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Storm Data Publication
FEBRUARY 2008 VOLUME 50 SSTORMTORM DDATAATA NUMBER 2 AND UNUSUAL WEATHER PHENOMENA WITH LATE REPORTS AND CORRECTIONS NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION noaa NATIONAL ENVIRONMENTAL SATELLITE, DATA AND INFORMATION SERVICE NATIONAL CLIMATIC DATA CENTER, ASHEVILLE, NC Cover: This cover represents a few weather conditions such as snow, hurricanes, tornadoes, heavy rain and flooding that may occur in any given location any month of the year. (Photos courtesy of NCDC) TABLE OF CONTENTS Page Outstanding Storm of the Month …..…………….….........……..…………..…….…..…..... 4 Storm Data and Unusual Weather Phenomena ....…….…....…………...…...........…............ 5 Reference Notes .............……...........................……….........…..….…............................................ 278 STORM DATA (ISSN 0039-1972) National Climatic Data Center Editor: William Angel Assistant Editors: Stuart Hinson and Rhonda Herndon STORM DATA is prepared, and distributed by the National Climatic Data Center (NCDC), National Environmental Satellite, Data and Information Service (NESDIS), National Oceanic and Atmospheric Administration (NOAA). The Storm Data and Unusual Weather Phenomena narratives and Hurricane/Tropical Storm summaries are prepared by the National Weather Service. Monthly and annual statistics and summaries of tornado and lightning events re- sulting in deaths, injuries, and damage are compiled by the National Climatic Data Center and the National Weather Service’s (NWS) Storm Prediction Center. STORM DATA contains all confi rmed information on storms available to our staff at the time of publication. Late reports and corrections will be printed in each edition. Except for limited editing to correct grammatical errors, the data in Storm Data are published as received. Note: “None Reported” means that no severe weather occurred and “Not Received” means that no reports were received for this region at the time of printing. -
…Top 10 Weather Events of 2012…
…Top 10 weather events of 2012… In terms of severe weather, 2012 started out fast and furious, and then petered out by late March. 1) By anyone’s measure, the tornado outbreak on the 2nd of March must qualify as our top event of 2012. The 49 mile long EF-4 tornado that tracked across southern Indiana became the first EF-4 in our forecast area since the northern Bullitt County tornado on May 28, 1996. Seven other tornadoes also developed on March 2, with 3 confirmed tornadoes in Trimble County alone. The image to the left shows two supercells following similar paths across southern Indiana. The first cell was producing an EF-4 tornado at this time. The second storm later brought softball sized hail and an EF-1 tornado just south of Henryville. Also, excessively large hail fell across both southern Indiana and south central Kentucky. Outside of several reports of softball-sized hail near Henryville, Indiana, associated with the second of two supercells that tracked over nearly the same path, our most damaging hailstorm developed across southwestern Adair County. This storm produced a hail swath more than 10 miles long, smashing the windshields of hundreds of vehicles before knocking out the skylights of a Walmart store in Columbia. The first picture, courtesy Simon Brewer of The Weather Channel, shows a large tornado in Washington County, IN. The image at left shows hail damage to a golf course near Henryville. 2) The Leap Day tornado outbreak on February 29 featured a squall line that spawned 6 tornadoes across central and south central Kentucky. -
A Winter Forecasting Handbook Winter Storm Information That Is Useful to the Public
A Winter Forecasting Handbook Winter storm information that is useful to the public: 1) The time of onset of dangerous winter weather conditions 2) The time that dangerous winter weather conditions will abate 3) The type of winter weather to be expected: a) Snow b) Sleet c) Freezing rain d) Transitions between these three 7) The intensity of the precipitation 8) The total amount of precipitation that will accumulate 9) The temperatures during the storm (particularly if they are dangerously low) 7) The winds and wind chill temperature (particularly if winds cause blizzard conditions where visibility is reduced). 8) The uncertainty in the forecast. Some problems facing meteorologists: Winter precipitation occurs on the mesoscale The type and intensity of winter precipitation varies over short distances. Forecast products are not well tailored to winter Subtle features, such as variations in the wet bulb temperature, orography, urban heat islands, warm layers aloft, dry layers, small variations in cyclone track, surface temperature, and others all can influence the severity and character of a winter storm event. FORECASTING WINTER WEATHER Important factors: 1. Forcing a) Frontal forcing (at surface and aloft) b) Jetstream forcing c) Location where forcing will occur 2. Quantitative precipitation forecasts from models 3. Thermal structure where forcing and precipitation are expected 4. Moisture distribution in region where forcing and precipitation are expected. 5. Consideration of microphysical processes Forecasting winter precipitation in 0-48 hour time range: You must have a good understanding of the current state of the Atmosphere BEFORE you try to forecast a future state! 1. Examine current data to identify positions of cyclones and anticyclones and the location and types of fronts. -
Soaring Weather
Chapter 16 SOARING WEATHER While horse racing may be the "Sport of Kings," of the craft depends on the weather and the skill soaring may be considered the "King of Sports." of the pilot. Forward thrust comes from gliding Soaring bears the relationship to flying that sailing downward relative to the air the same as thrust bears to power boating. Soaring has made notable is developed in a power-off glide by a conven contributions to meteorology. For example, soar tional aircraft. Therefore, to gain or maintain ing pilots have probed thunderstorms and moun altitude, the soaring pilot must rely on upward tain waves with findings that have made flying motion of the air. safer for all pilots. However, soaring is primarily To a sailplane pilot, "lift" means the rate of recreational. climb he can achieve in an up-current, while "sink" A sailplane must have auxiliary power to be denotes his rate of descent in a downdraft or in come airborne such as a winch, a ground tow, or neutral air. "Zero sink" means that upward cur a tow by a powered aircraft. Once the sailcraft is rents are just strong enough to enable him to hold airborne and the tow cable released, performance altitude but not to climb. Sailplanes are highly 171 r efficient machines; a sink rate of a mere 2 feet per second. There is no point in trying to soar until second provides an airspeed of about 40 knots, and weather conditions favor vertical speeds greater a sink rate of 6 feet per second gives an airspeed than the minimum sink rate of the aircraft. -
Art Directable Tornadoes
ART DIRECTABLE TORNADOES A Thesis by RAVINDRA DWIVEDI Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE May 2011 Major Subject: Visualization Art Directable Tornadoes Copyright 2011 Ravindra Dwivedi ART DIRECTABLE TORNADOES A Thesis by RAVINDRA DWIVEDI Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Approved by: Chair of Committee, Vinod Srinivasan Committee Members, John Keyser Wei Yan Head of Department, Tim McLaughlin May 2011 Major Subject: Visualization iii ABSTRACT Art Directable Tornadoes. (May 2011) Ravindra Dwivedi, B.E., Rajiv Gandhi Proudyogiki Vishwavidyalaya Chair of Advisory Committee: Dr. Vinod Srinivasan Tornado simulations in the visual effects industry have always been an interesting problem. Developing tools to provide more control over such effects is an important and challenging task. Current methods to achieve these effects use either particle systems or fluid simulation. Particle systems give a lot of control over the simulation but do not take into account the fluid characteristics of tornadoes. The other method which involves fluid simulation models the fluid behavior accurately but does not give control over the simulation. In this thesis, a novel method to model tornado behavior is presented. A tool based on this method was also created. The method proposed in this thesis uses a hybrid approach that combines the flexibility of particle systems while producing interesting swirling motions inherent in the fluids. The main focus of the research is on providing easy-to-use controls for art directors to help them achieve the desired look of the simulation effectively. -
Using Analogues to Simulate Intensity, Trajectory, and Dynamical Changes in Alberta Clippers with Global Climate Change
Using Analogues to Simulate Intensity, Trajectory, and Dynamical Changes in Alberta Clippers with Global Climate Change Item Type Thesis Authors Ward, Jamie L. Download date 07/10/2021 05:51:34 Link to Item http://hdl.handle.net/10484/5573 Using Analogues to Simulate Intensity, Trajectory, and Dynamical Changes in Alberta Clippers with Global Climate Change _______________________ A thesis Presented to The College of Graduate and Professional Studies Department of Earth and Environmental Systems Indiana State University Terre Haute, Indiana ______________________ In Partial Fulfillment of the Requirements for the Degree Master of Arts _______________________ by Jamie L. Ward August 2014 Jamie L. Ward, 2014 Keywords: Alberta Clippers, Storm Tracks, Lee Cyclogenesis, Global Climate Change, Atmospheric Analogues ii COMMITTEE MEMBERS Committee Chair: Gregory D. Bierly (Ph.D.) Professor of Geography Indiana State University Committee Member: Stephen Aldrich (Ph.D.) Assistant Professor of Geography Indiana State University Committee Member: Jennifer C. Latimer Associate Professor of Geology Indiana State University iii ABSTRACT Alberta Clippers are extratropical cyclones that form in the lee of the Canadian Rocky Mountains and traverse through the Great Plains and Midwest regions of the United States. With the imminent threat of global climate change and its effects on regional teleconnection patterns like El Niño-Southern Oscillation (ENSO), properties of Alberta Clipper could be altered as a result of changing atmospheric circulation patterns. Since the Great Plains and Midwest regions both support a large portion of the national population and agricultural activity, the effects of global climate change on Alberta Clippers could affect these areas in a variety of ways. -
A Synoptic-Climatology and Composite Analysis of the Alberta Clipper
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HS Science Distance Learning Activities
HS Science (Earth Science/Physics) Distance Learning Activities TULSA PUBLIC SCHOOLS Dear families, These learning packets are filled with grade level activities to keep students engaged in learning at home. We are following the learning routines with language of instruction that students would be engaged in within the classroom setting. We have an amazing diverse language community with over 65 different languages represented across our students and families. If you need assistance in understanding the learning activities or instructions, we recommend using these phone and computer apps listed below. Google Translate • Free language translation app for Android and iPhone • Supports text translations in 103 languages and speech translation (or conversation translations) in 32 languages • Capable of doing camera translation in 38 languages and photo/image translations in 50 languages • Performs translations across apps Microsoft Translator • Free language translation app for iPhone and Android • Supports text translations in 64 languages and speech translation in 21 languages • Supports camera and image translation • Allows translation sharing between apps 3027 SOUTH NEW HAVEN AVENUE | TULSA, OKLAHOMA 74114 918.746.6800 | www.tulsaschools.org TULSA PUBLIC SCHOOLS Queridas familias: Estos paquetes de aprendizaje tienen actividades a nivel de grado para mantener a los estudiantes comprometidos con la educación en casa. Estamos siguiendo las rutinas de aprendizaje con las palabras que se utilizan en el salón de clases. Tenemos una increíble -
Extratropical Cyclones and Anticyclones
© Jones & Bartlett Learning, LLC. NOT FOR SALE OR DISTRIBUTION Courtesy of Jeff Schmaltz, the MODIS Rapid Response Team at NASA GSFC/NASA Extratropical Cyclones 10 and Anticyclones CHAPTER OUTLINE INTRODUCTION A TIME AND PLACE OF TRAGEDY A LiFE CYCLE OF GROWTH AND DEATH DAY 1: BIRTH OF AN EXTRATROPICAL CYCLONE ■■ Typical Extratropical Cyclone Paths DaY 2: WiTH THE FI TZ ■■ Portrait of the Cyclone as a Young Adult ■■ Cyclones and Fronts: On the Ground ■■ Cyclones and Fronts: In the Sky ■■ Back with the Fitz: A Fateful Course Correction ■■ Cyclones and Jet Streams 298 9781284027372_CH10_0298.indd 298 8/10/13 5:00 PM © Jones & Bartlett Learning, LLC. NOT FOR SALE OR DISTRIBUTION Introduction 299 DaY 3: THE MaTURE CYCLONE ■■ Bittersweet Badge of Adulthood: The Occlusion Process ■■ Hurricane West Wind ■■ One of the Worst . ■■ “Nosedive” DaY 4 (AND BEYOND): DEATH ■■ The Cyclone ■■ The Fitzgerald ■■ The Sailors THE EXTRATROPICAL ANTICYCLONE HIGH PRESSURE, HiGH HEAT: THE DEADLY EUROPEAN HEAT WaVE OF 2003 PUTTING IT ALL TOGETHER ■■ Summary ■■ Key Terms ■■ Review Questions ■■ Observation Activities AFTER COMPLETING THIS CHAPTER, YOU SHOULD BE ABLE TO: • Describe the different life-cycle stages in the Norwegian model of the extratropical cyclone, identifying the stages when the cyclone possesses cold, warm, and occluded fronts and life-threatening conditions • Explain the relationship between a surface cyclone and winds at the jet-stream level and how the two interact to intensify the cyclone • Differentiate between extratropical cyclones and anticyclones in terms of their birthplaces, life cycles, relationships to air masses and jet-stream winds, threats to life and property, and their appearance on satellite images INTRODUCTION What do you see in the diagram to the right: a vase or two faces? This classic psychology experiment exploits our amazing ability to recognize visual patterns. -
Global Disease and Air Quality in a Changing Climate by Kim Frauhammer
YP Perspective Global Disease and Air Quality in a Changing Climate by Kim Frauhammer Through the lens of the current global pandemic, a look at some of the existing challenges, such as environmental degradation, decreasing air quality, and climate change, that continue to put the human population at risk. 2020 has already been a year to remember, defined by the Seasonality of the Virus novel Coronavirus and its far-reaching effects on our health With how expansive this virus has proven to be, examining and economy. This global pandemic has restructured our all methods of transport is vital to understanding the future lives, while existing global challenges that continue to put the of global diseases. According to the U.S. Global Change human population at risk remain. Environmental degradation, Research Program, a set of “vulnerability factors” determine decreasing air quality, and climate change continue to expose whether someone is at risk for adverse health outcomes: the human population to higher risks of illness and loss of exposure, sensitivity, and adaptive capacity.1 The climate and resources. COVID-19 has provided us with a unique window environment are a part of all three. The virus first emerged into identifying these underlying risks and highlights the and spread rampantly during the Northern Hemisphere benefits between preserving the future of not only our Winter and there is scientific evidence to point to why. health, but our environment as well. Humidity is the greatest factor. em • The Magazine for Environmental Managers • A&WMA • August 2020 YP Perspective In the midlatitudes of the Northern Hemisphere (broadly be - Recent research from Harvard University cites that people tween 30 and 60 degrees), the atmosphere cools down as the who live in areas of poor air quality are more likely to die Earth is tilted farther away from the sun during the winter. -
An Air Stagnation Index to Qualify Extreme Haze Events in Northern China
OCTOBER 2018 F E N G E T A L . 3489 An Air Stagnation Index to Qualify Extreme Haze Events in Northern China JIN FENG Institute of Urban Meteorology, China Meteorological Administration, Beijing, China, and National Center for Atmospheric Research, Boulder, Colorado JIANNONG QUAN Institute of Urban Meteorology, China Meteorological Administration, Beijing, China HONG LIAO Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing, China YANJIE LI State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China XIUJUAN ZHAO Institute of Urban Meteorology, China Meteorological Administration, Beijing, China (Manuscript received 27 November 2017, in final form 18 June 2018) ABSTRACT Stagnation weather affects atmospheric diffusion ability, and hence causes the occurrence of haze events, which have been happening frequently in northern China (NC). This work puts forward an air stagnation index (ASITS) to characterize the stagnation weather in NC, in which the processes of ventilation, vertical diffusion, and wet deposition potency are concerned. ASITS can be applied to analyze air stagnation conditions with daily to monthly time scale. It is shown that the ASITS and particulate matter smaller than 2.5 mmindiameter(PM2.5) concen- trations own similar lognormal probability distribution functions on both daily and monthly time scales. And the correlation analyses between the ASITS and PM2.5 concentrations indicate that the ASITS can reflect the monthly and daily variations in PM2.5 concentrations in NC. -
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.