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Journal articles on the topic 'Over the horizon'

Author: Grafiati

Published: 4 June 2021

Last updated: 15 February 2022

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1

Joshi, Yash Pal. "The Desirability Index: A Measure For The Desirability Of Stocks Over Bonds Over The Long Term." Journal of Applied Business Research (JABR) 10, no. 1 (September 27, 2011): 62. http://dx.doi.org/10.19030/jabr.v10i1.5964.

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<span>One of the long held beliefs in the field of investments is that stocks are more desirable as compared to bonds for long horizon portfolios. But how long is the long horizon? This paper defines two summary measuresthe Desirability Index and the Cutoff Horizonto measure the desirability of stocks over bonds, and concludes that, based on historical performance, stocks are more desirable than bonds for horizons longer than 15 years.</span>

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2

Georges, T. M., and J. A. Harlan. "New horizons for over-the-horizon radar?" IEEE Antennas and Propagation Magazine 36, no. 4 (August 1994): 14–24. http://dx.doi.org/10.1109/74.317763.

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3

Murphy, Richard W. "Over the horizon." Index on Censorship 25, no. 4 (July 1996): 69–72. http://dx.doi.org/10.1080/03064229608536119.

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4

Kamara, Avraham, Robert A. Korajczyk, Xiaoxia Lou, and Ronnie Sadka. "Horizon Pricing." Journal of Financial and Quantitative Analysis 51, no. 6 (December 2016): 1769–93. http://dx.doi.org/10.1017/s0022109016000685.

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The literature documents heterogeneity in the delay of stock price reaction to systematic shocks, implying that asset risk depends on investment horizon. We study the pricing of risk factors across investment horizons. Value (liquidity) risk is priced over intermediate (short) horizons. Conditioning horizon-factor exposures on firm characteristics indicates that characteristics, with the exception of momentum, are not priced beyond their contribution to systematic risk. Long-horizon institutional investors overweight assets with high intermediate-horizon exposures to value risk and high short-horizon exposures to liquidity risk. The results highlight the importance of investment horizon in determining risk premia.

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5

Gershon, Diane. "Still over the horizon." Nature 348, no. 6296 (November 1990): 7. http://dx.doi.org/10.1038/348007c0.

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6

Gruenewald, David Allan. "Drifting Over the Horizon." JAMA 326, no. 9 (September 7, 2021): 811. http://dx.doi.org/10.1001/jama.2021.14031.

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7

Kryzevicius, Z., D. Karcauskiene, E. Álvarez-Rodríguez, A. Zukauskaite, A. Slepetiene, and J. Volungevicius. "The effect of over 50 years of liming on soil aluminium forms in a Retisol." Journal of Agricultural Science 157, no. 1 (January 2019): 12–19. http://dx.doi.org/10.1017/s0021859619000194.

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AbstractThe aim of the current study was to evaluate the effect of long-term (56 years) liming on changes in soil pH and aluminium (Al) forms in the soil profile compared with an unlimed soil in a sandy moraine loam of a Dystric Glossic Retisol. Long-term liming had a significant influence on soil acidity of the whole profile, causing increased pH values in the following horizons to 120 cm depth: the ploughing horizon (Ahp), where humus accumulates; the eluvial horizon (E), from which clay particles are leached; a horizon having retic properties and predominantly coarser-textured albic material (E/B); and a horizon with retic properties and predominantly finer-textured argic material (B/E). In the solid phase, non-crystalline Al in limed soil decreased in the Ahp horizon; meanwhile a decrease in total organically bound Al (Alp) and organo–Al complexes of low to medium stability was detected in the deeper El and ElBt horizons. High-stability Al complexes with organic matter were the predominant form of Alp in the unlimed and limed whole soil profile. The concentration of total water-soluble Al ranged from 0.61 to 0.80 mg/l in the limed soil profile but 0.62–1.15 mg/l in the unlimed soil. The highest concentration of exchangeable Al was determined in the upper horizons of the unlimed soil profile and the concentration decreased significantly in the same horizons of the limed soil profile. Long-term liming promoted changes in Al compounds throughout the soil profile.

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8

Porter-O’Grady, Tim. "A Glimpse Over the Horizon…" Research and Theory for Nursing Practice 16, no. 1 (March 2002): 69–70. http://dx.doi.org/10.1891/rtnp.16.1.69.52998.

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9

Porter-O’Grady, Tim. "A Glimpse Over the Horizon." Research and Theory for Nursing Practice 16, no. 2 (June 2002): 139–40. http://dx.doi.org/10.1891/rtnp.16.2.139.53005.

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10

Porter-O’Grady, Tim. "A Glimpse Over the Horizon." Research and Theory for Nursing Practice 16, no. 3 (July 2002): 213–14. http://dx.doi.org/10.1891/rtnp.16.3.213.53010.

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11

Porter-O’Grady, Tim. "A Glimpse Over the Horizon." Research and Theory for Nursing Practice 16, no. 4 (December 2002): 291–92. http://dx.doi.org/10.1891/rtnp.16.4.291.53026.

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12

Pelopidas, Benoit. "Over the Horizon Proliferation Threats." Intelligence and National Security 28, no. 6 (December 2013): 926–28. http://dx.doi.org/10.1080/02684527.2013.786608.

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13

Porter-O??Grady, Tim. "A Glimpse Over the Horizon." Orthopaedic Nursing 17, Suppl. 2 (March 1998): 53. http://dx.doi.org/10.1097/00006416-199803001-00011.

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14

Maddox, John. "Time machines still over horizon." Nature 367, no. 6463 (February 1994): 509. http://dx.doi.org/10.1038/367509a0.

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15

Jones, Peter. "Prediction Remains Over the Horizon." British Journal of Psychiatry 172, no. 4 (April 1998): 315. http://dx.doi.org/10.1192/s0007125000149876.

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16

Lou, Yihuai, Bo Zhang, Tengfei Lin, and Danping Cao. "Seismic horizon picking by integrating reflector dip and instantaneous phase attributes." GEOPHYSICS 85, no. 2 (January 30, 2020): O37—O45. http://dx.doi.org/10.1190/geo2018-0303.1.

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Seismic horizons are the compulsory inputs for seismic stratigraphy analysis and 3D reservoir modeling. Manually interpreting horizons on thousands of vertical seismic slices of 3D seismic survey is a time-consuming task. Automatic horizon interpreting algorithms are usually based on the seismic reflector dip. However, the estimated seismic reflector dip is usually inaccurate near and across geologic features such as unconformities. We are determined to improve the quality of picked horizons using multiple seismic attributes. We assume that seismic horizons follow the reflector dip and that the same horizons should have similar instantaneous phase values. We first generate horizon patches using a reflector dip attribute, which is similar to current methods. We use seismic coherence attribute as the stop criteria for tracking the horizon within each patch. Considering the inaccuracy of reflector dip estimates at and near the discontinuous structures such as fault and unconformities, we use the seismic instantaneous phase attribute to improve the quality of the generated horizon patches. We generate horizons by merging the residual horizon patches and only outputting the best horizon in each iteration. Our method is capable of generating a horizon for each reflection within the 3D seismic survey, and the generated horizons strictly follow the seismic reflections over the whole seismic survey. Finally, each time sample of seismic traces is assigned a chronostratigraphic relative geologic time value according to the tracked horizons.

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17

Grishin, Vladimir A., and Igor A. Maslov. "Horizon Line Stability Observations over the Sea." Journal of Navigation 71, no. 2 (October 2, 2017): 437–53. http://dx.doi.org/10.1017/s0373463317000650.

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Increasing the stability and reliability of navigation for mobile objects of different classes is becoming increasingly significant. Satellite navigation systems have a fundamental defect: a vulnerability to hacking and spoofing. Observation of the horizon line is significant for two applications. The first is stellar inertial navigation systems. In this case, the horizon line can be used for local vertical estimation. Errors in local vertical estimation directly affect coordinate errors. The second is correlation-extremal navigation based on the observed horizon line shape (when islands or continents are observed from aerial vehicles). In both cases, instability of the horizon line produces navigation errors. A measurement procedure for horizon line position estimation was proposed and realised. Around-the-clock horizon line shooting was undertaken in 2013. Processing of the results shows a horizon line direction instability of about 5–7 angular minutes during the day time.

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18

Berquist, Thomas H. "New and Just Over the Horizon." American Journal of Roentgenology 195, no. 5 (November 2010): 1049. http://dx.doi.org/10.2214/ajr.10.5682.

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19

Kwon, Seog-Woon. "The KJH: Sailing over the horizon." Korean Journal of Hematology 45, no. 2 (2010): 77. http://dx.doi.org/10.5045/kjh.2010.45.2.77.

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20

Lincoln, Christie M., Ritodhi Chatterjee, and Marc H. Willis. "Augmented Radiology: Looking Over the Horizon." Radiology: Artificial Intelligence 1, no. 1 (January 2019): e180039. http://dx.doi.org/10.1148/ryai.2019180039.

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21

Headrick, J. M. "Looking over the horizon (HF radar)." IEEE Spectrum 27, no. 7 (July 1990): 36–39. http://dx.doi.org/10.1109/6.58421.

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22

Belov, V. V., M. V. Tarasenkov, V. N. Abramochkin, and V. O. Troitskii. "Over-the-Horizon Optoelectronic Communication Systems." Russian Physics Journal 57, no. 7 (November 2014): 963–68. http://dx.doi.org/10.1007/s11182-014-0331-6.

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23

Huebner, Stephen B. "Storm clouds over the environmental horizon." Society 36, no. 3 (March 1999): 57–67. http://dx.doi.org/10.1007/s12115-999-1010-z.

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24

Chen, Chunyu, Wenjie Dong, and Vladimir Djapic. "DistributedH2/H∞filtering over infinite horizon." International Journal of Adaptive Control and Signal Processing 32, no. 2 (December 11, 2017): 330–43. http://dx.doi.org/10.1002/acs.2847.

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25

Nelms, SE, J. Alfaro-Shigueto, JPY Arnould, IC Avila, S. Bengtson Nash, E. Campbell, MID Carter, et al. "Marine mammal conservation: over the horizon." Endangered Species Research 44 (March 25, 2021): 291–325. http://dx.doi.org/10.3354/esr01115.

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Marine mammals can play important ecological roles in aquatic ecosystems, and their presence can be key to community structure and function. Consequently, marine mammals are often considered indicators of ecosystem health and flagship species. Yet, historical population declines caused by exploitation, and additional current threats, such as climate change, fisheries bycatch, pollution and maritime development, continue to impact many marine mammal species, and at least 25% are classified as threatened (Critically Endangered, Endangered or Vulnerable) on the IUCN Red List. Conversely, some species have experienced population increases/recoveries in recent decades, reflecting management interventions, and are heralded as conservation successes. To continue these successes and reverse the downward trajectories of at-risk species, it is necessary to evaluate the threats faced by marine mammals and the conservation mechanisms available to address them. Additionally, there is a need to identify evidence-based priorities of both research and conservation needs across a range of settings and taxa. To that effect we: (1) outline the key threats to marine mammals and their impacts, identify the associated knowledge gaps and recommend actions needed; (2) discuss the merits and downfalls of established and emerging conservation mechanisms; (3) outline the application of research and monitoring techniques; and (4) highlight particular taxa/populations that are in urgent need of focus.

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26

Lou, Yihuai, Bo Zhang, Huijing Fang, Danping Cao, Kangning Wang, and Zhizhou Huo. "Simulating the procedure of manual seismic horizon picking." GEOPHYSICS 86, no. 1 (January 1, 2021): O1—O12. http://dx.doi.org/10.1190/geo2020-0021.1.

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Manual seismic horizon picking is the least efficient interpretation technique in terms of time and effort. The loop-tie is a key “element” and the most time-consuming task in manual horizon picking, which ensures the accuracy of horizon picking. Autopicking techniques have been used since the early 1980s. However, there are few studies simulating the procedure of manual seismic horizon picking and quantitatively evaluating the autopicked horizons. In our proposed method, we perform autopicking on inline and crossline seismic vertical slices independently, similar to the manual horizon picking procedure. We then evaluate the picked horizons using a loop-tie step similar to the loop-tie checking in manual horizon picking. To simulate the loop-tie step in manual picking, we define two dip attributes for each time sample of seismic traces, which are the “left” and “right” reflector dips. We only preserve the portions of the tracked horizons that meet the defined loop-tie checking. Next, we merge the tracked horizons centered at the seeded seismic traces. The two-way traveltime of the merged horizons functions as a “hard” control for the final step of autopicking. Finally, we use the seismic dip attribute to track the horizons over the seismic survey under the hard controls. The real data demonstrate that our algorithm can extract accurate horizons near discontinuities such as faults and unconformities.

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27

Brennan, Michael J., and Yuzhao Zhang. "Capital Asset Pricing with a Stochastic Horizon." Journal of Financial and Quantitative Analysis 55, no. 3 (October 24, 2018): 783–827. http://dx.doi.org/10.1017/s0022109018001412.

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In this paper we present empirical tests of an extended version of the capital asset pricing model (CAPM) that replaces the single-period horizon with a probability distribution over different horizons. Adopting a simple parameterization of the probability distribution of the length of the horizon, we estimate the parameters of the distribution as well as the parameters of the CAPM. We find that the extended model is not rejected for several different samples of common stocks, and for these samples it outperforms not only the standard CAPM but also the Fama–French (1993) 3-factor model. The probability distribution over horizon dates varies over time with the New York Stock Exchange (NYSE) turnover rate. We also find that returns satisfy the Euler equation of a representative financial institution that holds the market portfolio and has horizon probabilities estimated from 13F filings.

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28

Mohandes, Mohamed. "Multiple over-the-horizon radar track association." Optical Engineering 36, no. 3 (March 1, 1997): 716. http://dx.doi.org/10.1117/1.601269.

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29

Berrade, M. D., C. A. V. Cavalcante, and P. A. Scarf. "Modelling imperfect inspection over a finite horizon." Reliability Engineering & System Safety 111 (March 2013): 18–29. http://dx.doi.org/10.1016/j.ress.2012.10.003.

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30

Boland, C. Richard, and Daniel C. Demarco. "Preventing Colon Cancer: Looking Over the Horizon." Baylor University Medical Center Proceedings 16, no. 3 (July 2003): 344–45. http://dx.doi.org/10.1080/08998280.2003.11927923.

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31

Anonymous. "Over-the-horizon radar research consortium formed." Eos, Transactions American Geophysical Union 75, no. 27 (1994): 306. http://dx.doi.org/10.1029/94eo00967.

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32

Pijnappels, Kees. "Europese conventie over advocaten gloort aan horizon." Advocatenblad 98, no. 8 (October 2018): 43. http://dx.doi.org/10.5553/ab/0165-13312018098008017.

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33

Bean, James C., and Robert L. Smith. "Optimal Capacity Expansion Over an Infinite Horizon." Management Science 31, no. 12 (December 1985): 1523–32. http://dx.doi.org/10.1287/mnsc.31.12.1523.

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34

Andrianov, Vladimir, Valia Bourmpoula, Juan Chacaltana, Sukti Dasgupta, Marta Duda, Ekkehard Ernst, Salwa Haidar, et al. "Summary: Renewed Turbulence Over the Employment Horizon." World Employment and Social Outlook 2015, no. 1 (January 2015): i—4. http://dx.doi.org/10.1002/wow3.55.

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35

Ebrahimi, Nader, S. N. U. A. Kirmani, and Ehsan S. Soofi. "Predictability of operational processes over finite horizon." Naval Research Logistics (NRL) 58, no. 6 (June 17, 2011): 531–45. http://dx.doi.org/10.1002/nav.20465.

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36

Cervera, M. A., D. B. Francis, and G. J. Frazer. "Climatological Model of Over-the-Horizon Radar." Radio Science 53, no. 9 (September 2018): 988–1001. http://dx.doi.org/10.1029/2018rs006607.

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37

Diercks, Marie-Luise, Ursula von der Leyen, and Magnus Lerch. "Public Health Studiengänge: „Looking Over The Horizon” ..." Public Health Forum 8, no. 1 (March 1, 2000): 24. http://dx.doi.org/10.1515/pubhef-2000-1690.

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38

Otsubo, Hironori, and Amnon Rapoport. "Dynamic Volunteer's Dilemmas over a Finite Horizon." Journal of Conflict Resolution 52, no. 6 (July 28, 2008): 961–84. http://dx.doi.org/10.1177/0022002708321401.

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39

Nikitin, A. K., V. V. Gerasimov, A. G. Lemzyakov, B. A. Knyazev, and I. A. Azarov. "Over-the-Horizon Terahertz Surface Plasmon Locator." Journal of Infrared, Millimeter, and Terahertz Waves 41, no. 2 (December 9, 2019): 194–201. http://dx.doi.org/10.1007/s10762-019-00649-2.

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40

Dębicki, Krzysztof, Enkelejd Hashorva, and LanPeng Ji. "Parisian ruin over a finite-time horizon." Science China Mathematics 59, no. 3 (October 13, 2015): 557–72. http://dx.doi.org/10.1007/s11425-015-5073-6.

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41

H. Melad, Tarek Ibrahim. "Data Network Security Over The Horizon Radar." International Journal of Scientific and Research Publications (IJSRP) 11, no. 7 (July 24, 2021): 730–46. http://dx.doi.org/10.29322/ijsrp.11.07.2021.p11598.

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42

Pietranik, Anna, Jakub Kierczak, Rafał Tyszka, and Bernhard Schulz. "Understanding Heterogeneity of a Slag-Derived Weathered Material: The Role of Automated SEM-EDS Analyses." Minerals 8, no. 11 (November 8, 2018): 513. http://dx.doi.org/10.3390/min8110513.

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Slag heaps over years may evolve into complexly weathered zones, which are a challenging material for analyses as they contain phases from numerous sources and at different stages of weathering. However, the weathered zones are important parts of slag heaps, because they contain both primary and secondary phases enriched in metal(oid)s that may become soluble under specific conditions. The weathering reactions related to metal release or precipitation may be recorded in a heavy mineral fraction as the fraction contains predominately minerals with elevated toxic elements concentrations. Therefore, an automated SEM analysis on a polished section of included heavy mineral particles was applied in this paper for a rapid recognition of phases in a complex setting and their classification into detrital, primary and secondary phases. The approach was applied to a slag heap in Świętochłowice (Upper Silesia, Poland) and it consisted of analyzing magnetic and non-magnetic heavy mineral fractions from three distinct horizons noted A, B and C. Materials had been previously interpreted as being sourced from the heap itself (lowermost horizon C) and from artificially added materials used later for superficial site remediation (upper horizons A and B). Instead, automated SEM analysis demonstrated that horizon C is derived from the slag heap weathering, horizon B is derived predominately from the artificially added materials, whereas horizon A is a mixture of the B and C horizons. Additionally, when slag particles in horizons A and C are compared, the lowermost horizon C contains more slag-derived secondary phases, whereas horizon A contains more primary slag phases. Therefore, horizon A remains the most prone to releasing toxic elements because, considering its position as the uppermost horizon, it can be submitted to climatic solicitation (fast water circulation).

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43

PELTOLA, ARI, and JARMO MÄKELÄ. "RADIATION OF THE INNER HORIZON OF THE REISSNER–NORDSTRÖM BLACK HOLE." International Journal of Modern Physics D 15, no. 06 (June 2006): 817–43. http://dx.doi.org/10.1142/s0218271806008565.

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Despite over thirty years of research in black hole thermodynamics, our understanding of the possible role played by the inner horizons of Reissner–Nordström and Kerr–Newman black holes in black hole thermodynamics is still somewhat incomplete. There are derivations which imply that the temperature of the inner horizon is negative and it is not quite clear what this means. Motivated by this problem, we perform a detailed analysis of the radiation emitted by the inner horizon of the Reissner–Nordström black hole. As a result, we find that in a maximally extended Reissner–Nordström space–time virtual particle–antiparticle pairs are created at the inner horizon of the Reissner–Nordström black hole such that real particles with positive energy and temperature are emitted towards the singularity from the inner horizon and, as a consequence, antiparticles with negative energy are radiated away from the singularity through the inner horizon. We show that these antiparticles will be emitted from the white hole horizon in the maximally extended Reissner–Nordström space–time, at least when the hole is near extremality. The energy spectrum of the antiparticles leads to a positive temperature for the white hole horizon. In other words, our analysis predicts that in addition to the radition effects of black hole horizons, the white hole horizon also radiates. The black hole radiation is caused by the quantum effects at the outer horizon, whereas the white hole radiation is caused by the quantum effects at the inner horizon of the Reissner–Nordström black hole.

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44

Chakrabarty, Anindya, Rameshwar Dubey, and Anupam De. "An innovative approach to mitigating horizon mismatch." International Journal of Innovation Science 8, no. 2 (June 6, 2016): 161–80. http://dx.doi.org/10.1108/ijis-06-2016-011.

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Purpose This paper aims to propose an innovative approach to risk measurement for the abolition of selection bias arising from the specious selection of different horizons for investment and risk computation of equity-linked-saving schemes (ELSS). Design/methodology/approach ELSS has a lock-in period of three years, but shorter horizons’ (daily/weekly/monthly) return data are preferred, in practice, for risk computation. This results in horizon mismatch. This paper studies the consequences of this mismatch and provides a noble solution to diminish its effect on investors’ decision-making. To accomplish this objective, the paper uses an innovative methodology, maximal overlap discrete wavelet transformation, to segregate the price movements across different horizons. Risk across all horizons is measured using Cornish-Fisher expected shortfall and Cornish-Fisher value-at-risk methods. Findings The degree of consistency of risk-based rankings across horizons is examined by means of the Spearman and Kendall’s rank correlation tests. The risk-based ranking of ELSS is found to vary significantly with the change in investor’s horizon. Precisely, the rankings formulated using daily net asset values are significantly different from the rankings developed using fluctuations over longer horizons (two-four and four-eight years). Originality/value This finding indicates that the ranking exercise may mislead investors if horizon correction is not done while developing such rankings.

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45

Coskun, Yener, Christos Bouras, Rangan Gupta, and Mark E. Wohar. "Multi-Horizon Financial and Housing Wealth Effects across the U.S. States." Sustainability 13, no. 3 (January 28, 2021): 1341. http://dx.doi.org/10.3390/su13031341.

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We investigate for the presence of multi-horizon wealth effects across U.S. states over the period of 1975:Q2 to 2012:Q2 by utilizing multi-horizon non-causality testing and multi-horizon causality measurement. At the state/aggregate level, we document that housing wealth has more statistically significant and persistent impact on private consumption than financial wealth. We also find that state-level housing/financial wealth effects are present at long time horizons and exhibit heterogeneity across the U.S. From a policy perspective, we suggest that state-level policies may specifically utilize the housing market to support consumption and growth.

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46

Ewing, Blake. "Koselleck’s Historik and the Horizons of Politics." Contributions to the History of Concepts 13, no. 2 (December 1, 2018): 79–99. http://dx.doi.org/10.3167/choc.2018.130204.

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Political theorists, especially in the subfield of ideology studies, continue to draw insights from Begriffsgeschichte (conceptual history) to help them better analyze the morphology of political concepts over time. However, other aspects of Reinhart Koselleck’s work remain underutilized. This is especially true of the connections between Begriffsgeschichte and his development of a theory of history (Historik), dealing with the broader intersection of language, structure, and the experience of time. This article focuses on just one aspect of this intersection: on the potential relevance of Koselleck’s use of the concept of horizon to theorize a particular “horizonal mode” of the politics of time. After discussing some relevant features of the horizon metaphor, the article moves to reappraise Koselleck’s use of the concept before elaborating and expanding on it to claim that Koselleck helps to showcase the contestation of different temporal horizons as a core feature of political thinking.

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47

O. Etuk, Nyeneime, Mfoniso U. Aka, Okechukwu A. Agbasi, and Johnson C. Ibuot. "Evaluation of seismic attributes for reservoir characterization over Edi field, Niger delta, Nigeria using 3d seismic data." International Journal of Advanced Geosciences 8, no. 2 (September 19, 2020): 168. http://dx.doi.org/10.14419/ijag.v8i2.31043.

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Seismic attributes were evaluated over Edi field, offshore Western Niger Delta, Nigeria, via 3D seismic data. Manual mappings of the horizons and faults on the in-lines and cross-lines of the seismic sections were done. Various attributes were calculated and out put on four horizons corresponding to the well markers at different formations within the well were identified. The four horizons identified, which includes: H1, H2, H3 and H4 were mapped and interpreted across the field. The operational agenda was thru picking given faults segments on the in–line of seismic volume. A total of five faults coded as F1, F2, F3, F4 and F5, F1 and F5 were the major fault and were observed as extending through the field. Structural and horizon mappings were used to generate time structure maps. The maps showed the various positions and orientations of the faults. Different attributes which include: root mean square amplitude, instantaneous phase, gradient magnitude and chaos were run on the 3D seismic data. The amplitude and incline magnitude maps indicate direct hydrocarbon on the horizon maps; this is very important in the drilling of wells because it shows areas where hydrocarbons are present in the subsurface. The seismic attributes revealed information, which was not readily apparent in the raw seismic data.

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48

Chen, Hao, Feng Yang, Yongqi Wang, and Quan Pan. "An over-the-horizon radar multipath fusion algorithm." Journal of Shenzhen University Science and Engineering 31, no. 2 (2014): 130. http://dx.doi.org/10.3724/sp.j.1249.2014.02130.

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49

Dieker, A. B. "Extremes of Gaussian processes over an infinite horizon." Stochastic Processes and their Applications 115, no. 2 (February 2005): 207–48. http://dx.doi.org/10.1016/j.spa.2004.09.005.

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