Sunday, 13 June 1999

Size: px
Start display at page:

Download "Sunday, 13 June 1999"

Transcription

1 Sunday, 13 June 1999 Julian Day 164 Meteorological Summary A cold front moved in over night, cooling the air at low levels. Warming aloft occurred and stabilized the air in mid-levels, suppressing convective activity for the day. Operations Summary Sunday was a down day. Also, the Convair was down with an oil cooler leak. We did have some good discussions about how to make the operations a little more efficient and where further data gathering efforts should be concentrated. In general, it was felt that more high altitude data were needed, but only the Sabreliner could provide that. Also, it would be useful to get better measurements of the vertical structure of the storm, so that 5 kft. altitude separations may be attempted, if ATC agrees. Also if one of the aircraft could measure cloud base that would be useful for later analyses. More dual Doppler coverage at the expense of surveillance scans is probably in order. The pilots were also going to try to give ATC a little more warning about when and where they would be going up, to help alleviate some of the ATC problems we ve been having. 83

2 Data Type Source Aircraft T-28 Convair Sabreliner Ground CHILL Radars Pawnee NEXRAD Denver, CO NIDS data Cheyenne, WY (gif images) Grand Junction, CO Goodland, KS Upper Air Mobile CLASS Denver, CO Grand Junction, CO North Platte, NE Riverton, WY Dodge City, KS Profiler Platteville, CO Granada, CO CSU CHILL, CO Haviland, KS Hillsboro, KS Neodesha, KS McCook, NE Neligh, NE Fairbury, NE Merrinon, NE Medicine Bow, WY Goes 8 Denver (jpeg image) National METAR PIREPS Airmets Colorado Wyoming Nebraska Kansas U.S.A. U.S.A. Convective U.S.A. Sigmets Local Colorado Storm Wyoming Reports Nebraska Kansas Severe Rpts U.S.A. 13 June Hourly Collection of Data Time (UTC)

3 13 June surface analysis not available 13 June 500 mb analysis not available June 500 mb analysis not available

4 Denver, CO 13 June UTC CHILL Radar 13 June UTC 86

5 Monday, 14 June 1999 Julian Day 165 Meteorological Summary Monday turned out to be a very good day for multi-cell convection. Radar echo was observed over the mountains early in the day, and later a line propagated through the plains just north of CHILL, which became the target storms. Operations Summary The Convair was still down with an oil cooler problem, so only the T28 and the Sabreliner were available for this day. It was decided not to fly in formation today, but to treat each aircraft as separate flights. Sometimes the aircraft were flying within the same cell, and other times the aircraft were flying on different cells. The penetrations runs by the Sabreliner were designated Flight 9, by the T28 Flight 10. Both aircraft were off the ground by about 2030 UTC. Initial targets were two developing areas along a line each containing what appeared to be two cells. Cloud base at this time was about 15 kft. Flight 9 (Sabreliner) run 1 was through a developing system about 120 km north of CHILL at 27 kft., UTC. At about the same time Flight 10 (T28) Run 1 was executed at 20 kft. from south to north through a developing line centered about 20 km north of CHILL, and encountered severe turbulence. The T28 then turned around flying north to south through the same storm at 21 kft.; The Sabreliner was executing Run 2 from the north to the south through this system at 29 kft. from Turbulence reported as light chop with some rain. This system was evolving rapidly, and both aircraft lined up for Runs 3 and 4 as north-south passes on either the west or east sides of the line. The Sabreliner was at 29 kft. for Run 3, at 33 kft. for Run 4, and the T28 at 21 kft. for both runs. Times of penetration were Flight 9 (Sabreliner) Run 3: , and Run 4: ; Flight 10 (T28) Run 3: , and Run 4: Both aircraft reported light to moderate turbulence during these runs. Because a new storm was developing to the east of this line, the T28 was vectored to do a west to east penetration of this new cell. Flight 10 (T28) Run 5 was executed ; and reported a good bump at the updraft boundary. The Sabreliner meanwhile did another pass through the evolving line (which by this time contained three distinct cells) through the center line of the storm at a heading of about 130 deg and at an altitude of 30 kft. Light to moderate turbulence reported on this Flight 9 Run 5 between 2139-?. Flight 10 (T28) Run 6 was executed by turning the T28 around to do a westbound penetration between ; with no turbulence experienced. That was the last run for the T28. The Sabreliner made 3 more runs through the new line to the east. Run 6 was northbound through this line which now contained 2-3 cells at 28 kft. from For this run, the aircraft was guided through regions of the storm that showed little echo, but good CHILL-derived Doppler radial shears and elevated spectrum widths. The aircraft indeed experienced severe turbulence (pilot reported 300 ft. altitude excursion and kt. airspeed excursion). Run 7 was a turn 87

6 around now southbound at about 150 deg heading through the same storm at 27 kft. at , before diverting out to the east. Only light turbulence and rain reported. Run 8 was initiated by turning around again northbound on the east side of the storm, still at 27 kft. from Again the aircraft encountered moderate-severe turbulence while within green echo (rain, a little ice reported) in an area where the CHILL-derived spectrum widths were large. This was the last run of the day. Unfortunately the Sabreliner took a lightning hit on one of these runs, but the damage was minor. The position of these storms allowed most of the runs to be performed under dual Doppler coverage. Two radiosondes were launched, one at CHILL at 1800 UTC and the other to the south of CHILL at CHILL reflectivity at 4.04 degrees elevation. The scan time is UTC on 14 june 1999 and corresponds to Run 4 of Flight 9. The positions of the T-28 and the Sabreliner are shown as before. 88

7 Data Type Source Aircraft T-28 Convair Sabreliner Ground CHILL Radars Pawnee NEXRAD NIDS data (gif images) Upper Air Profiler Denver, CO Cheyenne, WY Grand Junction, CO Goodland, KS Mobile CLASS Denver, CO Grand Junction, CO North Platte, NE Riverton, WY Dodge City, KS Platteville, CO Granada, CO Greeley, CO Haviland, KS Hillsboro, KS Neodesha, KS McCook, NE Neligh, NE Fairbury, NE Merrinon, NE Medicine Bow, WY Goes 8 Denver (jpeg image) National METAR PIREPS Airmets Colorado Wyoming Nebraska Kansas U.S.A. U.S.A. Convective U.S.A. Sigmets Local Colorado Storm Wyoming Reports Nebraska Kansas Severe Rpts U.S.A. 14 June Hourly Collection of Data Time (UTC)

8 90

9 Denver, CO 14 June UTC CHILL Radar 14 June UTC 91

10 Tuesday, 15 June 1999 Julian Day 166 Meteorological Summary Cool, moist, upslope conditions in northeastern Colorado led to stable air and no opportunities for convection in the area. Operations Summary Down day. No CLASS balloons launched. 92

11 Data Type Source Aircraft T-28 Convair Sabreliner Ground CHILL Radars Pawnee NEXRAD Denver, CO NIDS data Cheyenne, WY (gif images) Grand Junction, CO Goodland, KS Upper Air Mobile CLASS Denver, CO Grand Junction, CO North Platte, NE Riverton, WY Dodge City, KS Profiler Platteville, CO Granada, CO CSU CHILL, CO Haviland, KS Hillsboro, KS Neodesha, KS McCook, NE Neligh, NE Fairbury, NE Merrinon, NE Medicine Bow, WY Goes 8 Denver (jpeg image) National METAR PIREPS Airmets Colorado Wyoming Nebraska Kansas U.S.A. U.S.A. Convective U.S.A. Sigmets Local Colorado Storm Wyoming Reports Nebraska Kansas Severe Rpts U.S.A. 15 June Hourly Collection of Data Time (UTC)

12 94

13 Denver, CO 15 June UTC No CLASS soundings taken on 15 June 95

14 Wednesday, 16 June 1999 Julian Day 167 Meteorological Summary Upslope conditions continue. Outlook: Tomorrow looks a little better. Operations Summary A down day was called. A sounding was launched near Cheyenne, WY at about 1900 UTC. The sounding confirmed the stability. 96

15 Data Type Source Aircraft T-28 Convair Sabreliner Ground CHILL Radars Pawnee NEXRAD Denver, CO NIDS data Cheyenne, WY (gif images) Grand Junction, CO Goodland, KS Upper Air Mobile CLASS Denver, CO Grand Junction, CO North Platte, NE Riverton, WY Dodge City, KS Profiler Platteville, CO Granada, CO CSU CHILL, CO Haviland, KS Hillsboro, KS Neodesha, KS McCook, NE Neligh, NE Fairbury, NE Merrinon, NE Medicine Bow, WY Goes 8 Denver (jpeg image) National METAR PIREPS Airmets Colorado Wyoming Nebraska Kansas U.S.A. U.S.A. Convective U.S.A. Sigmets Local Colorado Storm Wyoming Reports Nebraska Kansas Severe Rpts U.S.A. 16 June Hourly Collection of Data Time (UTC)

16 98

17 Denver, CO 16 June UTC Cheyenne, WY 16 June UTC 99

18 Thursday, 17 June 1999 Julian Day 168 Meteorological Summary This day was another multicell convection day, but with very low winds aloft. Operations Summary The aircraft were up at about 2220 UTC with storm targets to the west of CHILL. Cloud tops were at about 43 kft with echoes near 60 dbz. Cloud base was at about 10 kft., the freezing level was at about 13.5 kft. A total of 9 runs were made The Sabreliner flew alone at higher altitudes while the T28-Convair flew in formation at lower altitudes. The T28-Convair runs were designated Flight 11 and the Sabreliner runs Flight 12. Flight 11 (T28-Convair) runs. Run 1 was a west to east penetration of an older storm, with the Convair at 21 kft and the T28 at 22 kft. Start and end times of Run 1 were UTC respectively. Healthy updrafts were encountered, and light to moderate turbulence reported. Run 2 was a reverse course, i.e. roughly east to west, back through the same storm. Start and end times were Heavy rain and moderate turbulence were encountered. Run 3 was back through the same complex on about a 60 deg heading, with both aircraft then at 21 kft. Start and end time for Run 3 were Light turbulence and rain were reported. Run 4 was at 19 kft, with start and stop times of with light-moderate turbulence, rain, and ice encountered. Flight 12 (Sabreliner) runs. The same storm complex sampled by the T28 and Convair along eastwest headings was sampled by the Sabreliner at higher altitudes and at north-south headings. Run 1 was northwest to southeast along the west side of the storm at 28 kft from UTC. Light-moderate turbulence reported, mixed ice. Run 2 was back up south to north, again along the west side of the storm, from Light-moderate turbulence, rain, hail, and lightning were reported. Run 3 was back down the west side of the same storm, northwest to southeast at 32 kft, from Light-moderate turbulence, lightning reported. Run 4 was a return course at about a 340 deg heading on the east side of the storm now, still at 32 kft, from Cloud tops were now up to about 53 kft in this storm. Light-moderate turbulence was reported. Run 5 was back to the south on the eastern edge. Run 5 was started at 2337, but at 2343, the aircraft escaped from the storm to the east before the second cell in the complex was penetrated, due to a door seal problem and some smoke in the cockpit. No apparent serious damage resulted. All runs were in dual Doppler coverage. Three soundings were launched at 1800, 2100, and 2215 UTC from the CHILL radar site. 100

19 CHILL reflectivity shown at degrees elevation. The scan time is UTC on June 17, 1999 and corresponds to Run 1 of Flight 11 and Run 2 of Flight 12. The locations of the three aircraft are shown as before. Range rings are every 20 km. 101

20 Data Type Source Aircraft T-28 Convair Sabreliner Ground CHILL Radars Pawnee NEXRAD NIDS data (gif images) Upper Air Profiler Goes 8 Denver (jpeg image) National METAR PIREPS Airmets Convective Sigmets Local Storm Reports Denver, CO Cheyenne, WY Grand Junction, CO Goodland, KS Mobile CLASS Denver, CO Grand Junction, CO North Platte, NE Riverton, WY Dodge City, KS Platteville, CO Granada, CO CSU CHILL, CO Haviland, KS Hillsboro, KS Neodesha, KS McCook, NE Neligh, NE Fairbury, NE Merrinon, NE Medicine Bow, WY Colorado Wyoming Nebraska Kansas U.S.A. U.S.A. U.S.A. Colorado Wyoming Nebraska Kansas Severe Rpts U.S.A. 17 June Hourly Collection of Data Time (UTC)

21 103

22 Denver, CO 17 June UTC Cheyenne, WY 17 June UTC 104

07/16/02. Obs: Two strong cells near Miami Anvils blowing toward western ground site Will try E-W legs as far east as we can get FC:

07/16/02. Obs: Two strong cells near Miami Anvils blowing toward western ground site Will try E-W legs as far east as we can get FC: 07/16/02 Obs: Report: Two strong cells near Miami Anvils blowing toward western ground site Will try E-W legs as far east as we can get FC: Summary: Aircraft: Convection should develop mid-afternoon along

More information

VORTEX-2: SUNY Oswego Soundings Team Significant Observed Weather Events Kevin M. Smith

VORTEX-2: SUNY Oswego Soundings Team Significant Observed Weather Events Kevin M. Smith VORTEX-2: SUNY Oswego Soundings Team Significant Observed Weather Events Kevin M. Smith Summary Last Updated: Final Update The following is a chronological listing of significant weather conditions observed

More information

Anthony A. Rockwood Robert A. Maddox

Anthony A. Rockwood Robert A. Maddox Anthony A. Rockwood Robert A. Maddox An unusually intense MCS produced large hail and wind damage in northeast Kansas and northern Missouri during the predawn hours of June 7 th, 1982. Takes a look at

More information

Talking points for Water Vapor Imagery Analysis for Severe Thunderstorm Forecasting.

Talking points for Water Vapor Imagery Analysis for Severe Thunderstorm Forecasting. Talking points for Water Vapor Imagery Analysis for Severe Thunderstorm Forecasting. 1. Title. 2. Learning objectives. These are the topics we ll consider during this training session, the goal of the

More information

A Description of Convective Weather Containing Ice Crystals Associated with Engine Powerloss and Damage

A Description of Convective Weather Containing Ice Crystals Associated with Engine Powerloss and Damage A Description of Convective Weather Containing Ice Crystals Associated with Engine Powerloss and Damage The Boeing Company 1 Photo: courtesy of Ian McPherson The Boeing Company acknowledges the contributions

More information

Weather Legends in FOREFLIGHT MOBILE

Weather Legends in FOREFLIGHT MOBILE Weather Legends in FOREFLIGHT MOBILE 14th Edition Covers ForeFlight Mobile v9.4 on ipad Radar Legends (when from Internet) Snowy/Icy Precipitation Mixed Precipitation Rain Echo top (in 100 s of feet) ex:

More information

ATS 351, Spring 2010 Lab #11 Severe Weather 54 points

ATS 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 information

Thunderstorms. Ordinary Cell Thunderstorms. Ordinary Cell Thunderstorms. Ordinary Cell Thunderstorms 5/2/11

Thunderstorms. 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 information

Chapter 14 Thunderstorm Fundamentals

Chapter 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 information

Science Olympiad Meteorology Quiz #2 Page 1 of 8

Science 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 information

Answers to Clicker Questions

Answers to Clicker Questions Answers to Clicker Questions Chapter 1 What component of the atmosphere is most important to weather? A. Nitrogen B. Oxygen C. Carbon dioxide D. Ozone E. Water What location would have the lowest surface

More information

Mechanical Turbulence Wind forms eddies as it blows around hanger, stands of trees or other obstructions

Mechanical Turbulence Wind forms eddies as it blows around hanger, stands of trees or other obstructions Turbulence Low-level Turbulence below 15,000 feet consists of Mechanical Turbulence Convective Turbulence Frontal Turbulence Wake Turbulence Mechanical Turbulence Wind forms eddies as it blows around hanger,

More information

MET Lecture 34 Downbursts

MET Lecture 34 Downbursts MET 4300 Lecture 34 Downbursts Downbursts A strong downdraft that originates within the lower part of a cumulus cloud or thunderstorms and spreads out at the surface Downbursts do not require strong thunderstorms

More information

Recent observations of tornadoes using a mobile, rapid-scan, polarimetric, X-band, Doppler radar

Recent observations of tornadoes using a mobile, rapid-scan, polarimetric, X-band, Doppler radar Recent observations of tornadoes using a mobile, rapid-scan, polarimetric, X-band, Doppler radar Howard B. Bluestein 1, Jeffrey C. Snyder 2, Kyle J. Thiem 1, Zachary B. Wienhoff 1, Jana B. Houser 3, and

More information

Weather Legends in FOREFLIGHT MOBILE

Weather Legends in FOREFLIGHT MOBILE Weather Legends in FOREFLIGHT MOBILE 15th Edition Covers ForeFlight Mobile v9.6 on ipad Radar Legends (when from Internet) Snowy/Icy Precipitation Mixed Precipitation Rain Echo top (in 100 s of feet) ex:

More information

ENSTROM 480B OPERATOR S MANUAL AND FAA APPROVED ROTORCRAFT FLIGHT MANUAL SUPPLEMENT GARMIN GDL 69AH XM WX SATELLITE WEATHER/RADIO RECEIVER

ENSTROM 480B OPERATOR S MANUAL AND FAA APPROVED ROTORCRAFT FLIGHT MANUAL SUPPLEMENT GARMIN GDL 69AH XM WX SATELLITE WEATHER/RADIO RECEIVER ENSTROM 480B OPERATOR S MANUAL AND FAA APPROVED ROTORCRAFT FLIGHT MANUAL SUPPLEMENT GARMIN GDL 69AH XM WX SATELLITE WEATHER/RADIO RECEIVER * * * * * REPORT NO. 28-AC-062 HELICOPTER SERIAL NO. HELICOPTER

More information

Thunderstorms and Severe Weather. (Chapt 15)

Thunderstorms 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 information

P13A.4 THE AIR FRANCE 358 INCIDENT OF 2 AUGUST 2005 AT TORONTO INTERNATIONAL AIRPORT. Paul Joe

P13A.4 THE AIR FRANCE 358 INCIDENT OF 2 AUGUST 2005 AT TORONTO INTERNATIONAL AIRPORT. Paul Joe P13A.4 THE AIR FRANCE 358 INCIDENT OF 2 AUGUST 2005 AT TORONTO INTERNATIONAL AIRPORT Paul Joe Environment Canada, 4905 Dufferin St., Toronto, Ontario, CANADA M3H 5T4 email: paul.joe@ec.gc.ca tel: 416 739

More information

Meteorology 311. RADAR Fall 2016

Meteorology 311. RADAR Fall 2016 Meteorology 311 RADAR Fall 2016 What is it? RADAR RAdio Detection And Ranging Transmits electromagnetic pulses toward target. Tranmission rate is around 100 s pulses per second (318-1304 Hz). Short silent

More information

10/21/2012. Chapter 10 Thunderstorms. Part II. Growth and Development of ordinary Cell Thunderstorms Thunderstorm Electrification.

10/21/2012. 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 information

Flight Report Sunday September 21, 2014 Summary

Flight Report Sunday September 21, 2014 Summary Flight Report Sunday September 21, 2014 Summary 1 Flight Report: G1 Flight#10 & HALO AC14 1.1 Flight Strategy 2 1.2 Weather Conditions Before the Flight...3 1.3 Weather Conditions During the Flight...6

More information

ForeFlight Mobile Legends

ForeFlight Mobile Legends ForeFlight Mobile Legends ForeFlight, LLC 11th Edition - Covers ForeFlight Mobile v8.1 and later RADAR LEGENDS (WHEN FROM INTERNET) Snowy/Icy Precipitation Mixed Precipitation Rain Echo top (in 100 s of

More information

Chapter 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. 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 information

TOPICS: What are Thunderstorms? Ingredients Stages Types Lightning Downburst and Microburst

TOPICS: 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 information

Pilots watch the clouds, because clouds can indicate the kind of weather in store for a flight.

Pilots watch the clouds, because clouds can indicate the kind of weather in store for a flight. Low stratus Cumulonimbus Pilots watch the clouds, because clouds can indicate the kind of weather in store for a flight. FILL IN THE BLANKS OR CIRCLE ONE: A. Stratus means flat or on one level. Low stratus

More information

1 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 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 information

Severe Weather with a strong cold front: 2-3 April 2006 By Richard H. Grumm National Weather Service Office State College, PA 16803

Severe Weather with a strong cold front: 2-3 April 2006 By Richard H. Grumm National Weather Service Office State College, PA 16803 Severe Weather with a strong cold front: 2-3 April 2006 By Richard H. Grumm National Weather Service Office State College, PA 16803 1. INTRODUCTION A strong cold front brought severe weather to much of

More information

Test Form: A Key Final Exam: Spring 2011

Test 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 information

MET Lecture 20 Mountain Snowstorms (CH16)

MET Lecture 20 Mountain Snowstorms (CH16) MET 4300 Lecture 20 Mountain Snowstorms (CH16) Learning Objectives Provide an overview of the importance and impacts of mountain snowstorms in the western US Describe how topography influence precipitation

More information

Measuring In-cloud Turbulence: The NEXRAD Turbulence Detection Algorithm

Measuring In-cloud Turbulence: The NEXRAD Turbulence Detection Algorithm Measuring In-cloud Turbulence: The NEXRAD Turbulence Detection Algorithm John K. Williams,, Greg Meymaris,, Jason Craig, Gary Blackburn, Wiebke Deierling,, and Frank McDonough AMS 15 th Conference on Aviation,

More information

Friends & Partners in Aviation Weather: Part 135

Friends & Partners in Aviation Weather: Part 135 Friends & Partners in Aviation Weather: Part 135 Thursday, October 12, 2017 Jason E. Herman, CAM Chairman, NBAA Part 135 Subcommittee Part 135 On-Demand Operations A mix of many different operational environments

More information

Chapter 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 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 information

The Severe Weather Event of 7 August 2013 By Richard H. Grumm and Bruce Budd National Weather Service State College, PA 1. INTRODUCTION and Overview

The Severe Weather Event of 7 August 2013 By Richard H. Grumm and Bruce Budd National Weather Service State College, PA 1. INTRODUCTION and Overview The Severe Weather Event of 7 August 2013 By Richard H. Grumm and Bruce Budd National Weather Service State College, PA 1. INTRODUCTION and Overview A fast moving short-wave (Fig. 1) with -1σ 500 hpa height

More information

Science Olympiad Meteorology Quiz #1 Page 1 of 7

Science 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 information

AOPA. Mitigating Turbulence Impacts in Aviation Operations. General Aviation Perspective

AOPA. Mitigating Turbulence Impacts in Aviation Operations. General Aviation Perspective AOPA Mitigating Turbulence Impacts in Aviation Operations General Aviation Perspective Rune Duke Senior Director, Airspace & Air Traffic Services Aircraft Owners & Pilots Association AOPA Air Safety Institute

More information

Lightning AOSC 200 Tim Canty. Multicell Thunderstorms

Lightning 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 information

Storm Summary for Hurricane Joaquin

Storm Summary for Hurricane Joaquin Storm Summary for Hurricane Joaquin Wednesday, September 30, 2015 at 5 PM EDT (Output from Hurrevac, based on National Hurricane Center Forecast Advisory #12) Joaquin is currently a Category 1 hurricane

More information

Flight Report September 09, 2014 Summary

Flight Report September 09, 2014 Summary Flight Report September 09, 2014 Summary 1. HALO Flight Report - AC08... 2 1.1 Flight Strategy... 2 1.2 Weather Conditions Before the Flight... 3 1.3 Conditions During the Flight... 5 1. HALO Flight Report

More information

Fundamentals of Radar Display. Atmospheric Instrumentation

Fundamentals of Radar Display. Atmospheric Instrumentation Fundamentals of Radar Display Outline Fundamentals of Radar Display Scanning Strategies Basic Geometric Varieties WSR-88D Volume Coverage Patterns Classic Radar Displays and Signatures Precipitation Non-weather

More information

Department of Geosciences San Francisco State University Spring Metr 201 Monteverdi Quiz #5 Key (100 points)

Department 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 information

P474 SYDNEY AIRPORT WIND SHEAR ENCOUNTER - 15 APRIL 2007

P474 SYDNEY AIRPORT WIND SHEAR ENCOUNTER - 15 APRIL 2007 P474 SYDNEY AIRPORT WIND SHEAR ENCOUNTER - 15 APRIL 2007 Rodney Potts* 1, Barry Hanstrum 2 and Peter Dunda 2 1. CAWCR, Bureau of Meteorology, Melbourne, VIC, Australia 2. Bureau of Meteorology, Sydney,

More information

Issue of SIGMET/AIRMET warning

Issue of SIGMET/AIRMET warning Issue of SIGMET/AIRMET warning 1 Presentation Objectives After this presentation session you will be able to: Warn for Hazardous weather phenomena using the correct ICAO coding with regards to SIGMET/AIRMET

More information

Isolated severe weather and cold air damming 9 November 2005 By Richard H. Grumm National Weather Service Office State College, PA 16801

Isolated severe weather and cold air damming 9 November 2005 By Richard H. Grumm National Weather Service Office State College, PA 16801 Isolated severe weather and cold air damming 9 November 2005 By Richard H. Grumm National Weather Service Office State College, PA 16801 1. INTRODUCTION Two lines of convection moved over the State of

More information

Thunderstorm Downburst Prediction: An Integrated Remote Sensing Approach. Ken Pryor Center for Satellite Applications and Research (NOAA/NESDIS)

Thunderstorm Downburst Prediction: An Integrated Remote Sensing Approach. Ken Pryor Center for Satellite Applications and Research (NOAA/NESDIS) Thunderstorm Downburst Prediction: An Integrated Remote Sensing Approach Ken Pryor Center for Satellite Applications and Research (NOAA/NESDIS) Topics of Discussion Thunderstorm Life Cycle Thunderstorm

More information

AMDAR Forecast Applications. Richard Mamrosh NWS Green Bay, Wisconsin, USA

AMDAR Forecast Applications. Richard Mamrosh NWS Green Bay, Wisconsin, USA AMDAR Forecast Applications Richard Mamrosh NWS Green Bay, Wisconsin, USA AMDAR has many applications Aviation Low level wind shear Ceilings and visibilities Icing and turbulence Winter Storms Precipitation

More information

Refer to Figure 1 and what you have learned so far in this course when responding to the following:

Refer to Figure 1 and what you have learned so far in this course when responding to the following: Refer to Figure 1 and what you have learned so far in this course when responding to the following: 1.Looking down on a Northern Hemisphere extratropical cyclone, surface winds blow [(clockwise and outward)(counterclockwise

More information

Weather Technology in the Cockpit (WTIC) Shortfall Analysis of Weather Information in Remote Airspace Friends and Partners of Aviation Weather Summer

Weather Technology in the Cockpit (WTIC) Shortfall Analysis of Weather Information in Remote Airspace Friends and Partners of Aviation Weather Summer Weather Technology in the Cockpit (WTIC) Shortfall Analysis of Weather Information in Remote Airspace Friends and Partners of Aviation Weather Summer Meeting Tim Myers Metron Aviation August 26, 2015 2

More information

1st Tornado Photograph

1st Tornado Photograph Lecture 26 Part II Tornados Environment Storm Structure Life Cycle Source of Spin Forecasting Climatology Damage Marilee Thomas of Beaver City, NE took this photograph of her daughter Audra about two miles

More information

SATELLITE SIGNATURES ASSOCIATED WITH SIGNIFICANT CONVECTIVELY-INDUCED TURBULENCE EVENTS

SATELLITE SIGNATURES ASSOCIATED WITH SIGNIFICANT CONVECTIVELY-INDUCED TURBULENCE EVENTS SATELLITE SIGNATURES ASSOCIATED WITH SIGNIFICANT CONVECTIVELY-INDUCED TURBULENCE EVENTS Kristopher Bedka 1, Wayne Feltz 1, John Mecikalski 2, Robert Sharman 3, Annelise Lenz 1, and Jordan Gerth 1 1 Cooperative

More information

Exam 2 Results (20% toward final grade)

Exam 2 Results (20% toward final grade) Exam 2 Results (20% toward final grade) Score between 90-99: 6 students (3 grads, 3 under) Score between 80-89: 2 students Score between 70-79: 3 students Score between 60-69: 2 students Below 59: 1 student

More information

III. Section 3.3 Vertical air motion can cause severe storms

III. 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 information

The Ice Crystal Weather Threat to Engines

The Ice Crystal Weather Threat to Engines Jeanne Mason Boeing Commercial Airplanes The Ice Crystal Weather Threat to Engines BOEING is a trademark of Boeing Management Company. Filename.ppt 1 Agenda Introduction Recognition of engine power-loss

More information

P3.17 THE DEVELOPMENT OF MULTIPLE LOW-LEVEL MESOCYCLONES WITHIN A SUPERCELL. Joshua M. Boustead *1 NOAA/NWS Weather Forecast Office, Topeka, KS

P3.17 THE DEVELOPMENT OF MULTIPLE LOW-LEVEL MESOCYCLONES WITHIN A SUPERCELL. Joshua M. Boustead *1 NOAA/NWS Weather Forecast Office, Topeka, KS P3.17 THE DEVELOPMENT OF MULTIPLE LOW-LEVEL MESOCYCLONES WITHIN A SUPERCELL Joshua M. Boustead *1 NOAA/NWS Weather Forecast Office, Topeka, KS Philip N. Schumacher NOAA/NWS Weather Forecaster Office, Sioux

More information

P12.6 Multiple Modes of Convection in Moderate to High Wind Shear Environments

P12.6 Multiple Modes of Convection in Moderate to High Wind Shear Environments P12.6 Multiple Modes of Convection in Moderate to High Wind Shear Environments Adam J. French and Matthew D. Parker North Carolina State University, Raleigh, North Carolina 1. INTRODUCTION A principle

More information

Lawrence Carey 1, William Koshak 2, Harold Peterson 3, Retha Matthee 1 and A. Lamont Bain 1 1

Lawrence Carey 1, William Koshak 2, Harold Peterson 3, Retha Matthee 1 and A. Lamont Bain 1 1 Lawrence Carey 1, William Koshak 2, Harold Peterson 3, Retha Matthee 1 and A. Lamont Bain 1 1 Department of Atmospheric Science, University of Alabama in Huntsville (UAH), Huntsville, AL 2 Earth Science

More information

Examination #3 Wednesday, 28 November 2001

Examination #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 information

U.S. WIND, SCS, FLOOD, WINTER WEATHER

U.S. WIND, SCS, FLOOD, WINTER WEATHER U.S. WIND, SCS, FLOOD, WINTER WEATHER An unusually strong winter storm crossing the Central Plains continues to bring winter weather, strong winds, heavy precipitation and severe thunderstorms to areas

More information

DEPARTMENT OF EARTH & CLIMATE SCIENCES SAN FRANCISCO STATE UNIVERSITY. Metr Fall 2014 Test #1 September 30, 2014

DEPARTMENT OF EARTH & CLIMATE SCIENCES SAN FRANCISCO STATE UNIVERSITY. Metr Fall 2014 Test #1 September 30, 2014 DEPARTMENT OF EARTH & CLIMATE SCIENCES SAN FRANCISCO STATE UNIVERSITY NAME Metr 302.02 Fall 2014 Test #1 September 30, 2014 200 pts (4 pts each answer) Part I. Surface Chart Interpretation. Questions 1

More information

Weather - is the state of the atmosphere at a specific time & place

Weather - 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 information

Reading. What meteorological conditions precede a thunderstorm? Thunderstorms: ordinary or single cell storms, multicell storms, supercell storms

Reading. 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 information

Flight Dispatcher Aviation Meteorology Required Knowledge

Flight Dispatcher Aviation Meteorology Required Knowledge Flight Dispatcher Aviation Meteorology Required Knowledge 3.1 THE EARTH'S ATMOSPHERE 1 Properties 2 Vertical Structure 3 ICAO Standard Atmosphere 3.2 ATMOSPHERIC PRESSURE 1 Pressure Measurements 2 Station

More information

Charles A. Doswell III, Harold E. Brooks, and Robert A. Maddox

Charles A. Doswell III, Harold E. Brooks, and Robert A. Maddox Charles A. Doswell III, Harold E. Brooks, and Robert A. Maddox Flash floods account for the greatest number of fatalities among convective storm-related events but it still remains difficult to forecast

More information

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 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 information

Page 1. Name:

Page 1. Name: Name: 1) As the difference between the dewpoint temperature and the air temperature decreases, the probability of precipitation increases remains the same decreases 2) Which statement best explains why

More information

Traffic and Weather. Soaring Safety Foundation. Tom Johnson CFIG

Traffic and Weather. Soaring Safety Foundation. Tom Johnson CFIG Traffic and Weather Soaring Safety Foundation Tom Johnson CFIG Weather Contents Weather Gathering Sources Weather Acquisition Enroute Weather Analysis Weather Hazards Weather in the Landing Pattern Basic

More information

WEATHER FORECASTING Acquisition of Weather Information WFO Regions Weather Forecasting Tools Weather Forecasting Tools Weather Forecasting Methods

WEATHER FORECASTING Acquisition of Weather Information WFO Regions Weather Forecasting Tools Weather Forecasting Tools Weather Forecasting Methods 1 2 3 4 5 6 7 8 WEATHER FORECASTING Chapter 13 Acquisition of Weather Information 10,000 land-based stations, hundreds of ships and buoys; four times a day, airports hourly Upper level: radiosonde, aircraft,

More information

Meteorology Lecture 18

Meteorology 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 information

DEPARTMENT 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 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 information

ATS 351, Spring 2010 Lab #9 Weather Radar - 55 points

ATS 351, Spring 2010 Lab #9 Weather Radar - 55 points ATS 351, Spring 2010 Lab #9 Weather Radar - 55 points 1. (5 points) If a radar has a maximum unambiguous range of 300km, what is its PRF? (The speed of light, c, is equal to 3x10 8 m/s) 2. (5 points) Explain

More information

Meteorology. Review Extreme Weather a. cold front. b. warm front. What type of weather is associated with a:

Meteorology. 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 information

Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 05 SOME OBSERVING INSTRUMENTS. Instrument Enclosure.

Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 05 SOME OBSERVING INSTRUMENTS. Instrument Enclosure. Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology

More information

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 Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds

More information

Weather. Weather Patterns

Weather. 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 information

COLLINS WXR-2100 MULTISCAN RADAR FULLY AUTOMATIC WEATHER RADAR. Presented by: Rockwell Collins Cedar Rapids, Iowa 52498

COLLINS WXR-2100 MULTISCAN RADAR FULLY AUTOMATIC WEATHER RADAR. Presented by: Rockwell Collins Cedar Rapids, Iowa 52498 COLLINS WXR-2100 MULTISCAN RADAR FULLY AUTOMATIC WEATHER RADAR Presented by: Rockwell Collins Cedar Rapids, Iowa 52498 TABLE OF CONTENTS MultiScan Overview....................................................................................1

More information

ANSWER KEY. Part I: Synoptic Scale Composite Map. Lab 12 Answer Key. Explorations in Meteorology 54

ANSWER KEY. Part I: Synoptic Scale Composite Map. Lab 12 Answer Key. Explorations in Meteorology 54 ANSWER KEY Part I: Synoptic Scale Composite Map 1. Using Figure 2, locate and highlight, with a black dashed line, the 500-mb trough axis. Also, locate and highlight, with a black zigzag line, the 500-mb

More information

Doppler Weather Radars and Weather Decision Support for DP Vessels

Doppler Weather Radars and Weather Decision Support for DP Vessels Author s Name Name of the Paper Session DYNAMIC POSITIONING CONFERENCE October 14-15, 2014 RISK SESSION Doppler Weather Radars and By Michael D. Eilts and Mike Arellano Weather Decision Technologies, Inc.

More information

Questions. Making Better Weather-Based Management Decisions. Dual Polarization 5/1/2018

Questions. Making Better Weather-Based Management Decisions. Dual Polarization 5/1/2018 Making Better Weather-Based Management Decisions Brad Jakubowski, brj8@psu.edu Questions Should I irrigate? Should I be scouting for diseases? Can I spray today? Should I syringe? Should we start later

More information

MEA 214 Midterm Exam, Spring 2008 Tuesday 26 February

MEA 214 Midterm Exam, Spring 2008 Tuesday 26 February MEA 214 Midterm Exam, Spring 2008 Tuesday 26 February Name: As usual, feel free to ask me if you are confused about the meaning of any question. Good luck, and have a great spring break! Don t forget that

More information

Weather Patterns and Severe Storms

Weather 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 information

WEATHER THEORY. Stability. In general:

WEATHER 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 information

P3.13 GLOBAL COMPOSITE OF VOLCANIC ASH SPLIT ` WINDOW GEOSTATIONARY SATELLITE IMAGES

P3.13 GLOBAL COMPOSITE OF VOLCANIC ASH SPLIT ` WINDOW GEOSTATIONARY SATELLITE IMAGES P3.13 GLOBAL COMPOSITE OF VOLCANIC ASH SPLIT ` WINDOW GEOSTATIONARY SATELLITE IMAGES Frederick R. Mosher * Embry-Riddle Aeronautical University Daytona Beach, FL 1.0 Introduction Volcanic ash is exceptionally

More information

The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter

The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter S. Ellis 1*, R. Rauber 2, P. Tsai 1, J. Emmett 1, E. Loew 1, C. Burghart 1, M. Dixon 1, J. Vivekanandan

More information

Earth and Atmospheric Sciences. Sky condition. Prof. J. Haase EAS535 EAS535

Earth and Atmospheric Sciences. Sky condition. Prof. J. Haase EAS535 EAS535 Sky condition Prof. J. Haase Federal Meteorological Handbook http://www.ofcm.gov/fmh-1/fmh1.htm Estimating cloud height Report cloud levels to nearest 100 feet below 5000 feet (in practice, human observers

More information

Journal of Operational Meteorology Article Extreme Snowfall Variations and Cold-Air Damming in the Front Range Heavy Snowstorm of March 2003

Journal of Operational Meteorology Article Extreme Snowfall Variations and Cold-Air Damming in the Front Range Heavy Snowstorm of March 2003 Wesley, D. A., G. Poulos, J. Snook, P. Kennedy, M. Meyers, and G. Byrd, 2013: Extreme snowfall variations and cold-air damming in the Front Range heavy snowstorm of 17 19 March 2003. J. Operational Meteor.,

More information

WEATHER MODIFICATION ARTIFICIAL RAIN MAKING AND CLOUD SEEDING. Research done in this field goes back to as far as the early 1940s when the US military

WEATHER MODIFICATION ARTIFICIAL RAIN MAKING AND CLOUD SEEDING. Research done in this field goes back to as far as the early 1940s when the US military WEATHER MODIFICATION ARTIFICIAL RAIN MAKING AND CLOUD SEEDING Weather modification refers to willful manipulation of the climate or local weather. Research done in this field goes back to as far as the

More information

Convective downbursts are known to produce potentially hazardous weather

Convective downbursts are known to produce potentially hazardous weather Investigation of Convective Downburst Hazards to Marine Transportation Mason, Derek Thomas Jefferson High School for Science and Technology Alexandria, VA Abstract Convective downbursts are known to produce

More information

Thunderstorm. Thunderstorms result from the rapid upward movement of warm, moist air.

Thunderstorm. 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 information

AOG Add On Gauges FSWXR-2100 Users Manual Rev. 1.0 FSWXR Users Manual Rev. 1.0

AOG Add On Gauges FSWXR-2100 Users Manual Rev. 1.0 FSWXR Users Manual Rev. 1.0 FSWXR 2100 Users Manual Rev. 1.0 Realistic simulation of the real Collins WXR2100 for Microsoft Flightsimulator 9 AOG FSWXR2100 Page 1 1. Introduction Weather is the one of uncontrollable factors in aviation.

More information

Chapter 21. Weather Patterns and Severe Storms

Chapter 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 information

Evolution and Maintenance of the June 2003 Nocturnal Convection

Evolution and Maintenance of the June 2003 Nocturnal Convection Evolution and Maintenance of the 22-23 June 2003 Nocturnal Convection Jerilyn Billings NOAA/NWS Wichita, KS August 6 th, 2011 Work Completed at North Carolina State University for MS Thesis During the

More information

USE OF AIRCRAFT-BASED DATA TO EVALUATE FACTORS IN PILOT DECISION MAKING IN ENROUTE AIRSPACE

USE OF AIRCRAFT-BASED DATA TO EVALUATE FACTORS IN PILOT DECISION MAKING IN ENROUTE AIRSPACE USE OF AIRCRAFT-BASED DATA TO EVALUATE FACTORS IN PILOT DECISION MAKING IN ENROUTE AIRSPACE Bradley Crowe Rich DeLaura Michael Matthews Massachusetts Institute of Technology, Lincoln Laboratory Lexington,

More information

1 August 2006 An Investigation of a Bow Echo along the Wasatch Front. Randy Graham and Chris Gibson 6 April 2007

1 August 2006 An Investigation of a Bow Echo along the Wasatch Front. Randy Graham and Chris Gibson 6 April 2007 1 August 2006 An Investigation of a Bow Echo along the Wasatch Front Randy Graham and Chris Gibson 6 April 2007 Overview Environment review Review of terrain-induced discrete propagation Bow Echo interactions

More information

HAZARDOUS WEATHER 1. Dr. Julie Laity Geography 266

HAZARDOUS 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 information

KANSAS CLIMATE SUMMARY January 2018

KANSAS CLIMATE SUMMARY January 2018 KANSAS CLIMATE SUMMARY January 2018 Some welcome moisture After an extended period with little to no moisture, parts of Kansas recorded some significant precipitation. At Tribune, a small snow event on

More information

STUDY UNIT SEVENTEEN GRAPHICAL AIRMAN S METEOROLOGICAL ADVISORY (G-AIRMET)

STUDY UNIT SEVENTEEN GRAPHICAL AIRMAN S METEOROLOGICAL ADVISORY (G-AIRMET) STUDY UNIT SEVENTEEN GRAPHICAL AIRMAN S METEOROLOGICAL ADVISORY (G-AIRMET) 341 (10 pages of outline) 17.1 Product Description....................................................... 341 17.2 Issuance...............................................................

More information

CHAPTER 11 THUNDERSTORMS AND TORNADOES MULTIPLE CHOICE QUESTIONS

CHAPTER 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 information

MET 3502 Synoptic Meteorology. Lecture 8: September 16, AIRMASSES, FRONTS and FRONTAL ANALYSIS (2)

MET 3502 Synoptic Meteorology. Lecture 8: September 16, AIRMASSES, FRONTS and FRONTAL ANALYSIS (2) MET 3502 Synoptic Meteorology Lecture 8: September 16, 2010 AIRMASSES, FRONTS and FRONTAL ANALYSIS (2) Identifying a cold front on a surface weather map: 1. Surface front is located at the leading edge

More information

Sample Q4. Name: Class: Date: Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.

Sample Q4. Name: Class: Date: Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. Name: Class: Date: Sample Q4 Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The Fujita scale pertains to a. the size of a tornado producing

More information

3. As warm, moist air moves into a region, barometric pressure readings in the region will generally 1. decrease 2. increase 3.

3. As warm, moist air moves into a region, barometric pressure readings in the region will generally 1. decrease 2. increase 3. Teacher: Mr. Prizzi Castle Learning Review 1 1. Which process most directly results in cloud formation? 1. condensation 3. precipitation 2. transpiration 4. radiation 2. An air mass originating over north

More information

THE MESOSCALE CONVECTIVE SYSTEM FROM

THE MESOSCALE CONVECTIVE SYSTEM FROM RISCURI I CATASTROFE, NR.X, VOL.9, NR. 1/2011 THE MESOSCALE CONVECTIVE SYSTEM FROM 24.07.2010 ELZA HAUER, 1 C. NICHITA 1 ABSTRACT. The Mesoscale Convective System from 24.07.2010. A severe weather event

More information