ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Publication Date: 2021-03-29
    Description: Vergleichende Betrachtungen der neuesten Untersuchungsergebnisse in verschiedenen Marschgebieten Niedersachsens und der Niederlande führen zu der Feststellung, daß trotz örtlich sehr unterschiedlicher Einflüsse auf das Sedimentationsgeschehen der Aufbau der holozänen Schichten von überregional wirksamen Faktoren bestimmt sein muß. Der Aufbau der holozänen Schichten im südlichen Nordseeküstengebiet wird vor allem durch die von glazialeustatischen Meeresspiegelbewegungen bedingte Meerestransgression bestimmt. Einflüsse tektonischer Krustenbewegungen und anderer Faktoren sind demgegenüber nur von untergeordneter Bedeutung. Der Ablauf der holozänen Meerestransgression an der südlichen Nordseeküste wird auf Grund von 57 Radiokarbondatierungen und umfangreicher Kartierungsarbeiten in einem Diagramm dargestellt. Es gibt unter größtmöglicher Berücksichtigung der Sedimentsetzungen die mittleren Hochwasserstände zu den verschiedenen Zeitperioden wieder. Stärkere Anstiegsbewegungen des Meeresspiegels treten im Präboreal (8000—6750 v. Chr.), im Atlantikum (5500—2500 v. Chr.) und im Subatlantikum (ab 300 v. Chr.) bis heute auf. Die umgekehrten Tendenzen sind im Boreal (6750—5500 v. Chr.) und im Subboreal (2500—300 v. Chr.) festzustellen. Diese Verlangsamungen bzw. Unterbrechungen des Transgressionsablaufes sind in etwa zeitgleich mit bedeutenden Gletscherregenerationen auf dem nordamerikanischen Kontinent. Diese beiden bedeutendsten Einschnitte in der Kurve des holozänen Transgressionsablaufes im Boreal und Subboreal werden zu einer Untergliederung des Holozäns in 3 Unterabteilungen verwendet (Alt-, Mittel-, Jungholozän). Innerhalb dieser Unterabteilungen werden dann jeweils eine untere Stufe (Transgressionsbeschleunigung) und eine obere Stufe (Transgressionsverlangsamung) unterschieden. Im Jungholozän stehen wir z. Zt. noch in der unteren Stufe. Weitere Untergliederungen ergeben sich aus der Ausscheidung kleinerer Schwankungen des Transgressionsverlaufes, wobei im unteren Mittelholozän 3 Folgen, im oberen Mittelholozän 2 Folgen und im Jungholozän 4 Folgen unterschieden werden können. Jede dieser Folgen setzt sich aus einem Überflutungs- und einem Verlandungsabschnitt zusammen.
    Description: research
    Keywords: 551.7 ; VAR 000 ; Glazialgeologie ; niedersachsen ; nordseeküste ; holozän ; niederlande ; geochronologie ; meerestransgression ; holozängliederung ; marschgebiet ; sedimentation ; krustenbewegung ; meeresspiegelbewegung ; radiokarbondatierung ; hochwasserstand
    Language: German
    Type: article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-08-05
    Description: This work documents the ICON‐Earth System Model (ICON‐ESM V1.0), the first coupled model based on the ICON (ICOsahedral Non‐hydrostatic) framework with its unstructured, icosahedral grid concept. The ICON‐A atmosphere uses a nonhydrostatic dynamical core and the ocean model ICON‐O builds on the same ICON infrastructure, but applies the Boussinesq and hydrostatic approximation and includes a sea‐ice model. The ICON‐Land module provides a new framework for the modeling of land processes and the terrestrial carbon cycle. The oceanic carbon cycle and biogeochemistry are represented by the Hamburg Ocean Carbon Cycle module. We describe the tuning and spin‐up of a base‐line version at a resolution typical for models participating in the Coupled Model Intercomparison Project (CMIP). The performance of ICON‐ESM is assessed by means of a set of standard CMIP6 simulations. Achievements are well‐balanced top‐of‐atmosphere radiation, stable key climate quantities in the control simulation, and a good representation of the historical surface temperature evolution. The model has overall biases, which are comparable to those of other CMIP models, but ICON‐ESM performs less well than its predecessor, the Max Planck Institute Earth System Model. Problematic biases are diagnosed in ICON‐ESM in the vertical cloud distribution and the mean zonal wind field. In the ocean, sub‐surface temperature and salinity biases are of concern as is a too strong seasonal cycle of the sea‐ice cover in both hemispheres. ICON‐ESM V1.0 serves as a basis for further developments that will take advantage of ICON‐specific properties such as spatially varying resolution, and configurations at very high resolution.
    Description: Plain Language Summary: ICON‐ESM is a completely new coupled climate and earth system model that applies novel design principles and numerical techniques. The atmosphere model applies a non‐hydrostatic dynamical core, both atmosphere and ocean models apply unstructured meshes, and the model is adapted for high‐performance computing systems. This article describes how the component models for atmosphere, land, and ocean are coupled together and how we achieve a stable climate by setting certain tuning parameters and performing sensitivity experiments. We evaluate the performance of our new model by running a set of experiments under pre‐industrial and historical climate conditions as well as a set of idealized greenhouse‐gas‐increase experiments. These experiments were designed by the Coupled Model Intercomparison Project (CMIP) and allow us to compare the results to those from other CMIP models and the predecessor of our model, the Max Planck Institute for Meteorology Earth System Model. While we diagnose overall satisfactory performance, we find that ICON‐ESM features somewhat larger biases in several quantities compared to its predecessor at comparable grid resolution. We emphasize that the present configuration serves as a basis from where future development steps will open up new perspectives in earth system modeling.
    Description: Key Points: This work documents ICON‐ESM 1.0, the first version of a coupled model based on the ICON framework. Performance of ICON‐ESM is assessed by means of CMIP6 Diagnosis, Evaluation, and Characterization of Klima experiments at standard CMIP‐type resolution. ICON‐ESM reproduces the observed temperature evolution. Biases in clouds, winds, sea‐ice, and ocean properties are larger than in MPI‐ESM.
    Description: European Union H2020 ESM2025
    Description: European Union H2020 COMFORT
    Description: European Union H2020ESiWACE2
    Description: Deutsche Forschungsgemeinschaft TRR181
    Description: Deutsche Forschungsgemeinschaft EXC 2037
    Description: European Union H2020
    Description: Deutscher Wetterdienst
    Description: Bundesministerium fuer Bildung und Forschung
    Description: http://esgf-data.dkrz.de/search/cmip6-dkrz/
    Description: https://mpimet.mpg.de/en/science/modeling-with-icon/code-availability
    Description: http://cera-www.dkrz.de/WDCC/ui/Compact.jsp?acronym=RUBY-0_ICON-_ESM_V1.0_Model
    Keywords: ddc:550.285 ; ddc:551.63
    Language: English
    Type: doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2006-10-26
    Description: Geometric arrangement, energy absorber features, and deployment mechanisms for LEM landing system
    Keywords: SPACE VEHICLES
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2011-08-11
    Description: Full-scale and model test for dynamic effects of LEM landing
    Keywords: SPACE VEHICLES
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    In:  Other Sources
    Publication Date: 2019-01-25
    Description: Mineralogy and texture of chondrules have been reproduced experimentally and it was demonstrated that the abundance of heterogeneous nuclei is an important factor controlling chondrule textures. Cooling rates of chondrules were estimated from the zoning patterns of olivine. Low cooling rates (less than 100 C/h) yielded chemically homogeneous olivine crystals, whereas higher cooling rates, between 100 and 2000 C/h, produced olivine compositions similar to those observed in natural chondrules. We present a new approach to determining cooling rates of chondrules based on the microstructure of chondrule clinopyroxene and plagioclase. All observations were made on Allende chondrules. Two independent processes (Ca and Mg diffusion in pyroxene and Al/Si ordering in plagioclase) yield similar cooling rates on the order of 10-1 C/h for granular olivine pyroxene (GOP) chondrules in Allende. Our cooling rates are at least one order of magnitude lower than those derived from dynamic crystallization experiments.
    Keywords: ASTROPHYSICS
    Type: Lunar and Planetary Inst., Papers Presented to the Conference on Chondrules and the Protoplanetary Disk; p 43-44
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    In:  CASI
    Publication Date: 2016-06-07
    Description: The research to provide a mechanism for dissipation of impact energy in filled polymers by using fillers with a low modulus coating is reported which will dissipate energy through shearing and crazing instead of fracture. The approach offers the advantages of low cost, low toxicity, and applicability to various resins.
    Keywords: AIR TRANSPORTATION AND SAFETY
    Type: NASA. Ames Res. Center Conf. on Fire Resistant Mater.; p 251-264
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2019-05-30
    Description: Full-scale and model test for dynamic effects of LEM landing
    Keywords: SPACE VEHICLES
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2019-06-28
    Description: The mechanism of the gravitropic bending in stems of the cocklebur and castor bean are investigated. The results of these experiments demonstrate the quick stopping of growth and the increased tensions on the upper layer of a horizontal stem. It is suggested that bending apparently occurs as the resistance of the upper surface layers is extended to the inner cells below. A model of stem bending is developed which can explain the asymmetry of the stem-cell response.
    Keywords: LIFE SCIENCES (GENERAL)
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    In:  CASI
    Publication Date: 2019-06-27
    Description: The improved hemodialysis system utilizes a second polymeric membrane having dialyzate in contact with one surface and a urea decomposition solution in contact with the other surface. The membrane selectively passes urea from the dialyzate into the decomposition solution, while preventing passage of positively charged metal ions from the dialyzate into the solution and ammonium ions from the solution into the dialyzate.
    Keywords: AEROSPACE MEDICINE
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2019-06-28
    Description: Inorganic hydrate-salt filler coated with elastomer containing acidic groups imparts flame and smoke retardancy to thermoplastics while preventing degradation of impact resistance that results from high filler loadings in thermoplastic.
    Keywords: MATERIALS
    Type: NPO-14857 , NASA Tech Briefs (ISSN 0145-319X); 8; 1; P. 66
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...