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Sar Action Effectiveness Measures

. Proceedings of International Conference Maritime Transportation and Exploitation of Ocean and Coastal Resources, IMAM 2005. Lisbon 2005. International Aeronautical and Maritime Search and Rescue Manual. IMO/ICAO, London/Montreal, 1999. MSC/Circ.999-11 June 2001Provisions of conventions, plans, manuals and other documents affecting SAR — Changes to the IAMSAR Manual (First Edition). Proposed by the United States ICAO/IMO-JWG/7-WP.1 February, 2000. Adoption of amendments to the International Aeronautical and Maritime Search

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Reliability of Merchant Ship Used for Sar Action

życia na morzu, 1974 - SOLAS '74, Tekst jednolity, 2006, PRS 2006 MSC.1/Circ. 1228 Revised guidance to the master for avoiding dangerous situations in adverse weather and sea conditions Starosta A., Application of Bayesian network to estimate merchant ship usability for SAR action, Journal of KONES vol. 13 no. 3 Starosta A., Usage of AIS information to estimate merchant ship usability for SAR action, Proceedings of XIII International Scientific and Technical Conference on Marine Traffic

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A New Design of Metamaterials for SAR Reduction

). Bandwidth, SAR, and efficiency of internal mobile phone antennas. IEEE Transactions on Electromagnetic Compatibility , 46 (1), 71-86. [4] Okoniewski, M., Stuchly, M.A. (1996). A study of the handset antenna and human body interaction. IEEE Transactions on Microwave Theory and Techniques , 44, 1855-1864. [5] Islam, M.T., Faruque, M.R.I., Misran, N. (2010). Study of specific absorption rate (SAR) in the human head by metamaterial attachment. IEICE Electronics Express , 7 (4), 240-246. [6] Faruque, M.R.I., Islam, M

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Two-Dimensional l 1-Norm Minimization in SAR Image Reconstriction

References 1. Nicolas, J.-M., G. Vasile, M. Gay, F. Tupin, Em. Trouvé. SAR Processing in the Temporal Domain: Application to Direct Interferogram Generation and Mountain Glacier Monitoring Can. – J. Remote Sensing, Vol. 33 , 2007, No 1, pp. 52-59. 2. Leijen, V., F. R. Hanssen. Interferometric Radar Meteorology: Resolving the Acquisition Ambiguity. – In: CEOS SAR Workshop, Ulm Germany, 27-28 May 2004, pp. 6-14. 3. Colesanti, C., A. Ferretti, F. Novali, C. Prati, F. Rocca. SAR Monitoring of Progressive and Seasonal Ground Deformation Using the

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On The Estimation of Temporal Changes of Snow Water Equivalent by Spaceborne Sar Interferometry: A New Application for the Sentinel-1 Mission

Remote Sensing, 8, 8, 3773-3790. Leppänen, L., Kontu, A., Hannula, H.-R., Sjöblom, H., Pulliainen, J., 2016. Sodankylä manual snow survey program. Geoscientific Instrumentation, Methods and Data Systems, 5, 163-179. Longepe, N., Allain, S., Ferro-Famil, L., Pottier, E., Durand, Y., 2009. Snowpack characterization in mountainous regions using C-band SAR data and a meteorological model. IEEE Transactions on Geoscience and Remote Sensing, 47, 2, 406-418. Malnes, E., Guneriussen, T., 2002. Mapping of snow covered area with

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Effects of Electromagnetic Field Over a Human Body, Sar Simulation with and Without Nanotextile in the Frequency Range 0.9-1.8GHZ

References Software product MEFiSTo 2D Classic- http://www.faustcorp.com/products/ Overview of SAR, UGM Oct-07, T. Wittig. Microwave Journal, issue January-08. Progress in Electromagnetics Research Symposium -06, Cambridge. EMV Arbeitsschutztextil im Krankenhausbereich, Kompetenzzentrum Hörmann IMG GmbH, 2011. ICNIRP Guidelines (International Commission on Non-Ionizing Radiation Protection), Guidelines

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Constraints on the precision of SAR in equivalent dose estimations close to saturation in quartz

dating. Quaternary Science Reviews 22(10–13): 1169–1176, DOI 10.1016/S0277-3791(03)00019-2. http://dx.doi.org/10.1016/S0277-3791(03)00019-2 [4] Duller GAT, 2001. Analyst manual: 36pp. [5] Duller GAT, 2007. Assessing the error on equivalent dose estimates derived from single aliquot regenerative dose measurements. Ancient TL 25: 15–24. [6] Jacobs Z, Wintle AG and Duller GAT, 2006. Evaluation of SAR procedures for D e determination using single aliquots of

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Assessing the maximum limit of SAR-OSL dating using quartz of different grain sizes

susceptibility changes ( Timar-Gabor and Wintle, 2013 ). It was also observed in these studies that the corrected luminescence signals for fine grains are higher than the ones measured on coarse grains and thus a possible explanation for the lower equivalent doses measured on fine grains could reside in the interpolation of these values on the different single aliquot regenerative (SAR) dose response curves encountered for the two grain sizes at doses higher than 100 Gy. Furthermore, the 4–11 μm fraction has higher saturation characteristics (D 0 values) compared to the 63

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Feasibility of the Sar Technique on Quartz Sand of Terraces of NW Himalaya: A Case Study from Devprayag

Feasibility of the Sar Technique on Quartz Sand of Terraces of NW Himalaya: A Case Study from Devprayag

Optically Stimulated Luminescence (OSL) dating technique based on the Single Aliquot Regenerative dose (SAR) protocol is being used increasingly as a means of establishing sediment burial age in the late Quaternary studies. Thermal transfer, low and changing luminescence sensitivity of quartz grains of young sedimentary belts of the New Zealand Alps and the north-east Himalaya poses problems in using SAR protocol. Records of active tectonics and signatures of palaeo-climate are preserved in the Quaternary - Holocene terrace sediments. Therefore, to unfold the history of successive tectonic and palaeo-climate events, robust chronological technique is needed. Palaeoflood deposits in NW Lesser Himalayan region receive quartz from the weathering of various rock types such as quartzite and phyllite in the Alaknanda Basin. A series of tests e.g. dose recovery, preheat plateau, thermal recuperation and change in sensitivity, were performed to check the suitability of quartz grains collected from the terrace sediment of Devprayag of the NW Himalaya, for OSL studies. Inferences were drawn regarding the source of the quartz grains on the basis of the geochemistry and luminescence intensity of the terrace sediment. The study shows that though quartz from the North West Himalaya are low in luminescence intensity but the reproducibility of De value makes the quartz sand suitable for SAR dating technique. Relation between luminescence intensity with CIA values help to predict the provenance of quartz sand. Tests show that the quartz from NW Himalaya is suitable for SAR protocol in OSL.

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Spatial Distribution of Oil Spills at the Sea Surface in the Southeastern Baltic Sea According to Satellite Sar Data

Telecommunication , 16 (4): 296–304. 6. Espedal, H.A. (1999) Satellite SAR oil spill detection using wind history information. International Journal of Remote Sensing , 20 (1): 49-65. DOI: 10.1080/014311699213596. 7. HELCOM 2018. HELCOM Maritime Assessment 2018. (2018) in: Baltic Sea Environment Proceedings, no. 152. Helsinki: Helsinki Commission. 8. Indregard, M., Solberg, A., and Clayton, P. (2004) D2-Report on Benchmarking Oil Spill Recognition Approaches and Best Practice . Technical Report. Oceanids Project, European Commission, Archive No. 04-10225-A

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