Named after the French Scientist Gaspard Gustave Coriolis Because of the Earth’s rotation, free moving objects … deflected to the right in the Northern.

Slides:



Advertisements
Similar presentations
What we now know: Difference between weather and climate.
Advertisements

Chapter 8 (part II). Forces that Influence Winds Pressure Gradient Force: difference in pressure over distance Directed perpendicular to isobars from.
Factors Affecting Wind
Class #5: Air pressure and winds Chapter 8 1Class #5 Tuesday, July 13, 2010.
Chapter 4. Atmospheric Pressure and Wind
Chapter 13 The Atmosphere in Motion
What Makes the Wind Blow?
Air Pressure and Winds III
Warm Up 3/21/08 The deflection of wind due to the Coriolis effect is strongest at ____. a. the poles c. midnight b. the equator d. the midlatitudes.
AtmosphericCirculation Patterns Atmospheric Circulation Patterns Ally, Molly, Joe Atmosphere Jigsaw.
 XQ No Foldable – put in your journals; use markers or highlighters as needed.
Recitation Geostrophic Balance Thermal Wind Effect of Friction.
WIND Wind is movement of air caused by differences in air pressure.
12.2 Weather Systems Coriolis effect The Coriolis effect, which is a result of Earth’s rotation, causes moving particles such as air to be deflected.
Fronts Weather Systems
Unit 4 – Atmospheric Processes. Winds… Earth’s atmospheric circulation is an important transfer mechanism for both energy and mass The imbalance between.
Weather: A study in Variables Coriolis Effect & Mid- Latitude Cyclones.
Natural Environments: The Atmosphere
Chapter 10: Atmospheric Dynamics
What Makes the Wind Blow? ATS 351 Lecture 8 October 26, 2009.
Pressure and Winds. Aneroid Barometer Reading Pressure.
EOSC 112: THE FLUID EARTH CORIOLIS EFFECT AND GEOSTROPHY Atm3 Read: Kump et al. Chap.4, p Why do weather / climate vary around the globe? Why is.
Outline for Lecture 13 Factors Affecting Wind
Atmospheric Pressure and Wind. Atmospheric pressure: –force exerted by a column of air per unit area –Normal atmospheric pressure at sea level = 1013.
Air Pressure and Winds Dr. R. B. Schultz. Air Pressure Air pressure is the pressure exerted by the weight of air above. Average air pressure at sea level.
Warning! In this unit, we switch from thinking in 1-D to 3-D on a rotating sphere Intuition from daily life doesn’t work nearly as well for this material!
Geostrophic Balance The “Geostrophic wind” is flow in a straight line in which the pressure gradient force balances the Coriolis force. Lower Pressure.
What Causes the Wind Worksheet.
 What is pressure?  Pressure is accumulative force of gas particles   High Energy gas (HOT) has lots of movement, therefore.
Midterm #1 on Thursday!! - Bring your catcard
Weather Water Cycle: the continuous movement of water between the atmosphere, the land, and the oceans Evaporation occurs when solar energy heats water.
WIND Factors Affecting Wind  Wind is the result of horizontal differences in air pressure. Air flows from areas of higher pressure to areas of lower pressure.
Objectives Vocabulary
Guided Notes for Weather Systems
Science News. What is WIND? The horizontal motion of air across Earth’s surface; movement produced by differences in air pressure from an area of high.
Copyright © 2013 Pearson Education, Inc. The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland.
Lecture 5: General Circulation of the Atmosphere Questions? 1.Why do winds blow around a high or a low pressure center? 2.Why does a low area mean more.
Local Winds By Diana L. Duckworth Rustburg High School Campbell County, VA.
Winds Professor Jeff Gawrych De Anza College. Principle forces Q: What drives the weather in the atmosphere? The uneven heating of the earth Q: What causes.
Chapter 6: Air Pressure and Winds Atmospheric pressure Atmospheric pressure Measuring air pressure Measuring air pressure Surface and upper-air charts.
The Wind: PGF Pressure gradient force is what sets air in motion
Understanding Air Pressure
There are 3 major forces that determine how strongly the wind will blow and in what direction: 1. Pressure Gradient Force ◦ push from high pressure to.
Understanding Wind. Review: What is air pressure? Air pressure: the force of the weight of air on a surface – exerted in all directions.
Isobars and wind barbs sea level pressure. factors affecting wind wind is the result of horizontal differences in pressure air flows from higher to lower.
Weather Basics Air Pressure and Winds. Air Pressure Air has a mass and exerts a force called atmospheric pressure Air pressure is measured in millibars.
Warm-Up What is the device used for mearsuring air pressure called?
Inertial & Non-Inertial Frames
The Atmosphere has Wind Patterns.
OCEAN SURFACE CURRENTS
Understanding Air Pressure
12.2 Weather Systems.
Understanding Wind.
Is air moving away or towards each of these pressure centers?
Understanding Wind.
Winds Winds are created by pressure differences – pressure gradients.
Air Pressure Force exerted on an object by the air (molecules).
Air Pressure Force exerted on an object by the air (molecules).
Understanding Air Pressure
Air Pressure And Wind Chapter 19.
12.2 Weather Systems.
Pressure Centers and Winds
QUIZ BONUS List Four types of Air Masses (symbols are accepted)
19.2 Pressure Centers and Winds
Why do air pressures vary?
WIND.
Atmospheric Pressure Force exerted by the weight of the air above
Isobars and wind barbs sea level pressure.
Convection in the Atmosphere: Wind
Intro. to Atmospheric Sciences Plymouth State University
Presentation transcript:

Named after the French Scientist Gaspard Gustave Coriolis Because of the Earth’s rotation, free moving objects … deflected to the right in the Northern Hemisphere to the left in the Southern Hemisphere Depends on an object’s speed—higher speed means stronger Coriolis Force. The Coriolis Force

H L Pressure (mb) A pressure gradient causes wind to blow straight from High P to Low P and accelerate as it goes North Latitude Equator Just a Pressure Gradient

H L Pressure (mb) Wind doesn’t blow straight from High to Low … curves to the right of straight line. North Latitude Equator Pressure, Coriolis Force, Friction Rotation of Earth H and L don’t last forever without energy source … why?

Atmospheric Circulation on Slowly Rotating Earth

Actual flow around pressure systems are never this regular. Cyclonic FlowAnticyclonic Flow Curved Flow around High and Low

Around a surface low pressure center, net inward transport of air causes a convergence … air rises in the center. Cyclones and Anti–Cyclones Around a surface high pressure center, net outward transport of air causes a divergence … air falls in the center.

Anticyclones : high pressures with nearly circular isobars. Air descends toward surface due to convergence aloft. As air nears surface it is forced outward (divergence). Coriolis effect bends air to the right of its path creating a clockwise rotation. Under an anticyclone, air is descending, forming an area of higher pressure at the surface. Cloud formation is inhibited, so the weather is usually settled with only small amounts of cloud cover. Anti–Cyclones

Cyclones: Low pressures that exhibit nearly circular isobars. As air enters low pressure from all directions, Coriolis effect bends wind direction to the right of its path. This creates counterclockwise rotation around the low and convergence near the center. As air collides near center it is forced aloft where divergence takes air away from the center. Upper-level divergence maintains low pressure. Rising air cools,condenses helps cloud formation, so weather associated with cyclone is cloudy and wet. Cyclone

Solid rotation typifies the terrestrial planets: Every part of the object takes exactly the same time to complete one rotation. Differential rotation typifies Jupiter: Particles at different locations in the fluid take different lengths of time to complete one rotation.