Hull Speed 2017.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

Hull Speed 2017.Pdf HULL SPEED AN INSIGHT INTO THE PRINCIPAL BARRIER TO HIGH SPEED UNDER SAIL ALAN SKINNER HULL SPEED AN INSIGHT INTO THE PRINCIPAL BARRIER TO HIGH SPEED UNDER SAIL ALAN SKINNER PREFACE Sailboat design is an art and, as for all art, success demands not only the development of natural talent but also an intimate knowledge of the subject. For sailboat design, the accumulation of that knowledge has been a lengthy, evolutionary process, beginning in prehistory and achieving a significant level of advancement by the time of man's earliest records. The proas and double canoes of Oceania, the junks of Asia and the Viking ships of Europe typify the extraordinary refinement and diversification of evolutionary design evident throughout the history of the maritime world. Although aided by increasingly sophisticated technology, modern sailboat design is essentially an extension of that evolutionary process. Today, the theory of all boat design is regarded as an engineering science, whereby the behaviour of a vessel is explained by the application of mathematics. However, some factors that determine the performance of a boat, especially under sail, are still seemingly impossible to resolve other than by empirical methods. Consequently, the theory of certain aspects of sailboat design remains limited to broad principles, the interpretations of which are dependent on the adeptness of the designer. Shaping a hull to reduce resistance is the most fundamental, most studied but generally the least understood feature of design for all types of vessels. Surface waves caused by the forward motion of a hull represent a major component of a vessel‘s total resistance. But, despite being the most visible form of resistance and the principal barrier to high speed under sail, the causes and effects of wave-making are commonly misunderstood. Although detailed analyses of wave-making resistance are to be found in advanced texts on hydrodynamics and undoubtedly have their elaborate mathematical solutions in use in today's proliferation of hull design software, very little of that technical knowledge seems to have filtered through to the general world of boating by way of sensible, logical explanation. Hull Speed is not intended as an expert analysis of the resistance caused by the formation of waves but is the product of one layman‘s endeavour to gain an insight into what has always been a most challenging aspect of sailboat design, shaping a hull to reduce wave-making resistance. Presented in two parts, the first, From Theory to Evolution, is introductory, an historical prelude to A Component Waveform Theory, tendered as a fresh, unique and relatively uncomplicated interpretation of wave-making to demonstrate the effect that wave-making has on the performance of a vessel, how wave-making creates a barrier to high speed and, finally, how the resistance due to wave-making might be minimised. At the outset, I readily admit to being unqualified to attempt the analysis of a topic of such complexity, my interest in sailboat design simply stems from an inexplicable lifelong obsession with small boats and sailing. Inevitably, the use of a novel ‗component waveform theory‘ to simplify the technicalities of wave-making is likely to be dismissed as being a very naive approach to an exceptionally complex mathematical problem. It is, but the concept, no matter how elementary or flawed, does help to clarify for laymen an otherwise extremely vague area of hull design. Essentially, Hull Speed is the outcome of a project that began in the early 1970s as an attempt, by me, to design an NS14, an Australian small sailing dinghy capable of efficient planing. Being a novice to sailboat design, my original intention was merely to gain an understanding of the hull design process but almost immediately, because of an apparent lack of useful theoretical design information available, the exercise became, instead, a personal quest to derive a mathematical method for determining the optimum ‗curve of areas‘ for the immersed sections of a hull travelling at any speed, including speeds above ‗hull speed‘. To my knowledge, which remains very wanting in these matters, no one had previously achieved such an objective. Adding to my uncertainty at the time, the science of planing hulls was depicted in the boating publications of the day as almost a distinct discipline, somewhat detached from the traditional approach to the design of displacement hulls. Although that point of view had always seemed strange to me, young and practically ignorant of the history and technicalities of design, there appeared to be unanimous agreement amongst experienced designers of a virtual collapse of traditional design theories once planing began, an opinion that still seems to hold sway today, some four decades later. Nevertheless, having already witnessed first-hand the smooth transition of NS14 sailing dinghies from displacement to planing speeds and convinced that the supposed discontinuity in design philosophy that occurred at ‗hull speed‘ was implausible and seemed to lack a solid scientific basis, I persisted, developing my own lines of thought. During the next couple of years, while struggling to untangle the complexity of wave-making, I inadvertently developed the Component Waveform Theory, a logical approach to minimising the wave-making resistance of a hull at any practical speed, an approach that is straightforward and understandable, in the spirit of the early ‗amateur‘ theorists such as John Scott Russell and Colin Archer, whose theories on how to minimise wave-making resistance are included in the prelude. Subsequent investigation has led to my realisation that all of the know-how necessary to develop a component waveform theory was already common knowledge to designers when boats capable of planing were in the early stage of development, more than one hundred years ago, in the first decade of the 20th century. However, since independently developing the component waveform concept intuitively almost four decades ago, I have yet to encounter a more persuasive account of ‗hull speed‘ or of wave-making resistance generally in any boating publication, old or new. My ongoing exploration of the past and present ‗state-of-the-art‘ of boat design has, if anything, increased my confidence in the Component Waveform Theory which, for laymen at least, has the potential, I believe, to rationalize the conventional approach to sailboat design, hence the compulsion to subject the theory to criticism in the public arena. Alan Skinner Saratoga NSW Australia September, 2014 INDEX FROM THEORY TO EVOLUTION The Age of Sail A New Beginning The Trochoidal Wave Theory A Waveline Theory The Wake A Waveform Theory A Return to Evolution A COMPONENT WAVEFORM THEORY The Component Wave Hull Speed Below Hull Speed Semi-planing and Planing The Theory Applied Fact or Fiction? APPENDIX A Design for a Dinghy FROM THEORY TO EVOLUTION THE AGE OF SAIL A sailboat is unique. Travelling at the interface of two media, a sailboat is supported by the water, continually pitching, rolling, yawing, surging, heaving and heeling on that fluid‘s unpredictable surface while gaining propulsion from the air above, equally unpredictable. Attempts to study sailboat design, even at an elementary level, reveal a complex and indefinite topic. Design possibilities are infinite, exemplified in a broad sense by the multiplicity of traditional and commercial sailing craft that have evolved worldwide over countless generations of designers, builders and sailors. The modern sailboat, having its infancy in the decline of commercial sail during the nineteenth century, is a product of that evolutionary process. The origins of sail precede recorded history, possibly by many thousands of years. Archaeological evidence suggests that as early as the 4th millennium BC, commercial sailing vessels, as distinct from more ancient traditional craft, were in use on the Nile River in Egypt. Similar but unrecorded developments were undoubtedly occurring independently throughout Asia. From that period in the late Stone Age, until the Industrial Revolution more than five thousand years later, the sailing ship evolved at the forefront of man‘s technological achievements. Influenced by the demands of trade, exploration and warfare, development was generally cautious and deliberate, interspersed with the occasional revolutionary innovation and constantly reflecting the ingenuity of the societies involved. Constructed of bundles of reeds, lashed together and bent to form the shape of the hull, the first Egyptian ships were rowed with oars and steered with oars at the stern, a square sail being used for running downwind. These vessels were a development of smaller traditional craft that had been in use by Neolithic man on the Nile for thousands of years. Such had been the impact of reed boats on society that apart from weapons, they are reputed to be often the only manufactured product depicted in early Egyptian art. Although seemingly primitive, reed construction enabled vessels to be quickly and easily built from readily available materials and by using the simplest of tools. Testimony to the adequacy of reed construction and to the refinement of design possible within a stone-age culture is still to be found in several parts of the world and as remote from Egypt as Lake Titicaca, the world‘s highest navigable waterway, shared by Bolivia and Peru in South America. Located on a high plateau in the Andes Mountains, the area surrounding Lake Titicaca is bleak and treeless. Totora reeds growing along the shoreline have long provided the indigenous population with its only source of local boatbuilding material and, even today, using techniques strikingly similar to those of the ancient Egyptians, the reeds are meticulously fashioned into small traditional boats that are not only superbly functional works of art but have the advantage of being inherently buoyant. Usually poled through the shallows, the boats can be sailed downwind like their Egyptian counterparts, using a sail woven from the reeds.
Recommended publications
  • Trimarans and Outriggers
    TRIMARANS AND OUTRIGGERS Arthur Fiver's 12' fibreglass Trimaran with solid plastic foam floats CONTENTS 1. Catamarans and Trimarans 5. A Hull Design 2. The ROCKET Trimaran. 6. Micronesian Canoes. 3. JEHU, 1957 7. A Polynesian Canoe. 4. Trimaran design. 8. Letters. PRICE 75 cents PRICE 5 / - Amateur Yacht Research Society BCM AYRS London WCIN 3XX UK www.ayrs.org office(S)ayrs .org Contact details 2012 The Amateur Yacht Research Society {Founded June, 1955) PRESIDENTS BRITISH : AMERICAN : Lord Brabazon of Tara, Walter Bloemhard. G.B.E., M.C, P.C. VICE-PRESIDENTS BRITISH : AMERICAN : Dr. C. N. Davies, D.sc. John L. Kerby. Austin Farrar, M.I.N.A. E. J. Manners. COMMITTEE BRITISH : Owen Dumpleton, Mrs. Ruth Evans, Ken Pearce, Roland Proul. SECRETARY-TREASURERS BRITISH : AMERICAN : Tom Herbert, Robert Harris, 25, Oakwood Gardens, 9, Floyd Place, Seven Kings, Great Neck, Essex. L.I., N.Y. NEW ZEALAND : Charles Satterthwaite, M.O.W., Hydro-Design, Museum Street, Wellington. EDITORS BRITISH : AMERICAN : John Morwood, Walter Bloemhard "Woodacres," 8, Hick's Lane, Hythe, Kent. Great Neck, L.I. PUBLISHER John Morwood, "Woodacres," Hythc, Kent. 3 > EDITORIAL December, 1957. This publication is called TRIMARANS as a tribute to Victor Tchetchet, the Commodore of the International MultihuU Boat Racing Association who really was the person to introduce this kind of craft to Western peoples. The subtitle OUTRIGGERS is to include the ddlightful little Micronesian canoe made by A. E. Bierberg in Denmark and a modern Polynesian canoe from Rarotonga which is included so that the type will not be forgotten. The main article is written by Walter Bloemhard, the President of the American A.Y.R.S.
    [Show full text]
  • Tātou O Tagata Folau. Pacific Development Through Learning Traditional Voyaging on the Waka Hourua, Haunui
    Tātou o tagata folau. Pacific development through learning traditional voyaging on the waka hourua, Haunui. Raewynne Nātia Tucker 2020 School of Social Sciences and Public Policy, Faculty of Culture and Society A thesis submitted to Auckland University of Technology in fulfilment of the requirements for the degree of Master of Philosophy Table of Contents Table of Contents .......................................................................................................... i Abstract ........................................................................................................................ v List of Figures .............................................................................................................. vi List of Tables ............................................................................................................... vii List of Appendices ...................................................................................................... viii List of Abbreviations .................................................................................................... ix Glossary ....................................................................................................................... x Attestation of Authorship ............................................................................................. xiii Acknowledgements ..................................................................................................... xiv Chapter 1: Introduction ................................................................................................
    [Show full text]
  • Waves and Structures
    WAVES AND STRUCTURES By Dr M C Deo Professor of Civil Engineering Indian Institute of Technology Bombay Powai, Mumbai 400 076 Contact: [email protected]; (+91) 22 2572 2377 (Please refer as follows, if you use any part of this book: Deo M C (2013): Waves and Structures, http://www.civil.iitb.ac.in/~mcdeo/waves.html) (Suggestions to improve/modify contents are welcome) 1 Content Chapter 1: Introduction 4 Chapter 2: Wave Theories 18 Chapter 3: Random Waves 47 Chapter 4: Wave Propagation 80 Chapter 5: Numerical Modeling of Waves 110 Chapter 6: Design Water Depth 115 Chapter 7: Wave Forces on Shore-Based Structures 132 Chapter 8: Wave Force On Small Diameter Members 150 Chapter 9: Maximum Wave Force on the Entire Structure 173 Chapter 10: Wave Forces on Large Diameter Members 187 Chapter 11: Spectral and Statistical Analysis of Wave Forces 209 Chapter 12: Wave Run Up 221 Chapter 13: Pipeline Hydrodynamics 234 Chapter 14: Statics of Floating Bodies 241 Chapter 15: Vibrations 268 Chapter 16: Motions of Freely Floating Bodies 283 Chapter 17: Motion Response of Compliant Structures 315 2 Notations 338 References 342 3 CHAPTER 1 INTRODUCTION 1.1 Introduction The knowledge of magnitude and behavior of ocean waves at site is an essential prerequisite for almost all activities in the ocean including planning, design, construction and operation related to harbor, coastal and structures. The waves of major concern to a harbor engineer are generated by the action of wind. The wind creates a disturbance in the sea which is restored to its calm equilibrium position by the action of gravity and hence resulting waves are called wind generated gravity waves.
    [Show full text]
  • Arxiv:1903.11909V1 [Physics.Flu-Dyn] 28 Mar 2019
    Exact solution for progressive gravity waves on the surface of a deep fluid Nail S. Ussembayev∗ Computer, Electrical, and Mathematical Sciences and Engineering Divison King Abdullah University of Science and Technology, Thuwal 23955-6900, KSA Gerstner or trochoidal wave is the only known exact solution of the Euler equations for periodic surface gravity waves on deep water. In this Letter we utilize Zakharov’s variational formulation of weakly nonlinear surface waves and, without truncating the Hamiltonian in its slope expansion, derive the equations of motion for unidirectional gravity waves propagating in a two-dimensional flow. We obtain an exact solution of the evolution equations in terms of the Lambert W -function. The associated flow field is irrotational. The maximum wave height occurs for a wave steepness of 0.2034 which compares to 0.3183 for the trochoidal wave and 0.1412 for the Stokes wave. Like in the case of Gerstner’s solution, the limiting wave of a new type has a cusp of zero angle at its crest. Background.—The water waves problem even in the tial evaluated on the free surface. The expansion coef- completely idealized setting of a perfect fluid is notori- ficients simplify remarkably for two-dimensional waves ously difficult from a mathematical point of view. This propagating in the same direction and the infinite series is one of the reasons we have very few explicit solutions can be summed in a closed form if the wave steepness to the fully nonlinear free-surface hydrodynamics equa- is small. From the stationary periodic solution of the tions despite extensive research over hundreds of years.
    [Show full text]
  • Realistic Simulation of Ocean Surface Using Wave Spectra Jocelyn Fréchot
    Realistic simulation of ocean surface using wave spectra Jocelyn Fréchot To cite this version: Jocelyn Fréchot. Realistic simulation of ocean surface using wave spectra. Proceedings of the First International Conference on Computer Graphics Theory and Applications (GRAPP 2006), 2006, Por- tugal. pp.76–83. hal-00307938 HAL Id: hal-00307938 https://hal.archives-ouvertes.fr/hal-00307938 Submitted on 29 Jul 2008 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. REALISTIC SIMULATION OF OCEAN SURFACE USING WAVE SPECTRA Jocelyn Frechot´ LaBRI - Laboratoire bordelais de recherche en informatique Domaine universitaire, 351 cours de la Liber´ ation, 33405 Talence CEDEX, France [email protected] Keywords: Natural phenomena, realistic ocean waves, procedural animation, parametric energy spectra Abstract: We present a method to simulate ocean surfaces away from the coast, with correct statistical wave height and direction distributions. By using classical oceanographic parametric wave spectra, our results fit real world measurements, without depending on them. Since wave spectra are independent of the ocean model, Gerstner parametric equations and Fourier transform method can be used with them. Moreover, since they are simple to use and need very few parameters, they allow easy production of ocean surface animations usable in movies and games.
    [Show full text]
  • Micro Ocean Renewable Energy
    Micro Ocean Renewable Energy Harvesting ocean kinetic energy to power sonobuoys, navigational aids, weather buoys, emergency rescue devices, domain awareness sensors and fishery devices a Small Business Innovative Research proposal submitted to: The Naval Air Systems Command Acoustic Systems Division, Code 4.5.14 Naval Air Warfare Center Patuxent River, Maryland 20670 submitted by: Tocreo Mark Krawczewicz Eric Greene Labs Tocreo Labs Eric Greene Associates 410.562.9846 410.263.1348 e [email protected] [email protected] Tocreo Labs Eric Greene Associates, Inc. Table of Contents Background .....................................................................................................................................................2 Abstract ...........................................................................................................................................................2 Anticipated Benefits ........................................................................................................................................2 Keywords ........................................................................................................................................................2 Identification and Significance of the Problem or Opportunity.......................................................................3 Phase I Technical Objectives...........................................................................................................................5 Phase I Work Plan ...........................................................................................................................................5
    [Show full text]
  • Guide Wave Analysis and Forecasting
    WORLD METEOROLOGICAL ORGANIZATION GUIDE TO WAVE ANALYSIS AND FORECASTING 1998 (second edition) WMO-No. 702 WORLD METEOROLOGICAL ORGANIZATION GUIDE TO WAVE ANALYSIS AND FORECASTING 1998 (second edition) WMO-No. 702 Secretariat of the World Meteorological Organization – Geneva – Switzerland 1998 © 1998, World Meteorological Organization ISBN 92-63-12702-6 NOTE The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the World Meteorological Organization concerning the legal status of any country, territory, city or area, or of its authorities or concerning the delimitation of its fontiers or boundaries. CONTENTS Page FOREWORD . V ACKNOWLEDGEMENTS . VI INTRODUCTION . VII Chapter 1 – AN INTRODUCTION TO OCEAN WAVES 1.1 Introduction . 1 1.2 The simple linear wave . 1 1.3 Wave fields on the ocean . 6 Chapter 2 – OCEAN SURFACE WINDS 2.1 Introduction . 15 2.2 Sources of marine data . 16 2.3 Large-scale meteorological factors affecting ocean surface winds . 21 2.4 A marine boundary-layer parameterization . 27 2.5 Statistical methods . 32 Chapter 3 – WAVE GENERATION AND DECAY 3.1 Introduction . 35 3.2 Wind-wave growth . 35 3.3 Wave propagation . .36 3.4 Dissipation . 39 3.5 Non-linear interactions . .40 3.6 General notes on application . 41 Chapter 4 – WAVE FORECASTING BY MANUAL METHODS 4.1 Introduction . 43 4.2 Some empirical working procedures . 45 4.3 Computation of wind waves . 45 4.4 Computation of swell . 47 4.5 Manual computation of shallow-water effects . 52 Chapter 5 – INTRODUCTION TO NUMERICAL WAVE MODELLING 5.1 Introduction .
    [Show full text]
  • Forschergruppe CSG-II W O R K S H P Freitag, 18
    Wissen Forschergruppe CSG-II W O R K S H P Freitag, 18. März 2011 9:30 Rebekka Ladewig Glauben – Können – Wissen: Passagen des Impliziten bei Michael Polanyi 10:30 Kathrin Thiele Henri Bergson: Intuition und Spekulation 11:30 – Kaffeepause – 12:00 Melanie Sehgal Wissen als Glauben bei William James 13:00 – Mittagspause – 14:00 Martin Thiering Mentale Modelle: Schnittmenge ORT zwischen implizitem und explizitem Wissen? Topoi Haus Mitte Seminarraum 15:00 Iris Därmann Hannoversche Str. 6 Wirksame Handlungen: 10115 Berlin Die Techniken des Körpers KONTAKT 16:00 – Kaffeepause – Rebekka Ladewig 16:30 Colin G. King Exzellenzcluster TOPOI Der aristotelische Hexis-Begriff Hannoversche Str. 6 10115 Berlin 17:30 Anna Echterhölter [email protected] Feldhaftung: Bourdieus Habitus- Konzept und die Ordnung der www.topoi.org Körper The Body-Mind Relation [Michael Polanyi's "The Body-Mind Relation" was a paper delivered at a 1966 conference sponsored by the Western Behavioral Sciences Institute, the Salk Institute for Biological Sciences and the University of California, San Diego .. The conference and the book that grew out of it, Man and the Sciences of Man, edited by William R. Coulson and Carl R. Rogers (Columbus, Ohio: Charles E. Merrill Publishing Company, 1968) in which "The Body- Mind Relation was published, were part of the Western Behavioral Science Institute's project investigating the philosophy of the behavioral sciences. "The Body-Mind Relation" is posted on the Polanyi Society web site with the permission of William R.Coulson and John C. Polanyi.] When I point my finger at the wall and call out: "Look at this!" all eyes turn to the wall, away from my finger.
    [Show full text]
  • Downloaded 09/27/21 10:05 AM UTC 166 JOURNAL of PHYSICAL OCEANOGRAPHY VOLUME 43
    JANUARY 2013 C O N S T A N T I N 165 Some Three-Dimensional Nonlinear Equatorial Flows ADRIAN CONSTANTIN* King’s College London, London, United Kingdom (Manuscript received 28 March 2012, in final form 11 October 2012) ABSTRACT This study presents some explicit exact solutions for nonlinear geophysical ocean waves in the b-plane approximation near the equator. The solutions are provided in Lagrangian coordinates by describing the path of each particle. The unidirectional equatorially trapped waves are symmetric about the equator and prop- agate eastward above the thermocline and beneath the near-surface layer to which wind effects are confined. At each latitude the flow pattern represents a traveling wave. 1. Introduction The aim of the present paper is to provide an explicit nonlinear solution for geophysical waves propagating The complex dynamics of flows in the Pacific Ocean eastward in the layer above the thermocline and beneath near the equator presents certain specific features. The the near-surface layer in which wind effects are notice- equatorial region is characterized by a thin, permanent, able. The solution is presented in Lagrangian coordinates shallow layer of warm (and less dense) water overlying by describing the circular path of each particle. Within a deeper layer of cold water. The two layers are separated a narrow equatorial band the flow pattern describes an byasharpthermocline and a plausible assumption is that equatorially trapped wave that is symmetric about the there is no motion in the deep layer—see, for example, equator: at each fixed latitude we have a traveling wave Fedorov and Brown (2009).
    [Show full text]
  • Arxiv:1907.10998V2
    Parametric solutions of the generalized short pulse equations Yoshimasa Matsunoa Division of Applied Mathematical Science, Graduate School of Sciences and Technology for Innovation, Yamaguchi University, Ube, Yamaguchi 755-8611, Japan Abstract We consider three novel PDEs associated with the integrable generalizations of the short pulse equation classified recently by Hone et al (2018 Lett. Math. Phys. 108 927-947). In particular, we obtain a variety of exact solutions by means of a direct method analogous to that used for solving the short pulse equation. The main results reported here are the parametric representations of the multisoliton solutions. These solutions include cusp solitons, unbounded solutions with finite slope and breathers. In addition, the cusped periodic wave solutions are constructed from the cusp solitons by means of a simple procedure. As for non-periodic solutions, smooth breather solutions are of particular interest from the perspective of applications to real physical phenomena. The cycloid reduced from the periodic traveling wave with cusps is also worth remarking in connection with Gerstner’s trochoidal solution in deep gravity waves. A number of works are left for future study, some of which will be addressed in concluding remarks. arXiv:1907.10998v2 [nlin.SI] 17 Mar 2020 aE-mail address: [email protected] 1 1. Introduction The short pulse (SP) equation is a completely integrable partial differential equation (PDE) in the sence that it admits a Lax pair and an infinite number of conservation laws [1]. It can be written in an appropriate dimensionless form as 1 u = u + (u3) , (1.1) xt 6 xx where u = u(x, t) represents a scalar function of x and t, and subscripts x and t appended to u denote partial differentiations.
    [Show full text]
  • Riesenberg 1972 the Organisation of Navigational Knowledge on Puluwat
    THE ORGANISATION OF NAVIGATIONAL KNOWLEDGE ON PULUWAT Author(s): Saul H. Riesenberg Source: The Journal of the Polynesian Society, Vol. 81, No. 1 (MARCH 1972), pp. 19-56 Published by: The Polynesian Society Stable URL: https://www.jstor.org/stable/20704826 Accessed: 08-10-2018 13:49 UTC JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms The Polynesian Society is collaborating with JSTOR to digitize, preserve and extend access to The Journal of the Polynesian Society This content downloaded from 74.93.217.178 on Mon, 08 Oct 2018 13:49:56 UTC All use subject to https://about.jstor.org/terms THE ORGANISATION OF NAVIGATIONAL KNOWLEDGE ON PULUWAT Saul H. Riesenberg Smithsonian Institution This article describes some of the mnemonic devices and systems of classification employed by the navigators of the atoll of Puluwat (Central Caroline Islands) to arrange their knowledge of geography and of star courses into organised bodies of data. The word geography is used here in a very broad sense, to include both natural and mythical phenomena, and animate beings as well, when they are part of those bodies of data and are used as reference points by navigators in finding their way on the high seas.
    [Show full text]
  • Carolinian Voyaging in the New Millennium
    MICRONESIAN JOURNAL OF THE HUMANITIES AND SOCIAL SCIENCES Vol. 5, nº 1/2 Combined Issue November 2006 CAROLINIAN VOYAGING IN THE NEW MILLENNIUM Eric Metzgar Triton Films, Camarillo, CA A holistic view of the Carolinian voyaging movement to date, highlighting major voyaging achievements as well as the master navigators (palu) who have made significant contributions. The reinvigorization of long-distance voyaging has expanded beyond the Carolininan-Marianas voyaging renaissance into a pan-Carolinian movement with navigators using traditionally-made canoes to make two-way voyages from Yap to Palau in the west and from Polowat to Pohnpei in the east. Using ancient knowledge of non-instrument tion traditions. Many of these navigators have wayfinding that had been handed down for been recognized previously in published arti- generations, master navigators (palu) from cles but some have not, either because they Polowat and Satawal in the later part of the last were formerly apprentices who only recently century rediscovered the 500-mile1 sea route came of age as palu master navigators or the from their islands in the central Carolines2 to nature of their contribution has been that of Saipan and Guam in the Marianas archipelago. teacher more than voyager. In addition, there In so doing they sparked a renaissance of Caro- are many others in “the background” who have linian-Marianas voyaging that continues today. participated in significant ways to the re- First to rediscover the passage from the Caro- invigorization of the Carolinian voyaging line Islands to the Mariana Islands were Hipour movement — both men and women — whose (from Polowat) in 1969, Repunglap and Re- storied achievements and contributions have punglug (from Satawal) in 1970, and Ikuliman yet to come to light.
    [Show full text]