Rotating Coordinate Systems based on FW-6,7,8 Sometimes it is useful to analyze motion in a non inertial reference frame, e.g. when the observer is moving (accelerating). Inertial frame: orthonormal coordinate system (fixed) Rotating frame (“body fixed”): fixed 47 Infinitesimal rotations: we need to figure out how the body-fixed vectors change: (as seen from the inertial frame) can be expanded in the original basis we only need three components: similarly for the other two: infinitesimal rotations about each coordinate axes 48 Example: rotation about the 1st axis: 49 Change in an element of time: instantaneous angular velocity vector of the rotating frame as seen in the inertial frame now we know how the body-fixed vectors change: we get an important formula: valid for any vector! 50 operator equation, valid for any vector! Velocity: Rate of change of angular velocity: Acceleration: 51 Adding translations and rotations: if the origin of the body fixed frame is also moving with respect to the origin of the inertial reference frame: 52 Newton’s Laws in Accelerated Frames based on FW-10 Newton’s second law is valid in the inertial reference frame: and is experienced by an observer in accelerated frame as: force from the acceleration of the origin of the body system Coriolis force force from the angular acceleration centrifugal force 53 Motion on the Surface of the Earth . based on FW-11 is a simple example of what we have discussed. m center of the Sun (inertial frame) external forces (gravity from the Sun and from the Earth, and others) angular frequency from the circular trajectory about the Sun and from daily rotation (approximately constant) center of the Earth (rotating frame) 54 rotation of the Earth: gravity from Earth/Sun: circular trajectory about the Sun: Sun’s gravity cancels the second term at the center of the earth approximate equation of motion for a particle on the rotating earth: other forces on earth Coriolis force centrifugal force 55 Particle (stationary) on a scale: at the poles at the equator in spherical polar coordinates: net tangential component points toward the equator 56