Hurricane Visualizations: Modeling Conceptual Change ESPIRIT II: SV Saturday, March 7 th, 2009.

Slides:



Advertisements
Similar presentations
Hurricanes.
Advertisements

Most Hurricanes are Category 1-3 on the Saffir-Simpson scale. Few are 4 & climatology.
Science 4 Mr. Fraser By: Enrique Mayan and Erik Arias.
Chapter 11: Hurricanes Tropical weather Tropical weather Anatomy of a hurricane Anatomy of a hurricane Hurricane formation and dissipation Hurricane formation.
Part 4. Disturbances Chapter 12 Tropical Storms and Hurricanes.
Class #7: Monday, September 13, 2010 Hurricanes Chapter 15 1Class #7, Monday. September 13, 2010.
Tropical Storms. Tropical Cyclone Tropical cyclones are large, rotating, low- pressure storms that form over water during summer and fall in the tropics.
By:Ashleigh Richardson. Hurricanes are severe tropical storms that form in the southern Atlantic Ocean, Caribbean Sea, Gulf of Mexico, and in the eastern.
Planetary Atmospheres, the Environment and Life (ExCos2Y) Topic 8: Storm Systems Chris Parkes Rm 455 Kelvin Building.
Today Hurricanes Beginning of a video –the video will be at the library (“Hurricane Katrina: the storm that drowned a city”) on reserve in media services.
HURRICANE DEVELOPMENT What conditions are required? Water temperatures > 26.5°C Convergence of surface winds Upper air divergence Organized mass of thunderstorms.
Severe Weather. Hurricanes, Thunderstorms, and Tornadoes.
Tropical Cyclones Also: Hurricanes, Typhoons. Tropical Cyclone Ingredients Light winds  instability along I.T.C.Z. High humidity (oceans)  fuel (latent.
Typhoons and tropical cyclones
Lecture 21: Hurricanes Typhoons (Western Pacific) Tropical Cyclones (anywhere) Cyclones (Indian Ocean + others) Hurricanes (near N. America) 4/22/03.
Hurricanes ATS 351 Lecture 12 November 30, Outline Formation Stages of development Structure of hurricanes Saffir-Simpson scale Movement Dissipation.
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?
WEATHER SYSTEMS WEATHER AND CLIMATE.
Tropical Cyclones Lecture 11 November 18, L.
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.
Objective 02/14/2013 Describe global wind patterns. INTRO
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.
Hurricanes Hurricanes form in the water. From space they look like a huge cloud with an eye in the middle. Only a few hurricanes made it to land, when.
Caribbean Disaster Mitigation Project Caribbean Institute for Meteorology and Hydrology Tropical Cyclones Characteristics and Forecasting Horace H. P.
Hurricanes.
Atmospheric Circulation Patterns Unit 2 Section 6
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.
Homeroom READ!. Warm-up  Make a Venn Diagram comparing and contrasting Low Pressure Systems and High Pressure Systems.
Global and Local Winds. Why Air Moves Winds blow from areas of high pressure to areas of low pressure. The greater the pressure difference, the faster.
Hurricane Formation El Nino. Warm-up: water cycle review. Label the arrows with these terms: What are the 2 possibilities for precipitation that hits.
Naval Maritime Forecast Center - Norfolk, 9141 Third Ave, Norfolk VA Tropical Cyclone Quick Reference Guide 2010 Atlantic Tropical Cyclone Season:
GEOG 1112: Weather and Climate Violent Weather. Midlatitude Cyclone Well-organized low pressure system that migrates across a region as it spins Develops.
III. Winds & Fronts v=8i3Zy4u4oxo v=8i3Zy4u4oxo.
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.
Tropical Storms SWBAT identify where tropical cyclones originate; describe the life cycle of a tropical cyclone; recognize the dangers of hurricanes.
A hurricane is a huge storm! It can be up to 600 miles across and have strong winds spiralling inward and upward at speeds of 75 to 200 mph. Each hurricane.
HURRICANES. Ingredients for a hurricane to form: 1. Water temperature 80 ° or more. 2. Surface level low pressure 3. Upper level high pressure. L H.
Tornados Hurricanes And Water Cycles OH MY!! OH MY!!!
Paper 1 Physical Core Atmosphere and Weather 2 GeographyCambridge AS level syllabus 9696.
IV. Hurricanes. A. Introduction 1. June-November is hurricane season 2. hurricane- massive rotating tropical storm with wind speeds of 119 kilometers.
How are hurricanes formed ? A hurricane is a system of low pressure that originates over a tropical area. There are specific conditions that must be present.
Hurricanes Tornadoes  A huge storm that has strong winds that spiral inward and upward at speeds of mph  A violent rotating column of air extending.
© 2014 Pearson Education, Inc. Chapter 6 Air-Sea Interaction.
What Exactly Is a Hurricane? A hurricane can best be described as a huge tropical storm (up to 600 miles in diameter)!
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.
HURRICANES. Hurricane – a rotating tropical storm with winds of at least 74 mph that develops over the Atlantic or Eastern Pacific oceans Called cyclones.
Hurricane Alley Millions of people live, work, and vacation in Hurricane Alley.
What is a Hurricane ? Anatomy of a Hurricane What causes Hurricanes ? For Classroom lessons and hurricane information: SouthEast Atlantic.
Hurricanes (Tropical Cyclones).
Tropical Cyclone Quick Reference Guide 2010
Aim: How are Hurricanes different from large storms?
Aim: How are Hurricanes different from large storms?
Hurricanes and Tornadoes
Hurricanes.
Tropical Cyclone Quick Reference Guide 2010
Hurricanes.
Severe Weather 1.
WEATHER SYSTEMS WEATHER AND CLIMATE.
Tropical Cyclone Quick Reference Guide 2010
Hurricanes.
Tropical Storms and Hurricanes
How Does Air Move?.
Presentation transcript:

Hurricane Visualizations: Modeling Conceptual Change ESPIRIT II: SV Saturday, March 7 th, 2009

Phase 1: Brainstorm – 5 minutes Individually, describe the formation and characteristics (e.g., size, season, features, movement, etc.) of Atlantic basin hurricanes using text descriptions and diagrams on the notepad provided Please print your name in the upper corner of the notepad

Phase II: Collaboration – 5 minutes Self-aggregate into groups of 3 or 4 based on grade level or content area Using phase I product, develop a mutually acceptable group representation of hurricane development and characteristics Select one group member’s notebook to record your understanding – Label as Phase II

Phase III: Web-based Visualizations Multiple Grade Levels – impact selection ◦ weather/hurricanebasics.swf weather/hurricanebasics.swf ◦ f f ◦ cane_explainer/flash.htm cane_explainer/flash.htm ◦ es/framesource_flash.html es/framesource_flash.html ◦ ◦

Phase IV: Modification – 5 minutes As a group, supplement, delete or modify your Phase II product on a new page in the notebook Record in the Phase II notebook and label as Phase IV

Phase V: Target Model Example Grade Level – intro undergrad Formation ◦ Warm water - >80/81/82 to depth 100 m/200 m  unstable air Coriolis Force – 5 degrees N and S of Equator ◦ spin Weak Vertical Wind Shear ◦ humid air aloft Organizational Trigger ◦ airmass front, easterly wave, ITCZ convection

Phase V: Target Model Example Stages ◦ Tropical depression - numbered  <38 mph (<33 kt) ◦ Tropical storm - named  mph (34-63 kt) ◦ Hurricane  > 73 mph (64 kt) Structure ◦ Eye  Avg 300 miles wide, miles, calm ◦ Eyewall  Dense convection, highest winds ◦ Spiral bands  dense bands of thunderstorms ranging from a few miles to tens of miles wide and 50 to 300 miles long

Phase V: Target Model Example Season: June 1-November 30 Movement - hurricane's speed and path depend on complex ocean and atmospheric interactions, complexity of the flow makes it very difficult to predict the speed and direction of a hurricane. ◦ Trade winds, Westerlies, STH, Fronts Conditions ◦ Hurricane-force winds can extend outward to about 25 miles in a small hurricane and to more than 150 miles for a large one. Tropical storm-force winds can stretch out as far as 300 miles from the center of a large hurricane ◦ Worst impacts – right side

Phase V: Target Model Example Categorization – Saffir-Simpson More…min, max, history…

Phase V: Target Model Example – 5 minutes As group assess your Phase IV product with Target Model on new page in notebook Label page Phase V

Phase VI: Selection Criteria and Implementation Considerations – 10 minutes Based on this experience, individually, develop global criteria for selecting visualizations for use during instructional Record criteria in your notebook and label page Phase VI Lastly, consider pedagogical implications for the use of visualizations in your classroom ◦ Record positive and negative implications for use