Inertial & Non-Inertial Frames

Slides:



Advertisements
Similar presentations
Chapter 10 Geostrophic Balance.
Advertisements

Physics 430: Lecture 21 Rotating Non-Inertial Frames
Global and Local Winds.
Global and Local Winds.
Air Pressure and Winds III
Fronts and Coriolis. Fronts Fronts - boundaries between air masses of different temperature. –If warm air is moving toward cold air, it is a “warm front”.
Wind and the Coriolis Effect
Atmospheric Motion ENVI 1400: Lecture 3.
Wind.
Natural Environments: The Atmosphere
Chapter 10: Atmospheric Dynamics
What Makes the Wind Blow? ATS 351 Lecture 8 October 26, 2009.
Circular Motion and Other Applications of Newton’s Laws
Outline for Lecture 13 Factors Affecting Wind
AOSS 321, Winter 2009 Earth System Dynamics Lecture 8 2/3/2009 Christiane Jablonowski Eric Hetland
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!
Atmospheric Force Balances
Named after the French Scientist Gaspard Gustave Coriolis Because of the Earth’s rotation, free moving objects … deflected to the right in the Northern.
Sect. 4.10: Coriolis & Centrifugal Forces (Motion Relative to Earth, mainly from Marion)
NATS 101 Section 13: Lecture 15 Why does the wind blow? Part I.
Wind and the Coriolis Effect
Atmospheric Motion SOEE1400: Lecture 7. Plan of lecture 1.Forces on the air 2.Pressure gradient force 3.Coriolis force 4.Geostrophic wind 5.Effects of.
Global Wind Patterns. What is Wind? Wind is the movement of air from an area of higher pressure to an area of lower pressure. Warmer air expands, becoming.
Lecture 7 Forces (gravity, pressure gradient force)
Circular Motion and Other Applications of Newton’s Laws
Winds What causes winds?.
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.
Air Pressure and Winds II. RECAP Ideal gas law: how the pressure, the temperature and the density of an ideal gas relay to each other. Pressure and pressure.
Coriolis Effect. 2. Evidence for Rotation Coriolis Effect – the tendency of objects moving over the earth (air, water, planes, projectiles) to be deflected.
Global Wind Belts & the Jet Stream
Inertial & Non-Inertial Frames
Rotation and Revolution
Chapter 15 Section 3 Global and Local Winds.
Dynamics I: Basic forces
Wind and the Coriolis Effect
Winds
Global and Local Winds.
The Coriolis Effect.
Understand Land & Sea Breezes and their cause Unit 3
The Coriolis Force QMUL Interview 7th July 2016.
Dynamics in Earth’s Atmosphere
Handout (green) Atmospheric Circulation
Wind and the Coriolis Effect
Wind and Currents Heat from the sun makes wind. Wind causes currents and waves. Winds are named based on where they start.
Atmospheric Circulation
Global and Local Winds Why does Air Move ?
Wind and the Coriolis Effect
Wind and the Coriolis Effect
The Transfer of Heat Outcomes:
Global and Local Winds.
Global and Local Winds Why does Air Move ?
Wind.
Wind.
Wind.
Wind.
Winds What causes winds?.
Winds What causes winds?.
AOSS 401, Fall 2013 Lecture 3 Coriolis Force September 10, 2013
Wind.
Winds What causes winds?.
Dynamics III: Earth rotation L. Talley SIO 210 Fall, 2016
Global and Local Winds.
Wind and the Coriolis Effect
Isobars and wind barbs sea level pressure.
Wind.
Warm up What is the difference between conduction, convection, and radiation? What is wind?
WIND Pages
Winds What causes winds?.
Wind.
Global and Local Winds Why does Air Move ?
Presentation transcript:

Inertial & Non-Inertial Frames PGGC-11 DR BHANDARI

Inertial Reference Frame: Any frame in which Newton’s Laws are valid Any reference frame moving with uniform motion (non-accelerated) with respect to an “absolute” frame “fixed” with respect to the stars. Perfect Inertial Frame: The objects/bodies in the universe interact via Gravitational Forces and are present everywhere but are very weak. Hence we can neglect these forces. Best Approximation: Intergalatic space Non-Inertial Reference Frame: Is a frame of reference with a changing velocity. The velocity of a frame will change if the frame speeds up, or slows down, or travels in a curved path. is an accelerating frame of reference. is a frame of reference in which Newton's laws of motion do not hold. In a non-inertial frame of reference fictitious forces arise. PGGC-11 DR BHANDARI

Forces in a Rotating Frame Let’s take the Earth as the rotating frame. The angular frequency of rotation of the Earth is We will assume that the inertial frame S and rotating frame S’, so the only motion of S’ relative to S is a rotation with angular velocity ω. Newton's laws of motion govern the motion of an object in a (non-accelerating) inertial frame of reference. When Newton's laws are transformed to a uniformly rotating frame of reference, the Coriolis and centrifugal forces appear. PGGC-11 DR BHANDARI

Both forces are proportional to the mass of the object. The Coriolis force is proportional to the rotation rate and the centrifugal force is proportional to its square. The Coriolis force acts in a direction perpendicular to the rotation axis and to the velocity of the body in the rotating frame and is proportional to the object's speed in the rotating frame. The centrifugal force acts outwards in the radial direction and is proportional to the distance of the body from the axis of the rotating frame. These additional forces are termed inertial forces, fictitious forces or pseudo forces. They are correction factors that do not exist in a non-accelerating or inertial reference frame. The Coriolis effect is a deflection of moving objects when they are viewed in a rotating reference frame. the mathematical expression for the Coriolis force was given by French scientist Gaspard-Gustave Coriolis. PGGC-11 DR BHANDARI

Effect of Centrifugal force on g w q r w × r mg Non-Vertical Gravity Due to the centrifugal force, a plumb bob does not actually point in the direction to the center of the Earth except at the pole or equator. mge O E S PGGC-11 DR BHANDARI

Coriolis Force Coordinate system at latitude θ with x-axis east, y- axis north and z-axis upward (radially outward from center of sphere). PGGC-11 DR BHANDARI

Main effect will be due to horizontal component of Fcor Vertical comp. is along +ve z-direction, i.e. it acts in a direction opposite to acceleration due to gravity. So its effect will be neglected in most cases. Y vx O X Deflected path Y vy Deflected path O X i.e., particle will always be deflected towards its right in N-hemisphere. PGGC-11 DR BHANDARI

RIGHT-HAND RULE two vectors a and b that has a result which is a vector c perpendicular to both a and b. With the thumb, index, and middle fingers at right angles to each other (with the index finger pointed straight), the middle finger points in the direction of c when the thumb represents a and the index finger represents b. PGGC-11 DR BHANDARI

Direction of the Coriolis Force Case 1: in N-hemisphere If body is moving towards NORTH Coriolis force: EASTWARD Case 2: in N-hemisphere If body is moving towards SOUTH Coriolis force: WESTWARD for any body moving on the surface of the earth in the NORTHERN-hemisphere, the coriolis force deflects it to the RIGHT for any body moving on the surface of the earth in the SOUTHERN-hemisphere, the coriolis force deflects it to the LEFT PGGC-11 DR BHANDARI

Effect of Coriolis Force on Freely Falling objects Consider an object at the surface of the Earth in free-fall with no other forces acting (i.e. no air resistance), then deflection due to coriolis force is And coriolis acceleration is And therefore direction of deflection will also be along east and deflection is independent of mass of the object. PGGC-11 DR BHANDARI

Coriolis Effect For air travelling northwards in the northern hemisphere, there is an eastward acceleration For air travelling southwards in the northern hemisphere, there is a westward acceleration (always deflected towards RIGHT) For air travelling northwards in the southern hemisphere, there is an westward acceleration For air travelling southwards in the southern hemisphere, there is a eastward acceleration (always deflected towards LEFT) PGGC-11 DR BHANDARI

Coriolis Effect If air moves in east- west direction If it moves eastward, it would take less time to complete one entire rotation as it is travelling faster than the earth’s surface If it moves westward, it is opposing the earth’s rotation and would take longer to complete a rotation PGGC-11 DR BHANDARI

Geographical effects of Coriolis Force The Coriolis effect is caused by the rotation of the Earth and the inertia of the mass experiencing the effect. Because the Earth completes only one rotation per day, the Coriolis force is quite small, and its effects generally become noticeable only for motions occurring over large distances and long periods of time, such as large-scale movement of air in the atmosphere or water in the ocean. PGGC-11 DR BHANDARI

since Coriolis force depends on the velocity, the force would be minimum for something moving as slowly as a cloud in the atmosphere. However, a small force does not necessarily mean a small effect. The force on a slowly moving body can act over a long period of time (weeks in the case of a weather pattern), and so the effect can be important. PGGC-11 DR BHANDARI

Deflection of river water The water of rivers in N-hemisphere, which are flowing from north to south experience a deflection towards right bank (west). Hence right bank of such rivers is steeper than left bank. If river flows from south to north in N-hemisphere then deflection will be towards east, right bank of such rivers is steeper than left bank. In southern hemisphere, left bank of rivers will be steeper than right bank. PGGC-11 DR BHANDARI

Air pressure differences cause the movement of air Air moving parallel to the ground is called wind Winds are created because of the uneven heating the Earth As discussed before, air moves from high pressure to low pressure Areas that are warmer are low pressure areas, so wind blows toward low pressure Areas that are colder are high pressure areas, so wind blows away from high pressure Air moving up or down is called a current PGGC-11 DR BHANDARI

But the air doesn’t flow in a straight line Air generally moves from the poles to the equator, this is because air flows from high pressure to low pressure High pressure forms when cold air sinks (at the poles) Low pressure forms when warm air rises (at the equator) But the air doesn’t flow in a straight line PGGC-11 DR BHANDARI

Occurrence of Cyclones If planet: non-rotating, then, winds and currents tend to flow directly from areas of high pressure to low pressure But due to rotation of planet, coriolis force act due to which Rather than flowing directly from areas of high pressure to low pressure, winds and currents tend to flow to the right of this direction north of the equator, causing an Anticlockwise rotation around the low-pressure region. This effect is responsible for the rotation of large cyclones. In southern hemisphere, deflection of air is towards left , causing an Clockwise rotation around the low-pressure region. On equator, horizontal comp. of coriolis force =0, therefore no cyclones set up at equator. PGGC-11 DR BHANDARI