Weather Spotter's Field Guide
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Severe Storms in the Midwest
Informational/Education Material 2006-06 Illinois State Water Survey SEVERE STORMS IN THE MIDWEST Stanley A. Changnon Kenneth E. Kunkel SEVERE STORMS IN THE MIDWEST By Stanley A. Changnon and Kenneth E. Kunkel Midwestern Regional Climate Center Illinois State Water Survey Champaign, IL Illinois State Water Survey Report I/EM 2006-06 i This report was printed on recycled and recyclable papers ii TABLE OF CONTENTS Abstract........................................................................................................................................... v Chapter 1. Introduction .................................................................................................................. 1 Chapter 2. Thunderstorms and Lightning ...................................................................................... 7 Introduction ........................................................................................................................ 7 Causes ................................................................................................................................. 8 Temporal and Spatial Distributions .................................................................................. 12 Impacts.............................................................................................................................. 13 Lightning........................................................................................................................... 14 References ....................................................................................................................... -
Fatalities Associated with the Severe Weather Conditions in the Czech Republic, 2000–2019
Nat. Hazards Earth Syst. Sci., 21, 1355–1382, 2021 https://doi.org/10.5194/nhess-21-1355-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Fatalities associated with the severe weather conditions in the Czech Republic, 2000–2019 Rudolf Brázdil1,2, Katerinaˇ Chromá2, Lukáš Dolák1,2, Jan Rehoˇ rˇ1,2, Ladislava Rezníˇ ckovᡠ1,2, Pavel Zahradnícekˇ 2,3, and Petr Dobrovolný1,2 1Institute of Geography, Masaryk University, Brno, Czech Republic 2Global Change Research Institute, Czech Academy of Sciences, Brno, Czech Republic 3Czech Hydrometeorological Institute, Brno, Czech Republic Correspondence: Rudolf Brázdil ([email protected]) Received: 12 January 2021 – Discussion started: 21 January 2021 Revised: 25 March 2021 – Accepted: 26 March 2021 – Published: 4 May 2021 Abstract. This paper presents an analysis of fatalities at- with fatal accidents as well as a decrease in their percent- tributable to weather conditions in the Czech Republic dur- age in annual numbers of fatalities. The discussion of results ing the 2000–2019 period. The database of fatalities de- includes the problems of data uncertainty, comparison of dif- ployed contains information extracted from Právo, a lead- ferent data sources, and the broader context. ing daily newspaper, and Novinky.cz, its internet equivalent, supplemented by a number of other documentary sources. The analysis is performed for floods, windstorms, convective storms, rain, snow, glaze ice, frost, heat, and fog. For each 1 Introduction of them, the associated fatalities are investigated in terms of annual frequencies, trends, annual variation, spatial distribu- Natural disasters are accompanied not only by extensive ma- tion, cause, type, place, and time as well as the sex, age, and terial damage but also by great loss of human life, facts easily behaviour of casualties. -
From the Line in the Sand: Accounts of USAF Company Grade Officers In
~~may-='11 From The Line In The Sand Accounts of USAF Company Grade Officers Support of 1 " 1 " edited by gi Squadron 1 fficer School Air University Press 4/ Alabama 6" March 1994 Library of Congress Cataloging-in-Publication Data From the line in the sand : accounts of USAF company grade officers in support of Desert Shield/Desert Storm / edited by Michael P. Vriesenga. p. cm. Includes index. 1. Persian Gulf War, 1991-Aerial operations, American . 2. Persian Gulf War, 1991- Personai narratives . 3. United States . Air Force-History-Persian Gulf War, 1991 . I. Vriesenga, Michael P., 1957- DS79 .724.U6F735 1994 94-1322 959.7044'248-dc20 CIP ISBN 1-58566-012-4 First Printing March 1994 Second Printing September 1999 Third Printing March 2001 Disclaimer This publication was produced in the Department of Defense school environment in the interest of academic freedom and the advancement of national defense-related concepts . The views expressed in this publication are those of the authors and do not reflect the official policy or position of the Department of Defense or the United States government. This publication hasbeen reviewed by security andpolicy review authorities and is clearedforpublic release. For Sale by the Superintendent of Documents US Government Printing Office Washington, D.C . 20402 ii 9&1 gook L ar-dicat£a to com#an9 9zacL orflcF-T 1, #ait, /2ZE4Ent, and, E9.#ECLaL6, TatUlLE. -ZEa¢ra anJ9~ 0 .( THIS PAGE INTENTIONALLY LEFT BLANK Contents Essay Page DISCLAIMER .... ... ... .... .... .. ii FOREWORD ...... ..... .. .... .. xi ABOUT THE EDITOR . ..... .. .... xiii ACKNOWLEDGMENTS . ..... .. .... xv INTRODUCTION .... ..... .. .. ... xvii SUPPORT OFFICERS 1 Madzuma, Michael D., and Buoniconti, Michael A. -
American Meteorological Society Revised Manuscript Click Here to Download Manuscript (Non-Latex): JAMC-D-14-0252 Revision3.Docx
AMERICAN METEOROLOGICAL SOCIETY Journal of Applied Meteorology and Climatology EARLY ONLINE RELEASE This is a preliminary PDF of the author-produced manuscript that has been peer-reviewed and accepted for publication. Since it is being posted so soon after acceptance, it has not yet been copyedited, formatted, or processed by AMS Publications. This preliminary version of the manuscript may be downloaded, distributed, and cited, but please be aware that there will be visual differences and possibly some content differences between this version and the final published version. The DOI for this manuscript is doi: 10.1175/JAMC-D-14-0252.1 The final published version of this manuscript will replace the preliminary version at the above DOI once it is available. If you would like to cite this EOR in a separate work, please use the following full citation: Wang, Y., and B. Geerts, 2015: Vertical-plane dual-Doppler radar observations of cumulus toroidal circulations. J. Appl. Meteor. Climatol. doi:10.1175/JAMC-D-14- 0252.1, in press. © 2015 American Meteorological Society Revised manuscript Click here to download Manuscript (non-LaTeX): JAMC-D-14-0252_revision3.docx Vertical-plane dual-Doppler radar observations of cumulus toroidal circulations Yonggang Wang1, and Bart Geerts University of Wyoming Submitted to J. Appl. Meteor. Climat. October 2014 Revised version submitted in May 2015 1 Corresponding author address: Yonggang Wang, Department of Atmospheric Science, University of Wyoming, Laramie WY 82071, USA; email: [email protected] 1 Profiling dual-Doppler radar observations of cumulus toroidal circulations 2 3 Abstract 4 5 6 High-resolution vertical-plane dual-Doppler velocity data, collected by an airborne profiling 7 cloud radar in transects across non-precipitating orographic cumulus clouds, are used to examine 8 vortical circulations near cloud top. -
911 Communicator Questions to Ask Of
911 Communicator Questions to ask of Severe Weather Spotters 1. Name, home address, and telephone number. 2. Is caller a trained severe weather spotter. 3. Time of call. 4. Time of severe weather event (may be different than call time). 5. Location of severe weather event, which may be different from location where spotter called from. (If spotter doesn’t say 1.2 miles southeast of Anytown, then request names of streets at nearest intersection). 6. Type of Weather Event – (most common to least common order) a. If it’s a wind report, ask if the reported speed is measured or estimated. b. If it’s a wind damage report, ask caller to estimate how many trees are damaged, uprooted, etc., or extent and severity of structural damage. c. If it’s a hail event, ask if the reported size is measured or estimated. (penny, nickel, quarter, golf ball, soft ball, etc.) d. If it’s a flood report, ask caller to estimate depth of water on roads or on lawns, ask if the water is stationary or moving, and extent or severity of damage. e. If it’s a “rotating wall-cloud” report, i. Persistent rotation (usually on backside of storm) = true rotating wall-cloud. ii. No rotation = scary-looking cloud (scud), or a non-rotating wall-cloud. f. If it’s a funnel-cloud report, ask caller if the funnel-shaped cloud is actually rotating. If the caller is too far away from the funnel-cloud they may not be able to see rotation. i. No rotation = just a scary-looking cloud (scud). -
Downbursts: As Dangerous As Tornadoes? Winds Can Be Experienced Along the Leading Edge of This “Spreading Out” Air
DDoowwnnbbuurrssttss:: AAss DDaannggeerroouuss aass TToorrnnaaddooeess?? National Weather Service Greenville-Spartanburg, SC What is a Downburst? “It had to be a tornado!” This is a “updraft.” common statement made by citizens of the Carolinas and On a typical day in the warm season, North Georgia who experience once a cloud grows to 20,000 to damaging winds associated with 30,000 feet, it will begin to produce severe thunderstorms, especially heavy rain and lightning. The falling if those winds cause damage to rain causes a “downdraft,” or sinking their homes. However, the column of air to form. A thunderstorm combination of atmospheric may eventually grow to a height of ingredients that are necessary for 50,000 feet or more before it stops tornadoes occurs only rarely developing. Generally speaking, the across our area. In fact the 46 Fig. 1. Tracks of tornadoes across the “taller” the storm, the more likely it is Carolinas and Georgia from 1995 through counties that represent the to produce a strong downdraft. Once 2011. Compare this with the downburst Greenville-Spartanburg Weather reports during this time (Figure 3). the air within the downdraft reaches Forecast Offices’s County Warning the surface, it spreads out parallel to Area only experience a total of 12 the ground. Very strong to damaging to 15 tornadoes during an average year. However, thunderstorms and even severe thunderstorms are a relatively common occurrence across our area, especially from late spring through mid-summer. This is because a warm and humid (i.e., unstable) atmosphere is required for thunderstorm development. If some atmospheric process forces the unstable air Fig. -
Chapter 4 Atmospheric Moisture, Condensation, and Clouds
9/13/2012 Chapter 4 Atmospheric Moisture, Condensation, and Clouds. The sun’s electromagnetic spectrum and some of the descriptive names of each region. The numbers underneath the curve approximate the percent of energy the sun radiates in various regions. 0.4 μm = 400 nm 0.7 μm = 700 nm The daily variation in air temperature is controlled by incoming energy (primarily from the sun) and outgoing energy from the earth’s surface. Where incoming energy exceeds outgoing energy (orange shade), the air temperature rises. Where outgoing energy exceeds incoming energy (gray The hotter sun not only radiates more energy than that of the cooler earth (the area shade), the air under the curve), but it also radiates the majority of its energy at much shorter temperature falls. wavelengths. (The area under the curves is equal to the total energy emitted, and the scales for the two curves differ by a factor of 100,000.) 1 9/13/2012 The average annual incoming solar radiation (yellow line) absorbed by the earth and the atmosphere along with the average annual infrared radiation (red line) emitted by the earth and the atmosphere. Water can exist in 3 phases, depending Evaporation, Condensation, upon pressure and temperature. & Saturation • Evaporation is the change of liquid into a gas and requires heat. • Condensation is the change of a gas into a liquid and releases heat. • Condensation nuclei • Sublimation: solid to gaseous state without becoming a liquid. • Saturation is an equilibrium condition http://www.sci.uidaho.edu/scripter/geog100/l http://chemwiki.ucdavis.edu/Physical_Che in which for each molecule that ect/05‐atmos‐water‐wx/ch5‐part‐2‐water‐ mistry/Physical_Properties_of_Matter/Phas phases.htm e_Transitions/Phase_Diagrams_1 evaporates, one condenses. -
Äikesega) Kaasnevad Ohtlikud Ilmanähtused
TALLINNA TEHNIKAÜLIKOOL Eesti Mereakadeemia Merenduskeskus Veeteede lektoraat Raldo Täll RÜNKSAJUPILVEDEGA KAASNEVAD OHTLIKUD ILMANÄHTUSED LÄÄNEMEREL Lõputöö Juhendajad: Jüri Kamenik Lia Pahapill Tallinn 2016 SISUKORD SISUKORD ................................................................................................................................ 2 SÕNASTIK ................................................................................................................................ 4 SISSEJUHATUS ........................................................................................................................ 6 1. RÜNKSAJUPILVED JA ÄIKE ............................................................................................. 8 1.1. Äikese tekkimine ja areng ............................................................................................. 10 1.1.1. Äikese arengustaadiumid ........................................................................................ 11 1.2. Äikeste klassifikatsioon ................................................................................................. 14 1.2.1. Sünoptilise olukorra põhine liigitus ........................................................................ 14 1.2.2. Äikese seos tsüklonitega ......................................................................................... 15 1.2.3. Organiseerumispõhine liigitus ................................................................................ 16 2. RÜNKSAJUPILVEDEGA (ÄIKESEGA) KAASNEVAD OHTLIKUD ILMANÄHTUSED -
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. -
SKYWARN Weather Spotter Training Presentation
SKYWARN Spotter Training Chris Kimble National Weather Service Weather Forecast Office Gray, Maine www.weather.gov/gray Overview National Weather Service Definitions and Forecasting Tools Weather Spotters…Why they’re important? Thunderstorms Tornadoes Flash Flooding Storm Safety NWS Mission “To protect the lives and property of the citizens of the United States…” Watches and Warnings Outreach and Training NWS County Warning Areas Basic Definitions WATCH – conditions are favorable for severe weather to develop. Valid 4-6 hours. Contains several counties. WARNING – severe weather has been visually observed or detected on radar. Valid usually 1 hour or less, issued on a storm-by-storm basis. STATEMENT – provides follow-up information to a warning which is in effect. Basic Definitions TORNADO – a violently rotating column of air, attached to a thunderstorm, and in contact with the ground. SEVERE THUNDERSTORM – a thunderstorm which produces hail 1 inch diameter, and/or wind gusts 58 mph (50 knots) or stronger. FLASH FLOOD – a rapid rise in water, usually during or after a period of heavy rain. Tools for Detecting Storms Observations Copyright S. Hanes Computer models Satellite Radar Lightning Detection Network Observations We take many measurements of the atmosphere: Weather Balloons Releases twice a day all over the world at the same time – 900 stations worldwide Measures temperature, humidity, pressure as it goes up Flight lasts about 2 hrs and can reach as high as 115,000 ft Data is input into computer models Computer -
NCAR Annual Scientific Report Fiscal Year 1985 - Link Page Next PART0002
National Center for Atmospheric Research Annual Scientific Report Fiscal Year 1985 Submitted to National Science Foundation by University Corporation for Atmospheric Research March 1986 iii CONTENTS INTRODUCTION ............... ............................................. v ATMOSPHERIC ANALYSIS AND PREDICTION DIVISION ............... 1 Significant Accomplishments........................ 1 AAP Division Office................................................ 4 Mesoscale Research Section . ........................................ 8 Climate Section........................................ 15 Large-Scale Dynamics Section....................................... 22 Oceanography Section. .......................... 28 ATMOSPHERIC CHEMISTRY DIVISION................................. .. 37 Significant Accompl i shments........................................ 38 Precipitation Chemistry, Reactive Gases, and Aerosols Section. ..................................39 Atmospheric Gas Measurements Section............................... 46 Global Observations, Modeling, and Optical Techniques Section.............................. 52 Support Section.................................................... 57 Di rector' s Office. * . ...... .......... .. .. ** 58 HIGH ALTITUDE OBSERVATORYY .. .................. ............... 63 Significant Accomplishments .......... .............................. 63 Coronal/Interplanetary Physics Section ....................... 64 Solar Variability and Terrestrial Interactions Section........................................... 72 Solar -
Session 8.Pdf
MARTIN SETVÁK [email protected] CZECH HYDROMETEOROLOGICAL INSTITUTE ČESKÝ HYDROMETEOROLOGICKÝ ÚSTAV http://www.chmi.cz http://www.setvak.cz Anticipated benefits of improved temporal and spatial resolution (with focus on deep convective clouds) EUMeTrain Event Week on MTG-I Satellite, 7 – 11 November 2016 Martin Setvák version: 2016-11-11 Introduction The most significant impact of improved spatial resolution and shorter scan interval: observations (detection, monitoring, nowcasting, …) and studies of short-lived and small scale features or phenomena e.g. fires, valley fog, shallow convection, and tops of deep convective clouds (storms) – namely their overshooting tops Martin Setvák Introduction The most significant impact of improved spatial resolution and shorter scan interval: observations (detection, monitoring, nowcasting, …) and studies of short-lived and small scale features or phenomena e.g. fires, valley fog, shallow convection, and tops of deep convective clouds (storms) – namely their overshooting tops geometrical properties and characteristics (visible and near-IR bands), cloud microphysics, cloud-top brightness temperature (BT) Martin Setvák Overshooting tops definition and appearance OVERSHOOTING TOP (anvil dome, penetrating top): A domelike protrusion above a cumulonimbus anvil, representing the intrusion of an updraft through its equilibrium level (level of neutral buoyancy). It is usually a transient feature because the rising parcel's momentum acquired during its buoyant ascent carries it past the point where it is