The Climate of the Matanuska Valley
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2013 Washington State Enhanced Hazard Mitigation Plan Severe Storm Hazard Profile
Final - Hazard Profile – Severe Storm Severe Storm Frequency 50+ yrs 10-50 yrs 1-10 yrs Annually People <1,000 1,000-10,000 10,000-50,000 50,000+ Economy 1% GDP 1-2% GDP 2-3% GDP 3%+ GDP Environment <10% 10-15% 15%-20% 20%+ Property <$100M $100M-$500M $500M-$1B $1B+ Severe Storm Risk Level Hazard scale < Low to High > Frequency – Severe storms, which include any or a combination of: thunderstorms, hail, wind storms, lightning, or a tornado, happen annually in Washington. People – Looking at past history of injuries and deaths due to severe storms in Washington, the minimum threshold of a thousand injuries for this category is not met. Economy – According to the National Oceanic and Atmospheric Administration’s (NOAA) National Climatic Data Center, Washington has not experienced a severe weather event that totaled losses that met or exceeded the minimum dollar amount /percentage for this category.1 Environment – Severe storms do affect the environmental landscape of Washington, but their effect does not meet the minimum threshold for this category. Property – Severe storms can have a large impact on the property of the state, both residential and commercial. The December 2006 windstorm affected all 39 counties and the estimate for damage is still being tallied and is greater than $50 million. Total property damage from the greatest windstorm to hit Washington is estimated at $235 million (1962 dollars). This was the Columbus Day Storm of October 1962, which was the strongest non-tropical storm to ever hit the contiguous 48 states. Figure 5.7-1 and Figure 5.7-2 below show previous occurrences of tornado and hail events, respectively, from 1960 to 2012 as reported by the National Climatic Data Center. -
Chinook Vol. 9 No. 3
.+ Learning Weather • • • A resource study kit suitable for students grade seven and up, prepared by the Atmospheric Environment Service of Environment Canada Includes new revised poster·size cloud chart Decouvrons la meteO ... Pochettes destinees aux eleves du secondaire et du collegial, preparees par Ie service de I'environnement atmos heri ue d'Environnement Canada Incluant un tableau revise descriptif des nuages Learning Weather Decouvrons la meteo A resource study kit, contains: Pochette documentaire comprenant: 1. Mapping Weather 1. Cartographie de la meteo A series of maps with exercises. Teaches how Serie de cartes accompagnees d'exercices. Oecrit weather moves. Includes climatic data for 50 Cana les fluctuations du temps et fournit des donnees dian locations. climatologiques pour 50 localites canadiennes. 2. Knowing Weather 2. Apprenons a connaitre la meteo Booklet discusses weather events, weather facts Brochure traitant d'evenements, de faits et de legen· and folklore, measurement of weather and several des meteorologiques. Techniques de I'observation et student projects to study weather. de la prevision de la met eo. Projets scolaires sur la 3. Knowing Clouds meteorologie. A cloud chart to help students identify various cloud 3. Apprenons a connaitre les nuages formations. Tableau descriptif des nuages aidant les elilves a identifier differentes formations. Cat. No. EN56·5311983·E Each kit $4.95 Cat. N° EN56·5311983F Chaque pochette: 4,95 $ Order kits from: Commandez les pochettes au : CANADIAN GOVERNMENT PUBLISHING CENTRE CENTRE D'EDITION DU GOUVERNEMENT DU OTTAWA, CANADA CANADA, K1A OS9 OTTAWA (CANADA) K1A OS9 Order Form (please print) Bon de commande Veuillez m'ex pedier _ _ exemplaire(s) de la pochette Please send me _ _ copy(ies) of Learning Weather at $4.95 "Decouvrons la meteo" it 4.95 $ la co pie. -
Field-Trip Guide to Volcanic and Volcaniclastic Deposits of the Lower Jurassic Talkeetna Formation, Sheep Mountain, South-Central Alaska
Field-Trip Guide to Volcanic and Volcaniclastic Deposits of the Lower Jurassic Talkeetna Formation, Sheep Mountain, South-Central Alaska U.S. Department of the Interior U.S. Geological Survey Open-File Report 2006-1124 Field-Trip Guide to Volcanic and Volcaniclastic Deposits of the Lower Jurassic Talkeetna Formation, Sheep Mountain, South-Central Alaska Amy E. Draut U.S. Geological Survey, Pacific Science Center, Santa Cruz, CA 95060 Peter D. Clift School of Geosciences, University of Aberdeen, AB24 3UE, U.K. Robert B. Blodgett U.S. Geological Survey–Contractor, Anchorage, AK 99508 U.S. GEOLOGICAL SURVEY Open-File Report 2006-1124 2006 U.S. Department of the Interior P. Lynn Scarlett, Acting Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 Revised and reprinted: 2006 Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government To download a copy of this report from the World Wide Web: http://pubs.usgs.gov/of/2006/1124/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. LIST OF FIGURES FIGURE 1. Regional map of the field-trip area. FIGURE 2. Geologic cross section through Sheep Mountain. FIGURE 3. Stratigraphic sections on the south side of Sheep Mountain. -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Downslope Winds Chinook Wall
MET 4300 Lecture 21 Mountain Windstorms (CH17) Downslope Winds Chinook Wall --Hurricane force winds •Foehn in the European Alps (a general term for warm, dry downslope windstorms –Latin: west wind) •Bora in the Adriatic Sea SE of the Dinaric Alps (a general term for cold downslope windstorms—Greek: north wind) •Katabatic Winds: in high-latitude icefields in Alaska, Greenland and Antarctica (very cold winds) In US: •Chinook or Snow Eater in the east slope of the Rockies •Santa Ana in California: west slope of the San Bernardino, Santa Ana, and San Gabriel Mountains Downslope Winds in Western North America •Chinooks: can be extremely gusty (>100 kts), occur every year, mainly in late fall & winter. Chinooks extends from north to south along the plains of eastern Colorado from Fort Collins to Colorado Springs, including Denver and Boulder. The worst downslope winds are in Boulder. An example of Chinook Winds Jan 16-17, 1982 Chinook Wind Measurement at NCAR Boulder CO Chinooks are warm (or hot), strong and gusty, blowing from a fixed direction, generally away from the mountains Gusts may exceed 100 kts. Influence the plains of eastern CO, mainly Boulder. Gustiness (from 100mph to 10 mph within a minute) can cause a lot of roof damages, and psychological problems. Dynamics of Downslope Windstorms: Chinooks & Santa Ana are Dynamically-Driven Altocumulus Mountain Waves and Lenticularis Lenticular Clouds Dynamics: winds driven by strong pressure gradients that develop across mountain ranges; air rise on windward side and descend on the leeward -
THE MATANUSKA VALLEY Colony ■»
FT MEADE t GenCo11 MLCM 91/02119 ALASKAN L ENT ROUP SETTLE Copy fp THE MATANUSKA VALLEY coLony ■» BY 3 KIRK H.iSTONE i* D STATES ' M» DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT /! WASHINGTON # -1950- FOREWORD This study of the Matanuska Colony project in Alaska was undertaken for the Interior-Agriculture Committee on Group Settlement in Alaska. The study is one of several which were made at the request of the Committee, covering such subjects as land use capability, farm management and production, and marketing. The Committee on Group Settlement in Alaska consists of Harlan H. Barrows, Consultant, Chairman; E. H. Wiecking and 0. L. Mimms, Department of Agriculture; Marion Clawson and Robert K. Coote, Department of the Interior. While prepared primarily for the use of the Committee, the report contains such a wealth of information that it will be of interest and of value to all those concerned with the settlement and development of Alaska. It is recommended as a factual, objective appraisal of the Matanuska project. The author accepts responsibility for the accuracy of the data and the conclusions and recommendations are his own. It should be pointed out that subsequent to the time the report was written, several of the recommended scientific investigations have been undertaken and that present knowledge of certain areas, particularly the Kenai-Kasilof area on the Kenai Peninsula, is much more adequate than indicated in the report. TABLE OF CONTENTS Page Preface . i List of Figures . ..vii List of Tables.viii PART I Introduction Chapter 1. The Matanuska Valley as a Whole. -
Human Services Coordinated Transportation Plan for the Mat-Su Borough Area
Human Services Coordinated Transportation Plan For the Mat-Su Borough Area Phase III – 2011-2016 Final Draft January 2011 Table of Contents Introduction ..................................................................................................................... 3 Community Background .................................................................................................. 4 Coordinated Services Element ........................................................................................ 6 Coordination Working Group – Members (Table I) ................................................... 6 Inventory of Available Resources and Services (Description of Current Service / Public Transportation) .............................................................................................. 7 Description of Current Service / Other Transportation (Table II) .............................. 8 Assessment of Available Services – Public Transportation (Table III) ................... 13 Human Services Transportation Community Client Referral Form......................... 16 Population of Service Area: .................................................................................... 16 Annual Trip Destination Distribution – Current Service: ......................................... 19 Annual Trip Destination Distribution (Table V) ....................................................... 19 Vehicle Inventory .................................................................................................... 20 Needs Assessment ...................................................................................................... -
Total Maximum Daily Load (TMDL) for Residue Adjacent to the Waters of the Matanuska River in Palmer, Alaska Public Notice Draft
Alaska Department of Environmental Conservation 555 Cordova Street Anchorage, Alaska 99501 Total Maximum Daily Load (TMDL) for Residue Adjacent to the Waters of the Matanuska River in Palmer, Alaska Public Notice Draft July 2017 Draft TMDL for Residue Adjacent to the Matanuska River, AK July 2017 Table of Contents Executive Summary ........................................................................................................................................... 7 1 Overview ..................................................................................................................................................... 9 1.1 Location of TMDL Study Area ....................................................................................................... 9 1.2 Population ........................................................................................................................................ 13 1.3 Topography ...................................................................................................................................... 13 1.4 Land Use and Land Cover ............................................................................................................. 13 1.5 Soils and Geology ............................................................................................................................ 14 1.6 Climate .............................................................................................................................................. 17 1.7 Hydrology and Waterbody -
The Little Susitna River— an Ecological Assessment
The Little Susitna River— An Ecological Assessment Jeffrey C. Davis and Gay A. Davis P.O. Box 923 Talkeetna, Alaska (907) 733.5432. www.arrialaska.org July 2007 Acknowledgements This project was completed with support from the State of Alaska, Alaska Clean Water Action Plan program, ACWA 07-11. Laura Eldred, the DEC Project Manger provided support through comments and suggestion on the project sampling plan, QAPP and final report. Nick Ettema from Grand Valley State University assisted in data collection. ARRI—Little Susitna River July 2007 Table of Contents Summary............................................................................................................................. 2 Introduction......................................................................................................................... 3 Methods............................................................................................................................... 4 Sampling Locations ........................................................................................................ 4 Results................................................................................................................................. 6 Riparian Development .................................................................................................... 6 Index of Bank Stability ................................................................................................... 7 Chemical Characteristics and Turbidity......................................................................... -
Battle of the Chinook Wind at Havre, Mont
54 MONTHLY WEATHER REVIEW FEBRUARY1934 gations be carried out to determine the aniount of residual since it will, in general, be small in coriiparison to other air which should be left inside the pressure elements in uncertainties present. order to obtain R coiiipensat8ionpressure of about 600 nib. The mtliors desire to acknowledge the helpful sug- This work is now being done at the Weitt,lier Burenu and gestions of Dr. W. G. Brombacher, in charge of the the results will appear shortly. If this work gives satis- Aeronautic Instrument Section, United States Bureau of factory results, it is planned to recoinpensate the elements Standards, where these tests mere cnrried out. now in use and then to omit the temperature correctim BATTLE OF THE CHINOOK WIND AT HAVRE, MONT. By FRANKA. hhTH IWenther Bureau offire, Havre, Mont., January 1Y34] Appnrently Havre, Rlont., was on the battle front clown between zero and 19' F. Then at 6:55 p.m. of the between cold polar air and warm Pacific nir during most 10th the drift from the east gave way to a northerly wind of December 1933. Diiring the first week tlie weather and the full force of a west-southwest chinooli struck at was generally ikir and mild, and the ground bare of SIUJW. 7:40 p.m. Tlie velocities ranged from 20 to 33 miles per From the night of December 9 to Deceniher 12 a spell UI hour during the nest 3 hours with a temperature rise to cloudy weather with light-to-heavy snowfall prevailed. 41' by 8:15 p.m., a jump of 37Oin 1 hour and 15 minutes. -
Chapter 7 – Atmospheric Circulations (Pp
Chapter 7 - Title Chapter 7 – Atmospheric Circulations (pp. 165-195) Contents • scales of motion and turbulence • local winds • the General Circulation of the atmosphere • ocean currents Wind Examples Fig. 7.1: Scales of atmospheric motion. Microscale → mesoscale → synoptic scale. Scales of Motion • Microscale – e.g. chimney – Short lived ‘eddies’, chaotic motion – Timescale: minutes • Mesoscale – e.g. local winds, thunderstorms – Timescale mins/hr/days • Synoptic scale – e.g. weather maps – Timescale: days to weeks • Planetary scale – Entire earth Scales of Motion Table 7.1: Scales of atmospheric motion Turbulence • Eddies : internal friction generated as laminar (smooth, steady) flow becomes irregular and turbulent • Most weather disturbances involve turbulence • 3 kinds: – Mechanical turbulence – you, buildings, etc. – Thermal turbulence – due to warm air rising and cold air sinking caused by surface heating – Clear Air Turbulence (CAT) - due to wind shear, i.e. change in wind speed and/or direction Mechanical Turbulence • Mechanical turbulence – due to flow over or around objects (mountains, buildings, etc.) Mechanical Turbulence: Wave Clouds • Flow over a mountain, generating: – Wave clouds – Rotors, bad for planes and gliders! Fig. 7.2: Mechanical turbulence - Air flowing past a mountain range creates eddies hazardous to flying. Thermal Turbulence • Thermal turbulence - essentially rising thermals of air generated by surface heating • Thermal turbulence is maximum during max surface heating - mid afternoon Questions 1. A pilot enters the weather service office and wants to know what time of the day she can expect to encounter the least turbulent winds at 760 m above central Kansas. If you were the weather forecaster, what would you tell her? 2. -
The Glenn Highway EMBODIES ALL SIX QUALITIES of a SCENIC BYWAY
The Glenn Highway EMBODIES ALL SIX QUALITIES OF A SCENIC BYWAY. Scenic Historic Cultural Natural Recreational Archaeological This resource This resource Evidence and Those features of Outdoor Those offers a heightened encompasses expressions of the the visual recreational characteristics of visual experience legacies of the past customs or environment that activities are the scenic byways derived from the that are distinctly traditions of a are in a relatively directly associated corridor that are view of natural associated with distinct group of undisturbed state. with and physical evidence and man made physical elements people. Cultural These features dependent upon of historic or elements of the of the landscape, features include, predate the arrival the natural and prehistoric human visual environment whether natural or but are not limited of human cultural elements life or activity that of the scenic man made, that to crafts, music, populations and of the corridor’s are visible and byway corridor. are of such dance, rituals, may include landscape. capable of being The characteristics significance that festivals, speech, geological The recreational inventoried and of the landscape they educate the food, special formations, fossils, activities provide interpreted. The are strikingly viewer and stir an events, vernacular landform, water opportunities for scenic byway distinct and offer a appreciation of the architecture, etc. bodies, vegetation, active and passive corridor’s pleasing and most past. The historic and are currently and wildlife. There recreational archaeological memorable visual elements reflect practiced. The may be evidence of experiences. They interest, as experience. All the actions of cultural qualities of human activity but include, but are not identified through elements of the people and may the corridor could the natural features limited to downhill ruins, artifacts, landscape – include buildings, highlight one or reveal minimal skiing, rafting, structural remains landform, water, settlement more significant disturbances.