Not exact matches
The orbit of a body is described
by a
curve, given algebraically
by an
equation determining a «coordination» between two orders, that of the position, x, and that of the time, t.
the law of the continuous movement
by which the
curve is generated) to the
equation of the tangent giving its instantaneous direction.
Revision sheets sorted
by topic Algebra and functions Quadratics
Equations and inequalities Sketching
curves Coordinate geometry Sequences and series Differentiation Integration
The lesson includes: Starter - a quick question on area to get students occupied as they come in and thinking Learning Objectives - differentiated
by outcome Key Notation - explanation and detail given as this is often an area of confusion Teaching slides showing the process of integrating and substituting to find an original
equation and some superb graphics and slides to teach about the area under the
curve.
Sea level from
equations (3.3) and (3.4) is shown
by the blue
curves in figure 2, including comparison (figure 2c) with the Late Pleistocene sea - level record of Rohling et al. [47], which is based on analysis of Red Sea sediments, and comparison (figure 2b) with the sea - level chronology of de Boer et al. [46], which is based on ice sheet modelling with the δ18O data of Zachos et al. [4] as a principal input driving the ice sheet model.
From
Equation (7), Y = A ˜ / (X) b, if we divide the average weighted level
curve of satisfaction
by A ˜, we obtain the average adjusted weighted level
curve of satisfaction over time:
By dividing each country's weighted level curve by the average weighted level curve of satisfaction over time in Equation (7), Y = A ˜ / (X) b, we obta
By dividing each country's weighted level
curve by the average weighted level curve of satisfaction over time in Equation (7), Y = A ˜ / (X) b, we obta
by the average weighted level
curve of satisfaction over time in
Equation (7), Y = A ˜ / (X) b, we obtain