Tornadic Waterspouts Impacts on Coastal Australia
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A Study of Synoptic-Scale Tornado Regimes
Garner, J. M., 2013: A study of synoptic-scale tornado regimes. Electronic J. Severe Storms Meteor., 8 (3), 1–25. A Study of Synoptic-Scale Tornado Regimes JONATHAN M. GARNER NOAA/NWS/Storm Prediction Center, Norman, OK (Submitted 21 November 2012; in final form 06 August 2013) ABSTRACT The significant tornado parameter (STP) has been used by severe-thunderstorm forecasters since 2003 to identify environments favoring development of strong to violent tornadoes. The STP and its individual components of mixed-layer (ML) CAPE, 0–6-km bulk wind difference (BWD), 0–1-km storm-relative helicity (SRH), and ML lifted condensation level (LCL) have been calculated here using archived surface objective analysis data, and then examined during the period 2003−2010 over the central and eastern United States. These components then were compared and contrasted in order to distinguish between environmental characteristics analyzed for three different synoptic-cyclone regimes that produced significantly tornadic supercells: cold fronts, warm fronts, and drylines. Results show that MLCAPE contributes strongly to the dryline significant-tornado environment, while it was less pronounced in cold- frontal significant-tornado regimes. The 0–6-km BWD was found to contribute equally to all three significant tornado regimes, while 0–1-km SRH more strongly contributed to the cold-frontal significant- tornado environment than for the warm-frontal and dryline regimes. –––––––––––––––––––––––– 1. Background and motivation As detailed in Hobbs et al. (1996), synoptic- scale cyclones that foster tornado development Parameter-based and pattern-recognition evolve with time as they emerge over the central forecast techniques have been essential and eastern contiguous United States (hereafter, components of anticipating tornadoes in the CONUS). -
Employing the WSR-88D for Waterspout Forecasting
Employing the WSR-88D for Waterspout Forecasting Scott M. Spratt LT (jg) Barry K. Choy, NOAA Corps National Weather Service Melbourne, Florida 1. Introduction Waterspouts and weak coastal tornadoes or "landspouts" (hereafter referred to collectively as "spouts") account for much of Florida's severe weather during the "wet season" (Schmocker et al. 1990). The Melbourne NEXRAD Weather Service Office (NWSO) County Warning Area (CWA) includes 160 miles of coastline along the east central Florida peninsula. Within this area, spouts are most frequent from June through September (Fig. 1). In the past, warnings were issued for spouts only after reports of visual sightings were received. This delay was likely due to the seemingly benign atmospheric conditions in which spouts develop, combined with a lack of pronounced severe weather signatures on conventional radars. However, recent research utilizing the NWSO MLB WSR- 88D may now help forecasters warn for spouts prior to receiving visual reports. A preliminary forecast strategy was developed based on post analyses of archived WSR- 88D products and regional upper-air data from reported spout days (Choy and Spratt 1994). This strategy has proved useful by providing additional lead time for spout events. This paper will identify specific atmospheric conditions which have been observed to precede spout generations along the east central Florida coast. A unique WSR-88D Routine Product Set (RPS) list will be shown which can be implemented once these conditions become satisfied. Finally, case studies of two recent events will be illustrated to help familiarize WSR-88D users with the environmental conditions and radar signatures often evident prior to and during spout events. -
Meteorology – Lecture 19
Meteorology – Lecture 19 Robert Fovell [email protected] 1 Important notes • These slides show some figures and videos prepared by Robert G. Fovell (RGF) for his “Meteorology” course, published by The Great Courses (TGC). Unless otherwise identified, they were created by RGF. • In some cases, the figures employed in the course video are different from what I present here, but these were the figures I provided to TGC at the time the course was taped. • These figures are intended to supplement the videos, in order to facilitate understanding of the concepts discussed in the course. These slide shows cannot, and are not intended to, replace the course itself and are not expected to be understandable in isolation. • Accordingly, these presentations do not represent a summary of each lecture, and neither do they contain each lecture’s full content. 2 Animations linked in the PowerPoint version of these slides may also be found here: http://people.atmos.ucla.edu/fovell/meteo/ 3 Mesoscale convective systems (MCSs) and drylines 4 This map shows a dryline that formed in Texas during April 2000. The dryline is indicated by unfilled half-circles in orange, pointing at the more moist air. We see little T contrast but very large TD change. Dew points drop from 68F to 29F -- huge decrease in humidity 5 Animation 6 Supercell thunderstorms 7 The secret ingredient for supercells is large amounts of vertical wind shear. CAPE is necessary but sufficient shear is essential. It is shear that makes the difference between an ordinary multicellular thunderstorm and the rotating supercell. The shear implies rotation. -
Seasonal Buyer's Guide
Seasonal Buyer’s Guide. Appendix New South Wales Suburb table - May 2017 Westpac, National suburb level appendix Copyright Notice Copyright © 2017CoreLogic Ownership of copyright We own the copyright in: (a) this Report; and (b) the material in this Report Copyright licence We grant to you a worldwide, non-exclusive, royalty-free, revocable licence to: (a) download this Report from the website on a computer or mobile device via a web browser; (b) copy and store this Report for your own use; and (c) print pages from this Report for your own use. We do not grant you any other rights in relation to this Report or the material on this website. In other words, all other rights are reserved. For the avoidance of doubt, you must not adapt, edit, change, transform, publish, republish, distribute, redistribute, broadcast, rebroadcast, or show or play in public this website or the material on this website (in any form or media) without our prior written permission. Permissions You may request permission to use the copyright materials in this Report by writing to the Company Secretary, Level 21, 2 Market Street, Sydney, NSW 2000. Enforcement of copyright We take the protection of our copyright very seriously. If we discover that you have used our copyright materials in contravention of the licence above, we may bring legal proceedings against you, seeking monetary damages and/or an injunction to stop you using those materials. You could also be ordered to pay legal costs. If you become aware of any use of our copyright materials that contravenes or may contravene the licence above, please report this in writing to the Company Secretary, Level 21, 2 Market Street, Sydney NSW 2000. -
Central Region Technical Attachment 95-08 Examination of an Apparent
CRH SSD APRIL 1995 CENTRAL REGION TECHNICAL ATTACHMENT 95-08 EXAMINATION OF AN APPARENT LANDSPOUT IN THE EASTERN BLACK HILLS OF WESTERN SOUTH DAKOTA David L. Hintz1 and Matthew J. Bunkers National Weather Service Office Rapid City, South Dakota 1. Abstract On June 29, 1994, an apparent landspout occurred in the Black Hills of South Dakota. This landspout exhibited most of the features characteristic of traditional landspouts documented in eastern Colorado. The landspout lasted 3 to 8 minutes, had a width of less than 20 m and a path of 1 to 3 km, produced estimated wind speeds of Fl intensity (33 to 50 m s1), and emanated from a towering cumulus (TCU) cloud located along a quasi-stationary convergencq/cyclonic shear zone. No radar echo was observed with this event; however, a supercell thunderstorm was located 80-100 km to the east. National Weather Service meteorologists surveyed the “very localized” damage area and ruled out the possibility of the landspout being related to microburst, gustnado, or dust devil activity, as winds away from the landspout were less than 3 m s1. The landspout apparently “detached” from the parent TCU and damaged a farm which resulted in $1,000 dollars in expenses. 2. Introduction During the late 1980’s and early 1990’s researchers documented a phe nomenon with subtle differences from traditional tornadoes and waterspouts, herein referred to as the landspout (Seargent 1994; Brady and Szoke 1988, 1989; Bluestein 1985). The term “landspout” was actually coined by Bluestein (I985)(in the formal literature) when he observed this type of vortex along an Oklahoma squall line. -
Severe Weather Forecasting Tip Sheet: WFO Louisville
Severe Weather Forecasting Tip Sheet: WFO Louisville Vertical Wind Shear & SRH Tornadic Supercells 0-6 km bulk shear > 40 kts – supercells Unstable warm sector air mass, with well-defined warm and cold fronts (i.e., strong extratropical cyclone) 0-6 km bulk shear 20-35 kts – organized multicells Strong mid and upper-level jet observed to dive southward into upper-level shortwave trough, then 0-6 km bulk shear < 10-20 kts – disorganized multicells rapidly exit the trough and cross into the warm sector air mass. 0-8 km bulk shear > 52 kts – long-lived supercells Pronounced upper-level divergence occurs on the nose and exit region of the jet. 0-3 km bulk shear > 30-40 kts – bowing thunderstorms A low-level jet forms in response to upper-level jet, which increases northward flux of moisture. SRH Intense northwest-southwest upper-level flow/strong southerly low-level flow creates a wind profile which 0-3 km SRH > 150 m2 s-2 = updraft rotation becomes more likely 2 -2 is very conducive for supercell development. Storms often exhibit rapid development along cold front, 0-3 km SRH > 300-400 m s = rotating updrafts and supercell development likely dryline, or pre-frontal convergence axis, and then move east into warm sector. BOTH 2 -2 Most intense tornadic supercells often occur in close proximity to where upper-level jet intersects low- 0-6 km shear < 35 kts with 0-3 km SRH > 150 m s – brief rotation but not persistent level jet, although tornadic supercells can occur north and south of upper jet as well. -
Sydney for Dogs Pdf, Epub, Ebook
SYDNEY FOR DOGS PDF, EPUB, EBOOK Cathy Proctor | 234 pages | 20 Jun 2017 | Woodslane Pty Ltd | 9781925403541 | English | Mona Vale, Australia Sydney for Dogs PDF Book While dogs are permitted off-leash on the beach and in the water all day long on weekdays, come Saturdays, Sundays and Public Holidays they are only permitted before 9am and after 4pm. No wonder people drive here with their pup from all over Sydney! You can find more info on their website and download a map of the doggy designated areas here. Find out more about a dog-friendly getaway to Forster-Tuncurry. Access is from Foreshore Road, look for the signs for the boat ramp, where there is a large carpark. My Account My Profile Sign out. The wonders of a farm in the heart of a beautiful valley. While dogs are also meant to stay on leash on this beach, dogs are often let off leash, including when I visited. Starting from outside the Manly Beach Lifesaving Club, the walk leads you along the coast, past an assortment of unique sculptures and the historic Fairy Bower Pool. The largest dog-friendly park in Sydney, almost half of this huge park in Sydney is off-leash. The off-leash dog section is located adjacent to the Bonna Point Reserve carpark, in between the third and fourth rock groynes. As the name suggests, the Banksia track is brimming with beautiful native Australian wildflowers and banksias. The best time to visit this dog beach is during the cooler months of the year. Find out more about a dog-friendly getaway to Orange. -
Short-Term Forecasts of Left-Moving Supercells from an Experimental Warn-On-Forecast System
Jones, T. A., and C. Nixon, 2017: Short-term forecasts of left-moving supercells from an experimental Warn-on-Forecast system. J. Operational Meteor., 5 (13), 161-170, doi: https://doi.org/10.15191/nwajom.2017.0513 Short-term Forecasts of Left-Moving Supercells from an Experimental Warn-on-Forecast System THOMAS A. JONES Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, Norman, Oklahoma CAMERON NIXON Texas Tech University, Lubbock, Texas (Manuscript received 10 March 2017; review completed 23 June 2017) ABSTRACT Most research in storm-scale numerical weather prediction has been focused on right-moving supercells as they typically lend themselves to all forms of high-impact weather, including tornadoes. As the dynamics behind splitting updrafts and storm motion have become better understood, differentiating between atmospheric conditions that encourage right- and left-moving supercells has become the subject of increasing study because of its implication for these weather forecasts. Despite still often producing large hail and damaging winds, left- moving (anticyclonically rotating in the Northern Hemisphere) supercells have received much less attention. During the 2016, NOAA Hazardous Weather Testbed, the NSSL Experimental Warn-on-Forecast System for ensembles (NEWS-e) was run in real-time. One event in particular occurred on 8 May 2016 during which multiple left- and right- moving supercells developed in western Oklahoma and Kansas—producing many severe weather reports. The goal of this study was to analyze the near storm environment created by NEWS-e using wind shear and other severe weather parameters. Then, we sought to determine the ability of the NEWS-e system to forecast storm splits and the persistence of left- and right- moving supercells through qualitatively analyzing tracks of forecast updraft helicity. -
Mesoscale Organization of Convection
MesoscaleMesoscale OrganizationOrganization ofof ConvectionConvection SquallSquall LineLine • Is a set of individual intense thunderstorm cells arranged in a line. • Thy occur along a boundary of unstable air – e.g. a cold front. • Strong environmental wind shear causes the updraft to be tilted and separated from the downdraft. • The dense cold air of the downdraft forms a ‘gust front’. SquallSquall lineline fromfrom SpaceSpace Image courtesy of http://cnls.lanl.gov. This image has been removed due to copyright restrictions. Please see: http://www.floridalightning.com/Hurricane_Wilma.html This image has been removed due to copyright restrictions. Please see similar images on: http://www.bom.gov.au/wa/sevwx/ MesoscaleMesoscale ConvectiveConvective ComplexComplex • A Mesoscale Convective Complex is composed of multiple single-cell storms in different stages of development. • The individual thunderstorms must support the formation of other convective cells • In order to last a long time, a good supply of moisture is required at low levels in te atmosphere. InfraredInfrared imageimage ofof aa mesoscalemesoscale convectiveconvective complexcomplex overover Kansas,Kansas, JulyJuly 88 1997.1997. This image has been removed due to copyright restrictions. Please see similar images on: http://cimss.ssec.wisc.edu/goes/misc/970708.html TYPESTYPES OFOF THUNDERSTORMTHUNDERSTORM • SINGLE-CELL THUNDERSTORM • MULTICELL THUNDERSTORM • MESOSCALE CONVECTIVE C0MPLEX • SUPERCELL THUNDERSTORM Non-equilibrium Convection SUPERCELLSUPERCELL THUNDERSTORMSTHUNDERSTORMS • SINGLE CELL THUNDERSTORM THAT PRODUCES DANGEROUS WEATHER • REQUIRES A VERY UNSTABLE ATMOSPHERE AND STRONG VERTICAL WIND SHEAR - BOTH SPEED AND DIRECTION • UNDER THE INFLUENCE OF THE STRONG WIND SHEAR MUCH OF THE THUNDERSTORM ROTATES • FAVORED IN THE SOUTHERN GREAT PLAINS IN THE SPRING WindWind ShearShear Shear Vector Hodograph This image has been removed due to copyright restrictions. -
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. -
A WSR-88D Approach to Waterspout Forecasting
A WSR-88D Approach to Waterspout Forecasting LT(jg) Barry K. Choy, NOAA Corps and Scott M. Spratt National Weather Service Office Melbourne, FL Abstract The WSR-88D is being installed at National Weather Service (NWS) forecast and warning offices and many military installations across the county. The added capabilities of the WSR-88D over conventional radar provides the forecaster a multitude of products which allow a more complete interrogation of small scale weather features. In Florida, waterspouts and weak tornadoes account for much of the state's severe weather. They have been observed to form under certain synoptic conditions, most often during the summer and fall. Along the east-central Florida coast, waterspouts and weak tornadoes are most frequent in a relatively small area near Cape Canaveral. Observing and identifying small scale boundary interactions and the intensification of convective cells in this region using WSR-88D products from the Melbourne NWS office has proven useful in forecasting these situations. This paper will begin by providing a brief overview of the waterspout formation process. It also offers a forecast strategy developed for the east central Florida coast using specific WSR-88D products to recognize precursor signatures to waterspout and weak tornado formation. Once a high potential for waterspout formation exists, a special statement can be issued to heighten public awareness. An example of such a statement is provided. While the techniques introduced here were designed for the east-central Florida coast, they may be applicable at other coastal offices equipped with the WSR-88D. 1. Introduction The east-central Florida coast is affected by several waterspouts and tornadoes each year. -
Chapter 3 Mesoscale Processes and Severe Convective Weather
CHAPTER 3 JOHNSON AND MAPES Chapter 3 Mesoscale Processes and Severe Convective Weather RICHARD H. JOHNSON Department of Atmospheric Science. Colorado State University, Fort Collins, Colorado BRIAN E. MAPES CIRESICDC, University of Colorado, Boulder, Colorado REVIEW PANEL: David B. Parsons (Chair), K. Emanuel, J. M. Fritsch, M. Weisman, D.-L. Zhang 3.1. Introduction tion, mesoscale phenomena occur on horizontal scales between ten and several hundred kilometers. This Severe convective weather events-tornadoes, hail range generally encompasses motions for which both storms, high winds, flash floods-are inherently mesoscale ageostrophic advections and Coriolis effects are im phenomena. While the large-scale flow establishes envi portant (Emanuel 1986). In general, we apply such a ronmental conditions favorable for severe weather, pro definition here; however, strict application is difficult cesses on the mesoscale initiate such storms, affect their since so many mesoscale phenomena are "multiscale." evolution, and influence their environment. A rich variety For example, a -100-km-Iong gust front can be less of mesocale processes are involved in severe weather, than -1 km across. The triggering of a storm by the ranging from environmental preconditioning to storm initi collision of gust fronts can actually occur on a ation to feedback of convection on the environment. In the -lOO-m scale (the microscale). Nevertheless, we will space available, it is not possible to treat all of these treat this overall process (and others similar to it) as processes in detail. Rather, we will introduce s~veral mesoscale since gust fronts are generally regarded as general classifications of mesoscale processes relatmg to mesoscale phenomena.