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See the Scientific Petition
May 20, 2016 Implement the Endangered Species Act Using the Best Available Science To: Secretary Sally Jewell and Secretary Penny Prtizker We, the under-signed scientists, recommend the U.S. government place species conservation policy on firmer scientific footing by following the procedure described below for using the best available science. A recent survey finds that substantial numbers of scientists at the U.S. Fish and Wildlife Service (FWS) and the National Oceanic and Atmospheric Administration believe that political influence at their agency is too high.i Further, recent species listing and delisting decisions appear misaligned with scientific understanding.ii,iii,iv,v,vi For example, in its nationwide delisting decision for gray wolves in 2013, the FWS internal review failed the best science test when reviewed by an independent peer-review panel.vii Just last year, a FWS decision not to list the wolverine ran counter to the opinions of agency and external scientists.viii We ask that the Departments of the Interior and Commerce make determinations under the Endangered Species Actix only after they make public the independent recommendations from the scientific community, based on the best available science. The best available science comes from independent scientists with relevant expertise who are able to evaluate and synthesize the available science, and adhere to standards of peer-review and full conflict-of-interest disclosure. We ask that agency scientific recommendations be developed with external review by independent scientific experts. There are several mechanisms by which this can happen; however, of greatest importance is that an independent, external, and transparent science-based process is applied consistently to both listing and delisting decisions. -
Seventy Years of Exploration in Oceanography: a Prolonged
Seventy Years of Exploration in Oceanography Hans von Storch Klaus Hasselmann Seventy Years of Exploration in Oceanography A Prolonged Weekend Discussion with Walter Munk 123 Hans von Storch Klaus Hasselmann Institute of Coastal Research Max-Planck-Institut für Meteorologie GKSS Research Center Bundesstraße 55 Geesthacht 20146 Hamburg Germany Germany Center of Excellence CLISAP [email protected] University of Hamburg Germany [email protected] ISBN 978-3-642-12086-2 e-ISBN 978-3-642-12087-9 DOI 10.1007/978-3-642-12087-9 Springer Heidelberg Dordrecht London New York Library of Congress Control Number: 2010922341 © Springer-Verlag Berlin Heidelberg 2010 This work is subject to copyright. All rights are reserved, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable to prosecution under the German Copyright Law. The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. Typesetting and production: le-tex publishing services GmbH, Leipzig, Germany Cover design: WMXDesign GmbH, Heidelberg, Germany Printed on acid-free paper Springer is part of Springer Science+Business Media (www.springer.com) Foreword – Carl Wunsch Many scientists are impatient with, and uninterested in, the history of their subject – and young scientists are universally urged to focus on what is not understood – to “exercise some imagination” – to look forward and not back. -
Walter Heinrich Munk
WALTER HEINRICH MUNK 19 october 1917 . 8 february 2019 PROCEEDINGS OF THE AMERICAN PHILOSOPHICAL SOCIETY VOL. 163, NO. 3, SEPTEMBER 2019 biographical memoirs alter Heinrich Munk was a brilliant scholar and scientist who was considered one of the greatest oceanographers of W his time. He was born in Vienna, Austria in 1917 as the Austro-Hungarian Empire was declining and just before the death of one of its great artists, Gustav Klimt. Hedwig Eva Maria Kiesler, who later changed her name to Hedy Lamarr to accommodate her film career, was one of Walter’s childhood friends.1 Walter’s mother, Rega Brunner,2 the daughter of a wealthy Jewish banker, divorced Walter’s father in 1927 and married Dr. Rudolf Engelsberg in 1928. By age 14, Walter apparently had not distinguished himself in his school studies and announced that he intended to become a ski instructor. Walter later claimed that it was this that caused his mother to send him to work at a family bank in New York. The validity of this claim should be tempered by the political turmoil in Germany and its proximity to Austria. In any case, Walter left Vienna in 1932. In New York, he attended Silver Bay Preparatory School for Boys on Lake George and then became a lowly employee in the Cassel Bank, which was associated with the family’s Brunner Bank in New York. In the meantime, Walter restarted his education at Columbia’s Extension School. He greatly disliked the work at the bank and apparently made a number of mistakes, which didn’t endear him to the owners of the Cassel Bank. -
Walter Munk and JASON By
Walter Munk and JASON by Richard L. Garwin IBM Fellow Emeritus IBM Thomas J. Watson Research Center P.O. Box 218, Yorktown Heights, NY 10598 www.fas.org/RLG/ (The “Garwin Archive”) Search it with, e.g., [site:fas.org/RLG/ “Walter Munk”] Email: [email protected] Walter Munk Legacy Symposium Scripps Institution of Oceanography La Jolla, CA October 17, 2019 _10/17/19_ Walter Munk and JASON.docx 1 I met Walter Munk probably in 1962, when I briefed the JASON group at its second summer study. But our paths had crossed much earlier, anonymously to be sure, when Walter survived the first thermonuclear explosion, on a small raft in the vast Pacific Ocean. This was the 10-megaton MIKE test on Enewetak Atoll, in the Marshall Islands. In a few minutes we’ll hear Walter’s account of the experience1. I came to know Walter well when I joined JASON in 1966, and I was able to benefit from his insights and experience. Since about 1957 I had worked almost half time with the President’s Science Advisor Committee (PSAC), created late that year by President Dwight D. Eisenhower. Although not yet a PSAC member, I had been asked to chair its Military Aircraft Panel and its AntiSubmarine Warfare Panel. It was in that latter context that I appreciated Walter as a scientist—energetic, imaginative, bold, courageous, and thorough. We’ll see Walter later in this talk, commenting on JASON, but first I list the JASON reports which he authored, usually with others who drew on and extended Walter’s long experience and deep understanding of the oceans and the science and phenomenology involved. -
Modern and Ancient Hiatuses in the Pelagic Caps of Pacific Guyots and Seamounts and Internal Tides GEOSPHERE; V
Research Paper GEOSPHERE Modern and ancient hiatuses in the pelagic caps of Pacific guyots and seamounts and internal tides GEOSPHERE; v. 11, no. 5 Neil C. Mitchell1, Harper L. Simmons2, and Caroline H. Lear3 1School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK doi:10.1130/GES00999.1 2School of Fisheries and Ocean Sciences, University of Alaska-Fairbanks, 905 N. Koyukuk Drive, 129 O’Neill Building, Fairbanks, Alaska 99775, USA 3School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3AT, UK 10 figures CORRESPONDENCE: neil .mitchell@ manchester ABSTRACT landmasses were different. Furthermore, the maximum current is commonly .ac .uk more important locally than the mean current for resuspension and transport Incidences of nondeposition or erosion at the modern seabed and hiatuses of particles and thus for influencing the sedimentary record. The amplitudes CITATION: Mitchell, N.C., Simmons, H.L., and Lear, C.H., 2015, Modern and ancient hiatuses in the within the pelagic caps of guyots and seamounts are evaluated along with of current oscillations should therefore be of interest to paleoceanography, al- pelagic caps of Pacific guyots and seamounts and paleotemperature and physiographic information to speculate on the charac- though they are not well known for the geological past. internal tides: Geosphere, v. 11, no. 5, p. 1590–1606, ter of late Cenozoic internal tidal waves in the upper Pacific Ocean. Drill-core Hiatuses in pelagic sediments of the deep abyssal ocean floor have been doi:10.1130/GES00999.1. and seismic reflection data are used to classify sediment at the drill sites as interpreted from sediment cores (Barron and Keller, 1982; Keller and Barron, having been accumulating or eroding or not being deposited in the recent 1983; Moore et al., 1978). -
Report for the Academic Year 1999
l'gEgasag^a3;•*a^oggMaBgaBK>ry^vg^.g^._--r^J3^JBgig^^gqt«a»J^:^^^^^ Institute /or ADVANCED STUDY REPORT FOR THE ACADEMIC YEAR 1998-99 PRINCETON • NEW JERSEY HISTORICAL STUDIES^SOCIAl SC^JCE LIBRARY INSTITUTE FOR ADVANCED STUDY PRINCETON, NEW JERSEY 08540 Institute /or ADVANCED STUDY REPORT FOR THE ACADEMIC YEAR 1 998 - 99 OLDEN LANE PRINCETON • NEW JERSEY • 08540-0631 609-734-8000 609-924-8399 (Fax) http://www.ias.edu Extract from the letter addressed by the Institute's Founders, Louis Bamberger and Mrs. FeUx Fuld, to the Board of Trustees, dated June 4, 1930. Newark, New Jersey. It is fundamental m our purpose, and our express desire, that in the appointments to the staff and faculty, as well as in the admission of workers and students, no account shall be taken, directly or indirectly, of race, religion, or sex. We feel strongly that the spirit characteristic of America at its noblest, above all the pursuit of higher learning, cannot admit of any conditions as to personnel other than those designed to promote the objects for which this institution is established, and particularly with no regard whatever to accidents of race, creed, or sex. ni' TABLE OF CONTENTS 4 • BACKGROUND AND PURPOSE 7 • FOUNDERS, TRUSTEES AND OFFICERS OF THE BOARD AND OF THE CORPORATION 10 • ADMINISTRATION 12 • PRESENT AND PAST DIRECTORS AND FACULTY 15 REPORT OF THE CHAIRMAN 18 • REPORT OF THE DIRECTOR 22 • OFFICE OF THE DIRECTOR - RECORD OF EVENTS 27 ACKNOWLEDGMENTS 41 • REPORT OF THE SCHOOL OF HISTORICAL STUDIES FACULTY ACADEMIC ACTIVITIES MEMBERS, VISITORS, -
Once Again: Once Againmtidal Friction
Prog. Oceanog. Vol. 40~ pp. 7-35, 1997 © 1998 Elsevier Science Ltd. All rights reserved Pergamon Printed in Great Britain PII: S0079-6611( 97)00021-9 0079-6611/98 $32.0(I Once again: once againmtidal friction WALTER MUNK Scripps Institution of Oceanography, University of California-San Diego, La Jolht, CA 92093-0225, USA Abstract - Topex/Poseidon (T/P) altimetry has reopened the problem of how tidal dissipation is to be allocated. There is now general agreement of a M2 dissipation by 2.5 Terawatts ( 1 TW = 10 ~2 W), based on four quite separate astronomic observational programs. Allowing for the bodily tide dissipation of 0.1 TW leaves 2.4 TW for ocean dissipation. The traditional disposal sites since JEFFREYS (1920) have been in the turbulent bottom boundary layer (BBL) of marginal seas, and the modern estimate of about 2.1 TW is in this tradition (but the distribution among the shallow seas has changed radically from time to time). Independent estimates of energy flux into the mar- ginal seas are not in good agreement with the BBL estimates. T/P altimetry has contributed to the tidal problem in two important ways. The assimilation of global altimetry into Laplace tidal solutions has led to accurate representations of the global tides, as evidenced by the very close agreement between the astronomic measurements and the computed 2.4 TW working of the Moon on the global ocean. Second, the detection by RAY and MITCHUM (1996) of small surface manifestation of internal tides radiating away from the Hawaiian chain has led to global estimates of 0.2 to 0.4 TW of conversion of surface tides to internal tides. -
Geological Society of America Bulletin, Published Online on 2 May 2014 As Doi:10.1130/B30936.1
Geological Society of America Bulletin, published online on 2 May 2014 as doi:10.1130/B30936.1 Geological Society of America Bulletin Ka'ena Volcano−−A precursor volcano of the island of O'ahu, Hawai'i John M. Sinton, Deborah E. Eason, Mary Tardona, Douglas Pyle, Iris van der Zander, Hervé Guillou, David A. Clague and John J. Mahoney Geological Society of America Bulletin published online 2 May 2014; doi: 10.1130/B30936.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. -
The Luck of Walter Munk
015K1999_KP_LE_B_en.doc The Luck of Walter Munk Walter H. Munk We have been asked to talk about ourselves. For a title, I have chosen the title of a talk given by Roger Revelle in 1982＊. I was born in Austria soon after the end of World War I. My grandfather Lucian Brunner [photo 1] was a Viennese banker with political ambitions. He ran for mayor on a reform platform and was thoroughly defeated. He became a socialist and changed the name of his bank from “Lucian Brunner” to “Österreichische Volksbank” (Austrian People’s Bank), but kept all the shares. Grandfather was intrigued by high technology. He was on the board of the “Südbahn,” the railroad that developed the audacious route from Vienna to Trieste, and he built funiculars in the Dolomites. This area is now in Italy, but was then part of Austria. At the time it would have made some sense for an Austrian to become an oceanographer. Austria had inherited the northern Adriatic, down to Venice, from Napoleon, had a Navy and was doing respectable ocean research. But by the time I grew up the country was landlocked, and becoming an oceanographer made no sense at all. Lucian’s daughter, my mother [photo 2], read botany at Newnham, one of the two women’s colleges at Cambridge University. It was then unheard of for a girl from the continent to go to university in England. She married my father at the end of the war. They were divorced when I was very young, and father went to live and ski in Kitzbuehel. -
Hawaiian Helicinidae
HAWAIIAN HELICINIDAE BY MARIE C. NEAL BERNICE P. BISHOP MUSEUM BULLETIN 125 HONOLULU, HAWAII PUBLISHED BY THE MUSEUM 1934 CONTENTS PAG!I Introduction 3 Orobophana 9 Pleuropoma ...................................................................................................................................... 38 Pleuropoma (Sphaeroconia) ...................................................................................................... 83 Doubtful and exluded species........................................................................................................ g8 ILLUSTRATIONS PAGll FIGURES 1-17.-0robophana from Kauai ................................................................................ 12 18-29.-0robophana uberta and varieties and forms from Waianae Moun- tains, Oahu .................................................................................................. 20 30-43.-Varieties of Orobophana uberta from Koolau Range, Oahu.................. 28 44-61.-Pleuropoma laciniosa and varieties from Oahu........................................ 41 62-72.-Varieties of Pleuropoma laciniosa from Kauai and Niihau.................... 66 73-91.-Varieties and forms of Pleuropoma laciniosa from islands south of Oahu .............................................................................................................. 71 92-101.-Three other species of Pleuropoma (sensu stricto).............................. 80 102-117.-Species and varieties of Pleuropoma (Sphaeroconia)............................ 86 [i] Hawaiian Helicinidae -
Villa Heimann-Rosenthala2 | Gartenansicht 2 3
1 Villa Heimann-Rosenthala2 | Gartenansicht 2 3 a3 4 5 a4 6 a5 7 8 a6 9 10 a7 11 12 a8 13 a9 14 15 a10 16 17 a11 18 a12 19 20 a13 21 In View A Photo Essay by Arno Gisinger a1 Jewish Museum Hohenems / Villa Clara Heimann-Rosenthal, front a2 Jewish Museum Hohenems, back a3 Corner of former Jews’ Lane (left) and Christians’ Lane a4 Tenants of the former Jewish poorhouse (Burgauer house) a5 Former Jewish poorhouse, back a6 Salomon Sulzer Auditorium in the former synagogue a7 Square in front of the former synagogue with Brettauer house (left) and Sulzer house (right) a8 Tenant in the Brettauer house a9 Mikvah and former Jewish school before restoration a10 Emsbach a11 Villa Arnold Rosenthal (Schubertiade festival), back a12 Betting office in one of the court factors houses a13 View of the former Jew’s Lane between court factors houses and Sulzer house a14 - 26 Jewish Museum Hohenems, interior a27 Former Jewish poorhouse (left), in the former “Judenwinkel” (Jew’s Corner) a28 Tenants of the former “Judenwinkel” a29 Former inn “Zur Frohen Aussicht” (At the Happy Prospect) a30 Former Jewish school before restoration a31 Construction activity in the former Jewish quarter: Senior citizens home (right), Brunner house (left), and Elkan house (center) a32 Former court factors’ houses a33 View from the Emsbach a34 Tenants of the Kitzinger house a35 View from the Jewish quarter a36 The count’s palace a37 Jewish cemetery, entrance and hall a38 Jewish cemetery a39 Jewish cemetery [Israelitengasse in Hohenems, Fritz and Paul Tänzer (foreground), c. -
Young Tracks of Hotspots and Current Plate Velocities
Geophys. J. Int. (2002) 150, 321–361 Young tracks of hotspots and current plate velocities Alice E. Gripp1,∗ and Richard G. Gordon2 1Department of Geological Sciences, University of Oregon, Eugene, OR 97401, USA 2Department of Earth Science MS-126, Rice University, Houston, TX 77005, USA. E-mail: [email protected] Accepted 2001 October 5. Received 2001 October 5; in original form 2000 December 20 SUMMARY Plate motions relative to the hotspots over the past 4 to 7 Myr are investigated with a goal of determining the shortest time interval over which reliable volcanic propagation rates and segment trends can be estimated. The rate and trend uncertainties are objectively determined from the dispersion of volcano age and of volcano location and are used to test the mutual consistency of the trends and rates. Ten hotspot data sets are constructed from overlapping time intervals with various durations and starting times. Our preferred hotspot data set, HS3, consists of two volcanic propagation rates and eleven segment trends from four plates. It averages plate motion over the past ≈5.8 Myr, which is almost twice the length of time (3.2 Myr) over which the NUVEL-1A global set of relative plate angular velocities is estimated. HS3-NUVEL1A, our preferred set of angular velocities of 15 plates relative to the hotspots, was constructed from the HS3 data set while constraining the relative plate angular velocities to consistency with NUVEL-1A. No hotspots are in significant relative motion, but the 95 per cent confidence limit on motion is typically ±20 to ±40 km Myr−1 and ranges up to ±145 km Myr−1.