SOLAR GEOMETRY (AND SOLAR RADIATION)

Similar documents
SOLAR GEOMETRY (AND RADIATION)

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

Chapter Seven. Solar Energy

ME 476 Solar Energy UNIT THREE SOLAR RADIATION

announcements 5/1/08 L10 Analysis and Design Tools 5/1/08 Analysis and Design Tools

Lecture #03. January 20, 2010, Wednesday

Chapter 1 Solar Radiation

EE Properties of Sunlight. Y. Baghzouz Professor of Electrical Engineering

Gnomon (a thin, round stick at least a foot long and capable of being put into the ground or stood up vertically)

Astronomy 101: 9/18/2008

Module 2: Mapping Topic 2 Content: Determining Latitude and Longitude Notes

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

Sunlight and its Properties II. EE 446/646 Y. Baghzouz

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

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

Page 1. Name:

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

Practice Questions: Seasons #1

L.O: THE ANGLE OF INSOLATION ANGLE INSOLATION: THE ANGLE SUNLIGHT HITS THE EARTH

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

The Earth is a Rotating Sphere

LONGITUDE AND LATITUDE. Semi great circles joining the true or geographic poles of the earth (true meridians).

Which graph best shows the relationship between intensity of insolation and position on the Earth's surface? A) B) C) D)

ME 430 Fundamentals of Solar Energy Conversion for heating and Cooling Applications

Motion of the Sun. View Comments

The Sun. Fabio Peron Università IUAV - Venezia. Earth-Sun relationships. The Sun. Photosphere (Emits much of the solar radiant power)

The Celestial Sphere. Chapter 1. Constellations. Models and Science. Constellations. Diurnal vs. Annular Motion 9/16/2010

1.4j interpret simple shadow stick data to determine local noon and observer s longitude

Appearance of the Sky Orientation Motion of sky Seasons Precession (?)

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

Appearance of the Sky Orientation Motion of sky Seasons Precession (?)

APPENDIX F ACTIVITY #1 - CALCULATION OF THE TILT OF THE EARTH S AXIS AND THE OBSERVER S LATITUDE

Latitude and Longitude. North. Latitude. South

3. The Sun s Position

ILLUSTRATING SHADOWS TABLE OF CONTENTS

Chapter S1 Lecture. The Cosmic Perspective Seventh Edition. Celestial Timekeeping and Navigation Pearson Education, Inc.

Principles of Energy Conversion Part 11A. Solar Energy Insolation

Chapter 1: Discovering the Night Sky. The sky is divided into 88 unequal areas that we call constellations.

Penn State Project CANDLE

Oberth: Energy vs. Momentum

Time Zones. Doug Fischer Geog 106 LRS

Photovoltaic Systems Solar Radiation

Why does Earth rotate and what s the evidence? (besides watching it from space ships or satellites) Week 18 January 5, 2015

Latitude and Longitude

CA1 2.11: Designing an Equatorial Sundial Activity

LOCATING CELESTIAL OBJECTS: COORDINATES AND TIME. a. understand the basic concepts needed for any astronomical coordinate system.

Exercise 6. Solar Panel Orientation EXERCISE OBJECTIVE DISCUSSION OUTLINE. Introduction to the importance of solar panel orientation DISCUSSION

Polar Sundial. Cut carefully on this line. Cut on this line.

Complete the following: a. Lines of latitude are parallel to the equator. Name:

Earth-Sun Relationships. The Reasons for the Seasons

Earth Science Seasons Test Name Per Date

Designing with the Pilkington Sun Angle Calculator

Lecture 4: August 30, 2010

Chapter 2 Discovering the Universe for Yourself

The Earth, Moon, and Sky. Lecture 5 1/31/2017

Chapter S1 Celestial Timekeeping and Navigation. How do we define the day, month, year, and planetary time periods?

COMPUTER PROGRAM FOR THE ANGLES DESCRIBING THE SUN S APPARENT MOVEMENT IN THE SKY

3. Which color of the visible light has the shortest wavelength? A) violet B) green C) yellow D) red

Section 2. Locating Astronomical Objects in the Night Sky What Do You See? What Do You See? Think About It. Investigate.

ZW2000 and Your Vertical Sundial Carl Sabanski

What are Latitude and Longitude?

Geography Class 6 Chapters 3 and

Chapter 6. Solar Geometry. Contents

Motions of the Sun Model Exploration

Daily Motions. Daily Motions. Solar and Sidereal Days. Annual Motions of the Sun. Coordinate system on Earth. Annual Motion of the Stars.

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

PHYSICAL GEOGRAPHY. By Brett Lucas

MiSP Astronomy Seasons Worksheet #1 L1

Phys Lab #1: The Sun and the Constellations

Chapter 1 Image Slides. Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display.

Earth is tilted (oblique) on its Axis!

MiSP Astronomy - Seasons Worksheet #1 L2

Aileen A. O Donoghue Priest Associate Professor of Physics

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

b. Assuming that the sundial is set up correctly, explain this observation.

Solar Time, Angles, and Irradiance Calculator: User Manual

Time, coordinates and how the Sun and Moon move in the sky

3. This room is located in a building in New York State. On which side of the building is the window located? (1) north (3) east (2) south (4) west

Period 14 Activity Sheet: Energy in Nature

Discovering the Night Sky

Discovering the Night Sky

6/17. Universe from Smallest to Largest:

Chapter 2 Discovering the Universe for Yourself

Chapter 2 Discovering the Universe for Yourself. What does the universe look like from Earth? Constellations. 2.1 Patterns in the Night Sky

Knowing the Heavens. Chapter Two. Guiding Questions. Naked-eye (unaided-eye) astronomy had an important place in ancient civilizations

Chapter 2 Lecture. The Cosmic Perspective Seventh Edition. Discovering the Universe for Yourself Pearson Education, Inc.

CHAPTER 2 Strand 1: Structure and Motion within the Solar System

Astro 101 Lab #2. Start up the Stellarium program. If you do not remember how to use the user interface, please refer to Lab#1 or the user s guide.

Observer-Sun Angles. ), Solar altitude angle (α s. ) and solar azimuth angle (γ s )). θ z. = 90 o α s

Meridian Circle through Zenith, North Celestial Pole, Zenith Direction Straight Up from Observer. South Celestial Pole

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

Practice Questions: Seasons #2

Geometry of Earth Sun System

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

The Earth-Moon-Sun System

Observing the Universe for Yourself

Chapter 2 Discovering the Universe for Yourself. Copyright 2012 Pearson Education, Inc.

Lesson Overview. Climate. Lesson Overview. 4.1 Climate

Time Series Model of Photovoltaic Generation for Distribution Planning Analysis. Jorge Valenzuela

UNIT 1: THE PLANET EARTH

Transcription:

SOLAR GEOMETRY (AND SOLAR RADIATION) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 1 Solar Radiation Components glass will reflect some incoming radiation; absorb some; and transmit some SHGF (above) is solar heat gain factor a measure of the quantity of solar energy that will pass through a sheet of single-pane clear glass at a given time of the year for a given orientation under design conditions Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 2 1

Solar Radiation: A Resource or a Problem? force mitigating element: building envelope resultant radiation is an environmental force; it can be an asset or a liability depending upon site/project//context/opr Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 3 Solar Context Distance Sun Earth the solar constant is a mean value of the solar radiation intensity found at the edge of the Earth s atmosphere solar constant (Btuh/sq ft) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 4 2

Solar Context Tilt the tilt of the Earth s axis, relative to the sun s position, accounts for the seasons (as solar angle of incidence changes) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 5 Site Context Latitude Muncie s latitude is approximately 40 deg N (a convenient latitude often used in design data tables) latitude locates a site in the north-south context, relative to the equator Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 6 3

Mitad del Mundo, Quito marking the equator www.expedia.com Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 7 Site Context Longitude Muncie = apx. 85 deg W longitude locates a site in the east-west context, relative to the prime meridian (in Greenwich, England) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 8 4

Greenwich, England prime meridian Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 9 Solar-Site Context summer spring/fall NORTHERN HEMISPHERE winter the sun follows defined and predictable paths on a daily and annual basis Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 10 5

Solar Angles Altitude ALTITUDE ANGLE the angle between a horizontal ground plane and the line describing the position of the sun in the sky vault Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 11 Altitude Angle Patterns noon noon altitude angle; describes height of the sun in the sky varies with month and time of day Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 12 6

Altitude Angle Patterns << site latitude for any given month and time, altitude angle varies with latitude Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 13 Solar Angles Azimuth AZIMUTH ANGLE the angle between south and the position of the sun in the sky vault as projected onto the horizontal ground plane Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 14 7

Azimuth Angle Patterns azimuth angle varies with month and time of day; range is most extensive in summer Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 15 Solar Position Relative to Site conceptually simple, but three-dimensional Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 16 8

Solar Position Conventions Azimuth angle is usually measured from South in architecture but sometimes from the North in other disciplines (or in the Southern hemisphere) South is always solar South; not magnetic South or plan South see next slide Altitude angle is measured from the horizontal Times are always expressed as solar time see upcoming slide Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 17 South, Souther, Southiest Plan South is usually an arbitrary designation used for convenience Solar South is by definition the position of the sun at solar noon Solar South marks the center of symmetry of the daily solar path Solar South differs from Magnetic South (as read on a compass) by the local magnetic deviation value Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 18 9

Magnetic Deviation solar reference magnetic deviation compass reference magnetic deviation magnetic deviation varies with site location Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 19 Magnetic Deviation zero deviation line designing for east-central Indiana is not too deviant Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 20 10

Solar versus Clock Time LST CT + DST local solar time = clock time +/- equation of time value +/- (4)(local standard time meridian local longitude) +/- daylight saving time adjustment example, Muncie, June 21: latitude adjustment = (4)(75-85) = -40 minutes; DST adjustment = 60 minutes; ET adjustment = -3 minutes bottom line: solar and clock time are rarely identical, and can differ by +/- an hour; this matters when solar loads are combined with clock-based loads Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 21 Clock Time Influences equation of time www.sundials.co.uk/ US time zones (political devices) and time zone reference meridians; the sun is not influenced by politics Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 22 11

Sunpath Information The sun s location at any time can be accurately predicted. Such information is readily available in several formats: Graphic sunpath diagrams: Horizontal projection diagrams (including the SBSE Sun Angle Calculator) Vertical projection diagrams Sunpeg diagrams Tabular data (as in the ASHRAE Handbook) Online calculators (interactive databases) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 23 Sunpath Diagrams horizontal projection sunpath diagram l-e-s-s.co.uk/guides/physics/solargeometry.htm sun paths for selected days can be projected downward onto a horizontal plane (the plane is a surrogate for the Earth s surface) to generate a diagram Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 24 12

Sunpath Diagrams Pilkington Sun Angle Calculator available from SBSE via CERES www.sbse.org/resources/sac/index.htm sun paths for multiple latitudes are provided, with usability enhancements Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 25 Sunpath Diagrams vertical projection sunpath diagram sun paths for selected days can be plotted on a vertical surface (acting as a surrogate for the site horizon) to generate a diagram Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 26 13

Sunpath Diagrams sunpeg diagram primarily used to properly orient a scale model to the sun (real or simulated); the shadow cast by the peg (gnomon) shows date and time Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 27 Tabular Solar Position Data Mechanical and Electrical Equipment for Buildings (10 th ed) Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 28 14

Online Solar Position Data susdesign.com/sunangle/ Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 29 Why Architects Should Understand Solar Geometry www.newser.com/ abcnews.go.com/ www.dailymail.co.uk/ Ball State Architecture ENVIRONMENTAL SYSTEMS 1 Grondzik 30 15