A Liminal Experience Under the Surface of the Ocean

Total Page:16

File Type:pdf, Size:1020Kb

A Liminal Experience Under the Surface of the Ocean UNIVERSIDADE DE LISBOA FACULDADE DE BELAS-ARTES APNEA A liminal experience under the surface of the ocean Janna Nadjejda Ribow Guichet Dissertação Mestrado em Arte Multimedia Especialização em Fotografia Dissertação orientada pela Professora Doutora Maria João Pestana Noronha Gamito 2021 DECLARAÇÃO DE AUTORIA Eu Janna Nadjejda Ribow Guichet, declaro que a presente dissertação de mestrado intitulada “Apnéia”, é o resultado da minha investigação pessoal e independente. O conteúdo é original e todas as fontes consultadas estão devidamente mencionadas na bibliografia ou outras listagens de fontes documentais, tal como todas as citações diretas ou indiretas têm devida indicação ao longo do trabalho segundo as normas académicas. O Candidato [assinatura] Lisboa, 27.10.19 RESUMO O trabalho é sobre uma imersão no oceano e em nós mesmos. A questão é: como podemos obter um efeito positivo por meio do oceano? O primeiro capítulo analisará os pensamentos antigos e contemporâneos do sublime; A figura do vórtice foi usada nas artes e na literatura para criar sensações sublimes, Immanuel Kant e Edmund Burke afirmaram que o sublime pode trazer um efeito positivo que será discutido. Uma sensação sublime diferente é a Liminalidade, que encontrei durante a Apnéia. Muitos artistas descrevem seu poder transformador, que será comparado à pesquisa médica científica. Mas a mensagem fundamental permanece: “A experiência sublime é fundamentalmente transformadora, sobre a relação entre desordem e ordem, e a ruptura das coordenadas estáveis de tempo e espaço. Algo se precipita e somos profundamente alterados.” (Morley, 2010, p.12) O segundo capítulo define Ambientes Imersivos em Artes e Apnéia. Após a experiência liminar comecei a treinar o desporto e aprendi a controlar minha mente e corpo de forma imersiva, o que trouxe à tona os conceitos: ponto do silêncio (preparação), jogo mental (submersão) e foco (volta a superfície). “A imersão ... absorvendo mentalmente é um processo, uma mudança, uma passagem de um estado mental para outro. Caracteriza-se por diminuir a distância crítica em relação ao que é mostrado e aumentar o envolvimento emocional com o que está a acontecer.” (Grau, 2013, p.13) O terceiro capítulo é sobre Apnéia, que é ao mesmo tempo o título da dissertação, e a metodologia para chegar a mim mesma, que aplico na vida real. As minhas metodologias foram a pesquisa sobre o antigo e o sublime contemporâneo. Eu li, analisei e interpretei filosofia, mitos, lendas, literatura e obras de arte em contextos artísticos e científicos. Aprendi e pratiquei na vida real os conceitos imersivos encontrados. Para compartilhar o efeito, aprendi a fotografar debaixo d'água sem oxigênio. O trabalho final é um livro immersivo chamado Ocean Immersion, que tenta tirar o ser humano da vida stressante e contemporânea; acalme-o, deixe-o voltar a focar e preenchê-lo com admiração para abrir um ponto de vista subjetivo sobre nossa existência e como podemos lidar com ela. Palavras-chave: Sublime, Ambientes Imersivos, Liminalidade, Apnéia, Fotografia I II ABSTRACT The work is about an immersion into the ocean and into ourselves. The question is: how can we gain a positive effect through the ocean? The first chapter will analyze the old and contemporary thoughts of the sublime; the figure of the vortex was used in arts and literature to create sublime sensations, Immanuel Kant and Edmund Burke claimed that the sublime can bring up a positive effect which will be discussed. A different sublime sensation is liminality, which I encountered during apnea. Many artists describe it´s transformative power which will be compared to scientific medical research. But the fundamental message remains: “The sublime experience is fundamentally transformative, about the relationship between disorder and order, and the disruption of the stable coordinates of time and space. Something rushes in and we are profoundly altered. “ (Morley, 2010, p.12) The second chapter defines Immersive Environments in Arts and Apnea. After the liminal experience I started to train the sport and learned to control my mind and body in an immersive way, which brought up the concepts: still point (preparation), the mind game (submersion) and the focus (resurface). “Immersion…is mentally absorbing and a process, a change, a passage from one mental state to another. It characterized by diminishing critical distance to what is shown and increasing emotional involvement what is happening.”(Grau, 2013, p.13) The third chapter is about Apnea, which is at the same time the title of the dissertation, and the methodology to arrive to myself, which I apply in real life. My methodology was the research about the old and contemporary sublime. I read, analyzed, and interpreted philosophy, myths, legends, literature and artworks in artistic and scientific contexts. I learned and practiced in real life the immersive concepts which I found. To share the effect, I learned to photograph underwater without oxygen. The final work is an immersive book called Ocean Immersion which attempts to drag the human out of the stressful, contemporary life; calm him down, let him refocus and fulfill him with wonder to open a subjective point of view on our existence and how we should deal with it. Keywords: Sublime, Immersive Environments, Liminality, Apnea, Photography III IV A diver immerses under the surface to watch, a freediver to look into oneself.” Pelizzari, 2014, p.1281. Be free as a wild animal. Dive naked like a dolphin, into the abyss of the sea and fly high into the infinite blue of the sky and glide, silent, like an albatross in the petty world of man; to become air, to be immersed in water and to merge with it and to find yourself again. Jacques Mayol apud Dancini, 2005, p.202. Acknowledgements 1 Original: “El submarinista bucea para ver. El apneista lo hace para mirarse por dentro.” 2 Original: “Ser livre como um animal selvagem. Mergulhar nu, como um golfinho, no abismo do mar e voar bem alto no azul infinito do ceu e planar, silencioso, como um albatroz no mundo mesquinho do homem; tornar-se ar, imergir-se na agua e com ela fundir-se e reecontrar-se.” V Thank you to my love Tomás for bringing me back to the sea Thank you Maria João Gamito for orienting me on this difficult path Thank you, Mafalda and Mario from Spot-Freedive Team, for immersing me into the ocean and for all the free support. Thank you to my parents to grow up close to the sea Thank you to my sisters, brothers and cousins Thank you, my dear family and friends, for your existence Thank you to my dear mother, aunt & Grandma Thank you to Family Guichet VI Index Introduction………………………………………………..…………..…..….….01 1. Sublime……………………………………………….…….……………….….03 1.1 Vortex…………….………………………………………………….……….….04 1.2 Liminality………………………………………………………………………..12 2. Immersive Environments…………………………………….….....19 2.1 Still Point…………………………………………………………………….…..26 2.2 Mind Game……………………………………………………………………....29 2.3 Focus……………………………………………………………………………..35 3. Apnea………………………………………………………………...39 3.1 Description of the project………………………………………………………..43 3.2 Analysis of the artistic work……………………………………………………..68 Conclusion……………………………………………………….……..73 VII Index of Figures Fig.1. Harry Clark: Illustration in E.A.Poe, Descent into the Maelstrom, 1919. (Consulted: 15.04.19; http://rebloggy.com/post/illustration-art-ink-edgar-allan-poe-harry-clarke-descent- into-the-maelstrom-tal/74090937359) Fig.2. Olaus Magnus, Carta Marina, Sweden, 1539. (Consulted: 19.11.18; https://www.ecosia.org/images/?q=carte%20marine%20olaus%20magnus#id=3E6C8EEC0732 E0FFC66C056037C72E5593791424) Fig.3. Olaus Magnus, Carta Marina, Sweden, 1539. (Consulted: 20.10.19; https://fineartamerica.com/featured/carta-marina-map-of-scandinavia-by-olaus-magnus-1539- pablo-romero.html) Fig.4. Ivan Aivazovsky, The Ninth Wave, 1850. (Consulted: 15.04.19; http://the-creative- business.com/de/waves-10-amazing-sea-paintings-by-famous-artists/) Fig.5. Ivan Aivazovsky, Among the Waves, 1898. (Consulted: 15.04.19; https://en.wikipedia.org/wiki/Ivan_Aivazovsky#/media/File:Ayvaz_sredy_voln.jpg) Fig.6. Walter Crane, Neptune´s Horses, 1892. (Consulted: 19.11.18; https://upload.wikimedia.org/wikipedia/commons/c/c2/Walter_Crane_- _Neptune%27s_Horses_%281910%29.jpg) Fig.7. Katsushika Hokusai, The Great Wave of Kanagawa, ca. 1829–1833. (Consulted: 19.11.2018;https://en.wikipedia.org/wiki/The_Great_Wave_off_Kanagawa) Fig.8. Alex Botelho, Praia Norte Nazare, 2016. (Consulted: 20.10.19; http://swell- algarve.com/wp- content/uploads/2016/12/15036530_1447530751941718_716804498001721604_n-1- 750x450.jpg) Fig.9. Gary Hill, Learning Curve, 1993. (Consulted: 2010.19; http://garyhill.com/work/mixed_media_installation/learning-curve.html) Fig.10. Newman, Barnett, Onement VI, 1953. (Consulted: 15.04.19; http://antiquesandartireland.com/wp-content/uploads/2013/04/newman.jpg) Fig.11. Great Frieze of the Dionysiac Mystery, Pompeii, 60. B.C. (Consulted: 20.10.19; https://www.dailymail.co.uk/news/article-3004498/Italy-shows-restored-Pompeii-villa-EU- deadline-looms.html) Fig.12. Anton von Werner and 13 other Painters, The Battle of Sedan, Berlin, 1883. (Consulted: 20.10.19; http://rd.uqam.ca/AHWA/Meetings/2000.CIHA/Grau.html) Fig.13. Monet, Water Lilies series, 1915-1917. (Consulted: 15.01.20; http://content.time.com/time/travel/cityguide/article/0,31489,1937013_1936990_1936849,00.ht ml) Fig.14. Caspar David Friedrich, The Wanderer Above the Sea of Fog, 1818. (Consulted:10.01.20; https://www.geo.de/magazine/geo-epoche-edition/20083-rtkl-deutsche- romantik-caspar-david-friedrich-die-landschaft-der) Fig.15. James Turrell, The Light Inside, 1990. (Consulted: 15.01.20 VIII https://www.archdaily.com/380911/light-matters-seeing-the-light-with-james-turrell) Fig.16. Andrea Pozzo, Nave of Sant´Ignazio, 1694. (Consulted: 20.10.19; https://de.wikipedia.org/wiki/Andrea_Pozzo#/media/Datei:Decke-santignazio-rom.jpg) Fig.17. Gravure Skandalopetra, Greece, 1800. (Consulted: 21.10.19; http:divingheritage.com/greece2.htm) Fig.18-23. Janna Nadjejda, Okeanos, 2018. Fig.24-29. Janna Nadjejda, Immersion, 2018. Fig.30-35. Janna Nadjejda, Kimata, 2019.
Recommended publications
  • Observation of Rip Currents by Synthetic Aperture Radar
    OBSERVATION OF RIP CURRENTS BY SYNTHETIC APERTURE RADAR José C.B. da Silva (1) , Francisco Sancho (2) and Luis Quaresma (3) (1) Institute of Oceanography & Dept. of Physics, University of Lisbon, 1749-016 Lisbon, Portugal (2) Laboratorio Nacional de Engenharia Civil, Av. do Brasil, 101 , 1700-066, Lisbon, Portugal (3) Instituto Hidrográfico, Rua das Trinas, 49, 1249-093 Lisboa , Portugal ABSTRACT Rip currents are near-shore cellular circulations that can be described as narrow, jet-like and seaward directed flows. These flows originate close to the shoreline and may be a result of alongshore variations in the surface wave field. The onshore mass transport produced by surface waves leads to a slight increase of the mean water surface level (set-up) toward the shoreline. When this set-up is spatially non-uniform alongshore (due, for example, to non-uniform wave breaking field), a pressure gradient is produced and rip currents are formed by converging alongshore flows with offshore flows concentrated in regions of low set-up and onshore flows in between. Observation of rip currents is important in coastal engineering studies because they can cause a seaward transport of beach sand and thus change beach morphology. Since rip currents are an efficient mechanism for exchange of near-shore and offshore water, they are important for across shore mixing of heat, nutrients, pollutants and biological species. So far however, studies of rip currents have mainly relied on numerical modelling and video camera observations. We show an ENVISAT ASAR observation in Precision Image mode of bright near-shore cell-like signatures on a dark background that are interpreted as surface signatures of rip currents.
    [Show full text]
  • Part III-2 Longshore Sediment Transport
    Chapter 2 EM 1110-2-1100 LONGSHORE SEDIMENT TRANSPORT (Part III) 30 April 2002 Table of Contents Page III-2-1. Introduction ............................................................ III-2-1 a. Overview ............................................................. III-2-1 b. Scope of chapter ....................................................... III-2-1 III-2-2. Longshore Sediment Transport Processes ............................... III-2-1 a. Definitions ............................................................ III-2-1 b. Modes of sediment transport .............................................. III-2-3 c. Field identification of longshore sediment transport ........................... III-2-3 (1) Experimental measurement ............................................ III-2-3 (2) Qualitative indicators of longshore transport magnitude and direction ......................................................... III-2-5 (3) Quantitative indicators of longshore transport magnitude ..................... III-2-6 (4) Longshore sediment transport estimations in the United States ................. III-2-7 III-2-3. Predicting Potential Longshore Sediment Transport ...................... III-2-7 a. Energy flux method .................................................... III-2-10 (1) Historical background ............................................... III-2-10 (2) Description ........................................................ III-2-10 (3) Variation of K with median grain size................................... III-2-13 (4) Variation of K with
    [Show full text]
  • Microbial Community and Geochemical Analyses of Trans-Trench Sediments for Understanding the Roles of Hadal Environments
    The ISME Journal (2020) 14:740–756 https://doi.org/10.1038/s41396-019-0564-z ARTICLE Microbial community and geochemical analyses of trans-trench sediments for understanding the roles of hadal environments 1 2 3,4,9 2 2,10 2 Satoshi Hiraoka ● Miho Hirai ● Yohei Matsui ● Akiko Makabe ● Hiroaki Minegishi ● Miwako Tsuda ● 3 5 5,6 7 8 2 Juliarni ● Eugenio Rastelli ● Roberto Danovaro ● Cinzia Corinaldesi ● Tomo Kitahashi ● Eiji Tasumi ● 2 2 2 1 Manabu Nishizawa ● Ken Takai ● Hidetaka Nomaki ● Takuro Nunoura Received: 9 August 2019 / Revised: 20 November 2019 / Accepted: 28 November 2019 / Published online: 11 December 2019 © The Author(s) 2019. This article is published with open access Abstract Hadal trench bottom (>6000 m below sea level) sediments harbor higher microbial cell abundance compared with adjacent abyssal plain sediments. This is supported by the accumulation of sedimentary organic matter (OM), facilitated by trench topography. However, the distribution of benthic microbes in different trench systems has not been well explored yet. Here, we carried out small subunit ribosomal RNA gene tag sequencing for 92 sediment subsamples of seven abyssal and seven hadal sediment cores collected from three trench regions in the northwest Pacific Ocean: the Japan, Izu-Ogasawara, and fi 1234567890();,: 1234567890();,: Mariana Trenches. Tag-sequencing analyses showed speci c distribution patterns of several phyla associated with oxygen and nitrate. The community structure was distinct between abyssal and hadal sediments, following geographic locations and factors represented by sediment depth. Co-occurrence network revealed six potential prokaryotic consortia that covaried across regions. Our results further support that the OM cycle is driven by hadal currents and/or rapid burial shapes microbial community structures at trench bottom sites, in addition to vertical deposition from the surface ocean.
    [Show full text]
  • OCEANS ´09 IEEE Bremen
    11-14 May Bremen Germany Final Program OCEANS ´09 IEEE Bremen Balancing technology with future needs May 11th – 14th 2009 in Bremen, Germany Contents Welcome from the General Chair 2 Welcome 3 Useful Adresses & Phone Numbers 4 Conference Information 6 Social Events 9 Tourism Information 10 Plenary Session 12 Tutorials 15 Technical Program 24 Student Poster Program 54 Exhibitor Booth List 57 Exhibitor Profiles 63 Exhibit Floor Plan 94 Congress Center Bremen 96 OCEANS ´09 IEEE Bremen 1 Welcome from the General Chair WELCOME FROM THE GENERAL CHAIR In the Earth system the ocean plays an important role through its intensive interactions with the atmosphere, cryo- sphere, lithosphere, and biosphere. Energy and material are continually exchanged at the interfaces between water and air, ice, rocks, and sediments. In addition to the physical and chemical processes, biological processes play a significant role. Vast areas of the ocean remain unexplored. Investigation of the surface ocean is carried out by satellites. All other observations and measurements have to be carried out in-situ using research vessels and spe- cial instruments. Ocean observation requires the use of special technologies such as remotely operated vehicles (ROVs), autonomous underwater vehicles (AUVs), towed camera systems etc. Seismic methods provide the foundation for mapping the bottom topography and sedimentary structures. We cordially welcome you to the international OCEANS ’09 conference and exhibition, to the world’s leading conference and exhibition in ocean science, engineering, technology and management. OCEANS conferences have become one of the largest professional meetings and expositions devoted to ocean sciences, technology, policy, engineering and education.
    [Show full text]
  • Rip Currents and Alongshore Flows in Single Channels Dredged in the Surf
    PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Rip currents and alongshore flows in single channels dredged 10.1002/2016JC012222 in the surf zone Key Points: Melissa Moulton1,2 , Steve Elgar2 , Britt Raubenheimer2 , John C. Warner3 , and Rip currents, feeder currents, and Nirnimesh Kumar4 meandering alongshore currents were observed in single channels 1 2 dredged in the surf zone Applied Physics Laboratory, University of Washington, Seattle, Washington, USA, Department of Applied Ocean Physics 3 The model COAWST reproduces the and Engineering, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA, United States Geological observed circulation patterns, and is Survey, Coastal and Marine Geology Program, Woods Hole, Massachusetts, USA, 4Department of Civil and Environmental used to investigate dynamics for a Engineering, University of Washington, Seattle, Washington, USA wider range of conditions A parameter based on breaking-wave-driven setup patterns and alongshore currents predicts Abstract To investigate the dynamics of flows near nonuniform bathymetry, single channels (on average offshore-directed flow speeds 30 m wide and 1.5 m deep) were dredged across the surf zone at five different times, and the subsequent evolution of currents and morphology was observed for a range of wave and tidal conditions. In addition, Correspondence to: circulation was simulated with the numerical modeling system COAWST, initialized with the observed M. Moulton, incident waves and channel bathymetry, and with an extended set of wave conditions and channel [email protected] geometries. The simulated flows are consistent with alongshore flows and rip-current circulation patterns observed in the surf zone. Near the offshore-directed flows that develop in the channel, the dominant terms Citation: Moulton, M., S.
    [Show full text]
  • 1D Laboratory Study on Wave-Induced Setup Over A
    1 LES Modeling of Tsunami-like Solitary Wave Processes 2 over Fringing Reefs 3 4 Yu Yao1, 4, Tiancheng He1, Zhengzhi Deng2*, Long Chen1, 3, Huiqun Guo1 5 6 1 School of Hydraulic Engineering, Changsha University of Science and Technology, 7 Changsha, Hunan 410114, China. 8 2 Ocean College, Zhejiang University, Zhoushan, Zhejiang 316021, China. 9 3 Key Laboratory of Water-Sediment Sciences and Water Disaster Prevention of 10 Hunan Province, Changsha 410114, China. 11 4Key Laboratory of Coastal Disasters and Defence of Ministry of Education, 12 Nanjing, Jiangsu 210098, China 13 14 15 16 * Corresponding author: Zhengzhi Deng 17 E-mail: [email protected] 18 Tel: +86 15068188376 19 1 20 ABSTRACT 21 Many low-lying tropical and sub-tropical reef-fringed coasts are vulnerable to 22 inundation during tsunami events. Hence accurate prediction of tsunami wave 23 transformation and runup over such reefs is a primary concern in the coastal management 24 of hazard mitigation. To overcome the deficiencies of using depth-integrated models in 25 modeling tsunami-like solitary waves interacting with fringing reefs, a three-dimensional 26 (3D) numerical wave tank based on the Computational Fluid Dynamics (CFD) tool 27 OpenFOAM® is developed in this study. The Navier-Stokes equations for two-phase 28 incompressible flow are solved, using the Large Eddy Simulation (LES) method for 29 turbulence closure and the Volume of Fluid (VOF) method for tracking the free surface. 30 The adopted model is firstly validated by two existing laboratory experiments with 31 various wave conditions and reef configurations. The model is then applied to examine 32 the impacts of varying reef morphologies (fore-reef slope, back-reef slope, lagoon width, 33 reef-crest width) on the solitary wave runup.
    [Show full text]
  • Dataposter SUMERGIBLES
    TECNOLOGÍA DE LA 8 de junio EXPLORACIÓN MARINA DÍA MUNDIAL DE LOS OCÉANOS LOS EXPLORADORES LAS EXPLORADORAS HISTÓRICOS EN MÉXICO JAQUES VIVIANNE SOLÍS COUSTEAU WEISS (1910-1997) En 1985 se convirtió en la primera Ocial naval francés, explorador, investigadora en jefe de crucero investigador y biólogo marino en los buques de investigación interesado en el estudio del mar y PRESENTA "El Puma" y "Justo Sierra" de la la vida que alberga. Se le UNAM, los cuales también dirigió recuerda por haber presentado al en las expediciones de 1992 y mundo la escafandra autónoma 1993. Fue la primera cientíca con independencia de cables y latinoamericana a bordo del tubos de suministro de aire desde submarino Alvin, sumergiéndose la supercie. a más de 2000 metros de profundidad. JACQUES SUMERGIBLES ELVA ESCOBAR PICCARD BRIONES (1922-2008) Su línea de trabajo se centra en la Explorador, ingeniero y fauna asociada a los fondos oceanógrafo suizo, conocido por DE INVESTIGACIÓN marinos y en la macroecología de el desarrollo de vehículos los ambientes acuáticos. Ha subacuáticos para el estudio de descubierto nuevos ecosistemas las corrientes oceánicas. Piccard y La exploración de las profundidades marinas tiene por objetivo la investigación de las y descrito nuevas especies. Ha Don Walsh fueron, hasta 2012, las representado a México en temas únicas personas que alcanzaron condiciones físicas, químicas y biológicas del lecho marino con motivos científicos o comerciales. de conservación ante la el punto más bajo de la supercie Es una actividad relativamente reciente, pero ha resultado en grandes aportaciones al desarrollo Autoridad Internacional de los terrestre, el abismo Challenger, Fondos Marinos, las Naciones en la fosa de las Marianas.
    [Show full text]
  • Under High Pressure: Spherical Glass Flotation and Instrument Housings in Deep Ocean Research
    PAPER Under High Pressure: Spherical Glass Flotation and Instrument Housings in Deep Ocean Research AUTHORS ABSTRACT Steffen Pausch All stationary and autonomous instrumentation for observational activities in Nautilus Marine Service GmbH ocean research have two things in common, they need pressure-resistant housings Detlef Below and buoyancy to bring instruments safely back to the surface. The use of glass DURAN Group GmbH spheres is attractive in many ways. Glass qualities such as the immense strength– weight ratio, corrosion resistance, and low cost make glass spheres ideal for both Kevin Hardy flotation and instrument housings. On the other hand, glass is brittle and hence DeepSea Power & Light subject to damage from impact. The production of glass spheres therefore requires high-quality raw material, advanced manufacturing technology and expertise in Introduction processing. VITROVEX® spheres made of DURAN® borosilicate glass 3.3 are the hen Jacques Piccard and Don only commercially available 17-inch glass spheres with operational ratings to full Walsh reached the Marianas Trench ocean trench depth. They provide a low-cost option for specialized flotation and W instrument housings. in1960andreportedshrimpand flounder-like fish, it was proven that Keywords: Buoyancy, Flotation, Instrument housings, Pressure, Spheres, Trench, there is life even in the very deepest VITROVEX® parts of the ocean. What started as a simple search for life has become over (1) they need to have pressure- the years a search for answers to basic Advantages and resistant housings to accommodate questions such as the number of spe- Disadvantages sensitive electronics, and (2) they need cies, their distribution ranges, and the of Glass Spheres either positive buoyancy to bring the composition of the fauna.
    [Show full text]
  • Comparative Perspectives on the Rise of the Brazilian Novel COMPARATIVE LITERATURE and CULTURE
    Comparative Perspectives on the Rise of the Brazilian Novel COMPARATIVE LITERATURE AND CULTURE Series Editors TIMOTHY MATHEWS AND FLORIAN MUSSGNUG Comparative Literature and Culture explores new creative and critical perspectives on literature, art and culture. Contributions offer a comparative, cross- cultural and interdisciplinary focus, showcasing exploratory research in literary and cultural theory and history, material and visual cultures, and reception studies. The series is also interested in language-based research, particularly the changing role of national and minority languages and cultures, and includes within its publications the annual proceedings of the ‘Hermes Consortium for Literary and Cultural Studies’. Timothy Mathews is Emeritus Professor of French and Comparative Criticism, UCL. Florian Mussgnug is Reader in Italian and Comparative Literature, UCL. Comparative Perspectives on the Rise of the Brazilian Novel Edited by Ana Cláudia Suriani da Silva and Sandra Guardini Vasconcelos First published in 2020 by UCL Press University College London Gower Street London WC1E 6BT Available to download free: www.uclpress.co.uk Collection © Editors, 2020 Text © Contributors, 2020 The authors have asserted their rights under the Copyright, Designs and Patents Act 1988 to be identified as the authors of this work. A CIP catalogue record for this book is available from The British Library. This book is published under a Creative Commons 4.0 International licence (CC BY 4.0). This licence allows you to share, copy, distribute and transmit the work; to adapt the work and to make commercial use of the work providing attribution is made to the authors (but not in any way that suggests that they endorse you or your use of the work).
    [Show full text]
  • Wave-Breaking Turbulence in the Ocean Surface Layer
    JUNE 2016 T H O M S O N E T A L . 1857 Wave-Breaking Turbulence in the Ocean Surface Layer JIM THOMSON,MICHAEL S. SCHWENDEMAN, AND SETH F. ZIPPEL Applied Physics Laboratory, University of Washington, Seattle, Washington SAEED MOGHIMI Oregon State University, Corvallis, Oregon JOHANNES GEMMRICH University of Victoria, Victoria, British Columbia, Canada W. ERICK ROGERS Naval Research Laboratory, Stennis Space Center, Louisiana (Manuscript received 12 July 2015, in final form 17 March 2016) ABSTRACT Observations of winds, waves, and turbulence at the ocean surface are compared with several analytic formulations and a numerical model for the input of turbulent kinetic energy by wave breaking and the subsequent dissipation. The observations are generally consistent with all of the formulations, although some differences are notable at winds greater than 15 m s21. The depth dependence of the turbulent dissipation rate beneath the waves is fit to a decay scale, which is sensitive to the choice of vertical reference frame. In the surface-following reference frame, the strongest turbulence is isolated within a shallow region of depths much less than one significant wave height. In a fixed reference frame, the strong turbulence penetrates to depths that are at least half of the significant wave height. This occurs because the turbulence of individual breakers persists longer than the dominant period of the waves and thus the strong surface turbulence is carried from crest to trough with the wave orbital motion. 1. Introduction Gemmrich and Farmer 2004; Gemmrich 2010). The dynamic balance assumed is that the wave energy lost Wave breaking at the ocean surface limits wave during breaking S becomes a flux of turbulent ki- growth (Melville 1994), enhances gas exchange (Zappa brk netic energy F into the ocean surface layer that is dis- et al.
    [Show full text]
  • Research and Discoveries the Revolution of Science Through Scuba
    Smithsonian Institution Scholarly Press smithsonian contributions to the marine sciences • number 39 Smithsonian Institution Scholarly Press Research and Discoveries The Revolution of Science through Scuba Edited by Michael A. Lang, Roberta L. Marinelli, Susan J. Roberts, and Phillip R. Taylor SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of “diffusing knowledge” was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: “It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge.” This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, com- mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Botany Smithsonian Contributions to History and Technology Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Museum Conservation Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology In these series, the Institution publishes small papers and full-scale monographs that report on the research and collections of its various museums and bureaus. The Smithsonian Contributions Series are distributed via mailing lists to libraries, universities, and similar institu- tions throughout the world. Manuscripts submitted for series publication are received by the Smithsonian Institution Scholarly Press from authors with direct affilia- tion with the various Smithsonian museums or bureaus and are subject to peer review and review for compliance with manuscript preparation guidelines.
    [Show full text]
  • Protecting Surf Breaks and Surfing Areas in California
    Protecting Surf Breaks and Surfing Areas in California by Michael L. Blum Date: Approved: Dr. Michael K. Orbach, Adviser Masters project submitted in partial fulfillment of the requirements for the Master of Environmental Management degree in the Nicholas School of the Environment of Duke University May 2015 CONTENTS ACKNOWLEDGEMENTS ........................................................................................................... vi LIST OF FIGURES ...................................................................................................................... vii LIST OF TABLES ........................................................................................................................ vii LIST OF ACRONYMS ............................................................................................................... viii LIST OF DEFINITIONS ................................................................................................................ x EXECUTIVE SUMMARY ......................................................................................................... xiii 1. INTRODUCTION ...................................................................................................................... 1 2. STUDY APPROACH: A TOTAL ECOLOGY OF SURFING ................................................. 5 2.1 The Biophysical Ecology ...................................................................................................... 5 2.2 The Human Ecology ............................................................................................................
    [Show full text]