Identifying systems that can lead to extreme weather events in the Caribbean.

Slides:



Advertisements
Similar presentations
Part 3. Distribution and Movement of Air
Advertisements

The Inter-Tropical Convergence Zone. The greatest amount of rain falls across the coast of West Africa. Here rainfall can exceed 2000mm per year. The.
Global Average Barometric Pressure: January
El Niño.
Convection, Global Winds, and Jet Stream
Wind Notes.
Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 5 Winds and Global Circulation.
Factors Affecting Climate. Latitude How far north or south a place is on Earth can determine what type of climate it has Low latitudes – the area between.
Mid-latitude Climates

The Cayman Islands 2012 Significant Weather Events.
ITCZ ITCZ.
FACTORS INFLUENCING CLIMATE
The General Circulation of the Atmosphere
HURRICANE DEVELOPMENT What conditions are required? Water temperatures > 26.5°C Convergence of surface winds Upper air divergence Organized mass of thunderstorms.
Class #7: Thursday, July 15 Global wind systems Chapter 10 1Class #7, Thursday, July 15, 2010.
Factors which influence climate Today’s Aim - 1.To learn the different factors that affect climate. Keywords Latitude, Equator, Sea Breeze, Prevailing.
Typhoons and tropical cyclones
FACTORS INFLUENCING CLIMATE
Chapter 5: Other Major Current Systems
Climate. What Is Climate? Weather changes from day to day. However, the weather in any area tends to follow a pattern throughout the year. When you describe.
Atmospheric Pressure and Wind. Atmospheric pressure: –force exerted by a column of air per unit area –Normal atmospheric pressure at sea level = 1013.
Surface Currents (ocean) Affect water to a depth of several hundred meters Driven by winds Move in circular patterns in 5 major oceans. Because of Coriolis.
General Atmospheric Circulation
Global Winds and The Jet Streams How do global winds and the jet stream influence weather and climatic conditions?
Chapter 7: Atmospheric Circulations
WEATHER SYSTEMS WEATHER AND CLIMATE.
Chapter 11 Notes Hurricanes. Tropical Storms Boris and Christiana Together-2008 Profile of a Hurrican Most hurricanes form between the latitudes of 5.
GY205 Weather and Climate Lecture 4. Atmospheric Stability Atmospheric Stability Reviewed.
Seasonal Cycle, Monsoons and Tropical Convergence Zones Vernon E. Kousky NOAA/ Climate Prediction Center February 2013.
 Hurricanes are areas of low air pressure that form over oceans in tropical climate regions.  Hurricanes hit land with tremendous force, bringing.
September 20, 2012 Factors that affect climate. LAMECOWS Factors That Effect Climate.
WOW THIS IS FUN!  THE SUN : CLIMATE IS DIRECTLY LINKED TO THE SUN. SOME AREAS RECEIVE MORE OF THE SUN’S HEAT ENERGY THAN OTHERS.  WINDS : MOVEMENT.
Hurricanes.
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.
Climate of Mesoamerica and Caribbean Prepared by Adam Carpenter, based on research by Amy Huff, Battelle.
CLIMATE CHAPTER 3:. All of the world’s climates take place in the atmosphere: 1.its protects us from harmful things from space 2.gives us air 3.gives.
GEOG 1112: Weather and Climate Violent Weather. Midlatitude Cyclone Well-organized low pressure system that migrates across a region as it spins Develops.
MET 10 1 The General Circulation of the Atmosphere.
Weather Phenomena SOL WG.2a.
Ch 17 Section 2 Weather. Atmospheric pressure Atmosphere presses down on you with the equivalent to one kilogram per square centimeter. Pressure is caused.
Ocean Currents Chapter 5 Notes.
 Abnormally high surface ocean temperatures off the coast of South America  Causes unusual weather patterns across the globe El Nino.
Jet Stream S. Ashby. What are Jet Streams? Jet Streams narrow bands of strong wind in upper levels of the atmosphere. The wind blow from west to east.
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
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.
Atmospheric Circulation. Weather & Climate Weather Climate.
Atmospheric Circulation
Normal Conditions The trade winds move warm surface water towards the western Pacific. Cold water wells up along the west coast of South America (the Peru.
Air Masses and ITCZ. Topic 4: Air Masses and ITCZ Global wind circulation and ocean currents are important in determining climate patterns. These are.
Coriolis Effect Because the Earth rotates, and consists of a mixture of land and sea, the Coriolis Effect exists The Coriolis Effect is the movement of.
Atmospheric Circulation. Winds on a Non-Rotating Earth Air at the equator warms and rises. Once aloft, air flows back towards the poles where it cools.
Global Wind Belts.
Ocean/Air interaction
Ch 12 and 13 review game back.
By: Mike Vuotto and Jake Mulholland
Storms!.
Q2 What kinds of information can you get from a weather map?
Local Winds, Global Winds and The Jet Streams
Hurricanes.
700mb HEIGHT ANOMALIES (6/21 - 8/31) 2003 EASTERN NORTH PACIFIC TROPICAL STORM TRACKS Source: National Hurricane Center.
Oceans and Climate Review
WEATHER SYSTEMS WEATHER AND CLIMATE.
Georgia's Climate Chapter 1, Section 3.
Gairloch High School / Invergordon Academy
III. Climate Regions A. The Sun B. Winds
II. Climate Regions A. The Far North B. The Pacific Coast
Global Winds.
Oceanic Circulation and ENSO
Presentation transcript:

Identifying systems that can lead to extreme weather events in the Caribbean

Tropical Depressions, Storms and Hurricanes §Intense and high volume rainfall §Strong winds §Rough seas and surges

Other systems §Tropical waves §Inter-tropical convergence zone §Upper-level troughs §Cold fronts §El Niño-related drought

Tropical Waves §Perturbation in easterly wind flow §Move off the West Coast of Africa §Migrate across the Atlantic §May to October/November §One every 3 to 4 days §Spawn tropical storms and hurricanes §Potential for intense rainfall §Potential for high sea swells

ITCZ §Confluence of NE and SW Trades §Migrates north and south with the sun/seasons §Hot towers §Gives Guyana double rainfall peak §Potential for intense rainfall §Often interacts with Tropical Waves

Upper Level Troughs §Trough in the mid to upper level westerlies §Moves east to west §Interacts with TW which can result in explosive cloud development and intense rainfall

Cold Front Intrusion §Moves from the colder north in the tropics §Brings with it cold air §In the past has been a concern for banana and citrus farmers in Belize §Brings ‘unseasonal’? rainfall as far as eastern Caribbean during the dry season

Preparing/planning for climate variability now provides the initial framework for adaptation to any future change in climate