PERENCANAAN TEKNOLOGI & SISTEM BANGUNAN (PTSB) 03
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1 PERENCANAAN TEKNOLOGI & SISTEM BANGUNAN (PTSB) 03
2 OUTLINE What drives climate system on our earth?
3 Fact 1: Solar radiation drives the earth s climate system OUTLINE The sun is a giant ball of hot gases 70% hydrogen, 28% helium, 0.5% carbon, 0.5% nitrogen, 0.5% oxygen, and 0.5% other elements.
4 Fact 1: Solar radiation drives the earth s climate system OUTLINE The creation of each helium nucleus requires four hydrogen nuclei. The converts 600 million tons of hydrogen into 596 million tons of helium every second.
5 Fact 1: Solar radiation drives the earth s climate system OUTLINE
6 Fact 1: Solar radiation drives the earth s climate system OUTLINE Atmospheric Effects
7 Fact 1: Solar radiation drives the earth s climate system the scattered component makes the sky look bright and provides the ambient diffuse daylighting used in buildings Blue light arrives from all directions after scattering, red and yellow light arrives almost directly from the sun OUTLINE Atmospheric Effects
8 Fact 1: Solar radiation drives the earth s climate system the scattered component makes the sky look bright and provides the ambient diffuse daylighting used in buildings Blue light arrives from all directions after scattering, red and yellow light arrives almost directly from the sun OUTLINE Atmospheric Effects
9 Fact 2: The earth is turning while running on its orbit Aphelion Perihelion km km Summer sols>ce Vernal equinox 22 Mar 24 June 22 Dec Winter sols>ce OUTLINE 23 Sept Autumnal equinox
10 Fact 2: The earth is turning while running on its orbit OUTLINE
11 Fact 3: Coriolis effect develop atmospheric circulation cells Polar Front Low Polar High Polar Cell OUTLINE Subtropical High Ferrel Cell Intertropical Convergence Zone Low Hadley Cell Subtropical High Polar Front Low Polar High
12 Fact 3: Coriolis effect develop atmospheric circulation cells OUTLINE
13 Fact 3: Coriolis effect develop atmospheric circulation cells OUTLINE
14 OUTLINE What kind climate characterize our region?
15 OUTLINE Hadley cell dominates the atmospheric circulation in tropical zone like the Southeast Asia which creates monsoons (derived from the Sanscrit mausim which means a season )
16 OUTLINE
17 OUTLINE
18 OUTLINE Semarang; Lat ; Long (+7.0)
19 OUTLINE A typical house for hot-humid climates (Szokolay, 2004)
20 OUTLINE A typical house for hot-humid climates (Szokolay, 2004)
21 OUTLINE A typical house for hot-humid climates (Szokolay, 2004)
22 OUTLINE horizontal shadow angles (HSA) vertical shadow angle (VSA
23 OUTLINE vertical shadow angle (VSA) vertical shadow angle (VSA)
24 OUTLINE
25 Main parameters in daylight availability OUTLINE Climate and weather course (latitude, time/date)
26 OUTLINE DF = SC + ERC + IRC Sky Component (SC) - Directly from the sky, through an opening such as a window. Externally Reflected Component (ERC) - Reflected off the ground, trees or other buildings. Internally Reflected Component (IRC) - The inter-reflection of 1 and 2 off surfaces within the room.
27 OUTLINE BRS DAYLIGHT FACTOR PROTRACTOR NO. 2
28 SKY COMPONENT OUTLINE (1) ISC skala luar (2) Sudut rata2 skala dalam
29 SKY COMPONENT OUTLINE (2) Sdt rata2 lingkaran imajiner (3) FC jml angka garis lengkung
30 OUTLINE
31 INTERNALY REFLECTED COMPONENT (1) Hitung luas jendela, luas dinding, luas lantai, luas langit-langit à à à Luas total permukaan ruang Perbandingan luas jendela dan luas total permukaan Tandai di Nomogram A OUTLINE
32 INTERNALY REFLECTED COMPONENT OUTLINE
33 INTERNALY REFLECTED COMPONENT (2) Hitung perbandingan luas diding dan luas total permukaan ruang à Tandai pada kolom kiri tabel OUTLINE
34 INTERNALY REFLECTED COMPONENT (3) Pantulan dinding (%) OUTLINE à Lakukan interpolasi misal (56 54)/( )*0,06
35 INTERNALY REFLECTED COMPONENT OUTLINE
36 DAYLIGHT FACTOR OUTLINE
37 DAYLIGHT FACTOR OUTLINE
38 OUTLINE
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