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Analysis and Design Tools ARCH 331/431 Spring 2008 Lecture 10 announcements 5/1/08 Information Meeting: INDIA program winter 2009 Friday May 2, 12:30, Gould 208P Assignment 4: Shading Model Studies Available Friday, 5pm; due in 2 weeks (week 7) ARCH 3/431 Spring 2008 1

ARCH 3/431 Spring 2008 2

Contemporary vertical dials A contemporary vertical sundial in glass ARCH 3/431 Spring 2008 3

The Jantar-Mantar of Delhi These are extraordinary structures basically buildings and spaces as instruments of observation. ARCH 3/431 Spring 2008 4

ARCH 3/431 Spring 2008 5

Another type of horizontal sundial uses a vertical gnomon often called Flagpole Plots Sunpeg sundials can be found on pgs. 323-326 in Sun, Wind, & Light. ARCH 3/431 Spring 2008 6

Sundial & Model Orientation Magnetic Declination (Magnetic Variation) 2004 18.4 o www.ngdc.noaa.gov/seg/geomag/declination.shtml ARCH 3/431 Spring 2008 7

Clock time vs. solar time Solar time is unique for each location according to longitude and time of year, It is relatively straightforward to relate solar time to local standard time. 1. Standard Time vs. Daylight Savings Time 2. Longitude: distance from the standard meridian within a time zone (120 o, 105 o, 90 o, 75 o ) 3. Equation of Time ARCH 3/431 Spring 2008 8

2. Longitude: distance from the standard meridian within a time zone (120 o, 105 o, 90 o, 75 o ) Time zones = 1 hour segments 360 / 24 hours = 15 /hour or 1 degree every 4 minutes Time zones Standard meridians run at roughly 15 intervals ARCH 3/431 Spring 2008 9

Time zones Standard meridians run at roughly 15 intervals Is the sun always at its highest altitude at clock noon? Hint: The standard meridian is 120 for Pacific Standard Time. ARCH 3/431 Spring 2008 10

Pacific Standard Time datum (Standard Meridian): 120.00 Seattle s Longitude: 122.33 Our distance from the Standard Meridian: 2.33 The earth rotates 360 every 24 hours 360 /24 = 15 ; the earth rotates 15 every 1 hour 60 minutes/15 results in 1 every 4 minutes 2.33 x 4 minutes = 9.33 minutes (9 minutes 20 seconds) The sun will reach solar noon, the highest solar altitude for the day, at about 12:09 in Seattle (when it is noon, clock time, it is 11:51 solar time) Equation of Time ARCH 3/431 Spring 2008 11

Equation of Time today Converting Solar Time Local solar time (LSoT) is the local clock time adjusted for these factors: Step 1. Determine the local standard time, LST. This is clock time, adjusted for daylight savings time if necessary. If daylight savings is in effect, subtract one hour. Step 2. Determine the local standard meridian (LSTM) and the local longitude (LL). Step 3. Determine the equation of time, EoT, adjustment in minutes. LSoT = LST + (4 minutes * (LSTM - LL)) + EoT = 12:00 + (4 minutes * (120-122.33)) + (+4) = 11:54 ARCH 3/431 Spring 2008 12

A4 Shading Model Studies Analysis and Design Too Libby Owens Ford (LOF) Sun Angle Calculat ARCH 3/431 Spring 2008 13

Libbey-Owens Ford (LOF) Sun Angle Calculator trusted by architects for generations Visualizing Sun Paths: Polar Plot of the Sun s Path ARCH 3/431 Spring 2008 14

All Sun Path Diagrams represent the hemisphere of sky directly above and relative to the ground plane. Coordinates are altitude and azimuth. A polar Sun Path Diagram ARCH 3/431 Spring 2008 15

Construction of Sun Path Diagrams: a. Altitude and Azimuth b. 9 am March 21 c. Additional times on March 21 d. Plotting the sun for the 21st day of each month e. Hour lines (dotted) are added Sun, Wind & Light pgs. 297-300 MEEB 10th Appendix D.3 pgs. 1539-1542 ARCH 3/431 Spring 2008 16

Sun path diagrams combine coordinates of time and position and allow analysis of: 1 Sun Position at any time of day and year 2 Site Shading (fisheye imagery) 3 Window Shading Devices ARCH 3/431 Spring 2008 17

A LOF Sun Angle Calculator example: 36º NL Find the sun s position on Jan. 21 st at 11 AM 36 o N. Latitude: Altitude = 32 o Azimuth = 17 o β = 32º Φ = 17º E of S A LOF Sun Angle Calculator example: 36º NL Find the sun s position on Oct. 21 st at 3 PM β = 26.5º 36 o N. Latitude: Altitude = 26.5 o Azimuth = 51 o Φ = 51º W of S ARCH 3/431 Spring 2008 18

A rectilinear Sun Path Diagram ARCH 3/431 Spring 2008 19

Site Shading Masks Plotting a picture of the sun s path, and the landforms, buildings, trees and objects that block the sun. ARCH 3/431 Spring 2008 20