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Final Exam December 16, 2004 Name (Print, Last first): Signature: on My Honor, I Have Neither Given Nor Received Unauthorized Aid on This Examination
21111 21111 Instructor(s): Prof. Seiberling PHYSICS DEPARTMENT MET 1010 Final Exam December 16, 2004 Name (print, last ¯rst): Signature: On my honor, I have neither given nor received unauthorized aid on this examination. YOUR TEST NUMBER IS THE 5-DIGIT NUMBER AT THE TOP OF EACH PAGE. (1) Code your test number on your answer sheet (use 76{80 for the 5-digit number). Code your name on your answer sheet. DARKEN CIRCLES COMPLETELY. Code your UFID number on your answer sheet. (2) Print your name on this sheet and sign it also. (3) Do all scratch work anywhere on this exam that you like. Circle your answers on the test form. At the end of the test, this exam printout is to be turned in. No credit will be given without both answer sheet and printout with scratch work most questions demand. (4) Blacken the circle of your intended answer completely, using a #2 pencil or blue or black ink. Do not make any stray marks or some answers may be counted as incorrect. (5) The answers are rounded o®. Choose the closest to exact. There is no penalty for guessing. (6) Hand in the answer sheet separately. There are 33 multiple choice questions. Clearly circle the one best answer for each question. If more than one answer is marked, no credit will be given for that question, even if one of the marked answers is correct. Guessing an answer is better than leaving it blank. All questions are worth 3 points except 1, marked 4 points. Good Luck! 1. -
Information Contained in a METAR Example METAR Codes
METAR METAR is a format for reporting weather information. A METAR weather report is predominantly used by pilots in fulfillment of a part of a pre-flight weather briefing, and by meteorologists, who use aggregated METAR information to assist in weather forecasting. Raw METAR is the most common format in the world for the transmission of observational weather data. [citation needed] It is highly standardized through the International Civil Aviation Organization (ICAO), which allows it to be understood throughout most of the world. Information contained in a METAR A typical METAR contains data for the temperature, dew point, wind speed and direction, precipitation, cloud cover and heights, visibility, and barometric pressure. A METAR may also contain information on precipitation amounts, lightning, and other information that would be of interest to pilots or meteorologists such as a pilot report or PIREP, colour states and runway visual range (RVR). In addition, a short period forecast called a TRED may be added at the end of the METAR covering likely changes in weather conditions in the two hours following the observation. These are in the same format as a Terminal Aerodrome Forecast (TAF). The complement to METARs, reporting forecast weather rather than current weather, are TAFs. METARs and TAFs are used in VOLMET broadcasts. Example METAR codes International METAR codes The following is an example METAR from Burgas Airport in Burgas, Bulgaria. It was taken on 4 February 2005 at 16:00 Coordinated Universal Time (UTC). METAR LBBG 041600Z 12003MPS 310V290 1400 R04/P1500 R22/P1500U +S BK022 OVC050 M04/M07 Q1020 OSIG 9949//91= • METAR indicates that the following is a standard hourly observation. -
Types of Clouds
Types of Clouds What’s the Weather? Cirrus, Cirrocumulus and Cirrostratus (high 5000-16,000 m) . thin and often wispy . composed of ice crystals that originate from the freezing of supercooled water droplets. Generally occur in fair weather and point in the direction of air movement at their elevation. Cirrus . They are made of ice crystals and have long, thin, wispy streamers. Cirrus clouds are usually white and predict fair weather. cirrus cirrus cirrus cirrus cirrus cirrus Cirrocumulus . They are small rounded puffs that usually appear in long rows. Cirrocumulus are usually white, but sometimes appear gray. Cirrocumulus are usually seen in the winter time and mean that there will be fair, but cold weather. Cirrostratus . Sheetlike thin clouds that usually cover the entire sky. Cirrostratus clouds usually come 12-24 hours before a rain or snow storm. Altocumulus and Altostratus (middle 2,000 to 7, 000 m) . Middle clouds are made of ice crystals and water droplets. The base of a middle cloud above the surface can be anywhere from 2000-8000m in the tropics to 2000-4000m in the polar regions. An Altocumulus . They are grayish-white with one part of the cloud darker than the other. Usually form in groups. If you see altocumulus clouds on a warm sticky morning, then expect thunderstorms by late afternoon. Altostratus . An altostratus cloud usually covers the whole sky. The cloud looks gray or blue-gray. Usually forms ahead of storms that have a lot of rain or snow. Sometimes, rain will fall from an altostratus cloud. If the rain hits the ground, then the cloud is called a nimbostratus cloud. -
Metar Abbreviations Metar/Taf List of Abbreviations and Acronyms
METAR ABBREVIATIONS http://www.alaska.faa.gov/fai/afss/metar%20taf/metcont.htm METAR/TAF LIST OF ABBREVIATIONS AND ACRONYMS $ maintenance check indicator - light intensity indicator that visual range data follows; separator between + heavy intensity / temperature and dew point data. ACFT ACC altocumulus castellanus aircraft mishap MSHP ACSL altocumulus standing lenticular cloud AO1 automated station without precipitation discriminator AO2 automated station with precipitation discriminator ALP airport location point APCH approach APRNT apparent APRX approximately ATCT airport traffic control tower AUTO fully automated report B began BC patches BKN broken BL blowing BR mist C center (with reference to runway designation) CA cloud-air lightning CB cumulonimbus cloud CBMAM cumulonimbus mammatus cloud CC cloud-cloud lightning CCSL cirrocumulus standing lenticular cloud cd candela CG cloud-ground lightning CHI cloud-height indicator CHINO sky condition at secondary location not available CIG ceiling CLR clear CONS continuous COR correction to a previously disseminated observation DOC Department of Commerce DOD Department of Defense DOT Department of Transportation DR low drifting DS duststorm DSIPTG dissipating DSNT distant DU widespread dust DVR dispatch visual range DZ drizzle E east, ended, estimated ceiling (SAO) FAA Federal Aviation Administration FC funnel cloud FEW few clouds FG fog FIBI filed but impracticable to transmit FIRST first observation after a break in coverage at manual station Federal Meteorological Handbook No.1, Surface -
Thunderstorm Anatomy and Dynamics
THUNDERSTORM ANATOMY AND DYNAMICS An Overview Prepared by LCDR Bill Nisley MR 3421 • Cloud Physics Naval Postgraduate School • Monterey, California [email protected] Photo credits: Thunderstorm Cell and Mammatus Clouds by: Michael Bath; Tornado by Daphne Zaras / NSSL; Supercell Thunderstorm by: AMOS; Wall Cloud by: Greg Michels 1. Introduction The purpose of this paper is to present a broad overview of the various cloud structures displayed during the life cycle of a thunderstorm and the atmospheric dynamics associated with each. Knowledge of atmospheric dynamics provides for a keener understanding of the physical processes related to the “why and how” certain cloud features form. Accordingly, observation of cloud features presents visual queuing of changes in the atmosphere. 2. Thunderstorm Formation and Stages of Development Thunderstorm development is dependent on three basic components: moisture, instability, and some form of lifting mechanism. 2.1 Moisture – As air near the surface is lifted higher in the atmosphere and cooled, available water vapor condenses into small water droplets which form clouds. As condensation of water vapor occurs, latent heat is released making the rising air warmer and less dense than its surroundings (figure 1). The added heat allows the air (parcel) to continue to rise and form an updraft within the developing cloud structure. 2.1.1 In general1, low level moisture increases instability simply by making more latent heat available to the lower atmosphere. Increasing mid level moisture can decrease instability in the atmosphere because moist air is less dense than dry air and therefor is unable to evaporate • Figure 1 – Positive buoyancy / instability as a result of precipitation and cloud droplets as condensation and release of latent heat. -
Chapter 6 Clouds
Chapter 6 Clouds Chapter overview • Processes causing saturation o Cooling, moisturizing, mixing • Cloud identification and classification • Cloud Observations • Fog Why do we care about clouds in the atmosphere? Cloud Development Clouds form when air becomes saturated. How can unsaturated air become saturated? • Cooling • Adding moisture • Mixing Cooling and moisturizing The amount of cooling needed for air to become saturated is given by ΔT = Td - T The amount of additional moisture needed for air to become saturated is given by Δr = rs - r The change in temperature (ΔT) or the change in moisture (Δr) can be determined by evaluating the heat or moisture budget of an air parcel. Most clouds form as a result of rising air. How does the temperature and relative humidity of an air parcel change as it rises adiabatically? What processes are responsible for causing air to rise? Cumuliform clouds form in air that rises due to its buoyancy. Stratiform clouds form in are that is forced to rise. Mixing Mixing of two unsaturated air parcels can result in a saturated mixture. Why can the mixing of unsaturated air result in air becoming saturated? What are some examples of air becoming saturated in this way? The temperature and mixing ratio of the mixture can be calculated using: mx = mB + mC mBTB + mCTC Tx = mx mBrB + mCrC rx = mx Where the m is the mass of the air parcel, subscripts B and C indicate the two original air parcels, and subscript X indicates the mixture. Vapor pressure or specific humidity can be used in place in mixing ratio. -
Degradation of Radar Reflectivity by Cloud Attenuation at Microwave Frequency
640 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 24 Degradation of Radar Reflectivity by Cloud Attenuation at Microwave Frequency OLIVIER PUJOL AND JEAN-FRANÇOIS GEORGIS Laboratoire d’Aérologie, Observatoire Midi-Pyrénées, Université Paul Sabatier, Toulouse, France LAURENT FÉRAL Laboratoire AD2M, Université Paul Sabatier, Toulouse, France HENRI SAUVAGEOT Laboratoire d’Aérologie, Observatoire Midi-Pyrénées, Université Paul Sabatier, Toulouse, France (Manuscript received 2 November 2005, in final form 7 June 2006) ABSTRACT The main object of this paper is to emphasize that clouds—the nonprecipitating component of condensed atmospheric water—can produce a strong attenuation at operational microwave frequencies, although they present a low reflectivity preventing their radar detection. By way of a simple and realistic model, simu- lations of radar observations through warm precipitating targets are thus presented in order to quantify cloud attenuation. Simulations concern an airborne radar oriented downward and observing precipitation at four frequencies: 3, 10, 35, and 94 GHz. Two cases are first considered: a convective cell (vigorous cumulus congestus plus rain) and a stratiform one (nimbostratus plus drizzle) superimposed on the previous one. Other simulations are then performed on different types of cumulus (congestus, mediocris, and hu- milis) with various thicknesses characterized, in a microphysical sense, by their maximum liquid water content. Simulations confirm the low cumulus reflectivity ranging from Ϫ45 dBZ for the weakest cumulus (i.e., the humilis one) to Ϫ5dBZ for the strongest one (i.e., the vigorous cumulus congestus). It reaches Ϫ35 dBZ for the nimbostratus cloud. On the other hand, cumulus attenuation [precisely path-integrated cloud at- tenuation (PICA)] is not negligible and, depending on the frequency, can be very strong: the higher the frequency, the stronger the PICA. -
Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries
Open Research Online The Open University’s repository of research publications and other research outputs Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries Thesis How to cite: Aristeidou, Maria (2016). Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries. PhD thesis Institute of Educational Technology. For guidance on citations see FAQs. c [not recorded] https://creativecommons.org/licenses/by-nc-nd/4.0/ Version: Version of Record Copyright and Moral Rights for the articles on this site are retained by the individual authors and/or other copyright owners. For more information on Open Research Online’s data policy on reuse of materials please consult the policies page. oro.open.ac.uk Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries Maria Aristeidou BA Education Science and Primary Education MSc Technology Education and Digital Systems (e-Learning) Submitted for the degree of Doctor of Philosophy Institute of Educational Technology The Open University March 2016 1 Abstract Citizen Inquiry has been proposed as an informal science learning approach to enable widespread involvement in science and empower citizens with reasoning and problem-solving skills used by scientists. It combines aspects from citizen science and inquiry-based learning, producing science learning experiences within distributed communities of interest. A central challenge for Citizen Inquiry is to involve citizens in planning and implementing their own investigations, supported and guided by online systems and tools within an inquiry environment, while collaborating with science experts and non-experts. This thesis explores how to create an active and sustainable online community for citizens to engage in scientific investigations. -
The Ten Different Types of Clouds
THE COMPLETE GUIDE TO THE TEN DIFFERENT TYPES OF CLOUDS AND HOW TO IDENTIFY THEM Dedicated to those who are passionately curious, keep their heads in the clouds, and keep their eyes on the skies. And to Luke Howard, the father of cloud classification. 4 Infographic 5 Introduction 12 Cirrus 18 Cirrocumulus 25 Cirrostratus 31 Altocumulus 38 Altostratus 45 Nimbostratus TABLE OF CONTENTS TABLE 51 Cumulonimbus 57 Cumulus 64 Stratus 71 Stratocumulus 79 Our Mission 80 Extras Cloud Types: An Infographic 4 An Introduction to the 10 Different An Introduction to the 10 Different Types of Clouds Types of Clouds ⛅ Clouds are the equivalent of an ever-evolving painting in the sky. They have the ability to make for magnificent sunrises and spectacular sunsets. We’re surrounded by clouds almost every day of our lives. Let’s take the time and learn a little bit more about them! The following information is presented to you as a comprehensive guide to the ten different types of clouds and how to idenify them. Let’s just say it’s an instruction manual to the sky. Here you’ll learn about the ten different cloud types: their characteristics, how they differentiate from the other cloud types, and much more. So three cheers to you for starting on your cloud identification journey. Happy cloudspotting, friends! The Three High Level Clouds Cirrus (Ci) Cirrocumulus (Cc) Cirrostratus (Cs) High, wispy streaks High-altitude cloudlets Pale, veil-like layer High-altitude, thin, and wispy cloud High-altitude, thin, and wispy cloud streaks made of ice crystals streaks -
Climatology Climatic Zone
Climatology Climatic Zone 1320. At about what geographical latitude as average is assumed for the zone of prevailing westerlies? A) 10° N. B) 50° N. C) 80° N. D) 30° N. 1321. What is the type, intensity and seasonal variation of precipitation in the equatorial region? A) Rain showers, hail showers and thunderstorms occur the whole year, but frequency is highest during two periods: April-May and October- November. B) Precipitation is generally in the form of showers but continuous rain occurs also. The greatest intensity is in July. C) Warm fronts are common with continuous rain. The frequency is the same throughout the year D) Showers of rain or hail occur throughout the year; the frequency is highest in January. 1324. The reason for the fact, that the Icelandic low is normally deeper in winter than in summer is that: A) the strong winds of the north Atlantic in winter are favourable for the development of lows. B) the low pressure activity of the sea east of Canada is higher in winter. C) the temperature contrasts between arctic and equatorial areas are much greater in winter. D) converging air currents are of greater intensity in winter. 1328. The lowest relative humidity will be found: A) at the south pole. B) between latitudes 30 deg and 40 deg N in July. C) in equatorial regions. D) around 30 deg S in January. Tropical Climatology: 1329. Flying from Dakar to Rio de Janeiro in winter where would you cross the ITCZ? A) 7 to 120N. B) 0 to 70N. C) 7 to 120S. -
An Introduction to Clouds
Clouds National Meteorological Library and Archive Fact sheet 1 — An introduction to clouds The National Meteorological Library and Archive Many people have an interest in the weather and the processes that cause it, which is why the National Meteorological Library and Archive are open to everyone. Holding one of the most comprehensive collections on meteorology anywhere in the world, the Library and Archive are vital for the maintenance of the public memory of the weather, the storage of meteorological records and as aid of learning. The Library and Archive collections include: • around 300,000 books, charts, atlases, journals, articles, microfiche and scientific papers on meteorology and climatology, for a variety of knowledge levels • audio-visual material including digitised images, slides, photographs, videos and DVDs • daily weather reports for the United Kingdom from 1861 to the present, and from around the world • marine weather log books • a number of the earliest weather diaries dating back to the late 18th century • artefacts, records and charts of historical interest; for example, a chart detailing the weather conditions for the D-Day Landings, the weather records of Scott’s Antarctic expedition from 1911 • rare books, including a 16th century edition of Aristotle’s Meteorologica, held on behalf of the Royal Meteorological Society • a display of meteorological equipment and artefacts For more information about the Library and Archive please see our website at: www.metoffice.gov.uk/learning/library Introduction A cloud is an aggregate of very small water droplets, ice crystals, or a mixture of both, with its base above the Earth’s surface. -
Surface Weather Observations and Reports
U.S. DEPARTMENT OF COMMERCE/ National Oceanic and Atmospheric Administration OFFICE OF THE FEDERAL COORDINATOR FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH FEDERAL METEOROLOGICAL HANDBOOK No. 1 Surface Weather Observations andReports FCM-H1-1995 Washington, D.C. December 1995 FEDERAL COORDINATOR FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH 8455 COLESVILLE ROAD, SUITE 1500 SILVER SPRING, MARYLAND 20910 FEDERAL METEOROLOGICAL HANDBOOK NUMBER 1 SURFACE WEATHER OBSERVATIONS AND REPORTS FCM-H1-1995 Washington, D.C. December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