Chapter 9: Modeling Our World Lecture notes Math 1030 Section A

Similar documents
Student Exploration: Seasons in 3D

NAME; LAB # SEASONAL PATH OF THE SUN AND LATITUDE Hemisphere Model #3 at the Arctic Circle

Field Activitie< for Chapter 5 The Cycle of the Sun

Daylight Data: Days and Nights Around the World

For most observers on Earth, the sun rises in the eastern

Name Homeroom. Science Quiz Day/Night, Sun s Energy, Seasons September 24, 2012

L.O: EARTH'S 23.5 DEGREE TILT ON ITS AXIS GIVES EARTH ITS SEASONS March 21 (SPRING), June 21(SUMMER), Sept 22 (AUTUMN) & Dec 21(WINTER)

Earth-Sun Relationships. The Reasons for the Seasons

Page 1. Name:

November 20, NOTES ES Rotation, Rev, Tilt.notebook. vertically. night. night. counterclockwise. counterclockwise. East. Foucault.

Motion of the Sun. motion relative to the horizon. rises in the east, sets in the west on a daily basis. Basis for the unit of time, the DAY

Seasons and Ecliptic Simulator

Laboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons

Fall equinox means 12 hours of sunlight for everyone, everywhere

Laboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons and Daily Weather

The Seasons. Presented by Kesler Science

Lab 3. Orbital Configurations and Milankovitch Cycles

LAB 2: Earth Sun Relations

Student Exploration: Seasons: Earth, Moon, and Sun

6 - Planetarium. Q1) In what cardinal direction did the Sun rise? Be specific. Q2) Record the time of sunrise and sunset: /

Go to Click on the first animation: The north pole, observed from space

MiSP Astronomy - Seasons Worksheet #1 L2

Which table correctly shows the dates on which the apparent paths of the Sun were observed? A) B) C) D)

The Motion of the Sun in Different Locations

Sunlight and its Properties Part I. EE 446/646 Y. Baghzouz

Fall equinox levels the sunlight playing field all around the world

Viewed from Earth's north pole, the rotation of Earth and its moon are counter-clockwise.!

(1) Over the course of a day, the sun angle at any particular place varies. Why?

Name Period Date L.O: students will be able to describe air temperature and air pressure

Heat Transfer. Energy from the Sun. Introduction

Earth rotates on a tilted axis and orbits the Sun.

Which Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N

Insolation and Temperature variation. The Sun & Insolation. The Sun (cont.) The Sun

Spring 06/MAT 140/Worksheet 1 Name: Show all your work.

Aim: What causes Seasons?

HEATING THE ATMOSPHERE

Solutions Manual to Exercises for Weather & Climate, 8th ed. Appendix A Dimensions and Units 60 Appendix B Earth Measures 62 Appendix C GeoClock 63

THE LIGHT SIDE OF TRIGONOMETRY

Seasonal Path of the Sun and Latitude

THE SEASONS PART I: THE EARTH S ORBIT & THE SEASONS

LAB G - ATMOSPHERE AND CLIMATE LAB I TEMPERATURE AND PRESSURE PRESSURE PORTION

Latitude & Longitude Study Guide

Seasons Page 520. A. What Causes Seasons?

Practice Seasons Moon Quiz

Weather Review. What is the relative humidity when the temperature equals the dew point?

IMPROVING LIGHT PENETRATION FOR GOLF GREENS Scott Robinson ArborCom Technologies Halifax, Nova Scotia

5 - Seasons. Figure 1 shows two pictures of the Sun taken six months apart with the same camera, at the same time of the day, from the same location.

MiSP Astronomy Seasons Worksheet #1 L1

Cartesian Coordinates Need two dimensional system 2 number lines perpendicular to each other X-axis is horizontal Y-axis is vertical Position relative

What causes Earth to have seasons?

Moon, Planet, Star, Solar System, Galaxy, Universe

Bell Ringer: Page 31 Yes...you are skipping pages!!!!

8 - Planetarium. Purpose: To experience the motion of the Sun and the night sky at different times and different locations on Earth.

8.5. Modelling Data with Sinusoidal Functions. INVESTIGATE the Math

Practice Questions: Seasons #1

Lesson 20: The Earth in its Orbit

5 - Seasons. Figure 1 shows two pictures of the Sun taken six months apart with the same camera, at the same time of the day, from the same location.

Earth & Space Science, Interpreting Data DURATION Preparation: 5 minutes Activity: 40 minutes (total over one day)

Tilted Earth Lab Why Do We Have Seasons?

March 21. Observer located at 42 N. Horizon

Define umbra and penumbra. Then label the umbra and the penumbra on the diagram below. Umbra: Penumbra: Light source

Astronomy Review. Use the following four pictures to answer questions 1-4.

Geography Class 6 Chapters 3 and

S CIENCE O VERVIEW. 59 Lesson Plan. Standards Benchmarks. Science Overview. Lesson Overview. Answer Key. Resources. My Angle on Cooling ME S S EN G ER

2. Usually, the air pressure inside a building is the air pressure outside the building. a. greater than b. about the same as c.

The Earth-Moon-Sun System

LAB 3: THE SUN AND CLIMATE NAME: LAB PARTNER(S):

5. In which diagram is the observer experiencing the greatest intensity of insolation? A) B)

C) D) 2. The diagram below shows a large pendulum in motion over an 8-hour period.

Altitude of the Moon and # of Hours it is Up

1. Which continents are experiencing daytime? 2. Which continents are experiencing nighttime?

ASTRO Fall 2012 LAB #2: Observing the Night Sky

Weather Systems Study Guide:

Earth Moon Motions A B1

THE SEASONS PART I: THE EARTH S ORBIT & THE SEASONS

Prentice Hall EARTH SCIENCE. Tarbuck Lutgens

2. Would you expect convection in a lake? Why or why not?

Grade 6 Standard 2 Unit Test Astronomy

HNRS 227 Fall 2007 Chapter 14. Earth in Space presented by Prof. Geller 25 October 2007

Earth s Orbit. Sun Earth Relationships Ridha Hamidi, Ph.D. ESCI-61 Introduction to Photovoltaic Technology

Science - 4th grade practice test

Lesson: Why We Have Seasons

The Sun-Earth-Moon System

1)Write the integer that represents the opposite of each real-world. situation. In words, write the meaning of the opposite.

C) wavelength C) eastern horizon B) the angle of insolation is high B) increases, only D) thermosphere D) receive low-angle insolation

Graphing Sea Ice Extent in the Arctic and Antarctic

Section 1: Overhang. Sizing an Overhang

TILT, DAYLIGHT AND SEASONS WORKSHEET

Seasonal & Diurnal Temp Variations. Earth-Sun Distance. Eccentricity 2/2/2010. ATS351 Lecture 3

Celestial Sphere. Altitude [of a celestial object] Zenith. Meridian. Celestial Equator

The following terms are some of the vocabulary that students should be familiar with in order to fully master this lesson.

Dawood Public School Secondary Section Class VII

Multiple Choice Open-Ended Gridded Response Look at the coordinate plane below. In which quadrant is Point A located?

9/1/14. Chapter 2: Heating Earth s Surface and Atmosphere. The Atmosphere: An Introduction to Meteorology, 12 th. Lutgens Tarbuck

How can we describe the motion of the sun in the sky? Where is the Sun at noon today? What about the path of the Sun?

What Is the Relationship Between Earth s Tilt and the Seasons?

(1) How does the annual average sun angle at solar noon (that is, the sun angle at noon averaged over a full year) depend on latitude?

What causes the Seasons? - Part I

The rock probably formed 200million years ago. The mineral sample is purple.

Integers and Absolute Value

Transcription:

Section A.1: Functions: the Building Blocks of Mathematical Models Mathematical models The purpose of a mathematical model is to represent something real (like economic changes) and help us to understand it. Mathematical models are based on the relationships between quantities that can change. These relationships are described by mathematical tools called functions. Section A.2: Language and Notation of Functions Definition of function A function describes how a dependent variable changes with respect to one or more independent variables. When there are only two variables, we often summarize them as an ordered pair with the independent variable first: (independent variable, dependent variable) We say that the dependent variable is a function of the independent variable. If x is the independent variable and y is the dependent variable, we write the function as y = f(x) 1

Ex.1 Suppose we want to model the variation in temperature over the course of the day based on the data of the following table: Time Temperature Time Temperature 6:00 a.m. 50 F 1:00 p.m. 73 F 7:00 a.m. 52 F 2:00 p.m. 73 F 8:00 a.m. 55 F 3:00 p.m. 70 F 9:00 a.m. 58 F 4:00 p.m. 68 F 10:00 a.m. 61 F 5:00 p.m. 65 F 11:00 a.m. 65 F 6:00 p.m. 61 F 12:00 a.m. 70 F What is the dependent variable? What is the independent variable? Ex.2 For each situation, express the given function in words. Write the two variables as an ordered pair and write the function with the notation y = f(x). (1) You are riding in a hot-air balloon. As the balloon rises, the surrounding atmospheric pressure decreases. (2) You are on a barge headed south down the Mississippi River. You notice that the width of the river changes as you travel southward with the current. 2

Section A.3: Representing Functions How to represent a function There are 3 basic ways to represent a function: (1) We can represent a function with a data table. (2) We can draw a picture, or graph, of a function. (3) We can write a compact mathematical representation of a function in the form of an equation. The Coordinate Plane Coordinates in the plane The points in the coordinate plane are described by two coordinates: the x-coordinate gives the point s horizontal position relative to the origin, the y-coordinate gives the point s vertical position relative to the origin. We use the x-axis for the independent variable and the y-axis for the dependent variable. The axes divide the coordinate plane in 4 quadrants. 3

Section A.4: Creating Graphs of Functions Definition of domain and range The domain of a function is the set of values that both make sense and are of interest for the independent variable. The range of a function consists of the value of the dependent variable that correspond to the values in the domain. How to create graph of functions Step 1: Identify the independent and dependent variables of the function. Step 2: Identify the domain and the range of the function. Use this information to choose the scale and labels on the axes. Zoom in on the region of interest to make the graph easier to read. Step 3: Make a graph using the given data. If appropriate, fill in the gaps between data points. Step 4: before accepting any predictions of the model, be sure to evaluate the data and assumptions from which the model was built. Ex.3 Do all the steps for Example 1. 4

Ex.4 Imagine measuring the atmospheric pressure as you rise upward in the hot-air balloon. The table shows typical values you might find for the pressure at the different altitudes, with the pressure given in units of inches of mercury. This pressure unit is used with barometers, which measure pressure by the height of a column of mercury. Altitude Pressure 0 30 5, 000 25 10, 000 22 20, 000 16 30, 000 10 Use these data to graph a function showing how atmospheric pressure depends on altitude. Use the graph to predict atmospheric pressure at an altitude of 15, 000 feet, and discuss the validity of your prediction. 5

Ex.5 The number of hours of daylight varies with the seasons. Use the following data for 40 N latitude (the latitude of San Francisco, Denver, and Washington, D.C.) to model the change in the number of daylight hours with time. The number of hours of daylight is greatest on the summer solstice (June 21), when it is about 14 hours for latitude 40 N. The number of hours of daylight is smallest on the winter solstice (December 21), when it is about 10 hours for latitude 40 N. On the spring and fall equinoxes (March 21 and September 23, respectively), there are about 12 hours of daylight. According to the model, at which times of the year does the number of daylight hours change most gradually? most quickly? Discuss the validity of the model. 6