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  • 1
    Online-Ressource
    Online-Ressource
    Cham :Springer International Publishing AG,
    Schlagwort(e): Distributed artificial intelligence-Congresses. ; Electronic books.
    Materialart: Online-Ressource
    Seiten: 1 online resource (256 pages)
    Ausgabe: 1st ed.
    ISBN: 9783030946623
    Serie: Lecture Notes in Computer Science Series ; v.13170
    DDC: 006.3v
    Sprache: Englisch
    Anmerkung: Intro -- Preface -- Organization -- Contents -- The Power of Signaling and Its Intrinsic Connection to the Price of Anarchy -- 1 Introduction -- 2 Preliminaries -- 2.1 Cost-Minimization/Payoff-Maximization Games -- 2.2 Signaling Schemes and Equilibrium Concepts -- 3 The Power of Signaling (PoS) -- 4 PoS in Cost-Minimization Games -- 4.1 Proof of the PoS Upper Bounds -- 4.2 Tightness of the Upper-Bound for PoS -- 5 PoS in Payoff-Maximization Games -- 5.1 Tightness of PoS(Pri:Pub) at the Robber's Game -- 6 Discussions and Future Work -- A Omitted Proofs for Cost-Minimization PoS Bounds -- A.1 Tightness of the Upper-Bound for PoS(Pri:Pub) -- A.2 Tightness of the Upper-Bound for PoS(exP:Pri) -- B Omitted Proofs for Payoff-Maximization PoS Bounds -- B.1 Tightness of the Lower-Bound for PoS(Pub:FI) -- B.2 Tightness of the Lower-Bound for PoS(exP:Pri) -- C PoS w.r.t the No Information (NI) Benchmark -- D Non-tightness of PoS in ``Reverse'' Routing -- References -- Uncertainty-Aware Low-Rank Q-Matrix Estimation for Deep Reinforcement Learning -- 1 Introduction -- 2 Background -- 2.1 Reinforcement Learning -- 2.2 Approximate Rank and Matrix Reconstruction -- 3 Low-Rank Q-Matrix in DRL -- 3.1 Empirical Study of Low-Rank Q-Matrix in MuJoCo -- 3.2 Q-Matrix Reconstruction for DRL -- 4 DRL with Uncertainty-Aware Q-Matrix Reconstruction -- 4.1 Connection Between Rank and Uncertainty -- 4.2 Uncertainty-Aware Q-Matrix Reconstruction for DRL -- 5 Experiment -- 5.1 Experiment Setup -- 5.2 Results and Analysis -- 6 Conclusion -- A More Background on Matrix Estimation -- B Additional Experimental Details -- C Complete Learning Curves of Table2 -- References -- SEIHAI: A Sample-Efficient Hierarchical AI for the MineRL Competition -- 1 Introduction -- 2 Background -- 2.1 The MineRL Competition -- 2.2 The ObtainDiamond Task -- 2.3 The ObtainDiamond MDP. , 3 Method -- 3.1 The Overall Framework -- 3.2 Action Discretization -- 3.3 The ChopTree Agent -- 3.4 The CraftWoodenPickaxe Agent -- 3.5 The DigStone Agent -- 3.6 The CraftStonePickaxe Agent -- 3.7 The RandomSearch Agent -- 3.8 The Scheduler -- 4 Experiments -- 4.1 Overall Evaluation -- 4.2 Agent-Level Evaluation -- 5 Related Work -- 6 Conclusion -- References -- BGC: Multi-agent Group Belief with Graph Clustering -- 1 Introduction -- 2 Related Work -- 3 Background -- 3.1 Graph Attention Network -- 4 Method -- 4.1 Adjacent Matrix via kNN -- 4.2 Belief in Graph Clustering -- 4.3 Split Loss -- 4.4 Decentralization Execution -- 5 Experiment -- 5.1 Starcraft II -- 5.2 Representation -- 5.3 Ablation -- 5.4 Distributed Execution -- 6 Conclusion -- References -- Incomplete Distributed Constraint Optimization Problems: Model, Algorithms, and Heuristics -- 1 Introduction -- 2 Background -- 3 Incomplete DCOPs -- 4 Solving I-DCOPs -- 4.1 SyncBB -- 4.2 ALS-MGM -- 5 SyncBB Cost-Estimate Heuristic -- 6 ALS-MGM Cost-Estimate Heuristic -- 7 Theoretical Results -- 8 Related Work -- 9 Empirical Evaluations -- 10 Conclusions -- References -- Securities Based Decision Markets -- 1 Introduction -- 2 Related Work and Notation -- 2.1 Scoring Rules -- 2.2 Sequentially Shared Scoring Rules -- 2.3 Securities Based Prediction Markets -- 2.4 Decision Markets -- 3 Strictly Proper Securities Based Decision Markets -- 3.1 Design -- 3.2 Distribution of Realised Payoffs -- 4 Worst-Case Losses for Participants and Market Creator -- 4.1 Worst-Case Loss for Participants -- 4.2 Worst-Case Loss for Market Creator -- 4.3 Re-allocation of Worst-Case Losses -- 5 Conclusion and Discussion -- References -- MARL for Traffic Signal Control in Scenarios with Different Intersection Importance -- 1 Introduction -- 2 Basic Notation -- 2.1 Adaptive Traffic Signal Control -- 2.2 Network Markov Game. , 2.3 Deep Q-Learning and HDQN -- 3 Leader Follower Markov Game -- 4 Breadth First Sort Hysteretic DQN -- 5 Experiment -- 5.1 Scenarios Setting -- 5.2 Training Setting -- 5.3 Performance Comparison -- 6 Conclusion -- References -- Safe Distributional Reinforcement Learning -- 1 Introduction -- 2 Related Work -- 3 Background -- 4 Problem Formulation -- 5 Proposed Method -- 5.1 General Principle -- 5.2 Techniques for Efficient Implementation -- 6 Experimental Results -- 6.1 Safety Gym -- 6.2 Stock Investment -- 7 Conclusion -- A Performance Guarantee Bound -- B More Results -- B.1 Random CMDP -- B.2 Safety Gym -- C More Details on Experiments -- C.1 Random CMDP -- C.2 Stock Transaction -- C.3 Mujoco Simulator -- References -- The Positive Effect of User Faults over Agent Perception in Collaborative Settings and Its Use in Agent Design -- 1 Introduction -- 2 Related Work -- 3 The Model -- 4 Research Hypotheses -- 5 Experimental Framework -- 6 Experimental Design -- 6.1 Experimental Treatments -- 6.2 Measures -- 7 Results and Analysis -- 7.1 The Effect of User's Own Faults over Her Satisfaction with the Collaborative Agent -- 7.2 Incorporating User Faults in Agent Design - Proof of Concept -- 7.3 Participants' Qualitative (Textual) Responses -- 8 Discussion, Conclusions and Future Work -- A Experimental Framework Interface -- B Experimental Treatments Comparison -- C State Machines -- D Measures -- E Complementary Graphs -- E.1 Competence -- E.2 Recommendation -- F Participants' Qualitative (Textual) Responses -- References -- Behavioral Stable Marriage Problems -- 1 Introduction -- 2 Multialternative Decision Field Theory (MDFT) -- 3 Stable Marriage Problems (SMPs) -- 4 Behavioral Stable Marriage Problems (BSMPs) -- 5 Complexity Results -- 6 Algorithms for BSMPs -- 7 Experimental Results -- 8 Future Work -- A Proofs of Theorems -- B Algorithms. , C Convergence Analysis for B-LS -- References -- FUN-Agent: A HUMAINE Competitor -- 1 Introduction -- 2 Related Work -- 3 2020 HUMAINE Competition -- 3.1 Language Processing -- 3.2 Formal Specification of the Repeated Task Negotiation Problem -- 4 Strategy -- 4.1 Conversational Demeanor -- 4.2 Bundling -- 4.3 State Tracking -- 4.4 Conceding -- 4.5 Obfuscation as a Competitive Strategy -- 4.6 Initial Offer Generation -- 4.7 Counteroffer Generation -- 4.8 Guarding Against Competitor Sniping -- 5 Experimentation and Design -- 5.1 Competitor Agents -- 5.2 Human Negotiators -- 5.3 Negotiation Rounds -- 6 Results and Discussion -- 7 Conclusion -- References -- Signal Instructed Coordination in Cooperative Multi-agent Reinforcement Learning -- 1 Introduction -- 2 Methods -- 2.1 Preliminaries -- 2.2 Joint Policy Space with Coordination Signal -- 2.3 Signal Instructed Coordination -- 2.4 Implementation Details -- 3 Experiments -- 3.1 Rock-Paper-Scissors-Well (RPSW) -- 3.2 Particle Worlds -- 4 Related Works -- 5 Conclusions -- A Algorithm -- B Proof of Proposition 1 -- C Proof of Proposition 2 -- D Derivation of the Lower Bound -- E Experiment Details -- E.1 Matrix Game Experiment -- E.2 Particle World Experiment -- F Visualization for Joint Policy of Multi-step Matrix Game -- G Parameter Sensitivity -- References -- A Description of the Jadescript Type System -- 1 Introduction and Motivation -- 2 The Jadescript Type System -- 2.1 Basic Types -- 2.2 Collection Types -- 2.3 Concept, Action, Predicate, and Proposition Types -- 2.4 Ontology Types -- 2.5 Agent Types -- 2.6 Behaviour Types -- 2.7 Message Types -- 3 Related Work -- 4 Conclusions -- References -- Combining M-MCTS and Deep Reinforcement Learning for General Game Playing -- 1 Introduction -- 2 Background -- 2.1 General Game Playing -- 2.2 Memory-Augmented Monte Carlo Tree Search. , 2.3 Deep Reinforcement Learning -- 3 Method -- 3.1 M-MCTS for GGP -- 3.2 Combining M-MCTS with Deep Reinforcement Learning -- 4 Experimental Evaluation -- 4.1 Evaluation Methodology -- 4.2 Results and Analysis -- 5 Conclusion -- References -- A Two-Step Method for Dynamics of Abstract Argumentation -- 1 Introduction -- 2 Preliminaries -- 3 The Update of Argumentation Frameworks -- 4 Properties -- 5 Related Work -- 6 Conclusion and Further Work -- References -- Author Index.
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  • 2
    Publikationsdatum: 2023-01-30
    Beschreibung: This data describe the freezing experiment of rainwaters collected in Tibetan Plateau (TP). The data set includes two parts, which are results of untreated samples and samples after being heated to 95 °C in 10 minutes.
    Schlagwort(e): Date/time end; Date/time start; Frozen droplets; Frozen fraction; Ice Nucleating Particle; Ice nucleating particles, per air volume; Ice nucleating particles, per water volume; Identification; MULT; Multiple investigations; Nam_Co; Rainwater; Sample comment; Sample ID; Temperature, technical; Tibetan Plateau
    Materialart: Dataset
    Format: text/tab-separated-values, 164394 data points
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  • 3
    Publikationsdatum: 2023-01-30
    Beschreibung: This data gives the concentrations of water-soluble ions and organic carbon (WSOC), metal elements and black carbon in rainwater samples.
    Schlagwort(e): Aluminium; Ammonium; Barium 2+; Black carbon; Calcium; Carbon, organic, total per volume; Chloride; Chromium; Copper; Date/time end; Date/time start; Ice Nucleating Particle; Ion chromatograph, Dionex Corporation, ICS-2500/2000; Iron; Lead; Magnesium; Manganese 2+; MULT; Multiple investigations; Nam_Co; Nickel; Nitrate; Potassium; Rainwater; Sample ID; Sodium; Sulfate; Tibetan Plateau; TOC analyzer (Shimadzu, TOC-L CPH CN200); Zinc
    Materialart: Dataset
    Format: text/tab-separated-values, 770 data points
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  • 4
    Publikationsdatum: 2023-01-30
    Beschreibung: This data shows the calculated percentage of residence time when air masses passed over different land covers (vegetation,agriculture,bare area, water/ice and urban area), coupling the back forward trajectories analysis and land cover dataset obtained from Geographic Information System (GIS)
    Schlagwort(e): Date/time end; Date/time start; Ice Nucleating Particle; MULT; Multiple investigations; Nam_Co; Obtained from Geographic Information System (GIS); Rainwater; Residence time; Sample ID; Tibetan Plateau
    Materialart: Dataset
    Format: text/tab-separated-values, 272 data points
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  • 5
    Publikationsdatum: 2023-01-30
    Beschreibung: This data gives the contributions of different sources (Marine and salt-lake, dust, biomass burning and long-range transport anthropogenic pollutants) to chemical components measured in rainwater resulted from the Positive Matrix Factorization Model developed by Environmental Protection Agency (EPA-PMF).
    Schlagwort(e): Components, chemical; Date/time end; Date/time start; Ice Nucleating Particle; MULT; Multiple investigations; Nam_Co; Positive Matrix Factorization Model; Rainwater; Sample ID; Tibetan Plateau
    Materialart: Dataset
    Format: text/tab-separated-values, 238 data points
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  • 6
    Publikationsdatum: 2024-01-26
    Beschreibung: The ice-nucleating particles (INPs) modulate the microphysics and radiative properties of clouds. However, less is known concerning their abundance and sources in the most pristine and climatic sensitive regions, such as the Tibetan Plateau (TP). Here, to our best knowledge, we conduct the first investigation on INPs in rainwater collected in the TP region under mixed-phase cloud conditions. The INP concentrations vary from 0.002 to 0.675 L-1 Air over the temperature range from -7.1 to -27.5 °C, being within the INP spectra derived from precipitation under worldwide geophysical conditions, and are also comparable to those in the Arctic region. The heating-sensitive INPs account for 57%±30% of the observed INPs at -20 °C, and become increasingly important at warmer temperature regime, indicating biogenic particles as major contributors to INPs above -20 °C over the TP, especially, on the day with additional input of biogenic materials carried by dust particles. Chemical analysis demonstrates the rainwater components are mixture of dust particles, marine aerosol, and anthropogenic pollutants. Dust particles transported from the surrounding deserts and originated from ground surface of TP may contribute to the heating-resistant INPs at temperatures below -20 °C.
    Schlagwort(e): Ice Nucleating Particle; Rainwater; Tibetan Plateau
    Materialart: Dataset
    Format: application/zip, 4 datasets
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  • 7
    facet.materialart.
    Unbekannt
    Laboratoire EDYTEM - UMR5204, Université Savoie Mont Blanc, Bâtiment «Pôle Montagne»
    In:  EPIC35th European Conference on Permafrost, Book of Abstracts, Chamonix Mont-Blanc, France, 2018-06-23-2018-07-01Le Bourget du Lac cedex, France, Laboratoire EDYTEM - UMR5204, Université Savoie Mont Blanc, Bâtiment «Pôle Montagne», 1055 p.
    Publikationsdatum: 2018-07-15
    Beschreibung: Yedoma is vulnerable to thawing and degradation under climate warming, which can result in lowering of surface elevations due to thaw subsidence. Quantitative knowledge about elevation changes can help us better understand the freeze-thaw processes of the active layer and yedoma deposits. In this study, we utilize C-band Sentinel-1 InSAR measurements, characterized by frequent sampling, to study the elevation changes over ice-rich yedoma uplands on Sobo-Sise Island, Lena Delta. We observe significant seasonal thaw subsidence during summer months and inter-annual elevation changes from 2016 to 2017. Here, we demonstrate the capability of Sentinel-1 to estimate elevation changes over yedoma uplands. We observe interesting patterns of stronger seasonal thaw subsidence on elevated flat yedoma uplands when compared to surrounding yedoma slopes. Inter-annual analyses from 2016 to 2017 revealed mostly positive surface elevation changes that might be caused by delayed thaw seasonal progression associated with mean annual air temperature fluctuations.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev , info:eu-repo/semantics/conferenceObject
    Format: application/pdf
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  • 8
    facet.materialart.
    Unbekannt
    MDPI
    In:  EPIC3Remote Sensing, MDPI, 10(7), pp. 1152, ISSN: 2072-4292
    Publikationsdatum: 2018-10-15
    Beschreibung: Yedoma—extremely ice-rich permafrost with massive ice wedges formed during the Late Pleistocene—is vulnerable to thawing and degradation under climate warming. Thawing of ice-rich Yedoma results in lowering of surface elevations. Quantitative knowledge about surface elevation changes helps us to understand the freeze-thaw processes of the active layer and the potential degradation of Yedoma deposits. In this study, we use C-band Sentinel-1 InSAR measurements to map the elevation changes over ice-rich Yedoma uplands on Sobo-Sise Island, Lena Delta with frequent revisit observations (as short as six or 12 days). We observe significant seasonal thaw subsidence during summer months and heterogeneous inter-annual elevation changes from 2016–17. We also observe interesting patterns of stronger seasonal thaw subsidence on elevated flat Yedoma uplands by comparing to the surrounding Yedoma slopes. Inter-annual analyses from 2016–17 suggest that our observed positive surface elevation changes are likely caused by the delayed progression of the thaw season in 2017, associated with mean annual air temperature fluctuations.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev , info:eu-repo/semantics/article
    Format: application/pdf
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  • 9
    Publikationsdatum: 2021-05-16
    Beschreibung: Investigating the composition and distribution of pelagic marine sediments is fundamental in the field of marine sedimentology. The spatial distributions of surface sediment are unclear due to limited investigation along the Emperor Seamount Chain of the North Pacific. In this study, a suite of sedimentological and geochemical proxies were analyzed, including the sediment grain size, organic carbon, CaCO3, major and rare earth elements of 50 surface sediment samples from the Emperor Seamount Chain, spanning from ∼33°N to ∼52°N. On the basis of sedimentary components, we divide them into three Zones (I, II, and III) spatially with distinct features. Sediments in Zone I (∼33°N–44°N) and Zone III (49.8°N–53°N) are dominated by clayey silt, and mainly consist of sand and silty sand in Zone II. The mean grain size of the sortable silt shows that the hydrodynamic condition in the study area is significantly stronger than that of the abyssal plain, especially at the water depth of 1,000–2,500 m. The CaCO3 contents in sediments above 4,000 m range from 20 to 84% but decrease sharply to less than 1.5% below 4,000 m, confirming that the water depth of 4,000 m is the carbonate compensation depth of the study area. Strong positive correlations between Al2O3 and Fe2O3, TiO2, MgO, and K2O (R 〉 0.9) in the bulk sediments indicate pronounced contributions of terrigenous materials from surrounding continent mass to the study area. Furthermore, the eolian dust makes contributions to the composition of bulk sediments as confirmed by rare earth elements. There is no significant correlation between grain size and major and minor elements, which indicates that the sedimentary grain size does not exert important effects on terrigenous components. There is significant negative δCe and positive δEu anomalies at all stations. The negative Ce anomaly mainly exists in carbonate-rich sediments, inheriting the signal of seawater. The positive Eu anomaly indicates widespread volcanism contributions to the study area from active volcanic islands arcs around the North Pacific. The relative contributions of terrestrial, volcanic, and biogenic materials vary with latitude and water depth in the study area.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
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  • 10
    Publikationsdatum: 2021-10-18
    Beschreibung: Interactions between midlatitude westerlies and the Pamir–Tian Shan mountains significantly impact hydroclimate patterns in Central Asia today, and they played an important role in driving Asian aridification during the Cenozoic. We show that distinct westeast hydroclimate differences were established over Central Asia during the late Oligocene (ca. 25 Ma), as recorded by stable oxygen isotopic values of soil carbonates. Our climate simulations show that these differences are present when relief of the Pamir–Tian Shan is higher than 75% of modern elevation (∼3000 m). Integrated with geological evidence, we suggest that a significant portion of the Pamir–Tian Shan orogen had reached elevations of ∼3 km and acted as a moisture barrier for the westerlies since ca. 25 Ma.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , peerRev
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