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  • 2020-2024  (41)
  • 1
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-05-16
    Description: In the Northwestern Pacific, the meridionally propagating Rossby waves known as the Pacific-Japan (PJ) pattern is the dominant teleconnection pattern in the vicinity in East Asia, and it often accompanies heatwaves. In this study, the circulation and thermodynamic characteristics of the pattern was investigated based on a daily timescale to better understand their relationship with the likelihood of heatwaves/marine heatwaves in East Asia. According to thermodynamic budget calculations, horizontal heat advection crossing the climatological flow pattern is the key factor for the observed surface air warming. For the ocean warming, the increased solar radiation due to anti-cyclonic circulation is the most impact factor over the East Asia. The CESM2 simulation results show that the heat forcing in the tropical western Pacific and atmospheric/marine heatwaves over East Asia is closely relevant the meridionally propagating Rossby waves.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 2
    Publication Date: 2023-02-08
    Description: Highlights • Code comparisons build confidence in simulators to model interdependent processes. • International hydrate reservoir simulators are compared over five complex problems. • Geomechanical processes significantly impact response of gas hydrate reservoirs. • Simulators yielded comparable results, however many differences are noted. • Equivalent constitutive models are required to achieve agreement across simulators. Geologic reservoirs containing gas hydrate occur beneath permafrost environments and within marine continental slope sediments, representing a potentially vast natural gas source. Numerical simulators provide scientists and engineers with tools for understanding how production efficiency depends on the numerous, interdependent (coupled) processes associated with potential production strategies for these gas hydrate reservoirs. Confidence in the modeling and forecasting abilities of these gas hydrate reservoir simulators (GHRSs) grows with successful comparisons against laboratory and field test results, but such results are rare, particularly in natural settings. The hydrate community recognized another approach to building confidence in the GHRS: comparing simulation results between independently developed and executed computer codes on structured problems specifically tailored to the interdependent processes relevant for gas hydrate-bearing systems. The United States Department of Energy, National Energy Technology Laboratory, (DOE/NETL), sponsored the first international gas hydrate code comparison study, IGHCCS1, in the early 2000s. IGHCCS1 focused on coupled thermal and hydrologic processes associated with producing gas hydrates from geologic reservoirs via depressurization and thermal stimulation. Subsequently, GHRSs have advanced to model more complex production technologies and incorporate geomechanical processes into the existing framework of coupled thermal and hydrologic modeling. This paper contributes to the validation of these recent GHRS developments by providing results from a second GHRS code comparison study, IGHCCS2, also sponsored by DOE/NETL. IGHCCS2 includes participants from an international collection of universities, research institutes, industry, national laboratories, and national geologic surveys. Study participants developed a series of five benchmark problems principally involving gas hydrate processes with geomechanical components. The five problems range from simple geometries with analytical solutions to a representation of the world's first offshore production test of methane hydrates, which was conducted with the depressurization method off the coast of Japan. To identify strengths and limitations in the various GHRSs, study participants submitted solutions for the benchmark problems and discussed differing results via teleconferences. The GHRSs evolved over the course of IGHCCS2 as researchers modified their simulators to reflect new insights, lessons learned, and suggested performance enhancements. The five benchmark problems, final sample solutions, and lessons learned that are presented here document the study outcomes and serve as a reference guide for developing and testing gas hydrate reservoir simulators.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2023-08-15
    Description: Observations of rapid ongoing grounding line retreat, ice shelf thinning and accelerated ice flow from the West Antarctic Ice Sheet (WAIS) may forebode a possible collapse if global temperatures continue to increase. Understanding and reconstructing West Antarctic Ice Sheet dynamics in past warmer-than-present times will inform about its behavior as an analogue for future climate scenarios. International Ocean Discovery Program (IODP) Expedition 379 visited the Amundsen Sea sector of Antarctica to obtain geological records suitable for this purpose. During the expedition, cores from two drill sites at the Resolution Drift on the continental rise returned sediments whose deposition was possibly influenced by West Antarctic Ice Sheet dynamics from late Miocene to Holocene times. To examine the West Antarctic Ice Sheet dynamics, shipboard physical properties and sedimentological data are correlated with seismic data and extrapolated across the Resolution Drift via core-log-seismic integration. An interval with strongly variable physical properties, high diatom abundance and ice-rafted debris occurrence, correlating with partially high amplitude seismic reflection characteristics was identified between 4.2 and 3.2 Ma. Sedimentation during this interval is interpreted as having occurred during an extended warm period with a dynamic West Antarctic Ice Sheet in the Amundsen Sea sector. These records compare to those of other drill sites in the Ross Sea and the Bellingshausen Sea, and thus suggest an almost simultaneous occurrence of extended warm periods in all three locations.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 4
    Publication Date: 2023-09-24
    Description: Ecosystem dynamics at the northwest Antarctic Peninsula are driven by interactions between physical and biological processes. For example, baleen whale populations are recovering from commercial harvesting against the backdrop of rapid climate change, including reduced sea ice extent and changing ecosystem composition. Concurrently, the commercial harvesting of Antarctic krill is increasing, with the potential to increase the likelihood for competition with and between krill predators and the fishery. However, understanding the ecology, abundance, and spatial distribution of krill predators is often limited, outdated, or at spatial scales that do not match those desired for effective fisheries management. We update current knowledge of predator dependence on krill by integrating telemetry-based data, at-sea observational surveys, estimates of predator abundance, and physiological data to estimate the spatial distribution of krill consumption during the austral summer by three species of Pygoscelis penguin, 11 species of flying seabirds, one species of pinniped, and two species of baleen whale. Our models show that the majority of important areas for krill predator foraging are close to penguin breeding colonies in nearshore areas where humpback whales also regularly feed, and along the shelf-break, though we caution that not all known krill predators are included in these analyses. We show that krill consumption is highly variable across the region, and often concentrated at fine spatial scales, emphasizing the need for the management of the local krill fishery at relevant temporal and spatial scales. We also note that krill consumption by recovering populations of krill predators provides further evidence in support of the krill surplus hypothesis, and highlight that despite less than comprehensive data, cetaceans are likely to consume a significant proportion of the krill consumed by natural predators but are not currently considered directly in the management of the krill fishery. If management of the krill fishery is to be precautionary and operate in a way that minimizes the risks to krill predator populations, it will be necessary in future analyses, to include up-to-date and precise abundance and consumption estimates for pack-ice seals, finfish, squid, and other baleen whale species not currently considered.
    Description: Challenges 4, 9
    Description: Published
    Description: Refereed
    Keywords: Antarctic ecosystem ; Fisheries management ; Habitat modeling ; Humpback whales ; Penguins ; Seabirds ; Spatial ecology
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: 24pp.
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  • 5
    Publication Date: 2023-01-30
    Description: Despite the importance of surface energy budgets (SEBs) for land-climate interactions in the Arctic, uncertainties in their prediction persist. In situ observational data of SEB components - useful for research and model validation - are collected at relatively few sites across the terrestrial Arctic, and not all available datasets are readily interoperable. Furthermore, the terrestrial Arctic consists of a diversity of vegetation types, which are generally not well represented in land surface schemes of current Earth system models. This dataset describes the data generated in a literature synthesis, covering 358 study sites on vegetation or glacier (〉=60°N latitude), which contained surface energy budget observations. The literature synthesis comprised 148 publications searched on the ISI Web of Science Core Collection.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 6
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-24
    Description: Morphological variables (e.g., maximum dimension D〈sub〉max〈/sub〉, projected area, perimeter, width, and roundness) of ice crystals are fundamental information to represent microphysical and radiative properties of ice clouds in numerical models, which can be derived via in-situ aircraft measurements. Conventional airborne cloud probes are limited to a single observation angle to measure morphological variables. Non-spherical ice crystals may have different measured morphological variables depending on the observation angle, which causes uncertainties in the calculation of the microphysical and radiative properties of ice clouds. Thus, it is necessary to quantify uncertainties that depend on observation angles for determining the morphological variables of ice crystals. In this study, differences in determining the morphological variables of the ice crystals depending on observation angles were quantified using measurements of Particle Habit Imaging and Polar Scattering (PHIPS) probe that were acquired during the Arctic CLoud Observation Using airborne measurements during polar Day field campaign and the Southern Ocean Clouds Radiation Aerosol Transport Experimental Study field campaign. The PHIPS is a probe that provides stereo images of the sampled ice crystal from two different observation angles that are 120° apart. Morphological variables and habits of ice crystals were determined based on PHIPS stereo images. The uncertainties in determining morphological variables of ice crystals were quantified by calculating relative differences in morphological variables of ice crystals depending on observation angles. The nonsphericity of ice crystals sampled during ACLOUD and SOCRATES caused an average 14.69% (22.75%; 14.57%; 16.67%; 18.76%) uncertainty in determining Dmax (projected area; perimeter; width; roundness).
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 7
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-06-13
    Description: Korea has been frequently exposed to aerosol cloud precipitation interactions specifically in the polluted season such that the enhanced aerosols might slow down coalescence and accretion, and thus delay the conversion of cloud water to precipitation drop. This inadvertent weather modification was identified as a couple of possible evidence, which as a result would make weather forecast incorrect in terms of precipitation intensity and timing in the mid-Korean peninsula (Eun et al., 2016; 2021). Meanwhile, the advertent weather modification campaign has been made during the past decade in the eastern mountainous region (Yeongdong) where cloud active aerosols are relatively fewer than the metropolitan region. This ongoing campaign largely focuses on winter and early spring in order to secure water supply and further prevent wildfire in dry season. The previous experiments showed a significant response in precipitation of the target (downwind) domain in comparison with the control zone after AgI burning at a fixed site for the several events. In addition, using a multi-angle snowflake camera, a decrease in snow crystal size and an increase in riming degree were demonstrated after the seeding on 14 March 2017, that was also identified with smartphone photographs on 9 March 2016 and 21 March 2018. In Korea, the advertent seeding experiment has been ongoing in the eastern mountainous (relatively clean) region whereas some inadvertent weather modification events occurred largely in the west (urban) region probably through the similar mechanism in the different environments.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 8
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-05-25
    Description: Explosive volcanic eruptions are one of the major natural hazards in East Asia. The study of eruptive history and volcanic ash dispersal are the key to understand eruption frequency and to identify the level of risk from different volcanoes. Here we use cryptotephra extraction techniques to examine a marine core from the southwestern Sea of Japan. The results reveal that six tephra layers are preserved in the Holocene core section, four of which are cryptotephra layers. Glass compositions of tephra shards indicate that these ashes are the B-Tm from Changbaishan volcano (China/N Korea), the K-Ah from Kikai caldera (Japan) and four tephras (U-1 to U-4) from the Ulleungdo volcano (S Korea). Except for the U-1 tephra whose age is previously unknown, terrestrially-based ages of the other tephras are used to constrain the marine reservoir effect and the age-depth model of the record. Through 〈sup〉14〈/sup〉C dating of marine sediment and reservoir correction, we report for the first time, a precise eruptive age for the Ulleungdo U-1 eruption (3354-3080 cal yr BP, 95.4%). The Holocene eruptive history of the volcano is now fully revealed, with four eruptions occurred at ca. 10.2, 8.4, 5.6 and 3.2 cal ka BP. Using the identified ash layers, we can now synchronize the marine record with sedimentary archives from in and around the Sea of Japan, to as far as the Arctic and the tropical regions. Our cryptotephra study shows the potential of this approach for future studies in the region.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 9
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    In:  Guaymas Basin Tectonics and Biosphere | Proceedings of the International Ocean Discovery Program, 385: College Station, TX (International Ocean Discovery Program)
    Publication Date: 2023-03-20
    Type: info:eu-repo/semantics/bookPart
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  • 10
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    In:  Guaymas Basin Tectonics and Biosphere | Proceedings of the International Ocean Discovery Program, 385: College Station, TX (International Ocean Discovery Program)
    Publication Date: 2023-03-20
    Type: info:eu-repo/semantics/bookPart
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