Major Winter Storms in the Midwest During Winter 2006-2007
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Chapter 3 the Development of North American Cities
CHAPTER 3 THE DEVELOPMENT OF NORTH AMERICAN CITIES THE COLONIAL F;RA: 1600-1800 Beginnings The Character of the Early Cities The Revolutionary War Era GROWTH AND EXPANSION: 1800-1870 Cities as Big Business To The Beginnings of Industrialization Am Urhan-Rural/North-South Tensions ace THE ERA OF THE GREAT METROPOLIS: of! 1870-1950 bui Technological Advance wh, The Great Migration cen Politics and Problems que The Quality of Life in the New Metropolis and Trends Through 1950 onl tee] THE NORTH AMERICAN CIITTODAY: urb 1950 TO THE PRESENT Can Decentralization oft: The Sun belt Expansion dan THE COMING OF THE POSTINDUSTRIAL CIIT sug) Deterioration' and Regeneration the The Future f The Human Cost of Economic Restructuring rath wor /f!I#;f.~'~~~~'A'~~~~ '~·~_~~~~Ji?l~ij:j hist. The Colonial Era Thi: fron Growth and Expansion coa~ The Great Metropolis Emerges to tJ New York Today new SUMMARY Nor CONCLUSION' T Am, cent EUf( izati< citie weal 62 Chapter 3 The Development of North American Cities 63 Come hither, and I will show you an admirable cities across the Atlantic in Europe. The forces Spectacle! 'Tis a Heavenly CITY ... A CITY to of postmedieval culture-commercial trade be inhabited by an Innumerable Company of An· and, shortly thereafter, industrial production geL" and by the Spirits ofJust Men .... were the primary shapers of urban settlement Put on thy beautiful garments, 0 America, the Holy City! in the United States and Canada. These cities, like the new nations themselves, began with -Cotton Mather, seventeenth· the greatest of hopes. Cotton Mather was so century preacher enamored of the idea of the city that he saw its American urban history began with the small growth as the fulfillment of the biblical town-five villages hacked out of the wilder· promise of a heavenly setting here on earth. -
Climatic Summary of Snowfall and Snow Depth in the Ohio Snowbelt at Chardon1
Ohio J. Science ENVIRONMENTAL EDUCATION 101 Climatic Summary of Snowfall and Snow Depth in the Ohio Snowbelt at Chardon1 THOMAS W. SCHMIDLIN, Geography Department and Water Resources Research Institute, Kent State University, Kent, OH 44242 ABSTRACT. Snowfall records were examined for the period 1945-85 at Chardon, OH, the only station with a long climatic record in the snowbelt. Average seasonal snowfall was 269 cm (106 in) with a seasonal maxi- mum of 410 cm (161 in). Seasonal snowfall was positively correlated with other sites in the lower Great Lakes snowbelts and along the western slope of the Appalachians from Tennessee to Quebec, but was not correlated with snowfall in the snowbelts of the upper Lakes. The time series of seasonal snowfall was not random but showed weak year-to-year persistence. The average number of days with 2.5 cm (1 in) of snow- fall was 35. The average dates of the first and last 2.5 cm snowfalls of the winter were 10 November and 4 April. The largest two-day snowfall of the winter averaged 33 cm. The average number of days with 2.5 cm of snow cover was 82. Daily probability of snow cover reached the seasonal maximum of 86% in mid-January and early February. These results may be reasonably extrapolated throughout the Ohio snow- belt for applications in vegetation studies, animal ecology, hydrology, soil science, recreation, and transpor- tation studies. OHIO J. SCI. 89 (4): 101-108, 1989 INTRODUCTION Great Lakes (Muller 1966, Eichenlaub 1970). The Lake The Great Lakes exert a significant influence on the Erie snowbelt extends from the eastern suburbs of regional climate (Changnon and Jones 1972, Eichen- Cleveland through extreme northeastern Ohio into laub 1979). -
Synoptic Climatology of Lake-Effect Snow Events Off the Western Great Lakes
climate Article Synoptic Climatology of Lake-Effect Snow Events off the Western Great Lakes Jake Wiley * and Andrew Mercer Department of Geosciences, Mississippi State University, 75 B. S. Hood Road, Starkville, MS 39762, USA; [email protected] * Correspondence: [email protected] Abstract: As the mesoscale dynamics of lake-effect snow (LES) are becoming better understood, recent and ongoing research is beginning to focus on the large-scale environments conducive to LES. Synoptic-scale composites are constructed for Lake Michigan and Lake Superior LES events by employing an LES case repository for these regions within the U.S. North American Regional Reanalysis (NARR) data for each LES event were used to construct synoptic maps of dominant LES patterns for each lake. These maps were formulated using a previously implemented composite technique that blends principal component analysis with a k-means cluster analysis. A sample case from each resulting cluster was also selected and simulated using the Advanced Weather Research and Forecast model to obtain an example mesoscale depiction of the LES environment. The study revealed four synoptic setups for Lake Michigan and three for Lake Superior whose primary differences were discrepancies in a surface pressure dipole structure previously linked with Great Lakes LES. These subtle synoptic-scale differences suggested that while overall LES impacts were driven more by the mesoscale conditions for these lakes, synoptic-scale conditions still provided important insight into the character of LES forcing mechanisms, primarily the steering flow and air–lake thermodynamics. Keywords: lake-effect; climatology; numerical weather prediction; synoptic; mesoscale; winter weather; Great Lakes; snow Citation: Wiley, J.; Mercer, A. -
Downloaded 09/29/21 01:04 PM UTC 938 WEATHER and FORECASTING VOLUME 17 of Subsequent Deep Moist Convection
VOLUME 17 WEATHER AND FORECASTING OCTOBER 2002 Recognition of Negative Mesoscale Factors for Severe-Weather Potential: A Case Study CHARLES A. DOSWELL III* NOAA/OAR/National Severe Storms Laboratory, Norman, Oklahoma DONALD V. B AKER NOAA/NWS Weather Forecast Of®ce, Lubbock, Texas CHARLIE A. LILES NOAA/NWS Weather Forecast Of®ce, Albuquerque, New Mexico (Manuscript received 2 November 2001, in ®nal form 23 April 2002) ABSTRACT The case of 7±8 June 1998 in eastern New Mexico and western Texas is used to illustrate the challenge of recognizing possible negative effects created by mesoscale processes. In this case, a region of cloud-covered cool air (which was associated with early thunderstorms) may have limited the tornadic potential of severe convection. Although the tornado potential in the synoptic situation was not highly portentous, supercell storms did eventually form, one of which was persistent for many hours. There were only relatively brief and weak tornadoes reported from this storm early in its life, despite its persistence as a long-lived supercell that produced a long swath of large hail. In this case, the development of thunderstorms east of the threat area early in the day maintained cloudiness that apparently inhibited the destabilization of the surface-based air mass over which the afternoon thunderstorms eventually moved. The persistent supercell formed on the dryline but overrode this mesoscale cool air mass relatively soon after it developed. It was able to persist as an elevated supercell despite the relatively stable near-surface air mass, but its tornadic production may have been limited by its interaction with this mesoscale feature. -
In Numerical Forecasts of Mesoscale Convective Systems
Meteorol. Atmos. Phys. 49, 93-106 (1992) Meteorology and Atmospheric Physics ~ Springer-Verlag 1992 Printed in Austria 551.515.4 The Pennsylvania State University, University Park, U.S.A. The Role of the Convective "Trigger Function" in Numerical Forecasts of Mesoscale Convective Systems J. S. Kain and J. M. Fritsch With 7 Figures Received November 18, 1991 Revised April 27, 1992 Summary sary to know the location and configuration of active convective cells that comprised mesoscale Three-dimensional numerical model simulations of a meso- convective systems. Consequently, convective scale convective system are performed to evaluate the sensitivity of the simulations to differences in the convective parameterization techniques typically relied on trigger function. The Penn State/NCAR mesoscale model empirically-based relationships between observed with the Kain-Fritsch convective parameterization scheme larger-scale processes and convective activity to is used as the modeling system for the study. All simulations predict when and where convection should occur. are performed on the June 10-11, 1985 squall line from the For example, some parameterizations were designed OK PRE-STORM field experiment. Individual simulations differ only in their specification of the trigger function within to initiate convection when a threshold value of the Kain-Fritsch scheme. Comparison of results from 12 hour mass or moisture convergence was exceeded at a simulations indicates that the position, timing, and intensity grid point where the atmosphere was conditionally -
The State of Asian Pacific America
THE STATE OF ASIAN PACIFIC AMERICA THE STATE OFASIANPACIFICAMERICA: ECONOMIC DIVERSITY, ISSUES & POLICIES A Public Policy Report PAULONG Editor LEAP Asian Pacific American Public Policy Institute and UCLA Asian American Studies Center 1994 Leadership Education for Asian Pacifies (LEAP), 327 East Second Street, Suite 226, Los Angeles, CA 90012-4210 UCLA Asian American Studies Center, 3230 Campbell Hall, 405 Hilgard Avenue, Los Angeles, CA 90024-1546 Copyright© 1994 by LEAP Asian Pacific American Public Policy Institute and UCLA Asian American Studies Center All rights reserved. Printed in the United States of America. ISBN: 0-934052-23-9 Cover design: Mary Kao The State of Asian Pacific America: Economic Diversity, Issues & Policies Paul Ong, Editor Table of Contents Preface vii Don T. Nakanishi and J. D. Hokoyama Chapter 1 Asian Pacific Americans and Public Policy 1 Paul Ong Part I. Overviews Chapter 2 Historical Trends 13 Don Mar and Marlene Kim Chapter3 Economic Diversity 31 Paul Ong and Suzanne J. Hee Chapter4 Workforce Policies 57 Linda C. Wing Part II. Case Studies Chapter5 Life and Work in the Inner-City 87 Paul Ong and Karen Umemoto v Chapter6 Welfare and Work Among Southeast Asians 113 Paul Ong and Evelyn Blumenberg Chapter 7 Health Professionals on the Front-line 139 Paul Ong and Tania Azores Chapter 8 Scientists and Engineers 165 Paul Ong and Evelyn Blumenberg Part UI. Policy Essays Chapter9 Urban Revitalization 193 Dennis Arguelles, Chanchanit Hirunpidok, and Erich Nakano Chapter 10 Welfare and Work Policies 215 Joel F. Handler and Paul Ong Chapter 11 Health Care Reform 233 Geraldine V. -
14912441.Pdf
Khants' Time Hanna Snellman KIKIMORA PUBLICATIONS Series B: 23 Helsinki 2001 © 2001 Aleksanterl Institute © Hanna Snellman ©All photographs by U.T. Sirelius,The National Board of Antiquities Khants' Time ISBN 951-45-9997-7 ISSN 1455-4828 Aleksanteri Institute Graphic design: Vesa Tuukkanen Gummerus Printing Saarijärvi 2001 Table of Content FOREWORD 5 1. INTRODUCTION 7 1.1. Studying the Khants 7 1.2. Sirelius as a Fieldworker 13 1.3. Fieldwork Methodology 20 1.4. Investigating Time 34 2. METHOD OF RECORDING TIME 39 2.1. The Vernacular Calendar 39 2.2. The Christian Calendar 95 2.3. The Combination of the Vernacular and Russian Calendars 104 3. FOLK HISTORY 133 3.1. In the Old Days 138 3.2. From the Russians 141 3.3. After the Forest Fires 144 4. WHEN THE LEAVES ARE FALLING 149 BIBLIOGRAPHY 163 Foreword I started working on this book in August 1998. Almost two years had passed after my dissertation on the lumberjacks of Finnish Lapland. I was still occupied with forest history, but I knew that in order to develop as a scientist, I had to leave the familiar ri vers and fells of Finnish Lapland, and do research on something else. Professor Juhani U.E. Lehtonen at the University of Helsinki gave me a hint: there are copies of fieldwork notes written by U.T. Sirelius in our archive. Give them a look, Lehtonen advised me, no doubt with the hope that his student would not ignore one of the emphases of the ethnology department's activities, issues concerning Finno-Ugric peoples, including therefore both East Europe and Russia. -
Winter-Spring 2020 SCD Newsletter
Shiawassee Conservation District Your Land, Your Water ~ Your Michigan 1900 S. Morrice Road ● Owosso, MI 48867 ● (989) 723-8263, Ext. 3 Winter/Spring 2020 Shiawassee Conservation District Annual Meeting Thursday, February 20, 2020 Doors open at 5:30 PM, Dinner served at 6:00 PM D’Mar Banquet & Conference Center 1488 N. M-52, Owosso RSVP February 12, 2020 Shiawassee Conservation District (989) 723-8263, ext. 3 James Ziola will be honored as the 2019 Conservation Farmer of the Year Special presentation by Jerry Miller, President Michigan Association of Conservation Districts We are honored to be joined by Gerald “Jerry” Miller, Ph.D., CPSS, and President, MACD. As a leader in conservation, Jerry will discuss today’s conservation issues in Michigan and the nation. Dr. Miller served as a Professor of Agronomy at Iowa State University for 37 years, and later as an associate dean. During his academic career he conducted applied research in soil and water conservation, watershed management, and soil productivity and interpretation. Jerry was raised on a farm in the Shenandoah Valley, VA and currently resides in Cascade Township, Kent County, where he serves as the board chair of the Kent Conservation District Board. If you need accommodations to participate in this event, please contact the Shiawassee Conservation District at (989) 723-8263, ext. 3 by February 12, 2020. USDA is an equal opportunity employer, provider, and lender. High Pollution Levels Found in Maple River Watershed The Shiawassee Conservation human use. This study also finds that water for recreation. The high levels of District recently collected a series of human and bovine waste is found in bacteria found in Maple River water samples in the Maple River all surface water in the watershed. -
Intense Windstorms in the Northeastern United States Frederick Letson1, Rebecca J
Intense windstorms in the Northeastern United States Frederick Letson1, Rebecca J. Barthelmie2, Kevin I. Hodges3 and Sara C. Pryor1 1Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York, USA 2Sibley School of Mechanical and Aerospace Engineering, Cornell University, Ithaca, New York, USA 5 3Environmental System Science Centre, University of Reading, Reading, United Kingdom Correspondence to: F. Letson ([email protected]), S.C. Pryor ([email protected]) Abstract. Windstorms are a major natural hazard in many countries. The objective of this study is to identify and characterize iIntense windstorms during the last four decades in the U.S. Northeast are identified and characterizedand determine both the sources of cyclones responsible for these events and the manner in which those cyclones differ 10 from the cyclone climatology. The windstorm detection is based on using the spatial extent of locally extreme wind speeds at 100 m height from the ERA5 reanalysis database. During all the of the top 10 windstorms, wind speeds in excess of their local 99.9th percentile extend over at least one-third of land-based ERA5 grid cells in this high population density region of the U.S.. Maximum sustained wind speeds at 100 m during these windstorms range from 26 to over 43 ms-1, with wind speed return periods exceeding 6.5 to 106 years (considering the top 5% of grid cells 15 during each storm). Property damage associated with these storms, inflation adjusted to January 2020, ranges from $24 million to over $29 billion. Two of these windstorms are linked to decaying tropical cyclones, three are Alberta Clippers and the remaining storms are Colorado Lows. -
Hiawatha National Forest Non-Native Invasive Plant Control Project
Hiawatha National Forest Non-native Invasive Plant Control Project Environmental Assessment Hiawatha National Forest Alger, Chippewa, Delta, Mackinac, Marquette, and Schoolcraft counties, Michigan April 2007 Spotted knapweed (Centaurea biebersteinii ) Responsible Official: Thomas A. Schmidt Forest Supervisor Hiawatha National Forest 2727 North Lincoln Road Escanaba, MI 49829 For Further Information Contact: Kirk Piehler Forest Wildlife Biologist Hiawatha National Forest 2727 North Lincoln Road Escanaba, MI 49829 (906) 789-3374 HNF Non-native Invasive Plant Control Project Environmental Assessment The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual's income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, DC 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. Cover Photograph Credits: John M. Randall, The Nature Conservancy Inset: USDA APHIS Archives Both are spotted knapweed ( Centaurea biebersteinii ) This document was printed on recycled paper. 2 HNF Non-native Invasive Plant Control Project Environmental Assessment TABLE OF CONTENTS TABLE OF CONTENTS .................................................................................................. 2 Vicinity Map – Hiawatha National Forest (HNF) ............................................................. -
Clnclas CSCL O4B G3/47 0133292
A Multivariate Variational Objective Analysis - Assimilation Method, Part 11: Case Study Results with and without Satellite Data. Gary L. Achtemeier, Stanley Q. Kidder, and Robert W. Scott Climate and Meteorology Section Illinois State Water Survey Champaign, IL 61820 (NASA-CR-182653) A HULTIV ARI ATE VARIATIONAL N 8 8- 2 24 92 0 BJ ECTIVE ANALYSIS- AS SIRILBT ION PIETHO D, PART 2: CASE STUDY RESULTS WITH AND WITHOUT SATELLITE DITA IIllinois State Uater Clnclas Survey) 57 P CSCL O4B G3/47 0133292 ~. .- i' 4 A Multivariate Variational Objective Analysis - Assimilation Method, Part 11: Case Study Results with and without Satellite Data. Gary L. Achtemeier, Stanley Q. Kidder, and Robert W. Scott Climate and Meteorology Section Illinois State Water Survey Champaign, IL 61820 ABSTRACT The variational multivariate assimilation method described in a companion paper by Achtemeier and Ochs is applied to conventional and conventional plus satellite data. Ground-based and space-based meteorological data are weighted according to the respective "measurement" errors and blended into a data set that is a solution of numerical forms of the two nonlinear horizontal momentum equations, the hydrostatic equation, and an integrated continuity equation for a dry atmosphere. The analyses serve first, to evaluate the accuracy of the model, and second, to contrast the analyses with and without satellite data. Evaluation criteria measure the extent to which a) the assimilated fields satisfy the dynamical constraints, b) the assimilated fields depart from the observations, and c) the assimilated fields are judged to be realistic through c I pattern analysis. The last criterion requires that the signs, magnitudes, and patterns of the hypersensitive vertical velocity and local tendencies of the horizontal velocity components be physically consistent with respect to the larger scale weather systems. -
Forecasting Lake Effect Snow Off of Southern Lake Michigan a Primer
Forecasting Lake Effect Snow off of Southern Lake Michigan A Primer Anthony Patrick Acciaioli 8/1/2009 Anthony Acciaioli Valparaiso University August 2009 Forecasting Lake Effect Snow off of Southern Lake Michigan: A Primer January in The Great Lakes: its typical ingredients include bouts of heavy snow, waves of arctic cold, and bursts of biting wind. It’s a particularly brutal winter, and The Great Lakes Region is experiencing frequent winter storms. Yet another potent mid-latitude cyclone pulls northeast into Canada. Cities such as Chicago and Milwaukee, now covered in a clean and deep blanket of snow, are beginning to clear out as cold, Canadian High Pressure slowly noses into The Northern Plains. Yet, as some folks enjoy a brief respite from winter’s snowy grasp, residents of cities such as Gary and Valparaiso, Indiana, are wondering: “When is this snow going to end?” Unfortunately, it isn’t simply a matter of residual flurries; rather, it is just the beginning of a significant, northerly flow lake effect snow (LES) event over Northwest Indiana. In this paper, I will begin by presenting a basic overview of LES climatology in The Great Lakes region. Next, I will offer a brief review of parameters which are favorable for its generation and sustenance. Finally, I will utilize two case studies: December 20th, 2004 and February 3rd and 4th, 2009, both significant LES events for Northwest Indiana (a region which I will more precisely define later on), as windows into particular patterns which lead to significant LES accumulations off of Southern Lake Michigan. In a nutshell, lake effect snow occurs when Continental Polar (cP) air blows across relatively mild lake waters.