Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning
|
|
- Sylvia Manning
- 6 years ago
- Views:
Transcription
1 Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning
2 Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning Thunderstorms are responsible for most of what we refer to as severe weather, including high winds, lightning, tornadoes and hail - By official definition, a severe thunderstorm has at least one of the following: Large hail of ¾ inch diameter or greater Wind gusts of at least 50 knots A tornado
3 Keep in mind that a thunderstorm is a form of cumulus cloud, which means it's basically a plume of warm, cloudy air (i.e., an updraft) in a conditionally unstable environment. The fuel for a thunderstorm is condensation in the cloud, which keeps the ascending cloudy air warmer than the surroundings.
4 The Thunderstorm Cell: Labeling the Parts warm condensation evaporation cold The building block of a thunderstorm is the thunderstorm cell, consisting of a warm updraft and a relatively cold downdraft. The updraft is driven by condensation in the cloud, while the downdraft is driven by evaporation, as well as the drag produced by falling rain and hail.
5 The Thunderstorm Cell: Labeling the Parts entrainment warm condensation evaporation cold The evaporation that helps drive the downdraft happens two ways: Rain falls into the unsaturated air below and evaporates Dry air is mixed with cloudy air across the edges of the cloud, through a process called entrainment
6 The Thunderstorm Cell: Labeling the Parts entrainment warm condensation evaporation cold cold pool gust front As the downdraft reaches the ground, it spreads out and forms a region of relatively cold air called the cold pool. The leading edge of the cold pool is called the gust front, as the winds behind the gust front (on the cold side) are typically strong and gusty.
7 The Thunderstorm Cell: Labeling the Parts cold air warm air gust front As the gust front spreads along the ground, it forces warm air up and over the front. Under the right conditions, this lifting can initiate new updrafts, which is an important process for maintaining and propagating the system.
8 Photo of a gust front approaching outside the daycare. No walk today!
9 Recipe for a Thunderstorm The driving force behind a thunderstorm is the latent heating in the updraft. So to get things going, we'll need: A liberal supply of warm, humid air A conditionally unstable environment, allowing the air to rise A lifting mechanism (the trigger ) to raise the initially dry air to saturation And if it's a severe storm we're after, then we'll also need: A change in the background wind speed and direction with height (called wind shear) wind shear
10 The Dependence on Shear The type of storm we get (and hence the intensity and duration) is strongly influenced by the wind profile in the environment (i.e., the environmental shear) In general, more wind shear tends to produce longer-lived and more intense storm systems! To a rough approximation, this means that severe thunderstorms and tornadoes often form under a branch of the jet stream
11 Conditions for the April 15, 2011 Tornado Outbreak a change in wind speed and/or direction with height a trigger mechanism to provide lifting (cold front) a supply of warm humid air off the Gulf
12 Thunderstorm Classification A given thunderstorm can be classified as: A single-cell (or ordinary-cell) thunderstorm, consisting of a single updraft/downdraft system A multicell thunderstorm, consisting of several thunderstorm cells evolving together as a unit A supercell storm, consisting of a single intense, rotating updraft and either one or two associated downdrafts (run away, run away) In addition, we also classify systems in which many individual storms are evolving together in the same general region...what are called mesoscale convective systems (MCS). But we'll come back to that later.
13 Single-cell storms: A single-cell storm consists of a single updraft / downdraft pair Single-cells form in environments with weak wind shear The cell evolves through a series of stages, with the whole process taking roughly 30 to 60 minutes The motion of the storm follows the mean background wind
14 Life cycle of a single-cell storm: Growth stage: air parcels lifted to saturation by some trigger process. Clouds build into towering cumulus. Mature stage: evaporation leads to formation of a downdraft. Cold pool forms and begins to spread along the ground. Most intense stage. Dissipating stage: the spreading cold pool cuts the system off from warm air, killing the updraft and leading to dissipation.
15 A single-cell thunderstorm in the dissipating stage
16 Multicell storms: A multicell storm consists of a small group of cells evolving together, but in different stages of development Multicells are found in environments with weak to moderate shear Individual cells grow and die in 30 to 60 minutes, but the collection as a whole can last much longer The view from Lowes in Bryan, earlier this spring
17 Maintenance of a multicell storm: The key to multicell longevity is the spreading gust front As the gust front spreads it lifts warm air, initiating new updrafts The new updrafts form at the leading edge of the system, and the older cells shift to the back of the system and die mature cells move to the back of the system and eventually dissipate new updrafts are formed at the gust front
18 a shelf cloud formed as air is lifted up and over the edge of the gust front a rotating roll cloud just behind the leading edge of the gust front
19 Supercells: A supercell consists of a single intense, rotating updraft and either one or two associated downdrafts Supercells are typically found in high-shear environments The organization of a supercell is self-reinforcing, and a single supercell can last several hours rotating supercell wall cloud and associated tornado
20 Supercells: Most of our intense tornadoes in the US are produced by supercell storms rotating supercell wall cloud and associated tornado
21 Supercell Structure as Seen by Radar roughly N-S cross-section (A to B) radar echoes seen at various heights above the ground roughly E-W cross-section (C to D) B Bounded Weak Echo Region (BWER): a hole in the radar signal where the updraft is so fast that precipitation has no time to grow C hook echo A D updraft region
22 front-flank downdraft rear-flank downdraft front-flank gust front rear-flank gust front rotating updraft Tornadic supercells usually have two downdrafts, each with an associated gust front. The single, rotating updraft is located where the two gust fronts meet.
Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning
Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning Thunderstorms are responsible for most of what we refer to as severe weather,
More informationChapter 14 Thunderstorm Fundamentals
Chapter overview: Thunderstorm appearance Thunderstorm cells and evolution Thunderstorm types and organization o Single cell thunderstorms o Multicell thunderstorms o Orographic thunderstorms o Severe
More informationWeather Systems III: Thunderstorms and Twisters
Weather Systems III: Thunderstorms and Twisters Review 1. Definition of airmasses? Bergeron classification of air masses 2. Surface weather analysis: Station model, wind speed code, present weather 3.
More informationThunderstorms. Ordinary Cell Thunderstorms. Ordinary Cell Thunderstorms. Ordinary Cell Thunderstorms 5/2/11
A storm containing lightning and thunder; convective storms Chapter 14 Severe thunderstorms: At least one: large hail wind gusts greater than or equal to 50 kt Tornado 1 2 Ordinary Cell Ordinary Cell AKA
More informationChapter 8 cont. Clouds and Storms. Spring 2018
Chapter 8 cont. Clouds and Storms Spring 2018 Clouds and Storms Clouds cover ~ 50% of earth at any time. Clouds are linked to a number of condensation processes. Cloud morphology, cloud types, associated
More informationChapter 8 cont. Clouds and Storms
Chapter 8 cont. Clouds and Storms Spring 2007 Clouds and Storms Clouds cover ~ 50% of earth at any time. Clouds are linked to a number of condensation processes. Cloud morphology, cloud types, associated
More informationTOPICS: What are Thunderstorms? Ingredients Stages Types Lightning Downburst and Microburst
THUNDERSTORMS TOPICS: What are Thunderstorms? Ingredients Stages Types Lightning Downburst and Microburst What are Thunderstorms? A storm produced by a cumulonimbus cloud that contains lightning and thunder
More informationHAZARDOUS WEATHER 1. Dr. Julie Laity Geography 266
HAZARDOUS WEATHER 1 Dr. Julie Laity Geography 266 Violent Weather Thunderstorms Atmospheric turbulence Lightning and thunder Hail Derechos Tornadoes Tornado measurement and science Tropical Cyclones Hurricanes
More informationWeather Systems. The air around high-pressure weather systems tends to swirl in a clockwise direction, and usually brings clear skies.
Weather Systems A weather system is a set of temperature, wind, pressure, and moisture conditions for a certain region that moves as a unit for a period of several days. Low-pressure weather systems form
More informationATS 351, Spring 2010 Lab #11 Severe Weather 54 points
ATS 351, Spring 2010 Lab #11 Severe Weather 54 points Question 1 (10 points): Thunderstorm development a) Sketch and describe the stages of development of a single cell thunderstorm. About how long does
More informationThe Earth System - Atmosphere III Convection
The Earth System - Atmosphere III Convection Thunderstorms 1. A thunderstorm is a storm that produces lightning (and therefore thunder) 2. Thunderstorms frequently produce gusty winds, heavy rain, and
More informationChapter 3 Convective Dynamics Part VI. Supercell Storms. Supercell Photos
Chapter 3 Convective Dynamics Part VI. Supercell Storms Photographs Todd Lindley (This part contains materials taken from UCAR MCS training module) Supercell Photos 1 Introduction A supercel storm is defined
More informationPractical Use of the Skew-T, log-p diagram for weather forecasting. Primer on organized convection
Practical Use of the Skew-T, log-p diagram for weather forecasting Primer on organized convection Outline Rationale and format of the skew-t, log-p diagram Some basic derived diagnostic measures Characterizing
More information1 of 7 Thunderstorm Notes by Paul Sirvatka College of DuPage Meteorology. Thunderstorms
1 of 7 Thunderstorm Notes by Paul Sirvatka College of DuPage Meteorology Thunderstorms There are three types of thunderstorms: single-cell (or air mass) multicell (cluster or squall line) supercell Although
More information10/21/2012. Chapter 10 Thunderstorms. Part II. Growth and Development of ordinary Cell Thunderstorms Thunderstorm Electrification.
Chapter 10 Thunderstorms Part I Growth and Development of ordinary Cell Thunderstorms Thunderstorm Electrification Tornadoes Part II Simplified model depicting the life cycle of an ordinary thunderstorm
More informationTHUNDERSTORMS Brett Ewing October, 2003
THUNDERSTORMS Brett Ewing October, 2003 A natural hazard that occurs often on a daily basis in the lower and mid-latitudes is thunderstorms. Thunderstorms is a weather system that can produce lightning,tornadoes,
More informationDEPARTMENT OF EARTH & CLIMATE SCIENCES NAME SAN FRANCISCO STATE UNIVERSITY Fall ERTH FINAL EXAMINATION KEY 200 pts
DEPARTMENT OF EARTH & CLIMATE SCIENCES NAME SAN FRANCISCO STATE UNIVERSITY Fall 2016 Part 1. Weather Map Interpretation ERTH 365.02 FINAL EXAMINATION KEY 200 pts Questions 1 through 9 refer to Figure 1,
More informationThunderstorms and Severe Weather. (Chapt 15)
Thunderstorms and Severe Weather (Chapt 15) The Big Picture We ve emphasized horizontal transport of energy to balance the planetary energy budget: Hadley Cell Subtropical divergence Midlatitude cyclones
More informationMeteorology. Chapter 10 Worksheet 2
Chapter 10 Worksheet 2 Meteorology Name: Circle the letter that corresponds to the correct answer 1) Downdrafts totally dominate the in the development of a thunderstorm. a) dissipating stage b) mature
More informationAdvanced Spotter Training Lesson 4: The Nature of Thunderstorms
Advanced Spotter Training 2009 Lesson 4: The Nature of Thunderstorms From Last Time We discussed the different ways to make air rise. We discussed convection, convergence, and the different kinds of fronts.
More informationReading. What meteorological conditions precede a thunderstorm? Thunderstorms: ordinary or single cell storms, multicell storms, supercell storms
Thunderstorms: ordinary or single cell storms, multicell storms, supercell storms Reading Ahrens, Chapter 14: Thunderstorms and Tornadoes This lecture + next (Lightning, tornadoes) will cover the topic.
More informationCLOUDS & THUNDERSTORMS
Funding provided by NOAA Sectoral Applications Research Project CLOUDS & THUNDERSTORMS Basic Climatology Oklahoma Climatological Survey How are clouds made? Clouds form when air is cooled to its dewpoint
More informationAir Mass Thunderstorms. Air Mass Thunderstorms. Air Mass Thunderstorms. Lecture 26 Air Mass Thunderstorms and Lightning
Lecture 26 and Lightning Life Cycle Environment Climatology Lightning 1 2 Short-lived, isolated thunderstorms that are not severe are often called air-mass thunderstorms. There are three stages describing
More informationSevere Thunderstorms
Lecture 26 Severe Thunderstorms NWS Criteria Environment Structure Climatology 1 Severe Thunderstorms NWS Criteria Environment Structure Climatology 2 Severe Thunderstorms: NWS Criteria NWS Criteria: to
More informationcontact with ground for 1 hour plus, starting 1500 MDT moved N., covered about 37 km width varied m
Goal for today: Finish Ch. 11 Lightning, Thunder & Tornadoes 16 Nov., 2011 Edmonton tornado 31 July 1987 contact with ground for 1 hour plus, starting 1500 MDT moved N., covered about 37 km width varied
More informationExamination #3 Wednesday, 28 November 2001
Name & Signature Dr. Droegemeier Student ID Meteorology 1004 Introduction to Meteorology Fall, 2001 Examination #3 Wednesday, 28 November 2001 BEFORE YOU BEGIN!! Please be sure to read each question CAREFULLY
More informationSection 13-1: Thunderstorms
Section 13-1: Thunderstorms Chapter 13 Main Idea: The intensity and duration of thunderstorms depend on the local conditions that create them. Air-mass thunderstorm Mountain thunderstorm Sea-breeze thunderstorm
More informationTest Form: A Key Final Exam: Spring 2011
Test Form: A Key Final Exam: Spring 2011 Instructions: Write your name (last name and first name) on your bubble sheet. Write your student identification number on the bubble sheet, and carefully and completely
More informationDepartment of Geosciences San Francisco State University Spring Metr 201 Monteverdi Quiz #5 Key (100 points)
Department of Geosciences Name San Francisco State University Spring 2012 Metr 201 Monteverdi Quiz #5 Key (100 points) 1. Fill in the Blank or short definition. (3 points each for a total of 15 points)
More informationCHAPTER 11 THUNDERSTORMS AND TORNADOES MULTIPLE CHOICE QUESTIONS
CHAPTER 11 THUNDERSTORMS AND TORNADOES MULTIPLE CHOICE QUESTIONS 1. A thunderstorm is considered to be a weather system. a. synoptic-scale b. micro-scale c. meso-scale 2. By convention, the mature stage
More informationPrecipitation AOSC 200 Tim Canty. Cloud Development: Orographic Lifting
Precipitation AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Precipitation formation Rain Ice Lecture 14 Oct 11 2018 1 Cloud Development: Orographic Lifting
More informationModule 11: Meteorology Topic 6 Content: Severe Weather Notes
Severe weather can pose a risk to you and your property. Meteorologists monitor extreme weather to inform the public about dangerous atmospheric conditions. Thunderstorms, hurricanes, and tornadoes are
More informationMeteorology Lecture 19
Meteorology Lecture 19 Robert Fovell rfovell@albany.edu 1 Important notes These slides show some figures and videos prepared by Robert G. Fovell (RGF) for his Meteorology course, published by The Great
More informationWarm season forecasting! Some material adapted from Material Produced at COMET for their Residence Course in Hydrometeorology
Warm season forecasting! Some material adapted from Material Produced at COMET for their Residence Course in Hydrometeorology 1 Outline! Types of stability and application to forecasting! Dry and moist
More informationChap 14: Thunderstorms & Tornadoes
Chap 14: Thunderstorms & Tornadoes Ordinary thunderstorms Severe thunderstorms Microburst Mesoscale convective systems Squall line Mesoscale convective complex Multicell thunderstorms move to right of
More informationConvective Dynamics. Jeremy A. Gibbs. March 3, University of Oklahoma
Convective Dynamics Jeremy A. Gibbs University of Oklahoma gibbz@ou.edu March 3, 2015 1 / 70 Overview Administrative Homework 2 Exam 1 Convective Dynamics Introduction to Thunderstorms/Moist Atm. Convection
More informationFoundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa
Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Weather Patterns and Severe Weather Foundations, 6e - Chapter 14 Stan Hatfield Southwestern Illinois College Air masses Characteristics Large body
More informationFinal Exam Clicker Questions ATOC 1050 Spring 2011 Chapter 16: Mountain Snowstorms
Final Exam Clicker Questions ATOC 1050 Spring 2011 Chapter 16: Mountain Snowstorms True or false: Mean annual snowfall in the western United States always increases from south to north. Total precipitation
More informationAir Mass. 1. Air Mass : Large body of Air with similar temperature and humidity (or moisture) ; 4 types
Air Mass 1. Air Mass : Large body of Air with similar temperature and humidity (or moisture) ; 4 types A. Continental-relatively dry air masses that form over land. B. Maritime: relatively humid air masses
More informationSolutions to Comprehensive Final Examination Given on Thursday, 13 December 2001
Name & Signature Dr. Droegemeier Student ID Meteorology 1004 Introduction to Meteorology Fall, 2001 Solutions to Comprehensive Final Examination Given on Thursday, 13 December 2001 BEFORE YOU BEGIN!! Please
More informationLightning AOSC 200 Tim Canty. Multicell Thunderstorms
Lightning AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Thunderstorms Lightning Initiation Lightning Detection Upward lightning Lecture 22 Nov 14, 2017 1
More informationTornadoes forecasting, dynamics and genesis. Mteor 417 Iowa State University Week 12 Bill Gallus
Tornadoes forecasting, dynamics and genesis Mteor 417 Iowa State University Week 12 Bill Gallus Tools to diagnose severe weather risks Definition of tornado: A vortex (rapidly rotating column of air) associated
More information777 GROUNDSCHOOL Temperature, Stability, Fronts, & Thunderstorms
777 GROUNDSCHOOL 2018 Temperature, Stability, Fronts, & Thunderstorms The Atmosphere Heating Transfer of heat occurs thru Radiation Advection Convection Matter changes states due to the amount of heat
More informationTornadogenesis in Supercells: The Three Main Ingredients. Ted Funk
Tornadogenesis in Supercells: The Three Main Ingredients Ted Funk NWS Louisville, KY Spring 2002 Environmental Parameters Supercells occur within environments exhibiting several wellknown characteristics
More informationThunderstorm. Thunderstorms result from the rapid upward movement of warm, moist air.
Severe Weather Thunderstorm A thunderstorm (aka an electrical storm, a lightning storm, or a thundershower) is a type of storm characterized by the presence of lightning and its acoustic effect, thunder.
More informationGuided Notes: Atmosphere Layers of the Atmosphere
Guided Notes: Atmosphere Layers of the Atmosphere Atmosphere: Absorbs solar radiation, Burns up meteors, transports and recycles water, and other chemicals, and moderates climate Main Components: o Meteorology
More informationMeteorology. Review Extreme Weather a. cold front. b. warm front. What type of weather is associated with a:
Meteorology 5.08 Extreme Weather References: FTGU pages 132, 144, 145, 148-155 Air Command Weather Manual Chapters 9 and 15 Review What type of weather is associated with a: a. cold front b. warm front
More informationLightning. lightning: an electrical discharge in the atmosphere. Electricity. Lightning, Thunder and Tornados PHYS 189. Electricity.
, lightning: an electrical discharge in the atmosphere (), week 12 1 / 40 , lightning: an electrical discharge in the atmosphere cloud-to-cloud (80%) cloud-to-ground (20%) (), week 12 1 / 40 Fundamentals
More informationChapter 3 Convective Dynamics
Chapter 3 Convective Dynamics Photographs Todd Lindley 3.2 Ordinary or "air-mass storm 3.2.1. Main Characteristics Consists of a single cell (updraft/downdraft pair) Forms in environment characterized
More informationTornadoes forecasting, dynamics and genesis. Mteor 417 Iowa State University Week 12 Bill Gallus
Tornadoes forecasting, dynamics and genesis Mteor 417 Iowa State University Week 12 Bill Gallus Tools to diagnose severe weather risks Definition of tornado: A vortex (rapidly rotating column of air) associated
More informationMeteorology Lecture 18
Meteorology Lecture 18 Robert Fovell rfovell@albany.edu 1 Important notes These slides show some figures and videos prepared by Robert G. Fovell (RGF) for his Meteorology course, published by The Great
More informationScience Olympiad Meteorology Quiz #1 Page 1 of 7
1) What is generally true about the stratosphere: a) Has turbulent updrafts and downdrafts. b) Has either a stable or increasing temperature profile with altitude. c) Where the auroras occur. d) Both a)
More informationThunderstorms and Tornadoes. Chapter 14
Thunderstorms and Tornadoes Chapter 14 Thunderstorms A storm containing lightning and thunder convective storms Severe thunderstorms (NWS def) one of following: large hail - ¾ in dia Surface wind gusts
More informationWeather Pattern Notes
Weather Pattern Notes Please copy notes into you notebooks on pgs 72,74, and 76. Include 3 Questions that your notes answer on EACH of the pages you have notes on for full credit. Lesson 2-1 Pressure Systems
More informationSevere Thunderstorm Forecasting and Climatology in Arizona. Ken Drozd Warning Coordination Meteorologist NOAA/NWS Tucson, AZ
Severe Thunderstorm Forecasting and Climatology in Arizona Ken Drozd Warning Coordination Meteorologist NOAA/NWS Tucson, AZ THUNDERSTORM FORMATION All thunderstorms result from the same necessary conditions
More informationChapter Introduction. Weather. Patterns. Forecasts Chapter Wrap-Up
Chapter Introduction Lesson 1 Lesson 2 Lesson 3 Describing Weather Weather Patterns Weather Forecasts Chapter Wrap-Up How do scientists describe and predict weather? What do you think? Before you begin,
More informationMET Lecture 26 Tornadoes I
MET 4300 Lecture 26 Tornadoes I A Large Tornado approaches Lyndon, Kansas, on May 8, 2003 Outline Definition, life cycle Tornado formation within supercells Tornado formation within nonsupercell thunderstorms
More informationUnit 5 Part 2 Test PPT
Unit 5 Part 2 Test PPT Standard 1: Air Masses Air Mass An air mass is an immense body of air that is characterized by similar temperatures and amounts of moisture at any given altitude When an air mass
More informationThunderstorms. Stages in the development of a thunderstorm
Severe Weather Outcomes: S2-4-04 Explain the formation and dynamics of selected severe weather phenomena... S2-4-05 Collect, interpret, and analyze meteorological data related to a severe weather event.
More informationMr. P s Science Test!
WEATHER- 2017 Mr. P s Science Test! # Name Date 1. Draw and label a weather station model. (10 pts) 2. The is the layer of the atmosphere with our weather. 3. Meteorologists classify clouds in about different
More informationClouds and turbulent moist convection
Clouds and turbulent moist convection Lecture 2: Cloud formation and Physics Caroline Muller Les Houches summer school Lectures Outline : Cloud fundamentals - global distribution, types, visualization
More information20.1 Air Masses. Weather Patterns and Severe Storms. Four Types of Source Regions. Weather in North America Fronts
20.1 Air Masses Weather Patterns and Severe Storms Chapter 20 A huge body of air that has a uniform temperature and humidity. They move slowly, and take on the properties of their source regions. Four
More informationTornado Occurrences. Tornadoes. Tornado Life Cycle 4/12/17
Chapter 19 Tornadoes Tornado Violently rotating column of air that extends from the base of a thunderstorm to the ground Tornado Statistics Over (100, 1000, 10000) tornadoes reported in the U.S. every
More informationChapter 3 Convective Dynamics 3.4. Bright Bands, Bow Echoes and Mesoscale Convective Complexes
Chapter 3 Convective Dynamics 3.4. Bright Bands, Bow Echoes and Mesoscale Convective Complexes Photographs Todd Lindley Bright band associated with stratiform precipitation in a squall line system 1 Bright
More informationNOAA S National Weather Service
NOAA S National Weather Service Night Spotting Advanced Concepts of Severe Storm Spotting 2012 Rusty Kapela Milwaukee/Sullivan Weather.gov/milwaukee Problems Spotters Encounter Spotters can only see a
More informationClouds and atmospheric convection
Clouds and atmospheric convection Caroline Muller CNRS/Laboratoire de Météorologie Dynamique (LMD) Département de Géosciences ENS M2 P7/ IPGP 1 What are clouds? Clouds and atmospheric convection 3 What
More informationDEPARTMENT OF EARTH & CLIMATE SCIENCES SAN FRANCISCO STATE UNIVERSITY EARTH 365. Fall 2018 Test #2. November :00pm 7:15pm
1 DEPARTMENT OF EARTH & CLIMATE SCIENCES SAN FRANCISCO STATE UNIVERSITY EARTH 365 Fall 2018 Test #2 November 6 2018 6:00pm 7:15pm 200 points (4 points each answer) Answer on the answer sheet provided.
More informationTHUNDERSTORMS. Convective heavy rain accompanied by lightning and thunder. Ahrens
THUNDERSTORMS Convective heavy rain accompanied by lightning and thunder Ahrens Thunderstorms About 1,800 T-storms occur around the world at any instant Where do they occur the most? National Lightning
More informationToday s lecture. Charge separation in clouds Lightning and thunder
Today s lecture Charge separation in clouds Lightning and thunder Warming up knowledge Storm - convective precipitation (from cumulus and cumulonimbus (Cb) clouds) Prerequisite for a storm - cloud particles
More informationAir stability. About. Precipitation. air in unstable equilibrium will move--up/down Fig. 5-1, p.112. Adiabatic = w/ no exchange of heat from outside!
Air stability About clouds Precipitation A mass of moist, stable air gliding up and over these mountains condenses into lenticular clouds. Fig. 5-CO, p.110 air in unstable equilibrium will move--up/down
More informationThunderstorm Basics. Thunderstorm Climatology
Thunderstorm Basics Part of the fascination many people have with thunderstorms is the mystery that surrounds them. Leading researchers are still learning about many of the phenomena associated with thunderstorms.
More information6.2 Meteorology. A meteorologist is a person who uses scientific principles to explain, understand, observe, or forecast Earth s weather.
Water and Weather 6.2 Meteorology A meteorologist is a person who uses scientific principles to explain, understand, observe, or forecast Earth s weather. 6.2 Water in the Atmosphere Dew point is the temperature
More informationWeather Patterns and Severe Storms
Weather Patterns and Severe Storms 20.1 Air Masses Air Masses and Weather Air Masses An air mass is an immense body of air that is characterized by similar temperatures and amounts of moisture at any given
More informationConvective Dynamics. Jeremy A. Gibbs. March 10, University of Oklahoma
Convective Dynamics Jeremy A. Gibbs University of Oklahoma gibbz@ou.edu March 10, 2015 1 / 66 Overview Multicellular Storms Intro Lifecycle Thunderstorm Outflow as a Density Current Cell Regeneration 2
More informationUnit: Weather Study Guide
Name: Period: Unit: Weather Study Guide Define each vocabulary word on a separate piece of paper or index card. Weather Climate Temperature Wind chill Heat index Sky conditions UV index Visibility Wind
More informationChapter 21. Weather Patterns and Severe Storms
Chapter 21 Weather Patterns and Severe Storms 20.1 Air Masses Air Masses and Weather Air Masses An air mass is an immense body of air that is characterized by similar temperatures and amounts of moisture
More informationThunderstorms. Section. Overview of Thunderstorms
Section 3 3. SC.92.E.7.: Predict future weather conditions based on present observations and conceptual models and recognize limitations and uncertainties of such predictions. SC.92.E.7.6: Relate the formation
More informationChapter 3 Convective Dynamics Part V ñ Bright Bands, Bow Echoes and MCCs. Bright band associated with stratiform precipitation in a squall line system
Chapter 3 Convective Dynamics Part V ñ Bright Bands, Bow Echoes and MCCs Photographs Todd Lindley (This part contains materials taken from UCAR MCS training module) Bright band associated with stratiform
More informationStation A. 1. In the Northern Hemisphere, the general direction of the flow of the jet stream is toward the: a. north b. east c.
Station A 1. In the Northern Hemisphere, the general direction of the flow of the jet stream is toward the: a. north b. east c. south 2. The percentage of oxygen in the atmosphere is: a. 78% b. 99% c.
More informationScience Olympiad Meteorology Quiz #2 Page 1 of 8
1) The prevailing general direction of the jet stream is from west to east in the northern hemisphere: 2) Advection is the vertical movement of an air mass from one location to another: 3) Thunderstorms
More informationCondensation is the process by which water vapor changes from a gas to a liquid. Clouds form by this process.
CHAPTER 16 1 Water in the Air SECTION Understanding Weather BEFORE YOU READ After you read this section, you should be able to answer these questions: What is weather? How does water in the air affect
More informationType of storm viewed by Spotter A Ordinary, multi-cell thunderstorm. Type of storm viewed by Spotter B Supecell thunderstorm
ANSWER KEY Part I: Locating Geographical Features 1. The National Weather Service s Storm Prediction Center (www.spc.noaa.gov) has issued a tornado watch on a warm spring day. The watch covers a large
More informationNOAA S National Weather Service
NOAA S National Weather Service Elite Concepts of Severe Storm Spotting 2011 Rusty Kapela Milwaukee/Sullivan www.weather.gov/mkx Elite Spotter Outline Review Types of T storms Tornadic Supercell Classic,
More informationWeather. Weather Patterns
Weather Weather Patterns What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the statement or a D if you
More informationIII. Section 3.3 Vertical air motion can cause severe storms
III. Section 3.3 Vertical air motion can cause severe storms http://www.youtube.com/watch?v=nxwbr60tflg&feature=relmfu A. Thunderstorms form from rising moist air Electrical charges build up near the tops
More informationSummary of riming onset conditions for different crystal habits. Semi-dimension: width / lateral dimension (perpendicular to c-axis)
Summary of riming onset conditions for different crystal habits Semi-dimension: width / lateral dimension (perpendicular to c-axis) HEAT BALANCE FOR GRAUPEL PARTICLES Consider a graupel particle growing
More informationWEATHER THEORY. Stability. In general:
Weather Theory 69 Temperature, Pressure And Moisture WEATHER THEORY Pressure Systems (Cont) Every physical process of weather is a result of a heat exchange. The standard sea level temperature is 15 degrees
More informationMeteorology. I. The Atmosphere - the thin envelope of gas that surrounds the earth.
Meteorology I. The Atmosphere - the thin envelope of gas that surrounds the earth. A. Atmospheric Structure - the atmosphere is divided into five distinct layers that are based on their unique characteristics.
More informationsevere VOLUME 5, NUMBER 1, FEBRUARY 1980
severe VOLUME 5, NUMBER 1, FEBRUARY 1980 TORNADIC THUNDERSTORM DEVELOPMENT IN WEST TEXAS 27 MAY 1978 by Richard E. Peterson Atmospheric Science Group Texas University Lubbock, TX and Alan Johnson National
More informationWeather Maps. Name:& & &&&&&Advisory:& & 1.! A&weather&map&is:& & & & 2.! Weather&fronts&are:& & & & & &
Name: Advisory: Weather Maps 1. Aweathermapis: 2. Weatherfrontsare: a. Labelthefrontsbelow: 1. 2. 3. 4. 3. Clovercoversymbols 4. Precipitationsymbols 5. 6. 7. 8. 5. RadarEchoIntensityshows 6. Isobarsare
More informationReview of Basic Severe Thunderstorm & Tornado Spotting Concepts. Jim Allsopp National Weather Service Chicago/Romeoville, IL
Review of Basic Severe Thunderstorm & Tornado Spotting Concepts Jim Allsopp National Weather Service Chicago/Romeoville, IL Why Do We Need Spotters? Radar has limitations, only spotters can provide view
More informationLecture Outlines PowerPoint. Chapter 19 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 19 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More information10. Severe Local Storms (Thunderstorms)
10. Severe Local Storms (Thunderstorms) Hail. Can be larger than softball (10 cm in diameter) Smaller damage ratios, but over large areas In USA causes more than $1 billion crop and property damage each
More informationEarth Science, 11e. Weather Patterns and Severe Storms Chapter 19. Air masses. A cold Canadian air mass Figure Air masses. Air masses 9/5/2012
2006 Pearson Prentice Hall Lecture Outlines PowerPoint Chapter 19 Earth Science 11e Tarbuck/Lutgens This work is protected by United States copyright laws and is provided solely for the use of instructors
More informationWeather - is the state of the atmosphere at a specific time & place
Weather Section 1 Weather - is the state of the atmosphere at a specific time & place Includes such conditions as air pressure, wind, temperature, and moisture in the air The Sun s heat evaporates water
More information16.4 SENSITIVITY OF TORNADOGENESIS IN VERY-HIGH RESOLUTION NUMERICAL SIMULATIONS TO VARIATIONS IN MODEL MICROPHYSICAL PARAMETERS
1. SENSITIVITY OF TORNADOGENESIS IN VERY-HIGH RESOLUTION NUMERICAL SIMULATIONS TO VARIATIONS IN MODEL MICROPHYSICAL PARAMETERS Nathan A. Snook* and Ming Xue University of Oklahoma, Norman, Oklahoma 1.
More informationTornadoes. tornado: a violently rotating column of air
Tornadoes tornado: a violently rotating column of air Tornadoes What is the typical size of a tornado? What are typical wind speeds for a tornado? Five-stage life cycle of a tornado Dust Swirl Stage Tornado
More informationTuesday, September 13, 16
Weather Weather State Objectives 4.c, 4.d, 4.h. Discussion What are some ways in which weather affects your everyday life? Discussion What are some ways in which weather affects your everyday life? What
More informationESCI 1010 Lab 6 Midlatitude Cyclones and Thunderstorms
ESCI 1010 Lab 6 Midlatitude Cyclones and Thunderstorms Before Lab: Review pages 244-324 in your Weather and Climate textbook. Pay special attention to the sections entitled Fronts, Life Cyclone of a Midlatitude
More informationThe most abundant gas in the atmosphere by volume is. This gas comprises 78% of the Earth atmosphere by volume.
The most abundant gas in the atmosphere by volume is. This gas comprises 78% of the Earth atmosphere by volume. A. Oxygen B. Water Vapor C. Carbon Dioxide D. Nitrogen An isobar is a line of constant. A.
More information