Photovoltaic Systems Engineering

Slides:



Advertisements
Similar presentations
The Sun in the Sky And how it changes in the course of the year.
Advertisements

Comet Machholz passes the Pleiades. Comet Machholz C/2004 Q2 Discovered byDonald Machholz, Jr. on August 27, 2004 Period of about 120,000 years Just up.
Chapter S1 Celestial Timekeeping and Navigation
Earth’s Motions, Solar Radiation, and the Seasons
SEASONS AND THE SUN PATH
Celestial Sphere Stars seem to be on the inner surface of a sphere surrounding the Earth.
Observing and the Sky Astronomy 311 Professor Lee Carkner Lecture 3.
Observing Astronomy 315 Professor Lee Carkner Lecture 3.
Solar vs. Sidereal Day.
The Earth Rotates.
The Sky From Earth. Let’s Step Outside Where are the stars? What direction are we facing?
Constellations. Celestial Sphere Our Point of View.
Seasons Earth’s Tilt –Tilt of rotational axis with respect to its orbit around sun Solar Insolation –More Direct Sun Light –Longer Duration of Day Light.
Physics 202: Introduction to Astronomy – Lecture 2 Carsten Denker Physics Department Center for Solar–Terrestrial Research.
An Earth Day Sidereal Day: 23 hr 56 min 4 sec Motion relative to background stars Mean Solar Day: 24 hours The average time between meridian crossings.
Sun-Earth relationships Array Orientation Solar Radiation Data Sheets
Observing and the Sky Astronomy 311 Professor Lee Carkner Lecture 3.
The Celestial Sphere The 88 official constellations cover the celestial sphere. If you do not have a model of the celestial sphere to bring to class, you.
Daily Motion of the Sun Daily motion (diurnal motion) along a circle with center on the Earth’s axis Clockwise in the north temperate zone Counterclockwise.
Constellations A constellation is a region of the sky.
Chapter 1: The Cycles of the Sky
Equinoxes, Solstices, Insolation, and the Analemma
Terrestrial Coordinates (useful for specifying locations on the surface of the Earth) Longitude - Longitude -- East/West Coordinate -- 0  at the Prime.
Regents Alert*****.  To find out the date you must look at the position of sunrise and sunset.  June 21- Northeast to Northwest.  Dec. 21- Southeast.
South North East West Sunrise Sunset Azimuth Angle (From South) Altitude altitude angle horizontal surface perpendicular to surface zenith angle Sun Figure.
Where is it? On the Celestial Sphere. Longitude and Latitude On Earth: Longitude is how far you are, in degrees, East or West of the “Prime Meridian”
Coordinate Systems.
Celestial Sphere. Earthly Sphere Latitude measures the number of degrees north or south of the equator. –DeKalb at 41° 55’ N Longitude measures degrees.
Solar Resource Part 2 August 27, Session 03 Components Wrap-up of Session 02 The Solar Resource o Tracking the sun o Orientation considerations.
Chapter 1 Predicting the Motions of the Stars, Sun, and Moon.
24.2 Sun and Seasons
Day & Night.
The Motion of the Sun. ack-hole-powers-cosmic-flashlight- illuminating-the-cosmic-web
Motions of the Solar System. Earth’s Motions Earth has Three Motions 1. Daily 2. Yearly 3. Cyclic.
REVIEW The Electromagnetic Spectrum Figure 2.5 Figure 2.6.
The Seasons Seasonality: the variation of the sun’s position over the horizon; the changing daylength during the year Seasons result from: variations in.
Sky Motions  Diurnal Motion Annual Motion. DIURNAL MOTION o Daily East / West motion of the sky Due to the Earth’s rotation (15°/hour) [360°/24 hours.
Climatic System Energy Budget, Energy Flow, Spatial Variation Angle of Solar Insolation.
Earth-Sun Relationships p.p. 481 – 482 & Nearly all energy that drives our weather and climate on Earth comes from the Sun Earth only absorbs.
AstroLab-2 Locating Stars in the Sky Merav Opher-Fall 2004.
Unit III: The Earth in Space. Celestial Objects Celestial Sphere.
The Sun’s Path. Summer Solstice (approximately June 20-21) North Pole: The North Pole (90 degrees north latitude) receives 24 hours of daylight, as it.
Our Location on the Earth North South EastWest North South East you are here West.
Observational Astronomy Mapping the Heavens Coordinate Systems We have two different ways to locate objects in the sky: Celestial equatorial system -Right.
What is apparent motion? Important to understand what we see and what is actually happening. Apparent motion is what we see from Earth Actual motion is.
Lab 3: Earth Sun-Geometry
How do we locate objects in the sky? Angular separation: the angle between objects as seen from Earth (Degrees are separated into minutes (60 minutes of.
Seasons.
Altitude of the Sun- Solar Altitude
Ancient astronomers believed that the stars were attached to a celestial sphere surrounding the Earth.
Photovoltaic Systems Engineering
November 8,2010 Celestial Motions.
Photovoltaic Systems Engineering The Solar Resource, cont.
The HELIOCENTRIC Model
RELATIVE MOTION OF EARTH IN SOLAR SYSTEM
Astronomy Vocabulary Mr. Ahearn 2013.
Chapter 4A: SOLAR RADIATION- GEOMETRY
Caused by Earth’s 23.5o tilt as we revolve around the sun.
Sun-Earth System.
Tilt of the Earth’s Rotational Axis
The Sky (Celestial Sphere)
GEU 0047: Meteorology Lecture 3 Seasonal Cycle
On the Celestial Sphere
APPARENT PATH OF THE SUN
Earth, Sun, and Moon Interactions
Photovoltaic Systems Engineering The Solar Resource, cont.
On the Celestial Sphere
Chapter 4A: SOLAR RADIATION- GEOMETRY
Presentation transcript:

Photovoltaic Systems Engineering SEC598 Photovoltaic Systems Engineering (SEC501 Solar Engineering and Commercialization, I) Session 02 The Solar Resource August 22, 2018

Session 02 Components The Solar Resource Definitions Solar radiation Tracking the sun Orientation considerations

Learning Outcomes An elementary understanding of the solar resource Recognition of impact of PV system orientations

The Solar Resource – earth’s orbit Messenger & Abtahi, Fig 2.4

The Solar Resource – earth’s orbit

The Solar Resource – The annual motion from the perspective of the celestial sphere d - declination Markvart, Solar Electricity, Fig 2.6

Motion of Sun Diagram – Perspective view of daily motion

Motion of Sun Diagram – Example #1 Arbitrary Latitude zenith latitude Summer Solstice North Pole Equinox 23.5o Winter Solstice 23.5o N S

Motion of Sun Diagram – Example #2 zenith Tropic of Cancer Latitude = 23.5o Summer Solstice Equinox Winter Solstice 23.5o 23.5o North Pole N S

The Solar Resource – altitude and azimuth Markvart, Solar Electricity, Fig 2.7b