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2015 Annual Report
HOW THE BANK IS DRIVING CHANGE 2015 ANNUAL REPORT The bank for a changing world BNP PARIBAS, AN INTEGRATED MODEL, A GUARANTEE OF PERFORMANCE 3 QUESTIONS ABOUT BANKS ..................................................................................................... 29 Business model ................. 5 Key figures ......................... 6 International presence .... 7 The Board of Directors .... 8 Interview with the Chief Executive Officer .... 11 How do banks How do banks What will the bank of contribute to participate in the the future look like? ......... 49 The Executive ........... 33 ........... 41 Committee ......................... 13 the real economy? energy transition? Our business ...................... 14 Viewpoints .................... 34 Viewpoints .................... 42 Viewpoints .................... 50 ..................... Shareholders 18 Financing the real How BNP Paribas Digitalisation at the economy: a key role is accelerating the heart of BNP Paribas’ Human Resources ............. 20 for BNP Paribas energy transition transformation Corporate Social Highlights ...................... Highlights ...................... Highlights ...................... Responsibility .................... 22 36 44 52 BNP Paribas: BNP Paribas: BNP Paribas: supporting the furthering the driving change Our commitments ............ 24 real economy energy transition BNP Paribas is the bank for a changing world, aware of the changes affecting society, attuned to its concerns and committed to meeting its future needs. Through examples and highlights of the past year, the 2015 Annual Report presents not only the BNP Paribas Group, but also provides answers to questions in society on the role of banks. BNP PARIBAS AN INTEGRATED MODEL, A GUARANTEE OF PERFORMANCE BUSINESS MODEL AN INTEGRATED GROUP AND EUROPEAN LEADER The capacity to serve a diversified client base is at the include payments, deposits, traditional and specialised heart of BNP Paribas’ business model. financing, savings, protection insurance, wealth and asset management as well as real-estate services. -
Chapter 2 the Evolution of Seismic Monitoring Systems at the Hawaiian Volcano Observatory
Characteristics of Hawaiian Volcanoes Editors: Michael P. Poland, Taeko Jane Takahashi, and Claire M. Landowski U.S. Geological Survey Professional Paper 1801, 2014 Chapter 2 The Evolution of Seismic Monitoring Systems at the Hawaiian Volcano Observatory By Paul G. Okubo1, Jennifer S. Nakata1, and Robert Y. Koyanagi1 Abstract the Island of Hawai‘i. Over the past century, thousands of sci- entific reports and articles have been published in connection In the century since the Hawaiian Volcano Observatory with Hawaiian volcanism, and an extensive bibliography has (HVO) put its first seismographs into operation at the edge of accumulated, including numerous discussions of the history of Kīlauea Volcano’s summit caldera, seismic monitoring at HVO HVO and its seismic monitoring operations, as well as research (now administered by the U.S. Geological Survey [USGS]) has results. From among these references, we point to Klein and evolved considerably. The HVO seismic network extends across Koyanagi (1980), Apple (1987), Eaton (1996), and Klein and the entire Island of Hawai‘i and is complemented by stations Wright (2000) for details of the early growth of HVO’s seismic installed and operated by monitoring partners in both the USGS network. In particular, the work of Klein and Wright stands and the National Oceanic and Atmospheric Administration. The out because their compilation uses newspaper accounts and seismic data stream that is available to HVO for its monitoring other reports of the effects of historical earthquakes to extend of volcanic and seismic activity in Hawai‘i, therefore, is built Hawai‘i’s detailed seismic history to nearly a century before from hundreds of data channels from a diverse collection of instrumental monitoring began at HVO. -
Deep Carbon Science
From Crust to Core Carbon plays a fundamental role on Earth. It forms the chemical backbone for all essential organic molecules produced by living organ- isms. Carbon-based fuels supply most of society’s energy, and atmos- pheric carbon dioxide has a huge impact on Earth’s climate. This book provides a complete history of the emergence and development of the new interdisciplinary field of deep carbon science. It traces four cen- turies of history during which the inner workings of the dynamic Earth were discovered, and it documents the extraordinary scientific revolutions that changed our understanding of carbon on Earth for- ever: carbon’s origin in exploding stars; the discovery of the internal heat source driving the Earth’s carbon cycle; and the tectonic revolu- tion. Written with an engaging narrative style and covering the scien- tific endeavors of about 150 pioneers of deep geoscience, this is a fascinating book for students and researchers working in Earth system science and deep carbon research. is a life fellow at St. Edmund’s College, University of Cambridge. For more than 50 years he has passionately engaged in bringing discoveries in astronomy and cosmology to the general public. He is a fellow of the Royal Historical Society, a former vice- president of the Royal Astronomical Society and a fellow of the Geological Society. The International Astronomical Union designated asteroid 4027 as Minor Planet Mitton in recognition of his extensive outreach activity and that of Dr. Jacqueline Mitton. From Crust to Core A Chronicle of Deep Carbon Science University of Cambridge University Printing House, Cambridge CB2 8BS, United Kingdom One Liberty Plaza, 20th Floor, New York, NY 10006, USA 477 Williamstown Road, Port Melbourne, VIC 3207, Australia 314–321, 3rd Floor, Plot 3, Splendor Forum, Jasola District Centre, New Delhi – 110025, India 79 Anson Road, #06–04/06, Singapore 079906 Cambridge University Press is part of the University of Cambridge. -
Simon Stevin
II THE PRINCIPAL WORKS OF SIMON STEVIN E D IT E D BY ERNST CRONE, E. J. DIJKSTERHUIS, R. J. FORBES M. G. J. MINNAERT, A. PANNEKOEK A M ST E R D A M C. V. SW ETS & Z E IT L IN G E R J m THE PRINCIPAL WORKS OF SIMON STEVIN VOLUME II MATHEMATICS E D IT E D BY D. J. STRUIK PROFESSOR AT THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY, CAMBRIDGE (MASS.) A M S T E R D A M C. V. SW ETS & Z E IT L IN G E R 1958 The edition of this volume II of the principal works of SIMON STEVIN devoted to his mathematical publications, has been rendered possible through the financial aid of the Koninklijke. Nederlandse Akademie van Wetenschappen (Royal Netherlands Academy of Science) Printed by Jan de Lange, Deventer, Holland The following edition of the Principal Works of SIMON STEVIN has been brought about at the initiative of the Physics Section of the Koninklijke Nederlandse Akademie van Weten schappen (Royal Netherlands Academy of Sciences) by a committee consisting of the following members: ERNST CRONE, Chairman of the Netherlands Maritime Museum, Amsterdam E. J. DIJKSTERHUIS, Professor of the History of Science at the Universities of Leiden and Utrecht R. J. FORBES, Professor of the History of Science at the Municipal University of Amsterdam M. G. J. M INNAERT, Professor of Astronomy at the University of Utrecht A. PANNEKOEK, Former Professor of Astronomy at the Municipal University of Amsterdam The Dutch texts of STEVIN as well as the introductions and notes have been translated into English or revised by Miss C. -
Index of Articles and Authors for the First Twenty-Four Numbers
Index of Articles and Authors for the first Twenty-four Numbers MARCH 1923 — NOVEMBER 1935 0 THE HYDROGRAPHIC REVIEW The Directing Committee of the I nternational H ydrographic B u r e a u will be pleased to consider articles for insertion in the Hydrographic Review. Such articles should be addressed to : The Secretary-General, I nternational H ydrographic B u r e a u Quai de Plaisance Mo n te -C arlo (Principality of Monaco) and should reach him not later than 1st February or ist August for the May or November numbers respectively. INDEX OF ARTICLES AND AUTHORS for the First Twenty-four Numbers MARCH 1923 - NOVEMBER 1935 FOREWORD This Index is in two parts : P a r t I. — Classification of articles according to the Subjects dealt with. P a r t II. — Alphabetical Index of the names of Authors of articles which have been published in The Hydrographic Review. NOTE. — Articles marked (R ) are Reviews of publications. Articles marked (E) are Extracts from publications. When no author’s name is given, articles have been compiled from information received by the Interna tional Hydrographic Bureau. Reviews of Publications appear under the name or initials of the author of the review. Descriptions of instruments or appliances are given in the chapters relating to their employment, in Chapter XIV (Various Instruments), or occasionally in Chapter XXT (Hints to Hydrographic Surveyors). CLASSIFICATION OF ARTICLES ACCORDING TO THE SUBJECTS DEALT WITH List of subjects I . — H ydrographic Offic e s a n d o th er Mar itim e a n d S c ie n t ific Organisations (Patrols, Life- saving, Observatories, Institutes of Optics)..................................................................................... -
Goodman, Matthew (2018) from 'Magnetic Fever' to 'Magnetical Insanity': Historical Geographies of British Terrestrial Magnetic Research, 1833- 1857
Goodman, Matthew (2018) From 'magnetic fever' to 'magnetical insanity': historical geographies of British terrestrial magnetic research, 1833- 1857. PhD thesis. https://theses.gla.ac.uk/30829/ Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten: Theses https://theses.gla.ac.uk/ [email protected] From ‘magnetic fever’ to ‘magnetical insanity’: historical geographies of British terrestrial magnetic research, 1833-1857 Matthew Goodman Submitted in fulfilment of the requirements for the Degree of Doctor of Philosophy (PhD) School of Geographical and Earth Sciences College of Science and Engineering University of Glasgow Contents Abstract................................................................................................................................................................ 5 List of Figures .................................................................................................................................................... 6 Acknowledgements ......................................................................................................................................... -
Famous Geologist Fact Sheet Your Job Is to Research Information About
Famous Geologist Fact Sheet Your job is to research information about one of the geologists on the list and arrange the information you find into a fact sheet about that person. The fact sheet should only be one side of an 8 ½ x 11 inch paper. Include all of the following information about the scientist. You may turn your project into a wanted poster if you want starting your paper with “Be on the lookout for this man/woman. Wanted for ___________.” You may use bulleted lists where appropriate. A. Give the scientists full name – first, middle, last B. When they were born and when they died (if applicable) C. Where they were born – country, state, city D. Where they grew up if different from where they were born E. Family information – parents, siblings, wife, children F. Where they went to school – elementary, high school, college G. What they did for a job H. What they studied – field of expertise - give a complete description of what they studied I. What they are famous for specifically – include how their contributions affect us now and/or will in the future J. A quote from your scientist if you can find one K. Any other interesting facts about your scientist L. A picture of the scientist – not a cartoon M. A picture pertaining to what they are famous for N. List of important publications by the scientist O. List any awards given and the dates they were given to your scientist for their contributions to science P. Cite your source or sources according to the MLA Style Your grade will be determined by: * Overall presentation, neatness and creativity. -
The Search for Empirical Formulae for the Aftershocks Descriptions of a Strong Earthquake A.V
arXiv.org 2019 [physics.geo-ph] The search for empirical formulae for the aftershocks descriptions of a strong earthquake A.V. Guglielmi Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, ul. B. Gruzinskaya 10, Moscow, 123995 Russia, e-mail: [email protected] Abstract The paper is based on the report read by the author on October 24, 2018 at the meeting of the Scientific Council of the Institute of Earth Physics of the Russian Academy of Sciences. The report was dedicated to the 150th anniversary of the outstanding Japanese seismologist Fusakichi Omori. As is known, Omori established the first empirical law of the earthquakes physics, bearing his name. The Omori law states that the frequency of aftershocks on average decreases hyperbolically over the time. Three versions of Omori law are described briefly. The recent version allows to poses the inverse problem of the earthquake source, that “cools down” after the main shock. Keywords: earthquake source, aftershocks equation, deactivation coefficient, inverse problem Table of contents 1. Introduction 2. Three wordings of the Omori law 3. Inverse problem 4. Conclusion References 1. Introduction On October 24, 2018 at the meeting of the Academic Council of the Institute of Physics of the Earth RAS the author made a report dedicated to the 150th anniversary of the outstanding Japanese seismologist Fusakichi Omori (1868 – 1923). The presented paper summarizes the contents of this report. While still quite young, at the age of 26, Omori made an outstanding contribution to science, which has not lost its value these days [Davison, 1924; Guglielmi, 2017]. -
When the Earth Moves Seafloor Spreading and Plate Tectonics
This article was published in 1999 and has not been updated or revised. BEYONDBEYOND DISCOVERYDISCOVERYTM THE PATH FROM RESEARCH TO HUMAN BENEFIT WHEN THE EARTH MOVES SEAFLOOR SPREADING AND PLATE TECTONICS arly on the morning of Wednesday, April 18, the fault had moved, spanning nearly 300 miles, from 1906, people in a 700-mile stretch of the West San Juan Bautista in San Benito County to the south E Coast of the United States—from Coos Bay, of San Francisco to the Upper Mattole River in Oregon, to Los Angeles, California—were wakened by Humboldt County to the north, as well as westward the ground shaking. But in San Francisco the ground some distance out to sea. The scale of this movement did more than shake. A police officer on patrol in the was unheard of. The explanation would take some six city’s produce district heard a low rumble and saw the decades to emerge, coming only with the advent of the street undulate in front of him, “as if the waves of the theory of plate tectonics. ocean were coming toward me, billowing as they came.” One of the great achievements of modern science, Although the Richter Scale of magnitude was not plate tectonics describes the surface of Earth as being devised until 1935, scientists have since estimated that divided into huge plates whose slow movements carry the the 1906 San Francisco earthquake would have had a continents on a slow drift around the globe. Where the 7.8 Richter reading. Later that morning the disaster plates come in contact with one another, they may cause of crushed and crumbled buildings was compounded by catastrophic events, such as volcanic eruptions and earth- fires that broke out all over the shattered city. -
Earthquake Resistant Design of Reinforced Concrete Buildings Past and Future Shunsuke Otani1
Journal of Advanced Concrete Technology Vol. 2, No. 1, 3-24, February 2004 / Copyright © 2004 Japan Concrete Institute 3 Invited Paper Earthquake Resistant Design of Reinforced Concrete Buildings Past and Future Shunsuke Otani1 Received 9 September 2003, revised 26 November 2003 Abstract This paper briefly reviews the development of earthquake resistant design of buildings. Measurement of ground accel- eration started in the 1930s, and response calculation was made possible in the 1940s. Design response spectra were formulated in the late 1950s to 1960s. Non-linear response was introduced in seismic design in the 1960s and the capac- ity design concept was generally introduced in the 1970s for collapse safety. The damage statistics of reinforced con- crete buildings in the 1995 Kobe disaster demonstrated the improvement of building performance with the development of design methodology. Buildings designed and constructed using out-dated methodology should be upgraded. Per- formance-based engineering should be emphasized, especially for the protection of building functions following fre- quent earthquakes. 1. Introduction damage have been identified through the investigation of damages. Each damage case has provided important An earthquake, caused by a fault movement on the earth information regarding the improvement of design and surface, results in severe ground shaking leading to the construction practices and attention has been directed to damage and collapse of buildings and civil- the prevention of structural collapse to protect the oc- infra-structures, landslides in the case of loose slopes, cupants of building in the last century. and liquefaction of sandy soil. If an earthquake occurs Thank to the efforts of many pioneering researchers under the sea, the associated water movement causes and engineers, the state of the art in earthquake resistant high tidal waves called tsunamis. -
Mitteilungen Des Naturwissenschaftlichen Vereines
Prof. Dr. Rudolf Hoernes. Zur Erinnerung' an Rudolf Hoernes. •Von Franz He ritsch. Am 20. August 1912 hat Rudolf Hoerues seine Augen für immer geschlossen. Ein Meister, ein glänzender Vertreter unserer Wissenschaft, eine Zierde der alraa mater graecensis. ein Vorbild allen denen, die ihn gekannt haben, hat uns ver- lassen, um einzugehen in das Tor, aus dem es keine Rückkehr und jenseits dessen es kein Wiedersehen gibt. Er ist von hinnen gegangen, und in Trauer und Wehmut können wir, seine Schüler und seine Freunde, des Mannes gedenken, der nicht nur sich selbst in seinem Lebenswerk ein Denkmal gesetzt hat. aere perennius, der auch allen jenen, die mit ihm zu ver- kehren und an seinem Streben Anteil zu nehmen das Glück hatten, das Leben bereichert und verschönt hat. Denn nicht nur seine Wissenschaft hat ihn erfüllt, sondern er hat auch ein warmes Herz gehabt für seine Schüler, für die, welche ihm nahe standen. Und wir alle, die wir schmerzlich in Trauer an seinen sterblichen Überresten standen, haben ihm nichts anderes dafür bieten können als unsere verehrungsvolle Liebe. Denn in diesem Manne, der — wenn es üblich wäre, den Menschen, die wir verehren, einen Beinamen zu geben — nur einen Namen erhalten konnte : Hoernes. der Einzige, in diesem Manne haben wir nicht nur unseren Lehrer verehrt, dessen Wissen ganz außerordentlich war, wir haben in ihm nicht nur den ]\Ieister, den Mann mit einem Weltruf gesehen, sondern wir alle, seine Schüler, haben in ihm den väterlichen Freund geliebt, wir haben ihn um seiner unendlichen Güte willen, mit der er sieh um alle unsere großen und kleinen Schmerzen, um unsere persönlichen und Privatangelegenheiten angenommen hat, angebetet. -
Plate Tectonics
Plate tectonics tive motion determines the type of boundary; convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative move- ment of the plates typically varies from zero to 100 mm annually.[2] Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the globe remains the same. This predic- The tectonic plates of the world were mapped in the second half of the 20th century. tion of plate tectonics is also referred to as the conveyor belt principle. Earlier theories (that still have some sup- porters) propose gradual shrinking (contraction) or grad- ual expansion of the globe.[3] Tectonic plates are able to move because the Earth’s lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topog- raphy and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and Moon. The relative im- portance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.