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Daily Iowan (Iowa City, Iowa), 1953-10-22
The Weather Serving the State Partb c10., aDd eeoIH ·versity of Iowa toda,. CleariDc ....... Art slderlbb eooIer FrWar. Campus and JII,h ~aJ. T.; 1_. 52; Hla'h WednH41a7. II; low. he SUI art i.:wa City 67. attend the 1868 - A,P Leased Wile, Wirephot.o - Five Cent. Iowa City, Iowa, Thursday, Oct. 22, 1953 - Vol. 97, No. 276 the found- , Eat. College Art • ~---------------------------------------------- Department orlSin. Mln ./ '0 the rti.t trom .ohio the conter- ~ shown by ueen ·Will· Open Homecoming ence df 1he AcsthetJcs ege in. No- • Homecoming Mums Aqui Show To Feature Five Iowa sportscasters and Qne ------------ Varied Acts sports writer will judge the utes past any given point In the beauty, or~inallty and humor ot parade route. The 40 tloats wiU Three days ot 1953 Homecom , ' the I10nt entries In the fifth an- then move to the area just east In, frolic will let the ful\-steam- nual SUI Homecoming parade Frl- of Iowa stadium to remain throu,ll abead si,nal tonight when one ot day night at 7. Saturday's game as a post-parade Taking time out from their re- dISplay parade chairman Loren five campus lovelies is named porting responsibilities to score Hlcker ~on lays. Dolphin Queen for SUY'! 31st an- each of 40 floats ror beaut), will . nUIII poolsld~ sholl'. be Gene Claussen, KXIC Iowa Musical marching grou~s In the City and Gene Shumate KSO De parade will total 13, With nine Pre!\Cntatlon of the qucen-ror- Moines. • high school bands, Shriner bands a-weekend will come at 8 p.m. -
Annual Report COOPERATIVE INSTITUTE for RESEARCH in ENVIRONMENTAL SCIENCES
2015 Annual Report COOPERATIVE INSTITUTE FOR RESEARCH IN ENVIRONMENTAL SCIENCES COOPERATIVE INSTITUTE FOR RESEARCH IN ENVIRONMENTAL SCIENCES 2015 annual report University of Colorado Boulder UCB 216 Boulder, CO 80309-0216 COOPERATIVE INSTITUTE FOR RESEARCH IN ENVIRONMENTAL SCIENCES University of Colorado Boulder 216 UCB Boulder, CO 80309-0216 303-492-1143 [email protected] http://cires.colorado.edu CIRES Director Waleed Abdalati Annual Report Staff Katy Human, Director of Communications, Editor Susan Lynds and Karin Vergoth, Editing Robin L. Strelow, Designer Agreement No. NA12OAR4320137 Cover photo: Mt. Cook in the Southern Alps, West Coast of New Zealand’s South Island Birgit Hassler, CIRES/NOAA table of contents Executive summary & research highlights 2 project reports 82 From the Director 2 Air Quality in a Changing Climate 83 CIRES: Science in Service to Society 3 Climate Forcing, Feedbacks, and Analysis 86 This is CIRES 6 Earth System Dynamics, Variability, and Change 94 Organization 7 Management and Exploitation of Geophysical Data 105 Council of Fellows 8 Regional Sciences and Applications 115 Governance 9 Scientific Outreach and Education 117 Finance 10 Space Weather Understanding and Prediction 120 Active NOAA Awards 11 Stratospheric Processes and Trends 124 Systems and Prediction Models Development 129 People & Programs 14 CIRES Starts with People 14 Appendices 136 Fellows 15 Table of Contents 136 CIRES Centers 50 Publications by the Numbers 136 Center for Limnology 50 Publications 137 Center for Science and Technology -
Association of Unit Owners Contact List
Association of Unit Owners Contact List Project Name/Number AOUO Designated Officer for Direct Contact/Mailing Address Management Company/Telephone Number `AKOKO AT HO`OPILI Reg.# 8073 1001 QUEEN Reg.# 7675 1001 WILDER EMILY PRESIDENT 1001 WILDER #305 HAWAIIAN PROPERTIES, LTD. Reg.# 5 WATERS HONOLULU HI 96822 8085399777 1010 WILDER RICHARD TREASURER 1010 WILDER AVE, OFFICE SELF MANAGED Reg.# 377 KENNEDY HONOLULU HI 96822 8085241961 1011 PROSPECT RICHARD PRESIDENT 1188 BISHOP ST STE 2503 CERTIFIED MANAGEMENT INC dba ASSOCI Reg.# 1130 CONRADT HONOLULU HI 96813 8088360911 1015 WILDER KEVIN PRESIDENT 1015 WILDER AVE #201 HAWAIIANA MGMT CO LTD Reg.# 1960 LIMA HONOLULU HI 96822 8085939100 1037 KAHUAMOKU VITA PRESIDENT 94-1037 KAHUAMOKU ST 3 CEN PAC PROPERTIES INC Reg.# 1551 VILI WAIPAHU HI 96797 8085932902 1040 KINAU PAUL PRESIDENT 1040 KINAU ST., #1206 HAWAIIAN PROPERTIES, LTD. Reg.# 527 FOX HONOLULU HI 96814 8085399777 1041 KAHUAMOKU ALAN PRESIDENT 94-1041 KAHUAMOKU ST 404 CEN PAC PROPERTIES INC Reg.# 1623 IGE WAIPAHU HI 96797 8085932902 1054 KALO PLACE JUANA PRESIDENT 1415 S KING ST 504 HAWAIIANA MGMT CO LTD Reg.# 5450 DAHL HONOLULU HI 96814 8085939100 1073 KINAU ANSON PRESIDENT 1073 KINAU ST 1003 HAWAIIANA MGMT CO LTD Reg.# 616 QUACH HONOLULU HI 96814 8085939100 1108 AUAHI TODD PRESIDENT 1240 ALA MOANA BLVD STE. 200 HAWAIIANA MGMT CO LTD Reg.# 7429 APO HONOLULU HI 96814 8085939100 1111 WILDER BRENDAN PRESIDENT 1111 WILDER AVE 7A HAWAIIAN PROPERTIES, LTD. Reg.# 228 BURNS HONOLULU HI 96822 8085399777 1112 KINAU LINDA Y SOLE OWNER 1112 KINAU ST PH SELF MANAGED Reg.# 1295 NAKAGAWA HONOLULU HI 96814 1118 ALA MOANA NICHOLAS PRESIDENT 1118 ALA MOANA BLVD., SUITE 200 HAWAIIANA MGMT CO LTD Reg.# 7431 VANDERBOOM HONOLULU HI 96814 8085939100 1133 WAIMANU ANNA PRESIDENT 1133 WAIMANU STREET, STE. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
Worry Over Mistreating Clots Drove Push to Pause J&J Shot
P2JW109000-6-A00100-17FFFF5178F ****** MONDAY,APRIL 19,2021~VOL. CCLXXVII NO.90 WSJ.com HHHH $4.00 Last week: DJIA 34200.67 À 400.07 1.2% NASDAQ 14052.34 À 1.1% STOXX 600 442.49 À 1.2% 10-YR. TREASURY À 27/32 , yield 1.571% OIL $63.13 À $3.81 EURO $1.1982 YEN 108.81 Bull Run What’s News In Stocks Widens, Business&Finance Signaling More stocks have been propelling the U.S. market higher lately,asignal that fur- Strength ther gains could be ahead, but howsmooth the climb might be remains up fordebate. A1 Technical indicators WeWork’s plan to list suggestmoregains, stock by merging with a but some question how blank-check company has echoes of its approach in smooth theywill be 2019,when the shared-office provider’s IPO imploded. A1 BY CAITLIN MCCABE Citigroup plans to scale up its services to wealthy GES Agreater number of stocks entrepreneurs and their IMA have been propelling the U.S. businesses in Asia as the market higher lately,asignal bank refocuses its opera- GETTY that—if historyisany indica- tions in the region. B1 SE/ tor—moregains could be ahead. What remains up forde- A Maryland hotel mag- bate, however, is how smooth natebehind an 11th-hour bid ANCE-PRES FR the climb will be. to acquireTribune Publish- Indicatorsthat point to a ing is working to find new ENCE stronger and moreresilient financing and partnership AG stock market have been hitting options after his partner ON/ LL rare milestones recently as the withdrew from the deal. -
Planetary Constants and Models
JPL D-12947 PF-IOO-PMC-01 Mars Pathfinder ProJect PLANETARY CONSTANTS AND MODELS Mars at Launch Earth at La_ Dec 2, 1996 SunI, Earth at Mars at Aniva July 4, 1997 December 1995 JilL Jet Propulsion Laboratory California Institute of Technology Pasadena, California JPL D-I2947 PF-IOO-PMC-OI Mars Pathfinder Project PLANETARY CONSTANTS AND MODELS Prepared by: ' Robin Vaughan December 1995 JPL Jet Propulsion Laboratory California Institute of Technology Pasadena, California JPL D-12947 PFolOO-PMCoO1 Revision History Date Changes Status 10/95 Issued preliminary version for review by project person-el Draft 12/95 First official release; incorporated comments from prelimi- Final nary review. JPL D- !294 7 PFo 100-PMCo 01 Contents List of Figures V 4 List of Tables vii List of Acronyms and Abbreviations ix INTRODUCTION 1 1.1 Purpose ............ .......................... 1 1.2 Scope .................... ................... 1 2 COORDINATE SYSTEMS 3 2.1 Definitions 2.1.1 Frame • " • • • ° * ° • " ° • * • ° ° " ° ° * ° • • • ° " " " ' • • • • • • 3 2.1.2 Center • " " • ° " " " ' ° ° ° • * " • • " • " • • " • " " " ° • ° • • • . • 6 2.1.3 Type .................................... 7 2.2 Celestial Systems . ; ............................. 7 2.2.1 The Inertial Reference Frames ..................... 8 2.2.2 Sun-Centered Systems .......................... 9 2.2.3 Earth-Centered Systems ......................... 9 2.2.4 Mars-Centered Systems ......................... 11 2.2.5 Spacecraft-CenteredSystems ...................... 16 2.2.6 MiscellaneousSystems -
Turbulence and Aeolian Morphodynamics in Craters on Mars: Application to Gale Crater, Landing Site of the Curiosity Rover
16TH EUROPEAN TURBULENCE CONFERENCE, 21-24 AUGUST, 2017, STOCKHOLM,SWEDEN TURBULENCE AND AEOLIAN MORPHODYNAMICS IN CRATERS ON MARS: APPLICATION TO GALE CRATER, LANDING SITE OF THE CURIOSITY ROVER William Anderson1, Gary Kocurek2 & Kenzie Day2 1Mechanical Engineering Dept., Univ. Texas at Dallas, Richardson, Texas, USA 2Dept. Geological Sciences, Jackson School of Geosciences, Univ. Texas at Austin, Austin, Texas, USA Mars is a dry planet with a thin atmosphere. Aeolian processes – wind-driven mobilization of sediment and dust – are the dominant mode of landscape variability on the dessicated landscapes of Mars. Craters are common topographic features on the surface of Mars, and many craters on Mars contain a prominent central mound (NASA’s Curiosity rover was landed in Gale crater, shown in Figure 1a [1], while Figures 1b and 1c show Henry and Korolev crater, respectively). These mounds are composed of sedimentary fill and, therefore, they contain rich information on the evolution of climatic conditions on Mars embodied in the stratigraphic “layering” of sediments. Many other craters no longer house a mound, but contain sediment and dust from which dune fields and other features form (see, for example, Victoria Crater, Figure 1d). Using density-normalized large-eddy simulations, we have modeled turbulent flows over crater-like topographies that feature a central mound. Resultant datasets suggest a deflationary mechanism wherein vortices shed from the upwind crater rim are realigned to conform to the crater profile via stretching and tilting. This was accomplished using three- dimensional datasets (momentum and vorticity) retrieved from LES. As a result, helical vortices occupy the inner region of the crater and, therefore, are primarily responsible for aeolian morphodynamics in the crater (radial katabatic flows are also important to aeolian processes within the crater [2]). -
Russian Museums Visit More Than 80 Million Visitors, 1/3 of Who Are Visitors Under 18
Moscow 4 There are more than 3000 museums (and about 72 000 museum workers) in Russian Moscow region 92 Federation, not including school and company museums. Every year Russian museums visit more than 80 million visitors, 1/3 of who are visitors under 18 There are about 650 individual and institutional members in ICOM Russia. During two last St. Petersburg 117 years ICOM Russia membership was rapidly increasing more than 20% (or about 100 new members) a year Northwestern region 160 You will find the information aboutICOM Russia members in this book. All members (individual and institutional) are divided in two big groups – Museums which are institutional members of ICOM or are represented by individual members and Organizations. All the museums in this book are distributed by regional principle. Organizations are structured in profile groups Central region 192 Volga river region 224 Many thanks to all the museums who offered their help and assistance in the making of this collection South of Russia 258 Special thanks to Urals 270 Museum creation and consulting Culture heritage security in Russia with 3M(tm)Novec(tm)1230 Siberia and Far East 284 © ICOM Russia, 2012 Organizations 322 © K. Novokhatko, A. Gnedovsky, N. Kazantseva, O. Guzewska – compiling, translation, editing, 2012 [email protected] www.icom.org.ru © Leo Tolstoy museum-estate “Yasnaya Polyana”, design, 2012 Moscow MOSCOW A. N. SCRiAbiN MEMORiAl Capital of Russia. Major political, economic, cultural, scientific, religious, financial, educational, and transportation center of Russia and the continent MUSEUM Highlights: First reference to Moscow dates from 1147 when Moscow was already a pretty big town. -
Local Lunar Gravity Field Analysis Over the South Poleaitken Basin from SELENE Farside Tracking Data
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, E02005, doi:10.1029/2011JE003831, 2012 Local lunar gravity field analysis over the South Pole-Aitken basin from SELENE farside tracking data Sander Goossens,1,2,3 Yoshiaki Ishihara,1 Koji Matsumoto,1 and Sho Sasaki1 Received 16 March 2011; revised 22 November 2011; accepted 13 December 2011; published 14 February 2012. [1] We present a method with which we determined the local lunar gravity field model over the South Pole-Aitken (SPA) basin on the farside of the Moon by estimating adjustments to a global lunar gravity field model using SELENE tracking data. Our adjustments are expressed in localized functions concentrated over the SPA region in a spherical cap with a radius of 45° centered at (191.1°E, 53.2°S), and the resolution is equivalent to a 150th degree and order spherical harmonics expansion. The new solution over SPA was used in several applications of geophysical analysis. It shows an increased correlation with high-resolution lunar topography in the frequency band l =40–70, and admittance values are slightly different and more leveled when compared to other, global gravity field models using the same data. The adjustments expressed in free-air anomalies and differences in Bouguer anomalies between the local solution and the a priori global solution correlate with topographic surface features. The Moho structure beneath the SPA basin is slightly modified in our solution, most notably at the southern rim of the Apollo basin and around the Zeeman crater. Citation: Goossens, S., Y. Ishihara, K. Matsumoto, and S. Sasaki (2012), Local lunar gravity field analysis over the South Pole-Aitken basin from SELENE farside tracking data, J. -
Coalescence and Particle Self-Assembly of Inkjet-Printed Colloidal Drops
Coalescence and Particle Self-assembly of Inkjet-printed Colloidal Drops A Thesis Submitted to the Faculty of Drexel University by Xin Yang in partial fulfillment of the requirements for the degree of Doctor of Philosophy December 2014 ii © Copyright 2014 Xin Yang. All Rights Reserved. iii Acknowledgements I would like to thank my advisor Prof. Ying Sun. During the last 3 years, she supports and guides me throughout the course of my Ph.D. research with her profound knowledge and experience. Her dedication and passion for researches greatly encourages me in pursuing my career goals. I greatly appreciate her contribution to my growth during my Ph.D. training. I would like to thank my parents, my girlfriend, my colleagues (Brandon, Charles, Dani, Gang, Dong-Ook, Han, Min, Nate, and Viral) and friends (Abraham, Mahamudur, Kewei, Patrick, Xiang, and Yontae). I greatly appreciate Prof. Nicholas Cernansky, Prof. Bakhtier Farouk, Prof. Adam Fontecchio, Prof. Frank Ji, Prof. Alan Lau, Prof. Christopher Li, Prof. Mathew McCarthy, and Prof. Hongseok (Moses) Noh for their critical assessments and positive suggestions during my candidacy exam, proposal and my defense. I also appreciate the financial supports of National Science Foundation (Grant CAREER-0968927 and CMMI-1200385). iv TABLE OF CONTENTS LIST OF TABLES ............................................................................................................ vii LIST OF FIGURES ......................................................................................................... viii -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei -
The Composition of the Lunar Crust: Radiative Transfer Modeling and Analysis of Lunar Visible and Near-Infrared Spectra
THE COMPOSITION OF THE LUNAR CRUST: RADIATIVE TRANSFER MODELING AND ANALYSIS OF LUNAR VISIBLE AND NEAR-INFRARED SPECTRA A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI‘I IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN GEOLOGY AND GEOPHYSICS DECEMBER 2009 By Joshua T.S. Cahill Dissertation Committee: Paul G. Lucey, Chairperson G. Jeffrey Taylor Patricia Fryer Jeffrey J. Gillis-Davis Trevor Sorensen Student: Joshua T.S. Cahill Student ID#: 1565-1460 Field: Geology and Geophysics Graduation date: December 2009 Title: The Composition of the Lunar Crust: Radiative Transfer Modeling and Analysis of Lunar Visible and Near-Infrared Spectra We certify that we have read this dissertation and that, in our opinion, it is satisfactory in scope and quality as a dissertation for the degree of Doctor of Philosophy in Geology and Geophysics. Dissertation Committee: Names Signatures Paul G. Lucey, Chairperson ____________________________ G. Jeffrey Taylor ____________________________ Jeffrey J. Gillis-Davis ____________________________ Patricia Fryer ____________________________ Trevor Sorensen ____________________________ ACKNOWLEDGEMENTS I must first express my love and appreciation to my family. Thank you to my wife Karen for providing love, support, and perspective. And to our little girl Maggie who only recently became part of our family and has already provided priceless memories in the form of beautiful smiles, belly laughs, and little bear hugs. The two of you provided me with the most meaningful reasons to push towards the "finish line". I would also like to thank my immediate and extended family. Many of them do not fully understand much about what I do, but support the endeavor acknowledging that if it is something I’m willing to put this much effort into, it must be worthwhile.