The Southern Plains Cyclone
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Hurricane Knowledge
Hurricane Knowledge Storm conditions can vary on the intensity, size and even the angle which the tropical cyclone approaches your area, so it is vital you understand what the forecasters and news reporters are telling you. Tropical Depressions are cyclones with winds of 38 mph. Tropical Storms vary in wind speeds from 39-73 mph while Hurricanes have winds 74 mph and greater. Typically, the upper right quadrant of the storm (the center wrapping around the eye) is the most intense portion of the storm. The greatest threats are damaging winds, storm surge and flooding. This is in part why Hurricane Katrina was so catastrophic when bringing up to 28-foot storm surges onto the Louisiana and Mississippi coastlines. A Tropical Storm Watch is when tropical storm conditions are possible in the area. A Hurricane Watch is when hurricane conditions are possible in the area. Watches are issued 48 hours in advance of the anticipated onset of tropical storm force winds. A Tropical Storm Warning is when tropical storm conditions are expected in the area. A Hurricane Warning is when hurricane conditions are expected in the area. Warnings are issued 36 hours in advance of tropical storm force winds. Here are a few more terms used when discussing hurricanes: Eye: Clear, sometimes well-defined center of the storm with calmer conditions. Eye Wall: Surrounding the eye, contains some of the most severe weather of the storm with the highest wind speed and largest precipitation. Rain Bands: Bands coming off the cyclone that produce severe weather conditions such as heavy rain, wind and tornadoes. -
Severe Thunderstorms and Tornadoes Toolkit
SEVERE THUNDERSTORMS AND TORNADOES TOOLKIT A planning guide for public health and emergency response professionals WISCONSIN CLIMATE AND HEALTH PROGRAM Bureau of Environmental and Occupational Health dhs.wisconsin.gov/climate | SEPTEMBER 2016 | [email protected] State of Wisconsin | Department of Health Services | Division of Public Health | P-01037 (Rev. 09/2016) 1 CONTENTS Introduction Definitions Guides Guide 1: Tornado Categories Guide 2: Recognizing Tornadoes Guide 3: Planning for Severe Storms Guide 4: Staying Safe in a Tornado Guide 5: Staying Safe in a Thunderstorm Guide 6: Lightning Safety Guide 7: After a Severe Storm or Tornado Guide 8: Straight-Line Winds Safety Guide 9: Talking Points Guide 10: Message Maps Appendices Appendix A: References Appendix B: Additional Resources ACKNOWLEDGEMENTS The Wisconsin Severe Thunderstorms and Tornadoes Toolkit was made possible through funding from cooperative agreement 5UE1/EH001043-02 from the Centers for Disease Control and Prevention (CDC) and the commitment of many individuals at the Wisconsin Department of Health Services (DHS), Bureau of Environmental and Occupational Health (BEOH), who contributed their valuable time and knowledge to its development. Special thanks to: Jeffrey Phillips, RS, Director of the Bureau of Environmental and Occupational Health, DHS Megan Christenson, MS,MPH, Epidemiologist, DHS Stephanie Krueger, Public Health Associate, CDC/ DHS Margaret Thelen, BRACE LTE Angelina Hansen, BRACE LTE For more information, please contact: Colleen Moran, MS, MPH Climate and Health Program Manager Bureau of Environmental and Occupational Health 1 W. Wilson St., Room 150 Madison, WI 53703 [email protected] 608-266-6761 2 INTRODUCTION Purpose The purpose of the Wisconsin Severe Thunderstorms and Tornadoes Toolkit is to provide information to local governments, health departments, and citizens in Wisconsin about preparing for and responding to severe storm events, including tornadoes. -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Severe Weather/Tornado Response Procedure, # EP-08-002
UNIVERSITY OF TOLEDO SUBJECT: CODE GRAY Procedure No: EP-08-002 SEVERE STORM/TORNADO RESPONSE PROCEDURE PROCEDURE STATEMENT Clear, specific procedures shall be implemented to protect patients, staff, students, and visitors in the case of a severe storm and/or a tornado watch or warning. PURPOSE OF PROCEDURE To provide guidelines for actions to be taken in the event of a tornado watch and/or tornado warning. Definitions Tornado Watch as defined by the National Weather Service – defines an area where tornadoes are possible in the next several hours. In a watch you need to be alert and be prepared to go to safe shelter if tornadoes do happen or a warning is issued. Tornado Warning as defined by the National Weather Service – a tornado has been spotted or that Doppler radar indicates a thunderstorm circulation which can spawn a tornado. When a tornado warning is issued for your town or county take immediate safety precautions. PROCEDURE Switchboard The University Police dispatcher shall monitor the CAD system and the weather alert channels located in the dispatch offices. In the case where a tornado watch/warning has been issued or verified information has been received that a tornado has been sighted, the dispatcher shall notify the following: The switchboard operator on the Health Science Campus (HSC), who will issue a HSC campus-wide mass notification to all HSC buildings. The switchboard operators will also call the HSC departments or buildings listed below. The MC dispatcher shall also notify all police officers on duty of the tornado warning. Early Learning Center .................................................. 419-530-6710 Code Gray Watch or Warning shall be announced and cancelled based on information from the National Weather Service (via weather radio). -
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. -
P1.4 West Texas Mesonet Observations of Wake Lows and Heat Bursts Across Northwest Texas
P1.4 WEST TEXAS MESONET OBSERVATIONS OF WAKE LOWS AND HEAT BURSTS ACROSS NORTHWEST TEXAS Mark R. Conder*, Steven R. Cobb, and Gary D. Skwira National Weather Service Forecast Office, Lubbock, Texas 1. INTRODUCTION Wake lows (WLs) and heat bursts (HBs) are mesoscale phenomena associated with thunderstorms that can result in strong and sometimes severe (>25.5 m s-1), near-surface winds. The operational detection of severe winds is problematic because the associated convection can appear quite innocuous via WSR-88D data. The thermodynamic environment that supports WL and HB development is similar, and is often compared to the classic “onion” sounding structure as described by Zipser (1977). Observational studies such as Johnson et al. (1989) show that nearly dry-adiabatic lapse rates are prevalent in the lower to mid-troposphere, with a shallow stable layer near ground level. This type of environment is most commonly observed in the high plains during the warm season. While documented heat bursts were infrequent in the past, the recent expansion of surface mesonetworks are increasing the likelihood that these events will be sampled. One such network is the West Texas Mesonet (WTXM), a collection of over 40 meteorological stations spread across the Panhandle and South Plains of northwest Texas. During the period 1 June 2004 to 30 August 2006, the authors have FIG. 1. The Study area including the WTXM station recorded 10 WL/HB events that have been sampled by locations. Not all stations were available for every stations of the WTXM. Some of the more extreme event. measurements include a 15 degrees Celsius increase in temperature at the Pampa and McClean WTXM sites in -1 Meteorological data from each WTXM station is one event and 35 m s wind gusts at sites in Brownfield recorded in 5-minute intervals, representing average and Jayton on separate occasions. -
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). -
Hurricane Preparedness Guide (PDF)
hurricanes... Unleashing Nature’s Fury FEMA Hurricane Floyd, 1999/NOAA A PREPAREDNESS GUIDE U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Weather Service Revised August 2001 What is a Hurricane? The term hurricane has its origin in the indigenous religions of old civilizations. The Mayan storm god A hurricane is a type of tropical cyclone–an organized was named Hunraken. A god considered evil by rotating weather system that develops in the tropics. the Taino people of the Caribbean was called Huracan. Hurricanes rotate counterclockwise in the Northern Hurricanes may not be considered evil but they Hemisphere. Tropical cyclones are classified as follows: are one of nature’s most powerful storms. Their ■ Tropical Depression—An organized system of potential for loss of life and destruction of property persistent clouds and thunderstorms with a closed is tremendous. Those in hurricane-prone areas low-level circulation and maximum sustained winds need to be of 38 mph (33 knots) or less. prepared for hurricanes and ■ Tropical Storm—An organized system of strong tropical storms. thunderstorms with a well defined circulation and Even inland areas, maximum sustained winds of 39 to 73 mph well away from (34-63 knots). the coastline, ■ Hurricane—An intense tropical weather system can experience with a well defined circulation and sustained winds destructive winds, of 74 mph (64 knots) or higher. In the western North tornadoes and Pacific, hurricanes are called typhoons, and similar floods from storms in the Indian Ocean are called cyclones. tropical storms and hurricanes. Hurricane Iniki/NOAA 1998 Atlantic Ocean Hurricane Season Summary/NOAA 2 Tropical depressions and tropical storms, while generally less dangerous than hurricanes, still can be deadly. -
Severe Weather Preparedness Guide to Help Educate and Better Prepare Illinois Residents for All Hazards
1 Severe Weather Preparedness Severe weather can happen at any time of the year. Preparing for floods, tornadoes and severe thunderstorms before they strike will help you stay safe throughout the year. To help people better prepare for weather emergencies, the Illinois Emergency Management Agency and the National Weather Service developed this Severe Weather Preparedness Guide to help educate and better prepare Illinois residents for all hazards. Every year in the United States, hundreds of people are killed and thousands injured because of the weather. Dangerous weather can take make forms, ranging from violent tornadoes to crippling winter storms. While there is nothing we can do to stop dangerous weather from affecting us, there are things we can do to stay safe when the sky turns grey. Weather safety and survival – no matter the hazard – depends on the following key items: Know the Hazards – Be aware of the hazards that exist where you live. Know When to Expect Dangerous Weather – Monitor forecasts and information from your local National Weather Service, and always have more than one way to receive emergency alerts and notifications. Be Alert and Ready – Be aware of issued watches, warnings and advisories. Know what protective actions to take during each level of notification. Have a Plan to Stay Safe – Make sure that each member of your family knows what protective actions to take during each level of notification. The information in this guide will help you learn more about the dangers of floods, tornadoes, severe thunderstorms and lightning. Use the tips provided to prepare yourself and your family before severe storms impact Illinois again. -
Summer Weather Safety Know Your Risk Take Action Be a Force of Nature Summer Weather Safety Summer Weather Hazards
Summer Weather Safety Know Your Risk Take Action Be a Force of Nature Summer Weather Safety Summer Weather Hazards • Tornadoes, Thunderstorms, and Lightning • Flooding • Heat • Hurricanes • Rip Currents, Dangerous Waves • Wildfire and Air Quality • Drought © John Wetter weather.gov/safety Summer Weather Safety Severe Weather • Thunderstorms can produce tornadoes, strong wind, large hail, and lightning • Practice a severe weather plan for home and work • Make a communications plan so you can contact loved ones weather.gov/safety Summer Weather Safety Tornadoes • Winds from tornadoes can exceed 200 mph • Flying debris is most dangerous • Seek a sturdy shelter in an interior room away from windows on the lowest floor and cover your head weather.gov/safety Summer Weather Safety NWS Tornado Products weather.gov/safety Summer Weather Safety Thunderstorms • Severe thunderstorms produce strong wind and/or large hail • Take shelter in a sturdy structure away from windows • A vehicle is also a safe location when there is no other nearby shelter © Kevin Skow weather.gov/safety Summer Weather Safety Thunderstorms • Conditions can change rapidly with thunderstorms nearby or overhead • Don’t second-guess how a thunderstorm will evolve • Take shelter before the storm and remain there through an all-clear signal from the NWS weather.gov/safety Summer Weather Safety Thunderstorms • Strong wind gusts from thunderstorms can create dust storms • Dust storms can reduce visibility and make travel difficult • If travelling, prepare to reduce speed and pull over -
The Impact of Unique Meteorological Phenomena Detected by the Oklahoma Mesonet and ARS Micronet on Automated Quality Control Christopher A
The Impact of Unique Meteorological Phenomena Detected by the Oklahoma Mesonet and ARS Micronet on Automated Quality Control Christopher A. Fiebrich and Kenneth C. Crawford Oklahoma Climatological Survey, Norman, Oklahoma ABSTRACT To ensure quality data from a meteorological observing network, a well-designed quality control system is vital. Automated quality assurance (QA) software developed by the Oklahoma Mesonetwork (Mesonet) provides an effi- cient means to sift through over 500 000 observations ingested daily from the Mesonet and from a Micronet spon- sored by the Agricultural Research Service of the United States Department of Agriculture (USDA). However, some of nature's most interesting meteorological phenomena produce data that fail many automated QA tests. This means perfectly good observations are flagged as erroneous. Cold air pooling, "inversion poking," mesohighs, mesolows, heat bursts, variations in snowfall and snow cover, and microclimatic effects produced by variations in vegetation are meteorological phenomena that pose a problem for the Mesonet's automated QA tests. Despite the fact that the QA software has been engineered for most observa- tions of real meteorological phenomena to pass the various tests—but is stringent enough to catch malfunctioning sensors—erroneous flags are often placed on data during extreme events. This manuscript describes how the Mesonet's automated QA tests responded to data captured from microscale meteorological events that, in turn, were flagged as erroneous by the tests. The Mesonet's operational plan is to cata- log these extreme events in a database so QA flags can be changed manually by expert eyes. 1. Introduction and personnel at the central processing site for the Oklahoma Mesonet in Norman, Oklahoma. -
EXTREME WEATHER EVENTS and CROP PRICE SPIKES in a CHANGING CLIMATE Illustrative Global Simulation Scenarios
OXFAM RESEARCH REPORTS SEPTEMBER 2012 EXTREME WEATHER EVENTS AND CROP PRICE SPIKES IN A CHANGING CLIMATE Illustrative global simulation scenarios DIRK WILLENBOCKEL INSTITUTE OF DEVELOPMENT STUDIES, UNIVERSITY OF SUSSEX, UK Agriculture is highly sensitive to climate variability and weather extremes. Various impact studies have considered the effects on global food production and prices of projected long-run trends in temperature, precipitation and CO2 concentrations caused by climate change. But an area that remains underexplored is the impact on food prices that may result from an expected increase in the frequency and intensity of extreme weather events. This study uses a global dynamic multi-region computable general equilibrium (CGE) model to explore the potential impacts on food prices of a number of extreme weather event scenarios in 2030 for each of the main exporting regions for rice, maize, and wheat. Oxfam Research Reports are written to share research results, to contribute to public debate and to invite feedback on development and humanitarian policy and practice. They do not necessarily reflect Oxfam policy positions. The views expressed are those of the author and not necessarily those of Oxfam. www.oxfam.org CONTENTS 1 Introduction 4 2 Climate change and extreme weather events: A brief review of the current state of science 6 3 Methodology of the simulation analysis 15 4 The simulation scenarios 17 5 Simulation analysis 22 Appendices 40 2 Extreme Weather Events and Crop Price Spikes in a Changing Climate ABBREVIATIONS CO2