1 Carl Schreck Lifecycle Ingredients ClimatologyData.

Slides:



Advertisements
Similar presentations
Severe Weather.
Advertisements

{ How Hurricanes Form Tropical Cyclones.  As you watch the animation, record your observations about the motion of Hurricane Katrina. Hurricane Katrina.
Where Do the Hurricanes Come From?. Radiation Vapor/Cloud/precipitation Shallow convection Boundary layer turbulence Mesoscale convective system Thunderstorm.
Part 4. Disturbances Chapter 12 Tropical Storms and Hurricanes.
Class #7: Monday, September 13, 2010 Hurricanes Chapter 15 1Class #7, Monday. September 13, 2010.
HURRICANE The ancient Tainos tribe of Central America called their god of evil “Huracan.” The Carib Indians adopted this name for the storm.
Planetary Atmospheres, the Environment and Life (ExCos2Y) Topic 8: Storm Systems Chris Parkes Rm 455 Kelvin Building.
I. Hurricanes A.A hurricane is 1. The largest, most powerful storm 2. An intense area of tropical, low pressure 3. A storm with winds of at least, 120.
1 Carl Schreck History El Niño/La Niña Climate Modes.
Hurricanes. Tropical Weather Tropics: the belt between the Tropic of Cancer (23.5N) and the Tropic of Capricorn (23.5S) The weather is very different.
HURRICANE DEVELOPMENT What conditions are required? Water temperatures > 26.5°C Convergence of surface winds Upper air divergence Organized mass of thunderstorms.
Tropical Cyclones - genesis depends on ocean conditions - huge removal of heat energy from ocean - damage primarily from storm surge caused by strong.
Typhoons and tropical cyclones
Hurricane Principles Hurricane Isabel, Outline Definitions Formation and Conditions Needed Growth and Structure of a Hurricane Where do They Form?
CHAPTER 11 HURRICANES.
Hurricanes ATS 351 Lecture 12 November 30, Outline Formation Stages of development Structure of hurricanes Saffir-Simpson scale Movement Dissipation.
Do Now 1. What Factors influence air temperature? 2. What factors influence air pressure? 3. How does air move in and around a low pressure system? 4.
Weather: The state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity and direction,
Where Do the Hurricanes Come From?. Introduction A tropical cyclone is a rapidly- rotating storm system characterized by a low-pressure center, strong.
IntroIntro Objective 04/27/12 Describe the formation of hurricanes. What is the difference between a hurricane, a typhoon, and a cyclone?
+ Effects of Climate Change on Ocean Storms Chloe Mawer.
Weather study guide answer. Humidity  Humidity is the amount of water vapor in air.  The air cannot hold much more water when humidity is high so your.
Chapter 4 Ecosystems and the Physical Environment
Tropical Cyclones and Hurricanes Read Chapter 11
Chapter 15. Tropical Weather  Noon sun is always high, seasonal temperature changes small  Daily heating and humidity = cumulus clouds and afternoon.
Tropical Meteorology I Weather Center Event #4 Tropical Meteorology What is Tropical Meteorology? – The study of cyclones that occur in the tropics.
Chapter 11 Notes Hurricanes. Tropical Storms Boris and Christiana Together-2008 Profile of a Hurrican Most hurricanes form between the latitudes of 5.
Chapter 11: Hurricanes Tropical weather Anatomy of a hurricane
Do Now 2/14/13 1. The hardest mineral is _______ and the softest mineral is ________. 2. The highest point of a wave is called the ________. 3. Nitrogen.
Chapter 11 Hurricanes. Hurricane Katrina Flooded 80% of New Orleans The US’s deadliest hurricane in terms of deaths happened in 1900 in Galveston, Tx.
Hurricanes.
Lecture #2 Weather. Convection and Atmospheric Pressure Much of solar energy absorbed by the Earth is used to evaporate water. – Energy stored in water.
Hurricanes. I. How Hurricanes Form A. Start off the coast of Africa as a Low Pressure System or tropical disturbance B. Warm tropical water in the Atlantic.
© 2011 Pearson Education, Inc. CHAPTER 6 Air-Sea Interaction.
Weather Patterns (57) An air mass is a large body of air that has properties similar to the part of Earth’s surface over which it develops. Six major air.
Severe Storms. Thunderstorms Occur in warm, moist air masses and along fronts. Sinking rain, cooled air, and strong updrafts of warm air cause strong.
Tropical Severe Local Storms Nicole Hartford. How do thunderstorms form?  Thunderstorms result from moist warm air that rises due to being less dense.
Hurricane Formation El Nino. Warm-up: water cycle review. Label the arrows with these terms: What are the 2 possibilities for precipitation that hits.
Hurricanes.
Hurricanes Chapter 13.3.
Earth Science: Unit 1 (mini-unit) Hurricanes and Global Winds.
Chapter 11: Hurricanes Tropical weather Tropical weather Anatomy of a hurricane Anatomy of a hurricane Hurricane formation and dissipation Hurricane formation.
*Refer to Chapter 12 in your Textbook. Learning Goals 1. I can explain how a monsoon forms. 2. I can explain how a cyclone forms. 3. I can compare and.
1 SourcesSources n AWS/TR-95/001 n AWS TR240 n NAVEDTRA 40970/40971 n JTWC Forecasters Handbook n NEPRF TR n Tropical Weather Course (Keesler) n.
Chapter 17 Section 2 Severe Weather.
-Thunderstorms, hurricanes, tornadoes, blizzards, typhoons, cyclones -Dangerous to people, structures, and animals.
Section 1.2 The Causes of Weather
UNIT 1: Weather Dynamics Chapter 1: Inquiring about Weather The Causes of Weather Chapter 2: Weather Forecasting.
IV. Hurricanes. A. Introduction 1. June-November is hurricane season 2. hurricane- massive rotating tropical storm with wind speeds of 119 kilometers.
Severe Weather 1.Thunderstorms 2.Tornadoes 3.Hurricanes.
© 2014 Pearson Education, Inc. Chapter 6 Air-Sea Interaction.
Classwork Students will take turns reading a paragraph and another student will summarize for the group what was just read. After reading the section,
Chapter 11 Hurricanes. What is a hurricane? Fig Winds ≥74 mph Winds ≥74 mph Typically 300 miles in diameter Typically 300 miles in diameter HurricanesHurricanes.
Atmospheric Disturbances
HURRICANES. Hurricane – a rotating tropical storm with winds of at least 74 mph that develops over the Atlantic or Eastern Pacific oceans Called cyclones.
HURRICANES Source:
I. Hurricanes A hurricane is 1. The largest, most powerful storm
Chapter 13.1 Thunderstorms
Section 1.2 The Causes of Weather
Hurricanes
Madeline Frank EAS 4480 Course Project April 2016
The Nature of Storms Topic 7.
Hurricanes
How Hurricanes Form Tropical Cyclones.
Hurricanes This chapter discusses:
Patterns of Ocean Circulation
16: Severe Weather Unit 6: Meteorology March 13, 2012 Sanders.
Hurricanes
Presentation transcript:

1 Carl Schreck Lifecycle Ingredients ClimatologyData

2 Lifecycle Ingredients ClimatologyData

3  Winds < 35 kts  Numbered, but not named  Semi-organized group of thunderstorms Lifecycle Ingredients ClimatologyData

4  Winds 35–63 kts  ≈ 11 per year in the Atlantic  Named  More circular/spiral, but no eye Lifecycle Ingredients ClimatologyData

5  Winds ≥ 64 kts  ≈ 6 per year in the Atlantic  Eye develops  Different names around the world:  Hurricane in the Atlantic and East Pacific  Typhoon in West Pacific  Cyclone in Indian Ocean and South Pacific  “Tropical Cyclone” is the generic/scientific term Lifecycle Ingredients ClimatologyData

6  Winds ≥ 96 kts  ≈ 2-3 per year in the Atlantic  Category 3–5 on the Saffir–Simpson Scale  Strong and dangerous storms  Well-defined, circular eye Lifecycle Ingredients ClimatologyData

7  Deep warm ocean layer  Warm oceans are the energy source for hurricanes  But hurricanes can mix cold water upward if the warm water is too shallow  Conditionally unstable atmosphere  Warm air rises, but only if it’s warmer than its surroundings  Moist mid-troposphere  Dry air 2-3 km from the surface can cause cold downdrafts ww2010.atmos.uiuc.edu Lifecycle Ingredients ClimatologyData

8  Pre-existing convection  Needs organized thunderstorms to get things going  Cyclonic low-level vorticity  Counter-clockwise spinning winds help organize the thunderstorms  Associated with low pressure  Weak vertical wind shear  Tilting winds can knock the storm over Lifecycle Ingredients ClimatologyData

9  Wind shear is defined as the wind vector difference between the 850 and 200 mb level (arbitrary) High westerly shearLow easterly shear In general, low values (< 20 kt) of vertical wind shear are desired. Bad – convection torn apart Good – latent heat can concentrate in one area Courtesy of C.C. Hennon, UNC Asheville Lifecycle Ingredients ClimatologyData

10  Thunderstorm systems with wave-like properties  Move westward with a period of 3–6 days  Common over West Africa  Provides storms with cyclonic vorticity and convection Berry et al. (2007, Mon. Wea. Rev.) Lifecycle Ingredients ClimatologyData

11  Warm Ocean Temperatures  Supply of Tropical Waves from Africa  10°N to 20°N  20°W to 60°W or 80°W Lifecycle Ingredients ClimatologyData

12  Dry air from Sahara can weaken storms  Dust blocks the sun and cools the ocean Zipser et al. (2009, BAMS) climate.nasa.gov Lifecycle Ingredients ClimatologyData

13 Knapp et al. (2010, BAMS) Lifecycle Ingredients ClimatologyData

14  Bars depict number of named systems (open/yellow), hurricanes (hatched/green), and category 3 or greater (solid/red), nhc.noaa.gov/climo Lifecycle Ingredients ClimatologyData

15 Lifecycle Ingredients ClimatologyData

16 Lifecycle Ingredients ClimatologyData

17 Lifecycle Ingredients ClimatologyData

18 Lifecycle Ingredients ClimatologyData

19 Lifecycle Ingredients ClimatologyData

20 Lifecycle Ingredients ClimatologyData

21 Lifecycle Ingredients ClimatologyData

22  Historical record of tropical cyclone locations and intensities  Constructed after each season by the warning agencies  Best estimate using all available data nhc.noaa.gov Lifecycle Ingredients ClimatologyData

23  Weather stations  Buoys  Ships  Radar  Aircraft Reconnaissance  Visible/Infrared Satellites  Microwave satellites  Satellite estimates account for vast majority of the record Courtesy of Jack Beven (NOAA/NHC) Lifecycle Ingredients ClimatologyData

24  Weather stations  Buoys  Ships  Radar  Aircraft Reconnaissance  Visible/Infrared Satellites  Microwave satellites  Satellite estimates account for vast majority of the record Courtesy of Jack Beven (NOAA/NHC) Lifecycle Ingredients ClimatologyData

25 Which image on the right is the closest match for this image of Hurricane Katrina?