Oceanography: an Observer’S Guide
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Illustrations of Selected Works in the Various National Sections of The
SMITHSONIAN INSTITUTION libraries 390880106856C A«T FALACr CttNTRAL. MVIIION "«VTH rinKT OFFICIAI ILLUSTRATIONS OF SELECTED WORKS IN THE VARIOUS NATIONAL SECTIONS OF THE DEPARTMENT OF ART WITH COMPLETE LIST OF AWARDS BY THE INTERNATIONAL JURY UNIVERSAL EXPOSITION ST. LOUIS, 1904 WITH AN INTRODUCTION BY HALSEY C. IVES, CHIEF OF THE DEPARTMENT DESCRIPTIVE TEXT FOR PAINTINGS BY CHARLES M. KURTZ, Ph.D., ASSISTANT CHIEF DESCRIPTIVE TEXT FOR SCULPTURES BY GEORGE JULIAN ZOLNAY, superintendent of sculpture division Copyr igh r. 1904 BY THE LOUISIANA PURCHASE EXPOSITION COMPANY FOR THE OFFICIAL CATALOGUE COMPANY EXECUTIVE OFFICERS OF THE DEPARTMENT OF ART Department ' B’’ of the Division of Exhibits, FREDERICK J. V. SKIFF, Director of Exhibits. HALSEY C. IVES, Chief. CHARLES M. KURTZ, Assistant Chief. GEORGE JULIAN ZOLNAY, Superintendent of the Division of Sculpture. GEORGE CORLISS, Superintendent of Exhibit Records. FREDERIC ALLEN WHITING, Superintendent of the Division of Applied Arts. WILL H. LOW, Superintendent of the Loan Division. WILLIAM HENRY FOX Secretary. INTRODUCTION BY Halsey C. Ives “All passes; art alone enduring stays to us; I lie bust outlasts the throne^ the coin, Tiberius.” A I an early day after the opening of the Exposition, it became evident that there was a large class of visitors made up of students, teachers and others, who desired a more extensive and intimate knowledge of individual works than could be gained from a cursory view, guided by a conventional catalogue. 11 undreds of letters from persons especially interested in acquiring intimate knowledge of the leading char¬ acteristics of the various schools of expression repre¬ sented have been received; indeed, for two months be¬ fore the opening of the department, every mail carried replies to such letters, giving outlines of study, courses of reading, and advice to intending visitors. -
Analysis of Hydrometeorological Conditions in the South Baltic Sea During the Stormy Weather O N 2 7 Th November, 2016
ZESZYTY NAUKOWE AKADEMII MARYNARKI WOJENNEJ SCIENTIFIC JOURNAL OF POLISH NAVAL ACADEMY 2017 (LVIII) 2 (209) DOI: 10.5604/01.3001.0010.4062 Czesław Dyrcz ANALYSIS OF HYDROMETEOROLOGICAL CONDITIONS IN THE SOUTH BALTIC SEA DURING THE STORMY WEATHER O N 2 7 TH NOVEMBER, 2016 ABSTRACT The paper presents results of research concerning hydrological and meteorological conditions during the stormy weather on 27th November, 2016 in the South Baltic Sea and over the Polish coast. The wind which occurred the South Baltic Sea at that time reached the force of 7 Beaufort degree and in gusts 8 to 9 Beaufort degree. The south part of the Baltic Sea was affected by the low pressure system (981 hPa) which the centre was situated in South Finland and Northwest Russia. Some destroys were observed on the Polish coast line and in ports of the Gdansk Bay. The analysis is concerned on the wind force, the wind direction, the atmospheric pressure and the sea water level in some places of the Polish coast line and especially in the Gdansk Bay. Key words: sea water level, weather conditions, the South Baltic Sea. INTRODUCTION Occurrence of strong winds in the area of the Baltic Sea and on the Polish coast is related mainly with active cyclones. This means that the strong winds zone is of the synoptic scale, i.e. it extends in an area of over 500 NM across and it lasts for a few days. Storms cause serious difficulties or they are even threats to safety of sea navigation and work in harbors. They often destroy hydrotechnical devices and coast facilities. -
Tidal Hydrodynamic Response to Sea Level Rise and Coastal Geomorphology in the Northern Gulf of Mexico
University of Central Florida STARS Electronic Theses and Dissertations, 2004-2019 2015 Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico Davina Passeri University of Central Florida Part of the Civil Engineering Commons Find similar works at: https://stars.library.ucf.edu/etd University of Central Florida Libraries http://library.ucf.edu This Doctoral Dissertation (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Electronic Theses and Dissertations, 2004-2019 by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Passeri, Davina, "Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico" (2015). Electronic Theses and Dissertations, 2004-2019. 1429. https://stars.library.ucf.edu/etd/1429 TIDAL HYDRODYNAMIC RESPONSE TO SEA LEVEL RISE AND COASTAL GEOMORPHOLOGY IN THE NORTHERN GULF OF MEXICO by DAVINA LISA PASSERI B.S. University of Notre Dame, 2010 A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Civil, Environmental, and Construction Engineering in the College of Engineering and Computer Science at the University of Central Florida Orlando, Florida Spring Term 2015 Major Professor: Scott C. Hagen © 2015 Davina Lisa Passeri ii ABSTRACT Sea level rise (SLR) has the potential to affect coastal environments in a multitude of ways, including submergence, increased flooding, and increased shoreline erosion. Low-lying coastal environments such as the Northern Gulf of Mexico (NGOM) are particularly vulnerable to the effects of SLR, which may have serious consequences for coastal communities as well as ecologically and economically significant estuaries. -
Tide Simplified by Phil Clegg Sea Kayaking Anglesey
Tide Simplified By Phil Clegg Sea Kayaking Anglesey Tide is one of those areas that the more you learn about it, the more you realise you don’t know. As sea kayakers, and not necessarily scientists, we don’t have to know every detail but a simplified understanding can help us to understand and predict what we might expect to see when we are out on the water. In this article we look at the areas of tide you need to know about without having to look it up in a book. Causes of tides To understand tide is convenient to imagine the earth with an envelope of water all around it, spinning once every 24 hours on its north-south axis with the moon on a line parallel to the equator. Moon Gravity A B Earth Ocean C The tides are primarily caused by the gravitational attraction of the moon. Simplifying a bit, at point A the gravitational pull is the strongest causing a high tide, point B experiences a medium pull towards the moon, while point C has the weakest pull causing a second high tide. Because the earth spins once every 24 hours, at any location on its surface there are two high tides and two low tides a day. There are approximately six hours between high tide and low tide. One way of predicting the approximate time of high tide is to add 50 minutes to the high tide of the previous day. The sun has a similar but weaker gravitational effect on the tides. On average this is about 40 percent of that of the moon. -
Chapter 5 Water Levels and Flow
253 CHAPTER 5 WATER LEVELS AND FLOW 1. INTRODUCTION The purpose of this chapter is to provide the hydrographer and technical reader the fundamental information required to understand and apply water levels, derived water level products and datums, and water currents to carry out field operations in support of hydrographic surveying and mapping activities. The hydrographer is concerned not only with the elevation of the sea surface, which is affected significantly by tides, but also with the elevation of lake and river surfaces, where tidal phenomena may have little effect. The term ‘tide’ is traditionally accepted and widely used by hydrographers in connection with the instrumentation used to measure the elevation of the water surface, though the term ‘water level’ would be more technically correct. The term ‘current’ similarly is accepted in many areas in connection with tidal currents; however water currents are greatly affected by much more than the tide producing forces. The term ‘flow’ is often used instead of currents. Tidal forces play such a significant role in completing most hydrographic surveys that tide producing forces and fundamental tidal variations are only described in general with appropriate technical references in this chapter. It is important for the hydrographer to understand why tide, water level and water current characteristics vary both over time and spatially so that they are taken fully into account for survey planning and operations which will lead to successful production of accurate surveys and charts. Because procedures and approaches to measuring and applying water levels, tides and currents vary depending upon the country, this chapter covers general principles using documented examples as appropriate for illustration. -
Extreme Sea Levels at Selected Stations on the Baltic Sea Coast*
doi:10.5697/oc.56-2.259 Extreme sea levels at OCEANOLOGIA, 56 (2), 2014. selected stations on the pp. 259–290. C Copyright by Baltic Sea coast* Polish Academy of Sciences, Institute of Oceanology, 2014. KEYWORDS Baltic Sea Extreme sea levels Storm surges and falls Tomasz Wolski1,⋆, Bernard Wiśniewski2 Andrzej Giza1, Halina Kowalewska-Kalkowska1 Hanna Boman3, Silve Grabbi-Kaiv4 Thomas Hammarklint5, Jurgen¨ Holfort6 Zydruneˇ Lydeikaite˙ 7 1 University of Szczecin, Faculty of Geosciences, al. Wojska Polskiego 107/109, 70–483 Szczecin, Poland; e-mail: [email protected] ⋆corresponding author 2 Maritime University of Szczecin, Faculty of Navigation, Wały Chrobrego 1–2, 70–500 Szczecin, Poland 3 Finnish Meteorological Institute, Erik Palm´enin aukio 1, FI–00101 Helsinki, Finland 4 Estonian Meteorological and Hydrological Institute, Toompuiestee 24, 10149 Tallinn, Estonia 5 Swedish Meteorological and Hydrological Institute, Sven K¨allfelts Gata 15, 42471 G¨oteborg, Sweden 6 Bundesamt f¨ur Seeschifffahrt und Hydrographie, Neptunallee 5, 18057 Rostock, Germany 7 Environmental Protection Agency, Taikos pr. 26, LT–91149, Klaipeda, Lithuania Received 25 October 2013, revised 6 February 2014, accepted 11 February 2014. * This work was financed by the Polish National Centre for Science research project No. 2011/01/B/ST10/06470. The complete text of the paper is available at http://www.iopan.gda.pl/oceanologia/ 260 T. Wolski, B. Wiśniewski, A. Giza et al. Abstract The purpose of this article is to analyse and describe the extreme characteristics of the water levels and illustrate them as the topography of the sea surface along the whole Baltic Sea coast. The general pattern is to show the maxima and minima of Baltic Sea water levels and the extent of their variations in the period from 1960 to 2010. -
Adriatic Sea Fisheries: Outline of Some Main Facts
Adriatic Sea Fisheries: outline of some main facts Piero Mannini*, Fabio Massa, Nicoletta Milone Abstract Following a brief introduction to some principal characteristics of the Adriatic Sea, the paper focuses on two main aspects of Adriatic Sea fisheries: fishery production and the fishing fleet. The evolution of capture fisheries landings over thirty years (1970-2000) is outlined: demersal and pelagic fishery production is compared and the quantities landed of some key shared stocks are described. The evolution of the Adriatic fishing fleet is reported in terms of number of fishing units, length category and fishing technique. The importance of basic reliable, comparable and easily integrated statistics is underlined; in the case of Adriatic shared fisheries the need for international cooperation is fundamental together with increased multidisciplinary analysis for the management of shared fishery stocks for the achievement of effective sub-regional fishery management. 1. Brief introduction to the Adriatic Sea The Adriatic Sea is a semi-enclosed1 basin within the larger semi-enclosed sea constituted by the Mediterranean, it extends over 138000 km2 (Buljan and Zore-Armanda, 1976) it may be seen as characterised by Northern, Central and Southern sub-basins with decreasing depth from the south toward the north. Along the longitudinal axis of the Adriatic geomorphological and ecological changes can be observed, resulting in the remarkable differences of the northern and southern ends. Six countries, whose coastline development differs greatly, border the Adriatic. Some key-features of Adriatic coastal states for which marine fisheries are relevant are given in Table 1. The Adriatic is characterised by the largest shelf area of the Mediterranean, which extends over the Northern and Central parts where the bottom depth is no more than about 75 and 100 m respectively, with the exception of the Pomo/Jabuka Pit (200-260 m) in the Central Adriatic. -
NINETEENTH CENTURY AMERICAN PAINTINGS at BOWDOIN COLLEGE Digitized by the Internet Archive
V NINETEENTH CENTURY^ AMERIGAN PAINTINGS AT BOWDOIN COLLEGE NINETEENTH CENTURY AMERICAN PAINTINGS AT BOWDOIN COLLEGE Digitized by the Internet Archive in 2015 https://archive.org/details/nineteenthcenturOObowd_0 NINETEENTH CENTURY AMERICAN PAINTINGS AT BOWDOIN COLLEGE BOWDOIN COLLEGE MUSEUM OF ART 1974 Copyright 1974 by The President and Trustees of Bowdoin College This Project is Supported by a Grant from The National Endowment for The Arts in Washington, D.C. A Federal Agency Catalogue Designed by David Berreth Printed by The Brunswick Publishing Co. Brunswick, Maine FOREWORD This catalogue and the exhibition Nineteenth Century American Paintings at Bowdoin College begin a new chapter in the development of the Bow- doin College Museum of Art. For many years, the Colonial and Federal portraits have hung in the Bowdoin Gallery as a permanent exhibition. It is now time to recognize that nineteenth century American art has come into its own. Thus, the Walker Gallery, named in honor of the donor of the Museum building in 1892, will house the permanent exhi- bition of nineteenth century American art; a fitting tribute to the Misses Walker, whose collection forms the basis of the nineteenth century works at the College. When renovations are complete, the Bowdoin and Boyd Galleries will be refurbished to house permanent installations similar to the Walker Gal- lery's. During the renovations, the nineteenth century collection will tour in various other museiniis before it takes its permanent home. My special thanks and congratulations go to David S. Berreth, who developed the original idea for the exhibition to its present conclusion. His talent for exhibition installation and ability to organize catalogue materials will be apparent to all. -
Chapter 9 Tides and Tidal Currents
CHAPTER 9 TIDES AND TIDAL CURRENTS ORIGINS OF TIDES 900. Introduction superimposed upon non-tidal currents such as normal river flows, floods, and freshets. Tides are the periodic motion of the waters of the sea due to changes in the attractive forces of the Moon and Sun 902. Causes of Tides upon the rotating Earth. Tides can either help or hinder a mariner. A high tide may provide enough depth to clear a The principal tidal forces are generated by the Moon bar, while a low tide may prevent entering or leaving a and Sun. The Moon is the main tide-generating body. Due harbor. Tidal current may help progress or hinder it, may set to its greater distance, the Sun’s effect is only 46 percent of the ship toward dangers or away from them. By the Moon’s. Observed tides will differ considerably from understanding tides and making intelligent use of the tides predicted by equilibrium theory since size, depth, predictions published in tide and tidal current tables and and configuration of the basin or waterway, friction, land descriptions in sailing directions, the navigator can plan an masses, inertia of water masses, Coriolis acceleration, and expeditious and safe passage through tidal waters. other factors are neglected in this theory. Nevertheless, equilibrium theory is sufficient to describe the magnitude 901. Tide and Current and distribution of the main tide-generating forces across The rise and fall of tide is accompanied by horizontal the surface of the Earth. movement of the water called tidal current. It is necessary Newton’s universal law of gravitation governs both the to distinguish clearly between tide and tidal current, for the orbits of celestial bodies and the tide-generating forces relation between them is complex and variable. -
Rogue Giants at Sea
New York Times (www.nytimes.com) July 11, 2006 Rogue Giants at Sea By WILLIAM J. BROAD The storm was nothing special. Its waves rocked the Norwegian Dawn just enough so that bartenders on the cruise ship turned to the usual palliative — free drinks. Then, off the coast of Georgia, early on Saturday, April 16, 2005, a giant, seven-story wave appeared out of nowhere. It crashed into the bow, sent deck chairs flying, smashed windows, raced as high as the 10th deck, flooded 62 cabins, injured 4 passengers and sowed widespread fear and panic. “The ship was like a cork in a bathtub,” recalled Celestine Mcelhatton, a passenger who, along with 2,000 others, eventually made it back to Pier 88 on the Hudson River in Manhattan. Some vowed never to sail again. Enormous waves that sweep the ocean are traditionally called rogue waves, implying that they have a kind of freakish rarity. Over the decades, skeptical oceanographers have doubted their existence and tended to lump them together with sightings of mermaids and sea monsters. But scientists are now finding that these giants of the sea are far more common and destructive than once imagined, prompting a rush of new studies and research projects. The goals are to better tally them, understand why they form, explore the possibility of forecasts, and learn how to better protect ships, oil platforms and people. The stakes are high. In the past two decades, freak waves are suspected of sinking dozens of big ships and taking hundreds of lives. The upshot is that the scientists feel a sense of urgency about the work and growing awe at their subjects. -
Art of the Eclipse
COMMENT BOOKS & ARTS Howard Russell Butler’s 1925 triptych of solar eclipses was the first work by an artist to depict the solar corona accurately. ASTRONOMY Art of the eclipse As the next solar eclipse approaches, Jay Pasachoff and Roberta Olson ponder how artists from the early Renaissance onwards have interpreted the phenomenon. tate-of-the-art photography can occulted Sun on one side of the cross. In Abimelech. Although lacking details such capture a solar eclipse in all its eva- the fourteenth century the Florentine artist as the coronal ‘streamers’ jutting out from nescent glory — as will be seen on Taddeo Gaddi, a student of Giotto, took a active regions on the Sun, and otherwise S29 April, when the first solar eclipse of revolutionary step. On the inside shutter of a showing some artistic licence, it is roughly 2014 will be visible from Australia and Crucifixion triptych, he suggested the dark- representative. Judging by this, and evi- Antarctica. But long before such technol- ened sky and strange light of a solar eclipse dence from eclipse maps, Raphael probably ogy existed, artists from the fourteenth by painting a dark-blue wedge in one corner, witnessed the 8 June 1518 annular eclipse. to the early twentieth century portrayed rimmed faintly with now-tarnished silver. An even more accurate portrayal was this fleeting phenomenon in paint with And in his frescoed Annunciation to the achieved another two centuries later, when increasing accuracy, on the basis of direct Shepherds in the Basilica of Santa Croce in Cosmas Damian Asam painted his Vision of observations, scientific documents and con- Florence, Gaddi represented divine radiance St Benedict in 1735 for a monastery in Wel- temporary theory. -
NPRC) VIP List, 2009
Description of document: National Archives National Personnel Records Center (NPRC) VIP list, 2009 Requested date: December 2007 Released date: March 2008 Posted date: 04-January-2010 Source of document: National Personnel Records Center Military Personnel Records 9700 Page Avenue St. Louis, MO 63132-5100 Note: NPRC staff has compiled a list of prominent persons whose military records files they hold. They call this their VIP Listing. You can ask for a copy of any of these files simply by submitting a Freedom of Information Act request to the address above. The governmentattic.org web site (“the site”) is noncommercial and free to the public. The site and materials made available on the site, such as this file, are for reference only. The governmentattic.org web site and its principals have made every effort to make this information as complete and as accurate as possible, however, there may be mistakes and omissions, both typographical and in content. The governmentattic.org web site and its principals shall have neither liability nor responsibility to any person or entity with respect to any loss or damage caused, or alleged to have been caused, directly or indirectly, by the information provided on the governmentattic.org web site or in this file. The public records published on the site were obtained from government agencies using proper legal channels. Each document is identified as to the source. Any concerns about the contents of the site should be directed to the agency originating the document in question. GovernmentAttic.org is not responsible for the contents of documents published on the website.