APPENDIX C SYMBOLS, LINES, and MARKERS
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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). -
The Weather the Weather
The weather Área Lectura y Escritura Resultados de aprendizaje Conocer vocabulario relacionado al clima. Utilizar vocabulario relacionado al clima en contextos de escritura formal. Contenidos 1. General vocabulary words Debo saber - Simple present - Present continuous - Simple past - Past continuous The Weather Cold weather In Scandinavia, the chilly (1) days of autumn soon change to the cold days of winter. The first frosts (2) arrive and the roads become icy. Rain becomes sleet (3) and then snow, at first turning to slush (4) in the streets, but soon settling (5), with severe blizzards (6) and snowdrifts (7) in the far north. Freezing weather often continues in the far north until May or even June, when the ground starts to thaw (8) and the ice melts (9) again. - (1) cold, but not very - (2) thin white coat of ice on everything - (3) rain and snow mixed - (4) dirty, brownish, half- snow, half – water - (5) staying as a white covering - (6) snow blown by high winds - (7) Deep banks of snow against walls, etc. - (8) change from hard, frozen state to normal - (9) change from solid to liquid under heat Servicios Académicos para el Acompañamiento y la Permanencia - PAIEP Primera Edición - 2016 En caso de encontrar algún error, contáctate con PAIEP-USACH al correo: [email protected] 1 Warm / hot weather - Close: warm and uncomfortable. - Stifling: hot, uncomfortable, you can hardly breathe. - Humid: hot and damp, makes you sweat a lot. - Scorching: very hot, often used in positive contexts. - Boling: very hot, often used in negative contexts - Mild: warm at a time when it is normally cold - Heat wave last month: very hot, dry period Wet weather This wet weather scale gets stronger from left to right. -
WMO Solid Precipitation Measurement Intercomparison--Final Report
W O R L D M E T E O R O L O G I C A L O R G A N I Z A T I O N INSTRUMENTS AND OBSERVING METHODS R E P O R T No. 67 WMO SOLID PRECIPITATION MEASUREMENT INTERCOMPARISON FINAL REPORT by B.E. Goodison and P.Y.T. Louie (both Canada) and D. Yang (China) WMO/TD - No. 872 1998 NOTE The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the World Meteorological Organization concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. This report has been produced without editorial revision by the WMO Secretariat. It is not an official WMO publication and its distribution in this form does not imply endorsement by the Organization of the ideas expressed. FOREWORD The WMO Solid Precipitation Measurement Intercomparison was started in the northern hemisphere winter of 1986/87. The field work was carried out in 13 Member countries for seven years. The Intercomparison was the result of Recommendation 17 of the ninth session of the Commission for Instruments and Methods of Observation (CIMO-IX). As in previous WMO intercomparisons of rain gauges, the main objective of this test was to assess national methods of measuring solid precipitation against methods whose accuracy and reliability were known. It included past and current procedures, automated systems and new methods of observation. The experiment was designed to determine especially wind related errors, and wetting and evaporative losses in national methods of measuring solid precipitation. -
Student Name: ______Date: ______
Water Cycle Vocabulary Worksheet Student Name: _______________________ Date: _________ Teacher Name: LaTrecia Abero Score: _________ Define these terms: Atmosphere The different layers of gases that extend from the surface of the Earth into space. Boiling This is the change from a liquid to a gas. Boiling Point This is a temperature where the vapor pressure of a liquid equals the atmospheric pressure. Cloud The result of evaporation, this is a visible body of fine water droplets or ice particles suspended in Earth's atmosphere. Condensation This is the process of matter changing from a gaseous state to a liquid state. Dew This is when water vapor in the air condenses directly onto a surface, usually seen in the morning. Earth The third planet from the sun. Evaporation This is another term for vaporization, the part of the water cycle in which water changes from a liquid to a gas. Water moves from bodies of water on Earth to water vapor in the atmosphere. Fog This is a low-lying cloud. This is a collection of liquid water droplets or ice crystals suspended in the air at or near the Earth's surface. Freezing This is the process of matter changing from the liquid to the solid state. Groundwater This is water stored in the spaces between rocks inside Earth that is found within a few miles of the Earth's surface. Hail This is pellets of frozen rain that fall in showers from cumulonimbus clouds. Heat The transfer of thermal energy between two bodies which are at different temperatures. The SI unit for this is the Joule. -
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. -
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 -
Print Key. (Pdf)
Weather Map Symbols Along the center, the cloud types are indicated. The top symbol is the high-level cloud type followed by the At the upper right is the In the upper left, the temperature mid-level cloud type. The lowest symbol represents low-level cloud over a number which tells the height of atmospheric pressure reduced to is plotted in Fahrenheit. In this the base of that cloud (in hundreds of feet) In this example, the high level cloud is Cirrus, the mid-level mean sea level in millibars (mb) A example, the temperature is 77°F. B C C to the nearest tenth with the cloud is Altocumulus and the low-level clouds is a cumulonimbus with a base height of 2000 feet. leading 9 or 10 omitted. In this case the pressure would be 999.8 mb. If the pressure was On the second row, the far-left Ci Dense Ci Ci 3 Dense Ci Cs below Cs above Overcast Cs not Cc plotted as 024 it would be 1002.4 number is the visibility in miles. In from Cb invading 45° 45°; not Cs ovcercast; not this example, the visibility is sky overcast increasing mb. When trying to determine D whether to add a 9 or 10 use the five miles. number that will give you a value closest to 1000 mb. 2 As Dense As Ac; semi- Ac Standing Ac invading Ac from Cu Ac with Ac Ac of The number at the lower left is the a/o Ns transparent Lenticularis sky As / Ns congestus chaotic sky Next to the visibility is the present dew point temperature. -
Laboratory Simulations Show Diabatic Heating Drives Cumulus-Cloud Evolution and Entrainment
Laboratory simulations show diabatic heating drives cumulus-cloud evolution and entrainment Roddam Narasimhaa,1, Sourabh Suhas Diwana, Subrahmanyam Duvvuria,b,2, K. R. Sreenivasa, and G. S. Bhatc aJawaharlal Nehru Centre for Advanced Scientific Research, Bangalore 560064, India; bIndian Institute of Technology Madras, Chennai 600036, India; and cIndian Institute of Science, Bangalore 560012, India Contributed by Roddam Narasimha, August 3, 2011 (sent for review June 16, 2011) Clouds are the largest source of uncertainty in climate science, mining the evolution and entrainment dynamics of cumulus and remain a weak link in modeling tropical circulation. A major clouds. challenge is to establish connections between particulate micro- physics and macroscale turbulent dynamics in cumulus clouds. Background Here we address the issue from the latter standpoint. First we The ability to simulate cloud processes under controlled and show how to create bench-scale flows that reproduce a variety repeatable conditions in the laboratory has long been recognized of cumulus-cloud forms (including two genera and three species), as a potentially valuable aid in studying cloud physics and dy- and track complete cloud life cycles—e.g., from a “cauliflower” con- namics. Many laboratory studies have been directed toward gestus to a dissipating fractus. The flow model used is a transient understanding the effect of small-scale turbulence on droplet plume with volumetric diabatic heating scaled dynamically to simu- microphysics (5, 9), among other issues. Recent experiments on late latent-heat release from phase changes in clouds. Laser-based a jet of moist air in a cloud chamber (11) have shown that the small-scale turbulence at the cloud-clear air interface is aniso- diagnostics of steady plumes reveal Riehl–Malkus type protected tropic. -
Storm Spotting – Solidifying the Basics PROFESSOR PAUL SIRVATKA COLLEGE of DUPAGE METEOROLOGY Focus on Anticipating and Spotting
Storm Spotting – Solidifying the Basics PROFESSOR PAUL SIRVATKA COLLEGE OF DUPAGE METEOROLOGY HTTP://WEATHER.COD.EDU Focus on Anticipating and Spotting • What do you look for? • What will you actually see? • Can you identify what is going on with the storm? Is Gilbert married? Hmmmmm….rumor has it….. Its all about the updraft! Not that easy! • Various types of storms and storm structures. • A tornado is a “big sucky • Obscuration of important thing” and underneath the features make spotting updraft is where it forms. difficult. • So find the updraft! • The closer you are to a storm the more difficult it becomes to make these identifications. Conceptual models Reality is much harder. Basic Conceptual Model Sometimes its easy! North Central Illinois, 2-28-17 (Courtesy of Matt Piechota) Other times, not so much. Reality usually is far more complicated than our perfect pictures Rain Free Base Dusty Outflow More like reality SCUD Scattered Cumulus Under Deck Sigh...wall clouds! • Wall clouds help spotters identify where the updraft of a storm is • Wall clouds may or may not be present with tornadic storms • Wall clouds may be seen with any storm with an updraft • Wall clouds may or may not be rotating • Wall clouds may or may not result in tornadoes • Wall clouds should not be reported unless there is strong and easily observable rotation noted • When a clear slot is observed, a well written or transmitted report should say as much Characteristics of a Tornadic Wall Cloud • Surface-based inflow • Rapid vertical motion (scud-sucking) • Persistent • Persistent rotation Clear Slot • The key, however, is the development of a clear slot Prof. -
Flash Flooding
NationalNational OceanicOceanic andand AtmosphericAtmospheric AdministrationAdministration (NOAA)(NOAA) NationalNational WeatherWeather ServiceService (NWS)(NWS) PresentsPresents SevereSevere WeatherWeather ObserverObserver andand SafetySafety TrainingTraining 20052005 Severe Weather Spotter Line 1-888-668-3344 Spotter Reports E-mail: www.crh.noaa.gov/espotter Homepage Address: www.crh.noaa.gov/iwx 2 GoalsGoals ofof thethe TrainingTraining You will learn: • Definitions of important weather terms and severe weather criteria • How thunderstorms develop and why some become severe • How to correctly identify cloud features that may or may not be associated with severe weather • What information the observer is to report and how to report it • Ways to receive weather information before and during severe weather events • Observer Safety! 3 WFOWFO NorthernNorthern IndianaIndiana (WFO(WFO IWX)IWX) CountyCounty WarningWarning andand ForecastForecast AreaArea (CWFA)(CWFA) Work with public, state and local officials Dedicated team of highly trained professionals 24 hours a day/7 days a week Prepare forecasts and warnings for 2.3 million people in 37 counties 4 SKYWARNSKYWARN (Severe(Severe Weather)Weather) ObserversObservers Why Are You Critical to NWS Operations? • Help overcome Doppler Radar limitations • Provide ground truth which can be correlated with radar signatures prior to, during, and after severe weather • Ground truth reports in warnings heighten public awareness and allow us to have confidence in our warning decisions 5 SKYWARNSKYWARN (Severe(Severe Weather)Weather) ObserversObservers Why Are You Critical to NWS Operations? • The NWS receives hundreds of reports of “False” or “Mis-Identified” funnel clouds and tornadoes each year • We strongly rely on the “2 out of 3” Rule before issuing a warning. Of the following, we like to have 2 out of 3 present before sending out a warning. -
Glossary of Severe Weather Terms
Glossary of Severe Weather Terms -A- Anvil The flat, spreading top of a cloud, often shaped like an anvil. Thunderstorm anvils may spread hundreds of miles downwind from the thunderstorm itself, and sometimes may spread upwind. Anvil Dome A large overshooting top or penetrating top. -B- Back-building Thunderstorm A thunderstorm in which new development takes place on the upwind side (usually the west or southwest side), such that the storm seems to remain stationary or propagate in a backward direction. Back-sheared Anvil [Slang], a thunderstorm anvil which spreads upwind, against the flow aloft. A back-sheared anvil often implies a very strong updraft and a high severe weather potential. Beaver ('s) Tail [Slang], a particular type of inflow band with a relatively broad, flat appearance suggestive of a beaver's tail. It is attached to a supercell's general updraft and is oriented roughly parallel to the pseudo-warm front, i.e., usually east to west or southeast to northwest. As with any inflow band, cloud elements move toward the updraft, i.e., toward the west or northwest. Its size and shape change as the strength of the inflow changes. Spotters should note the distinction between a beaver tail and a tail cloud. A "true" tail cloud typically is attached to the wall cloud and has a cloud base at about the same level as the wall cloud itself. A beaver tail, on the other hand, is not attached to the wall cloud and has a cloud base at about the same height as the updraft base (which by definition is higher than the wall cloud).