim- ilarly, the daily mean total heating rate (6 K d−1) within a snowpack due to absorption by the ice was more than 1 order of magnitude larger than that of atmospheric BC (0.2 K d−1). Also, it was shown that the cooling by atmospheric BC of the near-surface air and the warming effect by BC embedded in snow are reduced in the presence of clouds.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
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  • 7
    Publikationsdatum: 2021-05-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Format: application/pdf
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  • 8
    Publikationsdatum: 2020-09-14
    Beschreibung: The concept of cloud radiative forcing (CRF)is commonly applied to quantify the impact of clouds onthe surface radiative energy budget (REB). In the Arctic,specific radiative interactions between microphysical andmacrophysical properties of clouds and the surface stronglymodify the warming or cooling effect of clouds, complicat-ing the estimate of CRF obtained from observations or mod-els. Clouds tend to increase the broadband surface albedoover snow or sea ice surfaces compared to cloud-free con-ditions. However, this effect is not adequately consideredin the derivation of CRF in the Arctic so far. Therefore,we have quantified the effects caused by surface-albedo–cloud interactions over highly reflective snow or sea ice sur-faces on the CRF using radiative transfer simulations andbelow-cloud airborne observations above the heterogeneousspringtime marginal sea ice zone (MIZ) during the ArcticCLoud Observations Using airborne measurements duringpolar Day (ACLOUD) campaign. The impact of a modi-fied surface albedo in the presence of clouds, as comparedto cloud-free conditions, and its dependence on cloud opti-cal thickness is found to be relevant for the estimation of theshortwave CRF. A method is proposed to consider this sur-face albedo effect on CRF estimates by continuously retriev-ing the cloud-free surface albedo from observations undercloudy conditions, using an available snow and ice albedoparameterization. Using ACLOUD data reveals that the esti-mated average shortwave cooling by clouds almost doublesover snow- and ice-covered surfaces (−62 W m−2instead of−32 W m−2), if surface-albedo–cloud interactions are con-sidered. As a result, the observed total (shortwave plus long-wave) CRF shifted from a warming effect to an almost neu-tral one. Concerning the seasonal cycle of the surface albedo, it is demonstrated that this effect enhances shortwave cool-ing in periods when snow dominates the surface and poten-tially weakens the cooling by optically thin clouds duringthe summertime melting season. These findings suggest thatthe surface-albedo–cloud interaction should be considered inglobal climate models and in long-term studies to obtain arealistic estimate of the shortwave CRF to quantify the roleof clouds in Arctic amplification.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
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  • 9
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    In:  EPIC3International Radiation Symposium, Auckland, New Zealand, 2016-04-16-2016-04-22
    Publikationsdatum: 2017-10-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
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  • 10
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    In:  EPIC3(AC3) Kick-off meeting, Kloster Nimbschen, Grimma, 2016-05-30-2016-06-01
    Publikationsdatum: 2017-10-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
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