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Supplying Rochester in the Age of the Erie Canal
SUPPLYING ROCHESTER IN THE AGE OF THE ERIE CANAL: AN EXAMINATION OF THE INVENTORIES OF CERAMIC AND GLASS MERCHANT BENJAMIN SEABURY by Sara McNamara A thesis submitted to the Faculty of the University of Delaware in partial fulfillment of the requirements for the degree of Master of the Arts in American Material Culture Spring 2018 © 2018 Sara McNamara All Rights Reserved SUPPLYING ROCHESTER IN THE AGE OF THE ERIE CANAL: AN EXAMINATION OF THE INVENTORIES OF CERAMIC AND GLASS MERCHANT BENJAMIN SEABURY by Sara McNamara Approved: __________________________________________________________ Thomas A. Guiler, Ph.D. Professor in charge of thesis on behalf of the Advisory Committee Approved: __________________________________________________________ Wendy Bellion, Ph.D. Acting Director of the Winterthur Program in American Material Culture Approved: __________________________________________________________ George H. Watson, Ph.D. Dean of the College of Arts & Sciences Approved: __________________________________________________________ Ann L. Ardis, Ph.D. Senior Vice Provost for Graduate and Professional Education ACKNOWLEDGMENTS As with all projects, this research would not have been possible without the help and support of many people. I am grateful and indebted to all those who assisted me in various stages of my research from the initial planning to the final editing. First and foremost, I thank my advisor Dr. Thomas Guiler for his indefatigable enthusiasm for my work. Tom was always there for me with a ready high five or conversation about Syracuse basketball to keep me from feeling overwhelmed. This thesis would not exist without his suggestions, edits, and advice. I am thankful to the University of Delaware, which granted Winterthur Program Professional Development Funds to this research. -
The Elevation-Dependence of Snowfall in the Appalachian Ridge and Valley Region of Northeastern Pennsylvania
Evans, M., M. Jurewicz, and R. Kline, 2017: The elevation-dependence of snowfall in the Appalachian Ridge and Valley region of northeastern Pennsylvania. J. Operational Meteor., 5 (8), 87-102, doi: https://doi.org/10.15191/nwajom.2017.0508. The Elevation-Dependence of Snowfall in the Appalachian Ridge and Valley Region of Northeastern Pennsylvania MICHAEL EVANS NOAA/NWS Binghamton, New York MICHAEL JUREWICZ NOAA/NWS Binghamton, New York RACHAEL KLINE State University of New York at Binghamton, New York (Manuscript received 13 November 2016; review completed 26 March 2017) ABSTRACT Northeastern Pennsylvania is located in the Appalachian Ridge and Valley region characterized by northeast– southwest oriented ridges running parallel to broad valleys. Snowfall in the region can vary considerably over short distances owing to differences in elevation. To study the impact of elevation on snowfall in this region, a collection of snow events from 2005 to 2014 was studied. The median high-elevation versus low-elevation snowfall ratio—or orographic ratio—for the events was 1.27; however, several cases were identified that departed substantially from the average. The primary goal of this study is to give forecasters an understanding of factors that modulate the impact of elevation on snowfall in this region. Nine events with a high-elevation dependency were compared to twelve events with a low-elevation dependency. High dependency was most likely with high-amplitude flow and deep surface cyclones along the East Coast, whereas low-dependency cases were associated with Miller type B cyclone tracks and flow that was less amplified. High-elevation dependency also was most likely for events with strong lower-tropospheric winds, along with surface temperatures >–1°C (30°F) at Avoca, Pennsylvania. -
Celebrating Hugh Miller
Photo: Andrew Dowsett Bust by William Brodie, 1857, in birthplace cottage, Cromarty (NTS). CELEBRATING THE LIFE AND TIMES OF HUGH MILLER Scotland in the Early 19th Century Ethnography & folklore, geology & natural history, church & society Edited by Lester Borley Copyrights © The Editor & Contributors severally 2003 Published by the Cromarty Arts Trust & the Elphinstone Institute of the University of Aberdeen with the financial support of Scottish Natural Heritage and Ross & Cromarty Enterprise * A collection of papers presented at an international conference held in Cromarty from 10-12 October 2002, to celebrate the bicentenary of Hugh Miller. Organised by the Cromarty Arts Trust in collaboration with the Elphinstone Institute of the University of Aberdeen and the Highland Theological College. * Under the patronage of Dr James Hunter, Rt Hon Lord Mackay of Clashfern, Mrs Marian McKenzie Johnston, Dr John Nightingale of Cromarty, Mrs Anne Short, Professor Duncan Rice and Professor Roger Wheater. ISBN NB insert number in black before printing, or delete this whole line Foreword Dr John Nightingale Chairman, Cromarty Arts Trust Hugh Miller used his understanding of fossils to transport his readers back in time to witness a spell-binding spectacle of the creation and unfolding of the world in geo- logical time. The papers collected in this bicentenary volume similarly use Hugh Miller’s life and writings to open up the great issues of geology, church and society, and ethnography in Scotland in the first half of the nineteenth century – a period of great scientific discoveries, revolution in the church, and of clearances, emigration, urbani- sation and rapid social change. Miller’s ability to combine the skills of a Highland story-teller with the visual imagery of new technologies of panoramas and dioramas to dramatise his subject may be hard to match, but these papers leave readers in no doubt that this period was every bit as formative as the Scottish Enlightenment. -
PREFACE ERWIN, UNICOI COUNTY, TENNESSEE (Data Compiled by Toney Insurance Agency)
INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6” x 9” black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. Bell & Howell Information and Learning 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA UIVII 800-521-0600 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. NOTE TO USERS This reproduction is the best copy availabie. UMI Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. -
P4.475 a Comparison of Wrf 3.2 and Wrf 3.1.1 Forecasts of Eight Nor’Easter Events
P4.475 A COMPARISON OF WRF 3.2 AND WRF 3.1.1 FORECASTS OF EIGHT NOR’EASTER EVENTS Stephen D. Nicholls* and Steven G. Decker Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, NJ, USA 1. INTRODUCTION cold bias was successfully reduced to within ±0.5 K day−1 of the standard cooling rates. Here, we will Since 1950 when a team of Princeton scientists compare the performance of WRF version 3.1.1 to WRF completed the first successful numerical weather version 3.2 during eight nor’easter simulations and also forecast on ENIAC, numerical weather prediction has determine to what degree the new RRTM 3.2 longwave become an integral aspect of atmospheric science. As scheme has contributed to these performance computer technology has advanced, so have the differences. complexity and capability of prognostic atmospheric models. Present day models, such as the Weather Research and Forecasting Model (WRF) Advanced 2. METHODOLOGY Research WRF (WRF-ARW; hereafter shortened to WRF), solve computationally intensive, fully This WRF-based study will solely focus on intense compressible, non-hydrostatic equations at specified wintertime cyclones that affect the Northeastern United time steps and using specified boundary conditions, States (nor’easters) given the complex interaction which allow simulations of the atmosphere at model between dynamics and thermodynamics that underpin resolutions of which the Princeton scientists could have their development and maintenance. Specifically for this only dreamed. Despite such advancements, the WRF study, we chose eight nor’easter cases that occurred model remains imperfect; thus, it is updated and refined between the months of October – April and the years annually as new errors are found and new schemes are 2006 – 2010 (See Table 1). -
Ith Orange and Newark, Replacing the Stage Coaches That Had Formerly Run on What Is Now South Orange Avenue
NP8 Form 10400 0MB No. 1024-001* (R«v. M6) United States Department of the Interior National Park Service National Register of Historic Places Registration Form This form Is for use In nominating or requesting determinations of eligibility for Individual properties or districts. See Instructions In Guidelines for Completing National Register Forms (National Register Bulletin 16). Complete each item by marking "x" in the appropriate box or by entering the requested Information. If an Item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, styles, materials, and areas of significance, enter only the categories and subcategorles listed In the Instructions. For additional space use continuation sheets (Form 10-900a). Type all entries. 1. Name of Proptrty historic name Stone House by the Stone House Brook other names/site number 2. Location street & number South Orange Avenue Mnot for publication city, town Township of South Orange Village ^vicinity state New Jersey code 034 county Essex code 013 zlpoode 07079 3. Claaalflcatlon Ownership of Property Category of Property Number of Resources within Property private 2 bulldlng(a) Contributing Noncontrlbutlng public-local district 1 ___ buildings public-State •Ite 1 ___sites public-Federal structure ___ ___ structures object ___ ___objects 2 0 Total Name of related multiple property listing: Number of contributing resources previously NA listed In the National Register ° 4. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act of 1986, as amended, I hereby certify that this DD nomination EH request for determination of eligibility meets the documentation standards for registering properties In the National Register of Historic Places and meets the procedural and professional requirements set forth In 36 CFR Part 60. -
National Assessment of Ia W Enforcement Anti-Gang Information Resources
If you have issues viewing or accessing this file contact us at NCJRS.gov. l NATIONAL ASSESSMENT OF IAW ENFORCEMENT ANTI-GANG INFORMATION RESOURCES FINAL REPORT ... ~" : ~ . o West Virginia University National Assessment SUlVey t;'''' ...... ~ .. ' ,.. .•.. ,~: '. ~ '. !r' ;: .......------------------ NA.TIONAL ASSESSMENT OF LAW ENFORCEMENT ANTI-GANG INFORMATION RESOURCES DRAFT 1992 FINAL REPORT G. David Curry, Robert J. Fox, Richard A. Ball, and Darryl Stone Department of Sociology & Anthropology West Virginia University * Funding for this research was provided by Cooperative Agreement Number 91-IJ-CX- KOO3 from the National Institute of Justice, U.S. Department of Justice. Points of view or opinions in this document are those of the author and do not necessarily represent the official position or policies of the U.S. Department of Justice. We wish to thank Mary Jo Ullom, William Mase, Michael Proffitt, and Lorrie Hardy for their assistance in gathering and preparing these data. Valuable comments were provided on earlier drafts by Winnie Reed, Craig Uchida, Joan McCord, and Richard Block. I I I I I I I 147399 U.S. Department of JLlstice I National Institute of Justice This document has been reproduced exactly as received from the person or organization originating it. Points of view or opinions stated in this document are those of the authors and do not necessarily represent I the official position or policies of the National Institute of Justice. Permission to reproduce this u:Si'}IrtI<.. material has been gra~11fhic Domain/NIJ I U.S. Department of Justice to the National Criminal Justice Reference Service (NCJRS). Further reproduction outside of the NCJRS system requires permission of the ~ owner.