Successfully reported this slideshow.
We use your LinkedIn profile and activity data to personalize ads and to show you more relevant ads. You can change your ad preferences anytime.

Tro arch pp

presentation not mine. credits to the owner

  • Login to see the comments

Tro arch pp

  1. 1. TROPICAL DESIGN = Minimize SUN + Maximize WIND
  2. 2. TROPICAL DESIGN TROPICAL DESIGN = passive cooling PASSIVE COOLING: design with no mechanical equipment used to induce comfort conditions in building interior PASSIVE COOLING = inducing air movements INDUCING AIR MOVEMENTS: relevant for areas with temperature variations of 10 and with high humidity INDUCING AIR MOVEMENTS: can improve thermal comfort up to building interiors 15 meters deep
  3. 3. Passive Systems for Various Climates HOT-HUMID CLIMATE: maximize wind exposure maximize internal airflow minimize radiant heat gain HOT-DRY CLIMATE: minimize radiant heat gain moderate wind resistance moderate internal airflow COOL CLIMATE: maximize thermal retention maximize radiant heat gain minimize wind resistance TEMPERATE CLIMATE: moderate thermal retention moderate radiant heat gain slight wind exposure (for humidity control) moderate internal airflow
  4. 4. AIR MOVEMENT ≡ wind Principles of Air Movement 1. Air flows from a high-pressure to a low-pressure area. 2. INERTIA. Once set in motion, air tends to continue to flow in its initial direction until some intervening force is met. 3. Air flows through the path of least resistance.
  5. 5. GLOBAL AIR MOVEMENT General Conditions 1. Equator receives more radiation than do polar regions. 2. Heat from equator move towards polar regions. 3. Hot air moves upwards going to polar regions. 4. Cold air moves to equator close to earth’s surface.
  6. 6. GLOBAL AIR MOVEMENT Specific Conditions 1. Rotation of earth deflects the air = Coriolis Force 2. Wind flows due to heat exchange. • Air temperature changes faster than ground temperature • Daily fluctuations of air temperature caused by physical conduction up to 3 meters above the ground • Marked differences of air temperature between night and day
  7. 7. GEOGRAPHICAL AIR MOVEMENT Land and Sea Breezes 1. Daytime Heating: land warms more rapidly than water • SEA BREEZE – wind from the sea directed toward land • Strongest in the afternoon when heating variance is greatest 2. Night Time Cooling: land cools faster than water • LAND BREEZE – wind from land directed to sea
  8. 8. WARM COOL Daytime Sea Breeze COOL WARM Night Time Land Breeze
  9. 9. MONSOONS IN THE PHILIPPINES Monsoon: large-scale seasonal currents 1. Northeast Monsoon = AMIHAN = the winter monsoon • • • • Appears in October Attains maximum strength in January Gradually weakens in March Disappears in April 2. Southwest Monsoon = HABAGAT = the summer monsoon • • • • Appears early May Maximum flows during August Disappears gradually in October Persists from November to December
  10. 10. AIR MOVEMENT IN BUILDINGS 1. Windward side = positive pressure Leeward side = negative pressure 2. Air enters through openings located in the positive pressure zone Air exits through openings located at the negative pressure zone 3. Air enters through lower level openings Air exits at higher level openings 4. Window width wall width = 50% to increase indoor air speed 5. Window heights = 1.10 meters for effective indoor air movement 6. Wind deflectors, horizontal and vertical, to redirect air flow 7. Prevent wind shadows by placing openings
  11. 11. EFFECT OF LANDSCAPE ELEMENTS 1. Hedges/shrubs should not be more than 3 meters from building 2. Tree foliage above openings promote air motion into openings 3. Combine tree, hedge and building to achieve air flow control 4. Lateral air channels to direct air flow 5. Arrange trees to determine wind shadow 6. Make use of earth mounds to achieve better air movement
  12. 12. SOLAR GEOMETRY 1. Rays of the sun vary with time and place (latitude) 2. Celestial Sphere: earth is static; sun moves from east to west 3. The sun moves across the sky at a rate of 15.04 per hour 4. The earth’s polar axis is inclined at 23 47’ from the vertical 5. June 21 is considered the longest day = summer solstice 6. December 21 is the shortest day = winter solstice 7. March 21 and September 21 = equinoxes
  13. 13. SUN PATH 1. Solar Altitude Angle = the angle with height above the horizon. Ranges from 0 when on horizon to 90 when directly above (noon) 2. Solar Azimuth Angle = the sun’s position as projected on a horizontal plane. 3. The two solar angles change with Latitude (location on Earth) 4. Metro Manila is located at 14.5 N Latitude 5. Two Methods for Calculating Solar Angles • Using graphs • By mathematical calculation 6. Solar Chart = Sun Path Diagrams 7. Different Solar Charts for Different Latitudes
  14. 14. 6 7 5 6 8 4 3 2 1 12 11 10 9 90 80 70 60 50 40 30 20 10