Mid-Latitude Atmospheric Dynamics: a First Course
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Balanced Flow Natural Coordinates
Balanced Flow • The pressure and velocity distributions in atmospheric systems are related by relatively simple, approximate force balances. • We can gain a qualitative understanding by considering steady-state conditions, in which the fluid flow does not vary with time, and by assuming there are no vertical motions. • To explore these balanced flow conditions, it is useful to define a new coordinate system, known as natural coordinates. Natural Coordinates • Natural coordinates are defined by a set of mutually orthogonal unit vectors whose orientation depends on the direction of the flow. Unit vector tˆ points along the direction of the flow. ˆ k kˆ Unit vector nˆ is perpendicular to ˆ t the flow, with positive to the left. kˆ nˆ ˆ t nˆ Unit vector k ˆ points upward. ˆ ˆ t nˆ tˆ k nˆ ˆ r k kˆ Horizontal velocity: V = Vtˆ tˆ kˆ nˆ ˆ V is the horizontal speed, t nˆ ˆ which is a nonnegative tˆ tˆ k nˆ scalar defined by V ≡ ds dt , nˆ where s ( x , y , t ) is the curve followed by a fluid parcel moving in the horizontal plane. To determine acceleration following the fluid motion, r dV d = ()Vˆt dt dt r dV dV dˆt = ˆt +V dt dt dt δt δs δtˆ δψ = = = δtˆ t+δt R tˆ δψ δψ R radius of curvature (positive in = R δs positive n direction) t n R > 0 if air parcels turn toward left R < 0 if air parcels turn toward right ˆ dtˆ nˆ k kˆ = (taking limit as δs → 0) tˆ R < 0 ds R kˆ nˆ ˆ ˆ ˆ t nˆ dt dt ds nˆ ˆ ˆ = = V t nˆ tˆ k dt ds dt R R > 0 nˆ r dV dV dˆt = ˆt +V dt dt dt r 2 dV dV V vector form of acceleration following = ˆt + nˆ dt dt R fluid motion in natural coordinates r − fkˆ ×V = − fVnˆ Coriolis (always acts normal to flow) ⎛ˆ ∂Φ ∂Φ ⎞ − ∇ pΦ = −⎜t + nˆ ⎟ pressure gradient ⎝ ∂s ∂n ⎠ dV ∂Φ = − dt ∂s component equations of horizontal V 2 ∂Φ momentum equation (isobaric) in + fV = − natural coordinate system R ∂n dV ∂Φ = − Balance of forces parallel to flow. -
16 Tropical Cyclones
Copyright © 2017 by Roland Stull. Practical Meteorology: An Algebra-based Survey of Atmospheric Science. v1.02 16 TROPICAL CYCLONES Contents Intense synoptic-scale cyclones in the tropics are called tropical cyclones. As for all cyclones, trop- 16.1. Tropical Cyclone Structure 604 ical cyclones have low pressure in the cyclone center 16.2. Intensity & Geographic distribution 605 near sea level. Low-altitude winds also rotate cy- 16.2.1. Saffir-Simpson Hurricane Wind Scale 605 clonically (counterclockwise in the N. Hemisphere) 16.2.2. Typhoon Intensity Scales 607 around these storms and spiral in towards their cen- 16.2.3. Other Tropical-Cyclone Scales 607 ters. 16.2.4. Geographic Distribution and Movement 607 Tropical cyclones are called hurricanes over 16.3. Evolution 608 the Atlantic and eastern Pacific Oceans, the Carib- 16.3.1. Requirements for Cyclogenesis 608 bean Sea, and the Gulf of Mexico (Fig. 16.1). They 16.3.2. Tropical Cyclone Triggers 610 are called typhoons over the western Pacific. Over 16.3.3. Life Cycle 613 the Indian Ocean and near Australia they are called 16.3.4. Movement/Track 615 cyclones. In this chapter we use “tropical cyclone” 16.3.5. Tropical Cyclolysis 616 to refer to such storms anywhere in the world. 16.4. Dynamics 617 Comparing tropical and extratropical cyclones, 16.4.1. Origin of Initial Rotation 617 tropical cyclones do not have fronts while mid-lati- 16.4.2. Subsequent Spin-up 617 tude cyclones do. Also, tropical cyclones have warm 16.4.3. Inflow and Outflow 618 cores while mid-latitude cyclones have cold cores. -
An Introduction to Dynamic Meteorology.Pdf
January 24, 2004 12:0 Elsevier/AID aid An Introduction to Dynamic Meteorology FOURTH EDITION January 24, 2004 12:0 Elsevier/AID aid This is Volume 88 in the INTERNATIONAL GEOPHYSICS SERIES A series of monographs and textbooks Edited by RENATADMOWSKA, JAMES R. HOLTON and H.THOMAS ROSSBY A complete list of books in this series appears at the end of this volume. January 24, 2004 12:0 Elsevier/AID aid AN INTRODUCTION TO DYNAMIC METEOROLOGY Fourth Edition JAMES R. HOLTON Department of Atmospheric Sciences University of Washington Seattle,Washington Amsterdam Boston Heidelberg London New York Oxford Paris San Diego San Francisco Singapore Sydney Tokyo January 24, 2004 12:0 Elsevier/AID aid Senior Editor, Earth Sciences Frank Cynar Editorial Coordinator Jennifer Helé Senior Marketing Manager Linda Beattie Cover Design Eric DeCicco Composition Integra Software Services Printer/Binder The Maple-Vail Manufacturing Group Cover printer Phoenix Color Corp Elsevier Academic Press 200 Wheeler Road, Burlington, MA 01803, USA 525 B Street, Suite 1900, San Diego, California 92101-4495, USA 84 Theobald’s Road, London WC1X 8RR, UK This book is printed on acid-free paper. Copyright c 2004, Elsevier Inc. All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system, without permission in writing from the publisher. Permissions may be sought directly from Elsevier’s Science & Technology Rights Department in -
NWC Library University of Oklahonur
U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration Environmental Research Laboratories NOAA Technical Mem.orandum. ERL NSSL-10 LIFE CYCLE OF FLORIDA KEYS' WATERSPOUTS Joseph H. Golden Property of NWC Library University of Oklahonur, National Severe Storm.s Laboratory Norm.an. Oklahom.a June 1974 TABLE OF CONTENTS LIST OF SYMBOLS v LIST OF TABLES vii ABSTRACT 1 1. INTRODUCTION 1 2. DATA SOURCES AND ANALYSIS TECHNIQUES 4 3. THE LIFE CYCLE OF KEYS' WATERSPOUTS 9 ,;, 3.1 OVerall View 9 3.2 Stage 1: The Dark Spot 10 3.3 Stage 2: The Spiral Pattern 13 3.4 Stage 3: The Spray Ring 16 3.5 Stage 4: TbeMature Waterspout 19 3.6 Stage 5: TbeDecay 26 3.7 Quantitative Aspects 31 3.7.1 Derived Wind and Pressure Distributions 31 3.7.2 Funnel Structure and Circuiation 33 3.7.3 Waterspout Spray-Vortex Structure and Circulation 36 4. ' FIVE INTERACTING SCALES OF MOTION PRODUCING THE 39 WATERSPOUT LIFE CYCLE 4.1 The Funnel Scale 39 4.1.1 Time-Lapse Photography Program 40 4.2 The Spiral Scale 43 4.3 The Individual Cumulus-Cloud Scale 45 4.4 The Cumulus C10udline Scale 49 4.4.1 ,Surface Heating Contributions 49 4.4.2 1969 RFF Aircraft Waterspout/Cloud1ine Mission 53 4.4.3 Sea-Surface Temperature Heating Mechanism 66 4.5 Synoptic-Scale Contributions 68 4.5.1 June 30, 1969 --An Active Waterspout Day With an 69 East'erly Wave Passage 4.5.2 September 10, 1969 --Large Waterspouts With a 71 Troughline 5. -
An Automatic Recognition Method for Airflow Field Structures Of
atmosphere Article An Automatic Recognition Method for Airflow Field Structures of Convective Systems Based on Single Doppler Radar Data Ping Wang, Kai Gu, Jinyi Hou * and Bingjie Dou School of Electrical and Information Engineering, Tianjin University, Tianjin 300072, China; [email protected] (P.W.); [email protected] (K.G.); [email protected] (B.D.) * Correspondence: [email protected]; Tel.: +86-182-0251-1093 Received: 23 October 2019; Accepted: 24 January 2020; Published: 27 January 2020 Abstract: Airflow structures within convective systems are important predictors of damaging convective disasters. To automatically recognize different kinds of airflow structures (the convergence, divergence, cyclonic rotation, and anticyclonic rotation) within convective systems, an airflow structure recognition method is proposed, in this paper, based on a regular hexagonal template. On the basis of single Doppler radar data, the template is designed according to the appearance model of airflows in radial velocity maps. The proposed method is able to output types and intensities of airflow structures within convective systems. In addition, the outputs of the proposed method are integrated into a projection map of the airflow field structure types and intensities (PMAFSTI), which is developed in this work to visualize three-dimensional airflow structures within convective cells. The proposed airflow structure automatic recognition method and the PMAFSTI were tested using three typical cases. Results of the tests suggest the following: (1) At different evolution stages of the convective systems, e.g., growth, split, and dissipation, the three-dimensional distribution of the airflow fields within convective systems could be clearly observed through the PMAFSTI and (2) on the basis of recognizing the structures of the airflow field, the complex airflow field, such as a squall line, could be further divided into several small parts making the analysis of convective systems more scientific and elaborate. -
A Comprehensive Glossary of Weather Terms for Storm Spotters
NOAA Technical Memorandum NWS SR-145 A COMPREHENSIVE GLOSSARY OF WEATHER TERMS FOR STORM SPOTTERS Michael Branick NOAA/NWS/WFO Norman Contents • Introduction • Glossary (A-B) • Glossary (C-H) • Glossary (I-R) • Glossary (S-Z) • Acknowledgements • Bibliography • Figures Introduction to the First Edition This glossary contains weather-related terms that may be either heard or used by severe local storm spotters or spotter groups. Its purposes are 1) to achieve some level of standardization in the definitions of the terms that are used, and 2) provide a reference from which the meanings of any terms, especially the lesser-used ones, can be found. The idea is to allow smooth and effective communication between storm spotters and forecasters, and vice versa. This is an important necessity within the severe weather warning program. Despite advances in warning and forecasting techniques (e.g., Doppler radar), the human eye will always be a vital part of any effective warning system. Storm spotters are, and always will be, an indispensable part of the severe local storm warning program. A complete list of terms probably is impossible to arrive at, but this list is as comprehensive as possible. Certainly it is not necessary for every spotter to know the meaning of every term contained herein. In this sense, the glossary serves as a reference. In fact, many of the terms may never be heard at all; they are included here just in case, someday, they are. (By the way, inclusion of a term in this glossary does not give license to use it freely in radio or phone communication. -
Occurrence of Anticyclonic Tornadoes in a Topographically Complex Region of Mexico
Hindawi Advances in Meteorology Volume 2019, Article ID 2763153, 11 pages https://doi.org/10.1155/2019/2763153 Research Article Occurrence of Anticyclonic Tornadoes in a Topographically Complex Region of Mexico Noel Carbajal ,1 Jose´ F. Leo´n-Cruz ,1 Luis F. Pineda-Martı´nez ,2 Jose´ Tuxpan-Vargas ,1 and Juan H. Gaviño-Rodrı´guez 3 1Divisio´n de Geociencias Aplicadas, Instituto Potosino de Investigacio´n Cient´ıfica y Tecnolo´gica A.C., San Luis Potos´ı, SLP 78216, Mexico 2Unidad Acade´mica de Ciencias Sociales, Universidad Auto´noma de Zacatecas, Zacatecas, ZAC 98066, Mexico 3Centro Universitario de Investigaciones Oceanolo´gicas, Universidad de Colima, Manzanillo, COL 28860, Mexico Correspondence should be addressed to Noel Carbajal; [email protected] Received 3 September 2018; Accepted 21 November 2018; Published 9 January 2019 Academic Editor: Tomeu Rigo Copyright © 2019 Noel Carbajal et al. (is is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Tornadoes are violent and destructive natural phenomena that occur on a local scale in most regions around the world. Severe storms occasionally lead to the formation of mesocyclones, whose direction or sense of rotation is often determined by the Coriolis force, among other factors. In the Northern Hemisphere, more than 99% of all tornadoes rotate anticlockwise. (e present research shows that, in topographically complex regions, tornadoes have a different probability of rotating clockwise or anti- clockwise. Our ongoing research programme on tornadoes in Mexico has shown that the number of tornadoes is significantly higher than previously thought. -
A Concentrated Outbreak of Tornadoes, Downbursts and Microbursts, and Implications Regarding Vortex Classification
A Concentrated Outbreak of Tornadoes, Downbursts and Microbursts, and Implications Regarding Vortex Classification G REGORY S. F ORBES Department of Meteorology, The Pennsylvania State University, University Park, PA 16802 R OGER M . W AKIMOTO Department ofthe Geophysical Sciences, The University of Chicago, Chicago, IL 60637 Reprinted from MONTHLY WEATH ER REVIEW, Vol. 111, No. I, January 1983 American Metcoro1ogical Society Printed in U. S. A. Reprinted from MONTHLY WEATHER REV IEW, Vol. 111, No. I, January 1983 American Meteorological Socie1 y Prin«d in U. S. A. A Concentrated Outbreak of Tornadoes, Downbursts and Microbursts, and Implications Regarding Vortex Classification GREGORY S. FORBES Department of Meteorology, The Pennsylvania State University, University Park, PA 16802 R OGER M. W AKIMOTO Department of the Geophysical Sciences, The University of Chicago, Chicago, IL 60637 (Manuscript received 6 November 1981 , in final form 13 August 1982) ABSTRACT A remarkable case of severe weather occurred near Springfield, Illinois on 6 August 1977. Aerial and ground surveys revealed that 17 cyclonic vortices, an anticyclonic vortex, I 0 down bursts and 19 microbursts occurred in a limited (20 km X 40 km) area, associated with a bow-shaped radar echo. About half of the vortices appeared to have occurred along a gust front. Some of the others appear to have occurred within the circulation of a mesocyclone accompanying the bow echo, but these vortices seem to have developed specifically in response to localized boundary-layer vorticity generation associated with horizontal and vertical wind shears on the periphery of microbursts. Some of these vortices, and other destructive vortices in the literature, do not qualify as tornadoes as defined in the Glossary ofMeteorology. -
MSE3 Ch10 Dynamics
chapter 10 Copyright © 2011, 2015 by Roland Stull. Meteorology for Scientists and Engineers, 3rd Ed. Dynamics contents We use winds to power our wind turbines, push our sailboats, cool our Winds and Weather Maps 290 houses, and dry our laundry on the Height Contours on Isobaric Surfaces 290 10 clothesline. But winds can also be destructive — in Plotting Winds 291 hurricanes, thunderstorms, or mountain downslope Newton’s Second Law of Motion 292 windstorms. We design our bridges and skyscrap- Lagrangian Momentum Budget 292 ers to withstand wind gusts. Airplane flights are Eulerian Momentum Budget 293 planned to compensate for headwinds and cross- Horizontal Forces 294 winds. Advection 294 Winds are driven by forces acting on air. But Pressure-Gradient Force 295 these forces can be altered by heat and moisture car- Centrifugal Force 296 ried by the air, resulting in a complex interplay we Coriolis Force 297 call weather. The relationship between forces and Turbulent-Drag Force 300 Summary of Forces 301 winds is called atmospheric dynamics. Newto- nian physics describes atmospheric dynamics well. Equations of Horizontal Motion 301 Pressure, drag, and advection are atmospheric Horizontal Winds 302 forces that act in the horizontal. Other forces, called Geostrophic Wind 302 apparent forces, are caused by the Earth’s rotation Gradient Wind 304 (Coriolis force) and by turning of the wind around a Boundary-Layer Wind 307 Boundary-Layer Gradient (BLG) Wind 309 curve (centrifugal and centripetal forces). Cyclostrophic Wind 311 These different forces are present in different Inertial Wind 312 amounts at different places and times, causing large Antitriptic Wind 312 variability in the winds. -
FLUID MECHANICS APPLIED to the STUDY of ATMOSPHERIC CIRCULATIONS (Research Conducted in Cooperation with U
PAPERS IN PHYSICAL OCEANOGRAPHY AND METEOROLOGY PUBLISHED BY MASSACHUSETTS INSTITUTE OF TECHNOLOGY AND WOODS HOLE OCEANOGRAPHIC INSTITUTION VOL. VII, NO. i FLUID MECHANICS APPLIED TO THE STUDY OF ATMOSPHERIC CIRCULATIONS (Research conducted in cooperation with U. S. Department of Agriculture under Bankhead-Jones Special Research Fund) PART I A STUDY OF FLOW PATTERNS WITH THE AID OF ISENTROPIC ANALYSIS A. On the Maintenance of the Westerlies South of the Polar Front BY CARL-GUSTAF ROSSBY B. Technique and Examples of Isentropic Analysis BY JEROME NAMIAS C. Isentropic Analysis of a Case of Anticyclogenesis BY RITCHIE G. SIMMERS CAMBRIDGE AND WOODS HOLE, MASSACHUSETTS December, 1938 CONTENTS PREFACEINTRODUCTION AND ACKNOWLEDGMENTS . 5 3 A.Gus/a! ON THE MAINTENANCE OFTHE WESTERLIES Rossby SOUTH OF THE POLAR FRONT-Car/- 9 B. TECHNIQUE AND EXAMPLES OF ISENTROPIC ANALYSis-Jerome Namias 18 i.i. Plotting Technique routine 18 a. Values chosen for representation 2.b. An Analysisalternate method of representing data. a. Preliminary construction of contour lines b. Isentropic flow patterns c. Non-adiabatic effects d. Weight of air contained between isentropic surfaces II. Isentropic Analysis for the Period June 21-30, 1937 38 I. The surface weather 2. General character of isentropic flow patterns 3. On the relation between shower activity and isentropic flow patterns III.IV.4. Detailed Summary day byPlates day analysis 51 49 C. ISENTROPIC ANALYSIS OF A CASE OF ANTlCYCLOGENESls-Ri/chie G. Simmers 72 II.i. TheIntroduction. Synoptic Situation 72 74 i. General features 2. Data available III.3. TheDetailed description305° Isentropic Charts 83 i. Day by day discussion IV.