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Authors and Affiliations

Marc Philippe
1
ORCID: ORCID

  1. Univ Lyon, UniversitéClaude Bernard Lyon 1, CNRS, ENTPE, UMR 5023 LEHNA, F-69622, Villeurbanne, France
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Abstract

We propose the proxy threshold signature scheme with the application of elegant construction of verifiable delegating key in the ID-based infrastructure, and also with the bilinear pairings. The protocol satisfies the classical security requirements used in the proxy delegation of signing rights. The description of the system architecture and the possible application of the protocol in edge computing designs is enclosed.
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Bibliography

[1] A. Boldyreva, ”Threshold signatures, multi-signatures and blind signatures based on the Gap Diffie-Hellman Group signature scheme”, LNCS, vol. 2567, pp. 31-44, 2003.
[2] D. Boneh, C. Gentry, H. Shacham, B. Lynn, ”Short signatures from the Weil pairing”, Journal of Cryptology, vol. 17, no. 4, pp. 297-319, 2004.
[3] D. Boneh, C. Gentry, H. Shacham, B. Lynn, ”Aggregate and verifiably encrypted signatures from bilinear pairing”, Proceedings of Eurocrypt 2003, LNCS 2656, pp. 416-432, 2003.
[4] Y. Desmedt, ”Society and group oriented cryptography”, Crypto 87, pp. 120-127, 1987.
[5] Y. Desmedt, Y. Frankel, ”Threshold cryptosystems”, LNCS, vol. 718, pp. 1-14, 1993.
[6] D. E. Kouicem, A. Bouabdallah, H. Lakhlef, ”Internet of things security: A top-down survey”, 2018
[7] W. Gao, G. Wang, X. Wang, Z. Yang, ”One-Round ID-Based Threshold Signature Scheme from Bilinear Pairings”, Informatica, Vol. 20, No. 4, pp. 461-476, 2009.
[8] K. Itakura, K. Nakamura, ”A public key cryptosystem suitable for digital multisignatures”, NEC Research and Development, pp. 1-8, vol. 71, 1983.
[9] A. Joux, ”A one-round protocol for tripartite Diffie-Hellman”, Journal of Cryptology, vol. 17, no. 4, pp. 263-276, 2004.
[10] S. Kim, S. Park, D. Won, ”Proxy signatures, revisited”, LNCS, vol. 1334, pp. 223-232, 1997.
[11] A. Lysyanskaya, ”Unique signatures and verifiable random functions from the DH-DDH separation”, Proceedings of the 22nd Annual International Cryptology Conference on Advances in Cryptology, pp. 597-612, 2002.
[12] M. Mambo, K. Usuda, E. Okamoto, ”Proxy signatures for delegating signing operation”, ACM Conference on Computer and Communications Security, pp. 48-57, 1996.
[13] A. Manzoor, M. Liyanagey, A. Braekenz, S. Kanherex, M. Ylianttila, ”Blockchain based Proxy Re-Encryption Scheme for Secure IoT Data Sharing”, 2018.
[14] B.C. Neuman, ”Proxy-based authorization and accounting for distributed systems”, Proceedings of the 13th International Conference on Distributed Computing Systems, pp. 283-291, 1993.
[15] K.G. Paterson, ”ID-based signatures from pairings on elliptic curves”, Journals and Magazines, Electronics Letters, Volume: 38 Issue: 18, pp. 1025 - 1026, 2002.
[16] J. Pomykała and T Warchoł, ”Threshold signatures in dynamic groups”, Proceedings of Future Generation Communication and Networking, IEEE Computer Science, pp. 32-37, 2007.
[17] J. Pomykała, B. ´ Zrałek, ”A model of ID-based proxy signature scheme”, Proc. of 6-th Collecter Iberoamerica, pp. 1-8, 2008.
[18] A. Shamir, ”How to share a secret”, Communications of the ACM, 22:612-613, 1979.
[19] N. Suryadevara and S. Mukhopadhyay, ”Internet of things: A review and future perspective” Reliance, 2018.
[20] R. Taylor, D. Baron, and D. Schmidt, ”The world in 2025-predictions for the next ten years”, Microsystems, Packaging, Assembly and Circuits Technology Conference (IMPACT), 2015 10th International. IEEE, pp. 192–195, 2015.
[21] V. Varadharajan, P. Allen, S. Black, ”An analysis of the proxy problem in distributed systems”, Proc. IEEE Computer Society Symposium on Research in Security and Privacy, pp. 255-275, 1991.
[22] H. Watanabe, S. Fujimura, A. Nakadaira, Y. Miyazaki, A. Akutsu, and J. Kishigami, ”Blockchain contract: Securing a blockchain applied to smart contracts”, Consumer Electronics (ICCE), 2016 IEEE International Conference on. IEEE, pp. 467–468, 2016.
[23] Z. Zheng, S. Xie, H. Dai, X. Chen, and H. Wang, ”An overview of blockchain technology: Architecture, consensus, and future trends”, Big Data (BigData Congress), 2017 IEEE International Congress IEEE, pp. 557–564, 2017.
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Authors and Affiliations

Jacek Pomykała
1
Henryk Kułakowski
1
Piotr Sapiecha
2
Błażej Grela
1

  1. Warsaw University of Technology, Poland
  2. National Institute of Telecommunications in Warsaw, Poland
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Abstract

We present the last millennium of history of a peatland located in northern Poland. Our results are based on two replicate monoliths taken from a Baltic raised bog. We applied a high-resolution approach and radio car bon dating to the peat material to obtain a de tailed palaeoenvironmental reconstruction. To reconstruct past peatland moisture, we used three prox ies: testate amoebae, plant macrofossils and pollen. Despite different peat accumulation and extensive hiatus in the formerly studied core, both monoliths show a similar pattern of changes. However, the core from this study provides us with more detailed data on S. fuscum disappear ance which correlates well with the data from the other Baltic bog, S³owiñskie B³oto. Our re search shows that pris tine Bal tic bogs can be dated to AD 1350. Słowiñskie Błoto palaeohydrology confirms AD 1300 as the beginning of the hydrological disturbance. In the case of the Stążki and Słowiñskie Błoto bogs, the Little Ice Age (LIA) is recorded between AD 1500 and AD 1800. However, this climatic change might have been blurred by human impact. In the case of the Baltic bogs, their reference virgin state can be dated to AD 1200. After this date, we observed in creasing human impact and climatic in stability connected with the LIA. However, between AD 1800 and 1900, bogs were wet, most possibly due to climatic forcing. This fact suggests that despite human impact, recent peat deposits can still reflect climate. Our research provided in formation related to the time of existence, location and characteristics of the natural/pristine state. High-resolution peatland palaeoecology is crucial for restoration activities, e.g., rewetting and environmental management. The palaeohydrological context (supported by other proxies) of the last 1000 years provides a reliable answer to the question: ‘To rewet or not to rewet?’

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Authors and Affiliations

Mariusz Lamentowicz
Mariusz Gałka
Jacek Pawlyta
Łukasz Lamentowicz
Tomasz Goslar
Grażyna Miotk-Szpiganowicz
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Abstract

The growing number of mobile devices and the increasing popularity of multimedia services result in a new challenge of providing mobility in access networks. The paper describes experimental research on media (audio and video) streaming in a mobile IEEE 802.11 b/g/n environment realizing network-based mobility. It is an approach to mobility that requires little or no modification of the mobile terminal. Assessment of relevant parameters has been conducted in an IPv6 testbed. During the tests, both Quality of Service (QoS) and Quality of Experience (QoE) parameters have been considered. Against the background of standard L3 and L2 handovers, an emerging mobility solution named Proxy Mobile IPv6 (PMIPv6) has been examined. Its advantages (L3 connectivity maintenance) and disadvantages (packet loss during handover) are emphasized based on the obtained results. Moreover, a new solution for handover optimization has been proposed. A handoff influence upon audio/video generation and transfer imperfections has been studied and found to be an interesting direction of future work.

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Authors and Affiliations

M. Hoeft
K. Gierlowski
T. Gierszewski
J. Konorski
K. Nowicki
J. Wozniak
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Abstract

The aim of this study was to reconstruct the evolution of the Eemian palaeolake in the Żabieniec site (Garwolin Plain, Central Poland); it identifies changes in the water level and the trophic status of the lake resulting from panregional factors, including climate changes occurring during individual phases of the last interglacial, and local geologic-geomorphological factors shaping the palaeoenvironment using multi-proxy methods (palaeobotanical analyses, subfossil Cladocera and diatoms analyses as well as determinations of the stable isotopes). A record was obtained of all seven Regional Pollen Assemblage Zones (RPAZs) according to Mamakowa’s description of the Eemian pollen succession (1989), and of the changes in microfossil assemblages and isotopes in palaeolake sediments associated with lake evolution. Special attention was paid to the Middle Eemian RPAZ 4 (i.e. hazel phase) of the climatic optimum; all proxies associate this with the highest water level and a warm humid climate. During the E5/E6 RPAZs, the eutrophic lake transformed very quickly, and a transitional peatbog was formed. The higher humidity of the late Eemian resulted in another increase in water level. The multi-proxy record of the Żabieniec palaeolake which we obtained was compared to those of other Eemian water bodies in the Garwolin Plain and in Central Poland that exhibit sedimentation gaps especially during the younger part of the E5 RPAZ.
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Authors and Affiliations

Marcin Żarski
Kamil Kultys
1 2
Joanna Mirosław-Grabowska
3
Abdelfattah Zalat
4
Anna Hrynowiecka
5
Karolina Łabęcka
1
Sławomir Terpiłowski
1
Irena Agnieszka Pidek
1
ORCID: ORCID

  1. Institute of Earth and Environmental Sciences, Maria Curie-Skłodowska University, al. Kraśnicka 2d, 20-718 Lublin, Poland
  2. ECOTECH-COMPLEX , Maria Curie-Skłodowska University, Głęboka 39, 20-612 Lublin, Poland
  3. Institute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818, Warszawa, Poland
  4. Geology Department, Faculty of Science, Tanta University, 31527 Tanta, Egypt
  5. Polish Geological Institute-National Research Institute, Marine Geology Branch, Kościerska 5, 80-328 Gdańsk, Poland
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Abstract

It is generally accepted that ice cores archive amount-weighted water stable isotope signals. In order to achieve an improved understanding of the nature of water stable isotope signals stored in ice cores annual δ18O and δ2H averages (i.e. amount-weighted) were calculated for two Antarctic meteorological stations, Vernadsky and Hal-ley Bay, using monthly precipitation amount and monthly net accumulation as weights, respectively. These were then compared with the annual mean δ18O δ2H and records of the nearest available ice cores. In addition, at the stations, both arithmetic means (i.e. time-weighted) and amount-weighted (precipitation amount and net accumulation used as weights) annual air temperature averages were calculated and then compared to amount weighted annual mean δ18O and δ2H using correlation- and regression analyses. The main hypothesis was that amount weighted annual mean water isotope and temperature records from the stations would be able to replicate the annual water isotope signal stored in ice cores to a higher degree. Results showed that (i) amount weighting is incapable of ameliorating the signal replication between the stations and the ice cores, while arithmetic means gave the stronger linear relationships; (ii) post depositional processes may have a more determining effect on the isotopic composition of the firn than expected; and (iii) mean annual air temperature provided the closest match to ice core derived annual water isotope records. This latter conveys a similar message to that of recent findings, in as much as ambient temperature, via equilibrium isotope fractionation, is imprinted into the uppermost snow layer by vapor exchange even between precipitation events. Together, these observations imply that ice core stable water isotope records can be a more continuous archive of near-surface temperature changes than hitherto believed.
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Authors and Affiliations

István Gábor Hatvani
Zoltán Kern

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