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climate
TOPIC
7.1 Shelter for hot-dry climate
7.2 Shelter for warm-humid climates
BOOK
MANUAL OF TROPICAL HOUSING AND BUILDING
Nature of the climate
HOT DRY AND SEMI DESERT CLIMATES
VERY HOT DRY AIR AND DRY GROUND
• DAY TIME
AIR TEMPERATURE : 27° TO 49 ° C
( > THAN SKIN TEMPERATURE
36° TO 37° C)
• NIGHT TIME
AIR TEMPERATURE : 22° C (FALLS)
• LOW HUMIDITY
• NO CLOUD COVER ( FROM DIRECT SOLAR RADIATION )
HOT - DRY CLIMATES
Nature of the climate
WARM – HUMID CLIMATES
• AIR TEMPERATURE : 21° TO 32° C
(LITTLE VARIATION IN DAY AND NIGHT)
( OFTEN EXCEEDS NORMAL SKIN TEM.)
• HIGH HUMIDITY
(ALL SEASONS )
• HEAVY CLOUD AND WATER VAPOUR
• MOSTURE WITH MODRATE HEAT AND HIGH RAIN FALL
• PLANT COVER
• WIND
Nature of the climate
Nature of the climate
Warm-humid climate
Physiological objectives
HOT DRY CLIMATE
• it is the PHYSICAL HUMAN COMFORT FROM THE ENVIOURMENT.
•PHYSICAL COMFORT OF HUMAN PER DAY DEPENDS ON THE
REDUCTION OF THE INTENCE RADIATION FROM SUN, GROUND AND
SURROUNDING BUILDINGS.
•MAINTAINANCE OF INNER SURFACE TEMP. is LESS THaN THE SKIN
TEMP.
•THE BODY DISSIPATE SOME OF ITS HEAT TO THE SURROUNDING
MAKING TEMP. COOL BY CONVECTION.
NIGHT
•AT NIGHT THE AIR TEMP. IS FREQUENTLY LOW PERMITS EFFECTIVE
TEMP. ( TEMP. OF COMFORT ) .
•SUCH EFFECTIVE TEMP. AT NIGHT BECOMES BENEFICIAL.
•DUE TO LOW HUMIDITY EVAPORATION IS HIGHER COMPARED TO
OTHER CLIMATE.
•SPECIAL ARRANGEMENT IS NOT NECESSARY EG. A.C COOLER ETC.
Physiological objectives
HOT DRY CLIMATE
DAY TIME
CLIMATE IS TOO HOT DURING DAY, ARRANGEMENTS ARE
REQUIRED AS THE AIR IS NOT COOLED AND DUST
FILTERED.
Physiological objectives
WARM-HUMID CLIMATE
TEMP. IS NEAR TO SKIN TEMP.
HEAT IS TRASMITTED BY CONVECTION AND
CONDUCTION, WHICH IS NEGLIGIBLE
• FOR PHYSICAL COMFORT THERE SHOULD BE HEAT
DISSIPATION FROM BODY=TO THE AMOUNT OF METABOLIC
HEAT PRODUCTION OF THE BODY.
• HIGH HUMIDITY - SATURATED AIR ENVELOPE
- BLOCKING EVAPORATION CYCLE
THE SATURATION CAN BE AVOIDED BY
ALLOWING OUTSIDE BREEZE TO
PASS THROUGH THE BUILDING AND
TO THE OCCUPANTS.
AT NIGHT. NO SIGNIFICANT COOLING IS DONE.
THE WALL AND ROOF SURFACE TEMP. SETTLE DOWN TO THE
SAME LEVEL AS THE AIR TEMP.
prevention
Physiological objectives
WARM-HUMID CLIMATE
Form and planning
HOT-DRY CLIMATE
•LESS ACCOMODATION UNDER ONE ROOF - LESS HOT AIR AND
THERMAL LOADING
FROM THE SUN.
• LARGER DIMENSIONS OF THE BUILDING SHOULD PREFERABLY
FACE NORTH AND SOUTH.
• WORST ORIENTATION IS WEST.
• NON - HABITABLE ROOMS CAN BE USED AS THERMAL
BARRIERS.
• SHADING OF ROOFS,WALLS AND OUTDOOR SPACES IS
CRITICAL.
• LOW THERMAL CAPACITY MATERIALS SHOULD BE USED FOR
SHADING DEVICES.
• TO HAVE CLOSE GROUPS OF BUILDINGS,NARROW ROADS AND
STREETS , ARCADES , COLLONADES AND SMALL ENCLOSED
COURTYARDS – GET MAXIMUM AMOUNT OF SHADE AND
COOLNESS.
• DIFFICULT SHADING OF ROOF DOUBLE ROOF IS PREFFERED.
• NECESSIATE THE USE OF METAL SURFACE.
Form and planning
WARM-HUMID CLIMATE
• AIR MOVEMENT IS THE ONLY AVAILABLE RELIEF FROM CLIMATIC
STRESS.
• ELONGATED PLANS,IN A LINEAR, ACROSS THE PREVAILING
WIND DIRECTION,AFFORD LOW RESISTANCE TO AIR MOVEMENT
AND IS THEREFORE THE IDEAL SOLUTION.
Form and planning
Hot dry climate
Warm humid
climate
Form and planning
Hot-dry climate
Form and planning
Hot-dry climate
Form and planning
Hot-dry climate
Form and planning
Warm-humid climate
Form and planning
Warm-humid climate
Form and planning
Warm-humid climate
External space
HOT-DRY CLIMATE
•EXTERNAL SPACES ARE NECESSARY TO TREAT AS
IMPORTANTLY AS THE BUILDING.
•ADJACENT BUILDINGS,
PAVEMENTS (FOOTPATH KIND OF) HEAT UP QUICKLY
DRY GROUND
NIGHT DAY
RERADIATE THE HEAT STORED PAINFUL GLARE
DURING THE DAY. RELECT HEAT RADIATION
TOWARDS THE BUILDING
DURING THE DAY.
• TREES , PLANTS , WATER body WILL COOL THE AIR BY
EVAPORATION.
• thermal regulators :- 1. courtyard
2. water body
• WATER BODY – COOL AIR at night IS RETAINED, AS cool
AIR IS HEAVIER THAN THE SURROUNDING WARM AIR.
External space
WARM-HUMID CLIMATE
EXTERNAL SPACES
SHADING FREE PASSAGE
[IMPORTANT FOR AIR MOVEMENT IN
EXTERNAL SPACES]
• PARGOLAS OR FRAMING TO BE COVERED BY CLIMBING
PLANTS.
• PRIVACY IS NOT OBTAINED – FOR PRIVACY
- PALING FENCES
- SCREEN WALLS DO NOT
PERMIT DIRECT VIEW BUT
ALLOW BREEZE TO PENETRATE
EG. LOUVERS.
• THE DENSITY OF HOT-DRY IS MORE THAN WARM-HUMID
REGIONS.
– THREE REASONS
• TO ALLOW FREE MOVEMENT OF AIR THROUGH BUILDINGS
AND SPACES BETWEEN BUILDINGS.
• TO PROVIDE PRIVACY BY DISTANCES,AS WALLS AND
SCREENS CANNOT BE USED FOR THIS PURPOSE.
• MANY ACTIVITIES ARE CARRIED OUT-OF-DOOR.
External space
Hot-dry climate
External space
Hot-dry climate
External space
Hot-dry climate
RO
OFS
, W
ALLS
AN
D O
PEN
IN
GHot – dry climate
•In hot dry climate roof and walls would absorb more heat during
day time due to heavy material.
• Thus the design of opening is governed by two requirements:
1.During the day the absence of opening would be most desirable,
or at least opening as small as possible, located high on the
walls.
2. During the night the openings should be large enough to
provide adequate ventilation for the dissipation of heat emitted
by the walls and roofs.
• Designer must study the occupancy pattern of the building.
• For eg.,
- office building must have time lag of 4-6 hours.
- residential building must have time lag of 9-12 hours.
• In regions where diurnal ranges are less extreme ,where the
night-time temperature does not fall below the comfort zone ,
the large thermal capacity should be restricted to internal
walls, partition and floors, whilst the outer walls and roof
would need to have a high resistive insulation.
• Alternatively separate day and night rooms could be provided in
the house.
RO
OFS
, W
ALLS
AN
D O
PEN
IN
GHot – dry climate
RO
OFS
, W
ALLS
AN
D O
PEN
IN
GHot – dry climate
RO
OFS
AN
D W
ALLS
WARM-HUMID CLIMATE
• THE CONSTRUCTION OF BUILDING OF LOW THERMAL CAPACITY
MATERIAL OF LIGHT WEIGHT IS ADVISABLE.
• THE ROOF IS PRACTICALLY THE ONLY ELEMENT WHICH HAS A
VERY GREAT SIGNIFICANCE.
• IT CANNOT IMPROVE THE CONDITIONS, I.E., IT WILL NOT PRODUCE
TEMPERATURES COOLER THAN THE OUT DOOR AIR, BUT ATLEAST ,
IF WELL DESIGNED ,IT CAN PREVENT THE INDOOR TEMPERATURE
INCREASING ABOVE THE OUT DOOR AIR TEMPERATURE , AND KEEP
THE CEILING TEMPERATURE AROUND THE SAME LEVEL AS OTHER
SURFACES.
• IT HAS BEEN SUGGESTED (97) AS A PERFORMANCE STANDARD,
THAT RHE CEILING TEMPERATURE SHOULD NOT EXCEED THE AIR
TEMPERATURE BY MORE THAN 4°C.
RO
OFS
AN
D W
ALLS
WARM-HUMID CLIMATE
RO
OF AN
D W
ALL S
UR
FAC
ES
HOT - DRY CLIMATE
IT DEPENDS UPON :
1. SURFACE MATERIAL
2. SURFACE TREATMENT
3. COLOUR
CONTROLS THERMAL
BEHAVIOUR AND PREVENTS
HEAT RADITAION
• COLOUR USED MUST BE LIGHT
• THE MATERIAL USED SHOULD BE SHINY
REFLECTS
LARGE AMOUNT
OF INCIDENT
RADIATION
ROOF
• ANY LOCATION NEAR THE EQUATOR RECIEVES GREATEST AMOUNT
OF SOLAR RADIATION DURING DAY TIME
•DURING NIGHT IT IS MOSTLY EXPOSED, THUS IT EMITS RADIATION
TO OUTER SPACES.
•ROOF SUFRACES MATTER MORE THAN THE WALL SURFACES.
•ABSORBANCE AND EMITTANCE VALUE REMAIN SAME FOR A
MATERIAL FOR SAME TEMPERATURE.
RO
OF AN
D W
ALL S
UR
FAC
ES
HOT - DRY CLIMATE
RO
OF AN
D W
ALLS
UR
FAC
ES
WARM-HUMID CLIMATE
• OPENINGS MUST BE PLACED SUITABLY IN RELATION TO THE
PREVAILING BREEZES TO PERMIT NATURAL AIR FLOW THROUGH
THE INTERNAL SPACES AT BODY LEVEL.
• SUCH OPENINGS SHOULD BE LARGE AND FULLY OPENABLE;
THERE IS NO POINT IN HAVING FIXED GLASS PANES.
• OPENINGS SHOULD BE FROM THE EFFECT OF OUTSIDE
OBSTRUCTIONS.
• AIR FLOW SHOULD NOT PASS OVER HOT SURFACES BEFORE
REACHING THE BUILDING.
• LARGE OPENINGS – GIVEN PROTECTION – DRIVING
RAIN,INSECTS,SMELLS AND NOISE WITHOUT RADICALLY
REDUCING AIR MOVEMENT.
• CEILING MOUNTED OR OTHER ELECTRIC FANS MAY BE USED
WHEN THERE IS LITTLE OR NO BREEZE,BUT THESE WILL
NORMALLY PROVIDE AN AIR MOVEMENT,NOT INDUCE THE
EXCHANGE OF AIR.
VEN
TILATIO
N AN
D AIR
FLO
WHOT - DRY CLIMATE
• DURING THE DAY-TIME OPENINGS SHOULD BE CLOSED AND
SHADED.
•AS THE HOTTEST SURFACE IS LIKELY TO BE THE CEILING OR THE
UNDESIRABLE OF THE ROOF, IT IS ADVISSABLE TO HAVE THE TOP
OF THE OPENINGS LEVEL WITH THE CEILING.
•ATTENTION MUST BE PAID TO THE DESIGN OF THE OPENINGS TO
THIS SPACE AND THEIR ORIENTATION IN RELATION TO THE
PREVAILING BREEZE.
•ROOF SLOPES SHOULD BE ORIENTED TOWARDS THE
PREVAILING BREEZE, AND ANY OBSTRUCTIONS WHICH WOULD
PREVENT THE AIR FLOW NEXT TO THE ROOF SURFACES SHOULD
BE AVOIDED.
•HIGH SOLID PARAPET WALLS AROUND THE ROOF WOULD ,
CREATE A STAGNANT POOL OF HOT AIR , AND SHOULD
THEREFORE BE AVOIDED.
VEN
TILATIO
N AN
D AIR
FLO
WHOT - DRY CLIMATE
VEN
TILATIO
NWARM-HUMID CLIMATE
• WITHOUT THE EXCHANGE OF AIR BOTH THE TEMP. AND THE
HUMIDITY OF ROOM AIR WILL INCREASE ABOVE THE OUT DOOR
VALUES, DUE TO THE HEAT AND MOISTURE OUTPUT OF HUMAN
BODIES AND OSF VARIOUS HUMAN ACTIVITIES (EG WASHING NAND
COOKING)
• IN THIS CLIMATE THERE IS A NEED FOR BOTH VENTILATION AND
FOR A SENSIBLE AIR MOVEMENT ACROSS THE BODY SURFACE.
• CARE MUST BE TAKEN TO AVOID AIR WHICH HAS PASSED
THROUGH A ROOF SPACED REACHING THE LIVING ZONE(EG.
VERANDAH) AS THIS WILL BE MUCH HOTTER THAN THE NORMAL
OUTDOOR AIR
VEN
TILATIO
NWARM-HUMID CLIMATE
TRAD
ITIO
NAL S
HELTER
HOT - DRY CLIMATE
DESERT REGION SHELTER
• HEAVY WALLS OF EARTH ,BRICK ,STONE AND ROOFS ARE OF
SAME MATERIALS .
•THICK WALLS PROVIDES GOOD
THERMAL CAPACITY
SECURITY
PROTECTION AGAINST NOISE
• STRUCTURES TENDS TO BE HOT AT NIGHT DURING HOT SEASONS.
OUTER PRIVATE SPACES SUCH AS
COURTYARDS AND ROOFS
PREVENTION
• ROOMS BUILT AROUND A CENTRAL COURTYARD WHICH PROVIDES
COOLER ATMOSPHERE AT NIGHT.
•WINDOW DOORS ARE SMALL IN SIZE AND LESS IN NUMBER.
•WINDOWS LOCATED HIGH ON WALLS.
ADMITTING LESS HEAT AND DUST,
REDUCING GROUND GLARE.
•VENTILATIONS ARE INADEQUATE AND ALSO THE HOUSES ARE
CLOSELY BUILT.
TRAD
ITIO
NAL S
heLTER
WARM- HUMID CLIMATE
BASICALLY TWO TYPES OF SHELTER
EARTH TIMBER
•POOR AND NON-INTENSIVE
AIR CREATES UNBEARABLE
CONDITION.
•INTENSE HEAVY RAIN
ERODE THE BASES AND
SURFACES OF EARTH
WALLS.
•ANNUAL MAINTAINANCE IS
ESSENTIAL.
•UNVENTILATED INTERIOR
REMAIN CONSTANTLY DAMP.
•SHELTER IS ELEVATED BY STILTS
•LOCAL TIMBER AND BAMBOO IS
USED.
•THATCH COVERS BAMBOO ROOF-
FRAME WITH OVERHANGING EAVES.
•THATCH IS BETTER THERMAL
INSULATOR.
•THATCH ROOF IS CONVENIENT TO
THE BREEDING OF INSECTS AND
TERMITES.
•LIGHTWEIGHT TIMBER HOLDS LESS
HEAT AND COLS ADEQUATELY AT
NIGHT
•ELEVATED SHELTER
BROAD EAVES
•SHADE THE WALLS AND OPENING, PROVIDE PROTECTION FROM
DRIVING RAIN AND SKY GLARE AND PERMIT THE OPENING TO BE
KEPT OPEN MOST OF THE TIME.
MAR
ITIM
E D
ES
ER
T C
LIM
ATES HOT-DRY CLIMATE
• THESE CLIMATES DIFFER ONLY SLIGHTLY FROM THE HOT DRY
DESERT REGIONS - THE MAIN DIFFERENCE BEING THE HIGH
HUMIDITY.
• THE COASTAL WIND BLOWING OF THE SEA DURING THE DAY
MAY BE UTILISED FOR BETTER THERMAL CONDITIONS.
• THE NIGHT TIME WIND BLOWING TOWARDS THE SEA , BRINGS
THE HOT INLAND DESERT AIR, POSSIBLY DUST,AND IT CAN BE
DECIDEDLY UNPLEASANT.
• THE ONLY SOLUTION TO PROVIDE –
• A) ONE WITH HIGH THERMAL CAPACITY WALLS AND ROOFS,
FOR USE AT NIGHT,ESPECIALLY DURING THE COOLER PART OF
THE YEAR. THIS SHOULD HAVE NO OPENINGS FACING THE
INLAND DIRECTION.
• B) ONE OF LIGHT WEIGHT CONSTRUCTION , THE ROOF ONLY TO
PROVIDE SHADE, THE SIDE FACING THE SEA, AS WELL AS THE
OPPOSITE SIDE BEING ALMOST COMPLETELY OPEN. THIS IS THE
BEST SOLUTION FOR DAY TIME USE, ESPECIALLY DURING THE
HOTTEST PART OF THE YEAR.
MAR
ITIM
E D
ES
ER
T C
LIM
ATES HOT-DRY CLIMATE
Warm-humid island climate
WARM-HUMID CLIMATE
• TEMPERATURES ARE SLIGHTLY LOWER, BUT THERE IS A
STEADY WIND OF 6-7 M/S AND ALMOST CONSTANT DIRECTION TO
RELY ON FOR COOLING .
• THE ORIENTATION AND CONSTRUCTION OF THE BUILDING TO
CATCH THE MAXIMUM AMOUNT OF AIR MOVEMENT WILL BE EVEN
MORE IMPERATIVE THAN IN WARM-HUMID CLIMATE.
• MOST OF THESE ISLANDS LIE IN THE TROPICAL CYCLONE
BELT.
• CONSTRUCTION AND STRUCTURE MUST BE DESIGNED TO
WITHSTAND THE WINDS OF UPTO 7O M/S .
Warm-humid island climate
WARM-HUMID CLIMATE
climate
Common factors
SHIVAM PATEL 12SA131
VAIBHAVI LUHANA 12SA139
MEET PATEL 11SA120
SHIVANI PATEL 12SA132
SWAPNIL PATEL 12SA137
RAHUL MAKWANA 12SA128