Climatological, Meteorological, and Societal
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New Methods in Tornado Climatology
Geography Compass 9/4 (2015): 157–168, 10.1111/gec3.12205 New Methods in Tornado Climatology Holly M. Widen*, Tyler Fricker and James B. Elsner Florida State University Abstract How climate change might affect tornadoes remains an open scientific question. Climatological studies are often contested due to inconsistencies in the available data. Statistical methods are used to overcome some of the data limitations. A few of these methods including using the proportion of tornadoes occur- ring on big tornado days, estimating tornado energy from the damage path, and modeling counts spatially are described here. The methods move beyond analyses of occurrences by damage ratings and spatial smoothing. Applications of these and related methods will help grow the nascent field of tornado climatology. 1. Introduction Climate change and the recent high-impact tornado events have bolstered interest in the field of tornado climatology (Agee and Childs, 2014; Dixon et al., 2011; Farney and Dixon, 2014; Simmons and Sutter, 2012; Standohar-Alfano and van de Lindt, 2014). There is much to learn about how tornadoes might collectively change as the earth continues to warm. For example, new research shows more tornadoes on fewer days (Brooks et al., 2014; Elsner et al., 2014a), perhaps related to the combination of addi- tional moisture and warming aloft (Elsner et al., 2014a). Yet there is greater uncertainty surrounding the interpretation of such results owing to the nature of the dataset (Kunkel et al., 2013). Methods are needed to model the data that allow more confident physical interpretations. The Storm Prediction Center (SPC) contains the most readily available tornado database in the world. -
Article a Climatological Perspective on the 2011 Alabama Tornado
Chaney, P. L., J. Herbert, and A. Curtis, 2013: A climatological perspective on the 2011 Alabama tornado outbreak. J. Operational Meteor., 1 (3), 1925, doi: http://dx.doi.org/10.15191/nwajom.2013.0103. Journal of Operational Meteorology Article A Climatological Perspective on the 2011 Alabama Tornado Outbreak PHILIP L. CHANEY Auburn University, Auburn, Alabama JONATHAN HERBERT and AMY CURTIS Jacksonville State University, Jacksonville, Alabama (Manuscript received 23 January 2012; in final form 17 September 2012) ABSTRACT This paper presents a comparison of the recent 27 April 2011 tornado outbreak with a tornado climatology for the state of Alabama. The climatology for Alabama is based on tornadoes that affected the state during the 19812010 period. A county-level risk index is produced from this climatology. Tornado tracks from the 2011 outbreak are mapped and compared with the climatology and risk index. There were 62 tornadoes in Alabama on 27 April 2011, including many long-track and intense tornadoes. The event resulted in 248 deaths in the state. The 2011 outbreak is also compared with the April 1974 tornado outbreak in Alabama. 1. Introduction population density (Gagan et al. 2010; Dixon et al. 2011). Tornadoes have been documented in every state in Alabama is affected in the spring and fall by the United States and on every continent except midlatitude cyclones, often associated with severe Antarctica. The United States has by far the most weather and tornadoes. During summer and fall tornado reports annually of any country, averaging tornadoes also can be produced by tropical cyclones. A about 1,300 yr-1. -
FMFRP 0-54 the Persian Gulf Region, a Climatological Study
FMFRP 0-54 The Persian Gulf Region, AClimatological Study U.S. MtrineCorps PCN1LiIJ0005LFII 111) DISTRIBUTION STATEMENT A: Approved for public release; distribution is unlimited DEPARTMENT OF THE NAVY Headquarters United States Marine Corps Washington, DC 20380—0001 19 October 1990 FOREWORD 1. PURPOSE Fleet Marine Force Reference Publication 0-54, The Persian Gulf Region. A Climatological Study, provides information on the climate in the Persian Gulf region. 2. SCOPE While some of the technical information in this manual is of use mainly to meteorologists, much of the information is invaluable to anyone who wishes to predict the consequences of changes in the season or weather on military operations. 3. BACKGROUND a. Desert operations have much in common with operations in the other parts of the world. The unique aspects of desert operations stem primarily from deserts' heat and lack of moisture. While these two factors have significant consequences, most of the doctrine, tactics, techniques, and procedures used in operations in other parts of the world apply to desert operations. The challenge of desert operations is to adapt to a new environment. b. FMFRP 0-54 was originally published by the USAF Environmental Technical Applications Center in 1988. In August 1990, the manual was published as Operational Handbook 0-54. 4. SUPERSESSION Operational Handbook 0-54 The Persian Gulf. A Climatological Study; however, the texts of FMFRP 0—54 and OH 0-54 are identical and OH 0-54 will continue to be used until the stock is exhausted. 5. RECOMMENDATIONS This manual will not be revised. However, comments on the manual are welcomed and will be used in revising other manuals on desert warfare. -
19.4 Updated Mobile Radar Climatology of Supercell
19.4 UPDATED MOBILE RADAR CLIMATOLOGY OF SUPERCELL TORNADO STRUCTURES AND DYNAMICS Curtis R. Alexander* and Joshua M. Wurman Center for Severe Weather Research, Boulder, Colorado 1. INTRODUCTION evolution of angular momentum and vorticity near the surface in many of the tornado cases is also High-resolution mobile radar observations of providing some insight into possible modes of supercell tornadoes have been collected by the scale contraction for tornadogenesis and failure. Doppler On Wheels (DOWs) platform between 1995 and present. The result of this ongoing effort 2. DATA is a large observational database spanning over 150 separate supercell tornadoes with a typical The DOWs have collected observations in and data resolution of O(50 m X 50 m X 50 m), near supercell tornadoes from 1995 through 2008 updates every O(60 s) and measurements within including the fields of Doppler velocity, received 20 m of the surface (Wurman et al. 1997; Wurman power, normalized coherent power, radar 1999, 2001). reflectivity, coherent reflectivity and spectral width (Wurman et al. 1997). Stemming from this database is a multi-tiered effort to characterize the structure and dynamics of A typical observation is a four-second quasi- the high wind speed environments in and near horizontal scan through a tornado vortex. To date supercell tornadoes. To this end, a suite of there have been over 10000 DOW observations of algorithms is applied to the radar tornado supercell tornadoes comprising over 150 individual observations for quality assurance along with tornadoes. detection, tracking and extraction of kinematic attributes. Data used for this study include DOW supercell tornado observations from 1995-2003 comprising The integration of observations across tornado about 5000 individual observations of 69 different cases in the database is providing an estimate of mesocyclone-associated tornadoes. -
Dixie Alley: Fact Or Fallacy : an in Depth Analysis of Tornado Distribution in Alabama
Mississippi State University Scholars Junction Theses and Dissertations Theses and Dissertations 1-1-2004 Dixie alley: Fact or Fallacy : An In Depth Analysis of Tornado Distribution in Alabama Kristin Nichole Hurley Follow this and additional works at: https://scholarsjunction.msstate.edu/td Recommended Citation Hurley, Kristin Nichole, "Dixie alley: Fact or Fallacy : An In Depth Analysis of Tornado Distribution in Alabama" (2004). Theses and Dissertations. 1549. https://scholarsjunction.msstate.edu/td/1549 This Graduate Thesis - Open Access is brought to you for free and open access by the Theses and Dissertations at Scholars Junction. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Scholars Junction. For more information, please contact [email protected]. DIXIE ALLEY:FACT OR FALLACY AN IN DEPTH ANALYSIS OF TORNADO DISTRIBUTION IN ALABAMA By Kristin Nichole Hurley A Thesis Submitted to the Faculty of Mississippi State University in Partial Fulfillment of the Requirements for the Degree of Master of Science in Geoscience in the Department of Geosciences Mississippi State, Mississippi May 2004 Copyright by Kristin Nichole Hurley 2004 DIXIE ALLEY: FACT OR FALLACY AN IN DEPTH ANALYSIS OF TORNADO DISTRIBUTION IN ALABAMA By Kristin Nichole Hurley ______________________________ ______________________________ Michael E. Brown Charles L. Wax Assistant Professor of Geosciences Professor of Geosciences (Director of Thesis) (Committee Member) ______________________________ ______________________________ John C. Rodgers, III John E. Mylroie Assistant Professor of Geosciences Graduate Coordinator of the Department (Committee Member) of Geosciences ______________________________ ______________________________ Mark S. Binkley Philip B. Oldham Professor and Head of the Department of Dean and Professor of the College of Geosciences Arts and Sciences Name: Kristin Nichole Hurley Date of Degree: May 8, 2004 Institution: Mississippi State University Major Field: Geoscience Major Professor: Dr. -
Florida's Tornado Climatology: Occurrence Rates, Casualties, and Property Losses Emily Ryan
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2018 Florida's Tornado Climatology: Occurrence Rates, Casualties, and Property Losses Emily Ryan Follow this and additional works at the DigiNole: FSU's Digital Repository. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF SOCIAL SCIENCES & PUBLIC POLICY FLORIDA'S TORNADO CLIMATOLOGY: OCCURRENCE RATES, CASUALTIES, AND PROPERTY LOSSES By EMILY RYAN A Thesis submitted to the Department of Geography in partial fulfillment of the requirements for the degree of Master of Science 2018 Copyright c 2018 Emily Ryan. All Rights Reserved. Emily Ryan defended this thesis on April 6, 2018. The members of the supervisory committee were: James B. Elsner Professor Directing Thesis David C. Folch Committee Member Mark W. Horner Committee Member The Graduate School has verified and approved the above-named committee members, and certifies that the thesis has been approved in accordance with university requirements. ii TABLE OF CONTENTS List of Tables . v List of Figures . vi Abstract . viii 1 Introduction 1 1.1 Definitions . 1 1.2 Where Tornadoes Occur . 3 1.3 Tornadoes in Florida . 4 1.4 Goals and Objectives . 6 1.5 Tornado Climatology as Geography . 6 1.6 Outline of the Thesis . 7 2 Data and Methods 9 2.1 Data . 9 2.1.1 Tornado Data . 9 2.1.2 Tropical Cyclone Tornado Data . 11 2.1.3 Property Value Data . 13 2.2 Statistical Methods . 15 2.3 Analysis Variables . 16 2.3.1 Occurrence Rates . 16 2.3.2 Casualties . 16 2.3.3 Property Exposures . -
Part 2 Severe Weather
34 INTRODUCTION to SEVERE WEATHER (from http://www.srh.noaa.gov/jetstream//) 34 35 Chapter 1. Tropical Cyclone (from http://www.srh.noaa.gov/srh/jetstream/tropics/tropics_intro.htm) 1. Introduction A tropical cyclone is a warm-core, low pressure system without any "front" attached, that develops over the tropical or subtropical waters, and has an organized circulation. Depending upon location, tropical cyclones have different names around the world. In the: • Atlantic/Eastern Pacific Oceans - hurricanes • Western Pacific - typhoons • Indian Ocean - cyclones Regardless of what they are called, there are several favorable environmental conditions that must be in place before a tropical cyclone can form. They are: • Warm ocean waters (at least 80°F / 27°C) throughou t a depth of about 150 ft. (46 m). • An atmosphere which cools fast enough with height such that it is potentially unstable to moist convection. • Relatively moist air near the mid-level of the troposphere (16,000 ft. / 4,900 m). • Generally a minimum distance of at least 300 miles (480 km) from the equator. • A pre-existing near-surface disturbance. • Low values (less than about 23 mph / 37 kph) of vertical wind shear between the surface and the upper troposphere. Vertical wind shear is the change in wind speed with height. 35 36 Tropical Cyclone Formation Basin Given that sea surface temperatures need to be at least 80°F (27°C) for tropical cyclones form, it is natural that they form near the equator. However, with only the rarest of occasions, these storms do not form within 5° latitude of the equator. -
Explaining the Trends and Variability in the United States Tornado Records
www.nature.com/scientificreports OPEN Explaining the trends and variability in the United States tornado records using climate teleconnections and shifts in observational practices Niloufar Nouri1*, Naresh Devineni1,2*, Valerie Were2 & Reza Khanbilvardi1,2 The annual frequency of tornadoes during 1950–2018 across the major tornado-impacted states were examined and modeled using anthropogenic and large-scale climate covariates in a hierarchical Bayesian inference framework. Anthropogenic factors include increases in population density and better detection systems since the mid-1990s. Large-scale climate variables include El Niño Southern Oscillation (ENSO), Southern Oscillation Index (SOI), North Atlantic Oscillation (NAO), Pacifc Decadal Oscillation (PDO), Arctic Oscillation (AO), and Atlantic Multi-decadal Oscillation (AMO). The model provides a robust way of estimating the response coefcients by considering pooling of information across groups of states that belong to Tornado Alley, Dixie Alley, and Other States, thereby reducing their uncertainty. The infuence of the anthropogenic factors and the large-scale climate variables are modeled in a nested framework to unravel secular trend from cyclical variability. Population density explains the long-term trend in Dixie Alley. The step-increase induced due to the installation of the Doppler Radar systems explains the long-term trend in Tornado Alley. NAO and the interplay between NAO and ENSO explained the interannual to multi-decadal variability in Tornado Alley. PDO and AMO are also contributing to this multi-time scale variability. SOI and AO explain the cyclical variability in Dixie Alley. This improved understanding of the variability and trends in tornadoes should be of immense value to public planners, businesses, and insurance-based risk management agencies. -
Understanding the Dominant Sources and Tracks of Moisture for Summer
Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Understanding the Dominant Sources and Tracks of Moisture 10.1029/2017JD027652 for Summer Rainfall in the Southwest United States Key Points: Srijita Jana1,2 , Balaji Rajagopalan1,2 , Michael A. Alexander3 , and Andrea J. Ray3 • The leading source of moisture varies depending on the part of the region 1Department of Civil, Environmental and Architectural Engineering, University of Colorado Boulder, Boulder, CO, USA, • Land is an important source of 2 3 moisture during the summer season Cooperative Institute of Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA, NOAA • Large-scale circulation features are Earth System Research Laboratory, Boulder, CO, USA consistent with major pathways of moisture Abstract We investigated the moisture sources and tracks that enable summer rainfall over the four-state Supporting Information: southwestern U.S. region of Arizona, New Mexico, Colorado, and Utah by employing a high-resolution • Supporting Information S1 Lagrangian particle tracking model. Six locations were selected—Cedar City (Utah), Grand Junction • Table S1 (Colorado), Eastonville (Colorado), Laveen (Arizona), Redrock (New Mexico), and Melrose (New Mexico) • Table S2 —together, they represent six spatial regions of summer precipitation for the Southwest. Moisture tracks – Correspondence to: were generated for all the rainy days at these stations for the historical period 1979 2013. Tracks were S. Jana and B. Rajagopalan, generated for a 3-day period ending with the day of rainfall, which were then used to identify the [email protected]; source of moisture, pathway or trajectory, and the modulation along the track. The four major sources of [email protected] moisture—Gulf of California, Gulf of Mexico (GoM), land, and the Pacific Ocean—were identified as responsible for summer rainfall over southwestern United States. -
A Sounding Derived Climatology of Significant Tornado Events in The
P12.14 A SOUNDING-DERIVED CLIMATOLOGY OF SIGNIFICANT TORNADO EVENTS IN THE GREENVILLE-SPARTANBURG, SOUTH CAROLINA COUNTY WARNING AREA (1948-2006) Justin D. Lane* NOAA/National Weather Service Greer, South Carolina 1. Introduction Based on these results, a region-specific climatology would be beneficial to Numerous climatological studies of forecasters in the southeast United States in soundings and sounding-derived parameters order to identify environments that may be associated with supercells and significant conducive to ST development. This study tornadoes (ST), defined as those rated F2 to will present a climatology of soundings and F5 on the Fujita Scale, exist in the sounding parameters associated with ST in meteorological literature (e.g., Rasmussen the Greenville-Spartanburg, SC (GSP) and Blanchard 1998; Rasmussen 2003; County Warning Area (CWA). Thompson et al. 2003). However, most of these studies have focused on events Section 2 contains the methodology and an occurring in the central portion of the United explanation of the various data sources States. The results of these studies used to create this climatology. Section 3 generally agree that supercell thunderstorms presents several composites of reanalysis and tornadoes typically require moderate to soundings associated with ST occurrence. large levels of instability and high values of Section 4 details the results of a statistical wind shear. However, experienced analysis of various parameters yielded by forecasters in the eastern United States can soundings that were constructed from attest to the fact that this combination is reanalysis data. The paper concludes with a extremely rare. This implies that supercells, discussion of the results in section 5. -
Extratropical Storms of the Gulf of Mexico and Their Ffece Ts Along the Northern Coast of a Barrier Island: West Ship Island, Mississippi
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1999 Extratropical Storms of the Gulf of Mexico and Their ffecE ts Along the Northern Coast of a Barrier Island: West Ship Island, Mississippi. Phillip Lynn Chaney Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Chaney, Phillip Lynn, "Extratropical Storms of the Gulf of Mexico and Their Effects Along the Northern Coast of a Barrier Island: West Ship Island, Mississippi." (1999). LSU Historical Dissertations and Theses. 6884. https://digitalcommons.lsu.edu/gradschool_disstheses/6884 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type o f computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. -
Copyrighted Material
Contents at a Glance Introduction. .1 Part 1: What in the World Is Weather?. 7 CHAPTER 1: Forecasts and Forecasting. .9 CHAPTER 2: Behind the Air Wars. .37 CHAPTER 3: Land, Sea, and Precipitation: Is This Any Way to Run a Planet?. 61 Part 2: Braving the Elements. 79 CHAPTER 4: Blowing in the Winds. 81 CHAPTER 5: Getting Cirrus. 103 CHAPTER 6: Climate Is What You Expect; Weather Is What You Get. 125 CHAPTER 7: The Greatest Storms On Earth. .147 Part 3: Some Seasonable Explanations. .169 CHAPTER 8: The Ways of Winter. .171 CHAPTER 9: Twists and Turns of Spring. 201 CHAPTER 10: Extremely Summer. .233 CHAPTER 11: Falling for Autumn . .255 Part 4: The Special Effects. .263 CHAPTER 12: Taking Care of the Air. .265 CHAPTER 13: Up in the Sky! Look! . 285 CHAPTER 14: Try This at Home. .301 Part 5: The Part of Tens. 315 CHAPTER 15: Ten (or So) Biggest U.S. Weather Disasters of the 20th Century . 317 CHAPTER 16: Ten (or So) Worst World Weather Disasters of the 20th Century. 325 CHAPTER 17: Ten Crafty Critters. 331 CHAPTER 18: Ten Grand Old Weather Proverbs. 337 Appendix:COPYRIGHTED Internet Resource MATERIAL Directory. 343 Index. 351 02_9781119806776-ftoc.indd iii Trim size: 7.375 in × 9.25 in December 11, 2020 2:18 PM 02_9781119806776-ftoc.indd iv Trim size: 7.375 in × 9.25 in December 11, 2020 2:18 PM Table of Contents INTRODUCTION ...................................................1 About This Book ...............................................1 Foolish Assumptions ...........................................2 How This Book Is Organized ....................................2 Part 1: What in the World Is Weather?.