DOCSLIB.ORG

A Blizzard Warning Remains in Effect from 3 Pm This Afternoon to 3 Pm Cst Wednesday

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
A Blizzard Warning Remains in Effect from 3 Pm This Afternoon to 3 Pm Cst Wednesday A BLIZZARD WARNING REMAINS IN EFFECT FROM 3 PM THIS AFTERNOON TO 3 PM CST WEDNESDAY. ACCUMULATING SNOW WILL DEVELOP AROUND THE INTERSTATE 80 CORRIDOR DURING THE EARLY TO MID AFTERNOON...SPREADING NORTH TO THE WISCONSIN STATE LINE BY MID TO LATE AFTERNOON. THE MOST SIGNIFICANT SNOW MAY COME IN A COUPLE OF WAVES...WITH THE FIRST WAVE LATE THIS AFTERNOON INTO EARLY THIS EVENING...FOLLOWED BY A SECOND WAVE OF INTENSE SNOW LATER THIS EVENING INTO THE OVERNIGHT. ACCUMULATING LAKE EFFECT SNOW SHOWERS WILL CONTINUE OVER NORTHEAST ILLINOIS WEDNESDAY MORNING...SPREADING INTO NORTHWEST INDIANA WEDNESDAY AFTERNOON. * ACCUMULATIONS...SNOW WILL BE HEAVY AT TIMES WITH ACCUMULATION RATES OF 1 TO 2 INCHES PER HOUR LIKELY. STORM TOTAL SNOWFALL OF 10 TO 18 INCHES IS LIKELY TOWARD ROCKFORD AND DIXON. THE HEAVIEST SNOWFALL TOTALS ARE LIKELY DOWNWIND OF LAKE MICHIGAN IN THE CHICAGO METROPOLITAN AREA INTO NORTHWEST INDIANA WHERE 12 TO 20 INCHES OF SNOW IS LIKELY...WITH ISOLATED AMOUNTS OF AROUND 2 FEET POSSIBLE. * WINDS...NORTHEAST WINDS WILL INCREASE TO 20 TO 35 MPH BY LATE THIS AFTERNOON. WIND GUSTS UP TO 40 MPH WILL BE POSSIBLE BY EVENING WITH GUSTS OF 40 TO 50 MPH LIKELY TONIGHT. EVEN STRONGER WINDS ARE LIKELY NEAR THE IMMEDIATE LAKESHORE WITH SUSTAINED WINDS OF 30 TO 40 MPH WITH GUSTS BETWEEN 50 AND 60 MPH. * BLIZZARD CONDITIONS...THE STRONG WINDS ALONG WITH BLOWING AND OCCASIONALLY HEAVY FALLING SNOW WILL REDUCE VISIBILITIES TO NEAR ZERO AT TIMES...PARTICULARLY TONIGHT. * THUNDERSTORMS...ISOLATED SNOW PRODUCING THUNDERSTORMS ARE EXPECTED TO DEVELOP TONIGHT...RESULTING IN LOCALLY VERY INTENSE SNOWFALL RATES. IT IS NOT UNCOMMON TO SEE SNOWFALL RATES IN EXCESS OF 4 INCHES PER HOUR IN THUNDERSNOW MAKING TRAVEL NEARLY IMPOSSIBLE. * TRAVEL...ROAD CONDITIONS WILL RAPIDLY DETERIORATE DURING THE MID TO LATE AFTERNOON AS SNOW DEVELOPS FROM SOUTH TO NORTH ACROSS THE AREA. TRAVEL IS EXPECTED TO BECOME TREACHEROUS BY LATE AFTERNOON...AND DOWNRIGHT DANGEROUS BY EARLY EVENING AS WINDS INCREASE RESULTING IN WHITE OUT CONDITIONS. SNOWFALL RATES WILL BE SO INTENSE AT TIMES THAT ROAD CREWS WILL BE UNABLE TO KEEP EVEN PRIMARY ROADS AND HIGHWAYS CLEARED. UNNECESSARY TRAVEL SHOULD BE AVOIDED AT ALL COSTS THIS AFTERNOON THROUGH EARLY WEDNESDAY MORNING AS MORE THAN HALF OF THE FATALITIES IN PREVIOUS ILLINOIS BLIZZARDS HAVE OCCURRED AS A RESULT OF TRAFFIC ACCIDENTS. BEFORE MAKING THE DECISION TO TRAVEL...CONSIDER IF GETTING TO YOUR DESTINATION IS WORTH PUTTING YOUR LIFE AT RISK. * POWER OUTAGES...THE COMBINATION OF STRONG AND GUSTY WINDS ALONG WITH POSSIBLY HEAVY WET SNOW STICKING TO POWERLINES COULD RESULT IN POWER OUTAGES. DUE TO THE PROLONGED NATURE OF VERY ADVERSE CONDITIONS...PLAN ACCORDINGLY FOR THE POSSIBILITY OF A PROLONGED DISRUPTION IN COMMERCIAL POWER. * OTHER IMPACTS...THE HEAVY NATURE OF THE SNOW WILL MAKE SHOVELING EXTREMELY DIFFICULT...AND POTENTIALLY DEADLY. DURING AND IMMEDIATELY FOLLOWING THE BLIZZARD OF 1999 OVER 40 PEOPLE IN THE CHICAGO AREA ALONE LOST THEIR LIVES TO HEART ATTACKS WHILE SHOVELING THE HEAVY SNOWFALL. IF YOU MUST SHOVEL THE SNOW...TAKE FREQUENT BREAKS INDOORS AND DO NOT UNDERESTIMATE THE TASK AT HAND. PRECAUTIONARY/PREPAREDNESS ACTIONS... A BLIZZARD WARNING MEANS SEVERE WINTER WEATHER CONDITIONS ARE EXPECTED OR OCCURRING. FALLING AND BLOWING SNOW WITH STRONG WINDS AND POOR VISIBILITIES ARE LIKELY. THIS WILL LEAD TO WHITEOUT CONDITIONS...MAKING TRAVEL EXTREMELY DANGEROUS. DO NOT TRAVEL! IF YOU ABSOLUTELY MUST TRAVEL...HAVE A WINTER SURVIVAL KIT WITH YOU. IF YOU GET STRANDED...STAY WITH YOUR VEHICLE. .
Load more

Recommended publications
  • PRECIPITATION What Does a 60 Percent Chance of Precipitation Mean?
    PRECIPITATION What does a 60 percent chance of precipitation mean? http://www.cbc.ca/news/canada/ottawa/canada-weather-forecast-no-50-per-cent-forecast-1.4206067 The probability of (PoP) does not mean • the percent of time precipitation will be observed over the area; or • the percentage of meteorologists who believe precipitation will fall! The most common definition among meteorologists is the probability that at least one one-hundredth inch of liquid-equivalent precipitation will fall in a single spot. Here’s a good way to grasp a PoP of 60 percent: If we had ten tomorrows with identical weather conditions, any given point would receive rain on six (60 percent) of those days. And rain would not fall on four of those days — on any given point. Remember: this PoP is a forecast for 10 potential tomorrows, not a forecast for the next 10 days! Although this may be confusing, weather forecasters have no problem thinking of tomorrow’s weather as a group of potential tomorrows. One thing you can take to the bank: as the PoP increases, precipitation grows more likely. In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. So many types… Rain Sleet Drizzle Hail Snow Graupel Thundersnow Fog and mist are technically SUSPENSIONS and not precipitation SYMBOLS RAINSHOWERS are identified on weather maps as a dot over a triangle Heavier rain as a series of dots, more when rain is heavier Rain - and other forms of precipitation - occur when Basically… warm moist air cools and condensation occurs.
    [Show full text]
  • Proximity Sounding Composites of Midwestern Thundersnow Events
    P4.2 PROXIMITY SOUNDING COMPOSITES OF MIDWESTERN THUNDERSNOW EVENTS Patrick S. Market*,1, Angela M. Oravetz1, David Gaede2, Evan Bookbinder2, Brian Pettegrew1, and Rashida Thomas1 1Department of Atmospheric Science 2National Weather Service Forecast Office University of Missouri-Columbia Springfield, MO Columbia, MO 1. INTRODUCTION Sounding profiles of the atmosphere during thundersnow analysis of rawinsonde data. are examined. Horizontal composite fields (Market et al. This work is patterned after Curran and Pearson 2004, this volume) paint a vivid portrait of an active (1971); a reanalysis of their sounding profile is snowstorm, but fail to distinguish clearly a typical cyclone reproduced in Figure 1. Proximity soundings were found from one that harbors an electrified cloud and in 12 thundersnow events and are discussed and defined thundersnow. Proximity soundings were found in 12 presently. Four of the events occurred at the exact time thundersnow events and are defined and discussed and location of a sounding. Four of the events occurred presently. at the exact time of a sounding but were not at the exact These profiles add value to the horizontal composites location the sounding occurred; the location of produced previously, which revealed thundersnow events thundersnow was within 90 nautical miles (nmi; 166.68 to be occurring in otherwise unremarkable, snow bearing km) of the sounding station. The remaining four cases extratropical cyclones. Working on the assumption that occurred within 90 nmi of the sounding station and the some feature (instability) makes these events unique, and thundersnow report occurred in a window of zero to that convection resulting from instability is the source of three hours after the rawinsonde was released.
    [Show full text]
  • Analysis of Thundersnow Storms Over Northern Colorado
    DECEMBER 2015 K U M J I A N A N D D E I E R L I N G 1469 Analysis of Thundersnow Storms over Northern Colorado MATTHEW R. KUMJIAN Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania WIEBKE DEIERLING Research Applications Laboratory, National Center for Atmospheric Research,* Boulder, Colorado (Manuscript received 13 January 2015, in final form 12 August 2015) ABSTRACT Lightning flashes during snowstorms occur infrequently compared to warm-season convection. The rarity of such thundersnow events poses an additional hazard because the lightning is unexpected. Because cloud electrification in thundersnow storms leads to relatively few lightning discharges, studying thundersnow events may offer insights into mechanisms for charging and possible thresholds required for lightning dis- charges. Observations of four northern Colorado thundersnow events that occurred during the 2012/13 winter are presented. Four thundersnow events in one season strongly disagrees with previous climatologies that used surface reports, implying thundersnow may be more common than previously thought. Total lightning information from the Colorado Lightning Mapping Array and data from conterminous United States light- ning detection networks are examined to investigate the snowstorms’ electrical properties and to compare them to typical warm-season thunderstorms. Data from polarimetric WSR-88Ds near Denver, Colorado, and Cheyenne, Wyoming, are used to reveal the storms’ microphysical structure and determine operationally relevant signatures related to storm electrification. Most lightning occurred within convective cells containing graupel and pristine ice. However, one flash occurred in a stratiform snowband, apparently triggered by a tower. Depolarization streaks were observed in the radar data prior to the flash, indicating electric fields strong enough to orient pristine ice crystals.
    [Show full text]
  • February 9-10, 2017
    Northeast U.S. Winter Storm February 9 - 10, 2017 By: Allison Santorelli, WPC meteorologist Meteorological Overview: A quick moving, yet intense, storm brought heavy snowfall and blizzard conditions to portions of the Northeast U.S. between 9 - 10 February, 2017. A strong cold front moved through the Northeast on 8 February, with sections of eastern New York and New Jersey seeing afternoon high temperatures near 60 degrees Fahrenheit prior to its passage. By the next day however, high temperatures struggled to get above 30 degrees Fahrenheit with heavy snow and blizzard conditions. Around the same time that the strong cold front was ushering very cold air into the Northeast, an upper level shortwave was intensifying as it moved eastward across the middle Mississippi and Tennessee Valleys (Figure 1). Initially, this produced light to moderate snowfall, generally less than 6”, across portions of the Ohio Valley (Figure 2). Meanwhile, the energy at the base of this trough interacted with the cold front and a wave of low pressure formed along the boundary in the Mid-Atlantic. Moderate to heavy snowfall spread eastward into northern portions of the Mid-Atlantic and eventually the Northeast by 12 UTC on 9 February. This low pressure center rapidly deepened as it moved up the Northeast coast on 9 February 2017, with the central pressure dropping more than 24 hPa in 24 hours, undergoing what can be referred to as “bombogenesis”. A strong baroclinic zone in the lower levels combined with favorable upper level divergence also helped to intensify snowfall across the Northeast on 9 February, with several reports across New York and southern New England of snowfall rates as high as 4 inches per hour, very low visibility, blizzard conditions, and even thundersnow.
    [Show full text]
  • THUNDERSNOW Krista Debehnke Eastern Washington University
    Eastern Washington University EWU Digital Commons EWU Masters Thesis Collection Student Research and Creative Works 2014 THUNDERSNOW Krista DeBehnke Eastern Washington University Follow this and additional works at: http://dc.ewu.edu/theses Part of the Creative Writing Commons Recommended Citation DeBehnke, Krista, "THUNDERSNOW" (2014). EWU Masters Thesis Collection. 201. http://dc.ewu.edu/theses/201 This Thesis is brought to you for free and open access by the Student Research and Creative Works at EWU Digital Commons. It has been accepted for inclusion in EWU Masters Thesis Collection by an authorized administrator of EWU Digital Commons. For more information, please contact [email protected]. THUNDERSNOW _____________________________________________________________ A Thesis Presented To Eastern Washington University Cheney, Washington _____________________________________________________________ In Partial Fulfillment of the Requirements for the Degree Masters of Fine Arts _____________________________________________________________ By Krista Marie DeBehnke Spring 2014 MASTER’S THESIS In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Eastern Washington University, I agree that the JFK Library shall make copies freely available for inspection. I further agree that copying of this project in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without my written permission. Signature ______________________________________ Date ___________________________________________ Thundersnow Poems by Krista Marie DeBehnke ii Acknowledgements I want to thank Jonathan Johnson and Christopher Howell for the knowledge, support, wisdom and patience they’ve showed me throughout my time in this program. I also want to thank my colleagues Lindsey Jones, Casey Guerin, Megan Charles and Joanna King-Yost for their unwavering encouragement to keep writing.
    [Show full text]
  • A Comparison of Two Cases of Low-Latitude Thundersnow
    Atmósfera 22(3), 315-330 (2009) A comparison of two cases of low-latitude thundersnow G. DOLIF NETO Centro de Previsao del Tempo e Estudos Climáticos- Instituto Nacional de Pesquisas Espaciais, São Paulo, Brazil P. S. MARKET, A. E. BECKER, B. PETTEGREW, C. MELICK, C. SCHULTZ, P. I. BUCKLEY, J. V. CLARK, A. R. LUPO Department of Soil, Environmental and Atmospheric Sciences, University of Missouri-Columbia, MO, USA Corresponding author: P. S. Market; e-mail: [email protected] R. HOLLE, N. DEMETRIADES Vaisala Incorporated, Tucson, AZ, USA C. E. BARBIERI Department of Parks, Recreation, and Tourism, University of Missouri-Columbia, MO, USA Received April 16, 2008; accepted May 11, 2009 RESUMEN Se examinan dos eventos de nevada con relámpagos en latitudes bajas a fin de identificar sus características. Ambos eventos se originaron a escala sinóptica y tuvieron impactos de pequeña escala (por ejemplo, ascenso orográfico e inestabilidad elevada). El primer evento ocurrió en el hemisferio sur y se desarrolló a finales del invierno influenciado por la orografía subyacente. Este evento presentó abundancia de relámpagos (94 destellos nube-suelo en la región); sin embargo, la acumulación de nieve fue insignificante. Este evento fue dominado por relámpagos con polaridad negativa, con una amplitud máxima promedio de -43.2 kA. El segundo evento fue un caso de convección elevada en el hemisferio norte con frontogénesis debajo de una capa extensa de inestabilidad potencial. Este evento también presentó abundantes relámpagos (706 destellos nube-suelo en la región), así como considerable acumulación de nieve sobre un área extensa. Este evento también fue dominado por relámpagos con polaridad negativa, con una amplitud máxima promedio de -23.7 kA.
    [Show full text]
  • Lake-Effect Snowstorms in Northern Utah and Western New York with and Without Lightning
    DECEMBER 1999 NOTES AND CORRESPONDENCE 1023 Lake-Effect Snowstorms in Northern Utah and Western New York with and without Lightning DAVID M. SCHULTZ NOAA/National Severe Storms Laboratory, Norman, Oklahoma 26 March 1999 and 3 June 1999 ABSTRACT Lake-effect snowstorms in northern Utah and western New York with and without lightning/thunder are examined. Lake-effect snowstorms with lightning have signi®cantly higher temperatures and dewpoints in the lower troposphere and signi®cantly lower lifted indices than lake-effect snowstorms without lightning. In contrast, there is little difference in dewpoint depressions between events with and without lightning. Surface-to-700-hPa temperature differences (a surrogate for lower-tropospheric lapse rate) for events with and without lightning differ signi®cantly for events in northern Utah, but not for those in western New York. Nearly all events have no convective available potential energy, regardless of the presence of lightning. These results are discussed in the context of current models of storm electri®cation. 1. Introduction lightning-related casualties and damage during the winter is less than during the rest of the year. For example, only Observations of lightning and thunder occurring dur- 0.6% of lightning deaths and 0.7% of lightning injuries ing snowstorms (also known as thundersnow) have been occur during December, January, and February (Holle et reported at least as early as the nineteenth century in al. 1997). Third, thunderstorms with snow tend to pro- Western literature (e.g., Herschel 1888). Thundersnow in duce fewer lightning strikes than thunderstorms with rain. China, however, was viewed as a precursor to military For example, in the eastern U.S.
    [Show full text]
  • American Meteorological Society Weather Analysis and Forecasting (WAF) Committee 2013 Annual Report
    American Meteorological Society Weather Analysis and Forecasting (WAF) Committee 2013 Annual Report Due to the active involvement and enthusiasm of our members, the AMS WAF Committee had an extremely successful and productive year. The committee was comprised of fourteen members, three student members, and a chair. The committee met in person at the AMS annual meeting. Three formal teleconference meetings of the full committee were also conducted, a short conference call to finalize annual awards, as well as numerous discussions by the 2014 conference planning committee. Our largest effort was planning for the 26th Weather Analysis and Forecast Conference and the 22nd Numerical Weather Prediction Conference (26 WAF/22 NWP), both to be held in conjunction with the 94th AMS Annual Meeting in Atlanta, February 2014. Here are the specific report details as requested by the STAC Commissioner: 1. Members rotating off the committee after completing six years of dedicated service: a. John Cannon b. Kevin Sharfenberg c. Edward Szoke 2. New members (subject to AMS Council approval): a. Cyrena-Marie Briede (Mount Washington, NH, Observatory) b. Walter Drag (NWS, Mount Holly, NJ) c. Jason Furtado (AER, Lexington, MA) d. Gail Hartfield (NWS, Raleigh, NC) e. Alex Tardy (NWS, San Diego, CA) 3. Conferences, symposiums held during 2013: a. Special Symposium (Jan 9, 2013): We conducted a special symposium, largely at the request of AMS President Louis Uccellini, at the 93rd Annual Meeting in Austin. The one day symposium was entitled “Advancing Weather and Climate Forecasts: Innovative Techniques and Applications.” Kelly Mahoney and Andrew Molthan were the co-chairs and they did a superb job putting it all together, from writing the call for papers to inviting our lead speakers.
    [Show full text]
  • How to Overcome Whiteout
    How to overcome whiteout How to overcome whiteout 1. Lt (R) Jørgen W. Eriksen, Scholarship Holder, Norwegian School of Sports Sciences, Defence Institute A couple of year ago I was skiing in the Norwegian mountains when I suddenly found myself in a total whiteout. I saw an animal in front of me that appeared to be moving back and forth as if searching for something in the snow. I found it impossible to decide how far away the animal actually was. Just the day before I had for the first time in my life seen a wolverine. Maybe that was why I thought I was standing watching this rare and shy animal again. The next thing that happened was that the animal appeared to be walking towards me. Before I could think “now what do I do” I had an incredible experience. It was not a wolverine I was staring at but a lemming, which was only a couple of meters in front of me…. If you have never experienced whiteout, it may be hard to imagine what kind of experiences and consequences this weather condition may cause. In short; it becomes impossible to separate the snowy surface from the air. Everything appears to be the same colour of white and it becomes impossible to tell how far away the snowy surface is. “Whiteout is a weather condition in which visibility and contrasts are reduced by snow and diffuse lighting from overcast clouds” Whiteout There are three different forms of a whiteout: 1. In clear air conditions, when there is no snow falling, diffuse lighting from overcast cloud may cause all surface definition to disappear, and a kind of optical illusion is created.
    [Show full text]
  • A Climatology of Thundersnow Events Over the Contiguous United States
    1290 WEATHER AND FORECASTING VOLUME 17 A Climatology of Thundersnow Events over the Contiguous United States PATRICK S. MARKET,CHRIS E. HALCOMB, AND REBECCA L. EBERT Department of Soil and Atmospheric Sciences, University of MissouriÐColumbia, Columbia, Missouri 15 November 2001 and 21 June 2002 ABSTRACT A ``climatology'' (climatological description of spatial, temporal, and synoptic characteristics) of snow events with thunder is presented for the contiguous United States. Based upon 30 yr of 3-hourly reports from 204 stations in the 48 contiguous United States, 229 reports are extracted from the 3-hourly observations (consistently bearing the present-weather group in each surface observation) that featured thunder with snow only. When these reports are plotted spatially, the central United States, the intermountain west, and the Great Lakes region emerge as the preferred regions for thundersnow occurrence. A thundersnow event is then de®ned. Isolated thundersnow reports clearly constitute a thundersnow event. Also, multiple thundersnow reports that are not separated spatially by over 1100 km or temporally by 6 h are considered part of one event. The location reporting the ®rst occurrence of thunder with snow in such a collection of stations then carries the representative time and location for the event. The 229 individual reports make up 191 thundersnow events. Temporal analysis of thundersnow events reveals a nationwide seasonal preference for occurrence in March but no clear diurnal preference. Most thundersnow events are typically reported at only one station and only rarely in consecutive 3-hourly observations. These results thus reinforce the notion of thundersnow as a fairly localized phenomenon of limited duration.
    [Show full text]
  • Presentation
    Remote sensing observations of a Palma de Mallorca, Balearic Islands, Spain Mediterranean 3 - 7 October 2011 thundersnow and low-altitude heavy snowfall event MODIS, NASA MODIS, NASA Joan Bech, Montserrat Aran, Clara Brucet, Nicolau Pineda, Tomeu Rigo, and Eliseu Vilaclara [email protected] Content 1. Introduction (Thundersnow & low altitude snowfalls in Catalonia) 2. Synoptic conditions 3. Remote sensing observations (total lightning, radar) 4. Tower triggered lightning 5. Concluding remarks Introduction • Heavy low altitude snowfalls: in Catalonia are relatively rare events (16 cases in Barcelona from 1947 to 2009; 2 severe) Pages et al (Plinius 2003), Pascual et al (AMS RAD2003), Aran et al (Plinius 2010) • Thundersnows: thunderstorms with snowfall; relatively rare anywhere compared to snowfall & thunderstorm occurrence Miyake et al (IEEE TPD1990), Market et al (WAF 2002), Schultz & Vavrek (Weather 2009), Becker (2007) - Most studies over Japan and USA - Low number of strokes compared to summer tx - Typically CG correlated with heavy snow band Introduction • Heavy low altitude snowfalls: in Catalonia are relatively rare events (16 cases in Barcelona from 1947 to 2009; 2 severe) Pages et al (Plinius 2003), Pascual et al (AMS RAD2003), Aran et al (Plinius 2010) 8 March 2010 • Thundersnows: thunderstorms with snowfall; Heavy low altitude relatively rare anywhere compared to snowfall & Snowfall and thunderstorm occurrence thundersnow Miyake et al (IEEE TPD1990), Market et al (WAF 2002), event in Catalonia Schultz & Vavrek (Weather 2009),
    [Show full text]
  • 2004 ITS Architecture
    Anchorage Regional ITS Architecture FINAL REPORT Prepared for: Municipality of Anchorage Prepared by: PB Farradyne In cooperation with Battelle Version 1.1 Revised and Approved by AMATS Policy Committee 10-14-04 Municipality of Anchorage Regional ITS Architecture, Version 1.1 Document Contents DOCUMENT CONTENTS Summary Report................................................................................................................................ SR-i Chapter 1: User Needs......................................................................................................................... 1-i Chapter 2: User Services ..................................................................................................................... 2-i Chapter 3: ITS Long-Range Vision....................................................................................................... 3-i Chapter 4: Concept of Operations........................................................................................................ 4-i Chapter 5: Physical ITS Architecture.................................................................................................... 5-i Chapter 6: Implementation Plan........................................................................................................... 6-i ITS Standards............................................................................................................Technical Appendix Alaska IWAYS Maintenance Plan .................................................................................................(Insert)
    [Show full text]