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ARCHITECTURE IN COLD & DRY
REGIONS
SUBMITTED BY:-
SARTHAK GOYAL
SAYAN MUNSHI
SHARDUL GARG
SHUBHAM KUMAR
RADHIKA
PURU SHARMA
VANSHIKA TYAGI
SWATI SHABNAM
SUBMITTED TO:-
Ar.GAURAV RANA
CLIMATEININDIA
India is home to an extraordinary variety
of climatic regions, ranging from tropical in
the south to temperate and alpine in the
Himalayan north, where elevated regions
receive sustained winter snowfall. The
nation's climate is strongly influenced by the
Himalayas and the Thar Desert.
COLD AND DRY
Regions that lie in the cold climate zone are
situated at high altitudes. The temperatures
range between 20–30 ºC in summers; while in
winters, it can range from -3 ºC to 8 ºC, making
it quite chilly.
Humidity
Avg - 76%
Max - 0%
Min - 0%
Wind: 3
km/h ↑ from
NorthwestVisibility: 4 km
Ladakh’s climate is a little
extreme – the summers can get a
little harsh with direct sunlight
falling at such a high altitude and
winters can be really cold, with
temperatures dropping below
freezing point.
Pressure: 1007 mb.
Cloud Cover: 57 %.
Solar radiation-
5530 whr/sq m/
day at 35°south
facing
Climate data for Leh (1951–1980)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high
°C (°F)
8.3
(46.9)
12.8
(55)
19.4
(66.9)
23.9
(75)
28.9
(84)
34.8
(94.6)
34.0
(93.2)
34.2
(93.6)
30.6
(87.1)
25.6
(78.1)
20.0
(68)
12.8
(55)
34.8
(94.6)
Average high
°C (°F)
−2.0
(28.4)
1.5
(34.7)
6.5
(43.7)
12.3
(54.1)
16.2
(61.2)
21.8
(71.2)
25.0
(77)
25.3
(77.5)
21.7
(71.1)
14.6
(58.3)
7.9
(46.2)
2.3
(36.1)
12.8
(55)
Average low
°C (°F)
−14.4
(6.1)
−11.0
(12.2)
−5.9
(21.4)
−1.1
(30)
3.2
(37.8)
7.4
(45.3)
10.5
(50.9)
10.0
(50)
5.8
(42.4)
−1.0
(30.2)
−6.7
(19.9)
−11.8
(10.8)
−1.3
(29.7)
Record low
°C (°F)
−28.3
(−18.9)
−26.4
(−15.5)
−19.4
(−2.9)
−12.8
(9)
−4.4
(24.1)
−1.1
(30)
0.6
(33.1)
1.5
(34.7)
−4.4
(24.1)
−8.5
(16.7)
−17.5
(0.5)
−25.6
(−14.1)
−28.3
(−18.9)
Average
rainfall mm
(inches)
9.5
(0.374)
8.1
(0.319)
11.0
(0.433)
9.1
(0.358)
9.0
(0.354)
3.5
(0.138)
15.2
(0.598)
15.4
(0.606)
9.0
(0.354)
7.5
(0.295)
3.6
(0.142)
4.6
(0.181)
105.5
(4.154)
Avg. rainy
days
1.3 1.1 1.3 1.0 1.1 0.4 2.1 1.9 1.2 0.4 0.5 0.7 13.0
January, February and December: One of the coldest
times of the season. The nights are chilling and
temperatures hover around -20°C. Days are still
bearable with 2°C as average temperature.
March and April: March is colder than April.
Temperatures hover between 6°C in the day and -5°C
in the night. April is still better and day temperatures
go up as much as 12°C. There is still the occasional
snowfall that further dips the mercury down.
May, June, July and August: Temperatures are a
pleasant 16°C during the day and a barely manageable
3°C in the night. The breeze still carries the winter
chill and one may feel the bite if sitting in shade for
too long. June is when the mercury really kicks up and
temperatures soar up to 21°C (day).
September, October and November: All through
September, the weather is somewhat similar to that in
May. The days are a lovely 20-22°C and all of Ladakh is
rinsed by ample sunshine. The nights are back to being
bitterly cold the months of October and November that
Ladakh goes back to its gloomy self.
ESSENTIALFEATUREINTHEDESIGNINGOF
HOUSE
BUILDING WILL HAVE SLOPING ROOF.
WINDOWS WILL HAVE WOODEN PANNEL.
TIMBER PANNELED WALL WILL BE USED INSTEED
OF BRICK OR STONE MASONRY.
THICK WALL WILL BE USED WITH SOUND
INSULATION.
BEDROOM WILL BE ON SOUTH WEST OF THE
BUILDING.
KITCHEN WILL BE ON SOUTH EAST OF THE
HOUSE.
DINNING WILL BE ON THE SOUTH.
BATHROOM WILL BE ON THE NORTH WEST OF
THE HOUSE.
ESSENTIALFEATUREINTHEDESIGNINGOF
HOUSE
Natural light is important in the house.
Flooring of the house must be of timber .
Noisy place is avoided for building.
Living area should be in the north of the
building.
Utility rooms [washing and domestic works]
should be in the south.
Cross ventilation is very important for
healthy living.
Trees can be planted near windows to block
cold air.
The sun’s movement through the day and
through the year is one of the most crucial
environmental factors to understand when
designing high performance buildings.
Altitude is the vertical angle the sun makes with the ground plane (0° < alt < 90°).
Azimuth is the horizontal angle between the sun and true north (–180° < azi < 180°, positive in a
clockwise direction from north)
Resist heat loss
Decrease exposed surface area
Increase thermal resistance
Increase thermal capacity
Increase buffer spaces
Decrease air exchange rate
Increase absorptivity.
COLD AND DRY
Gable roofs are used in hilly areas, as
these roof types are able to shed snow in
hilly areas.
The main used material for roofing in hilly
areas is timber, as it is locally available
from trees.
Trees which are used for this purpose are:
cedar.
Vegetation regions are natural
environments that provide the stage
for human activities such as farming,
raising livestock, and producing
timber. Soil, temperature, and
moisture influence the type of
vegetation that thrives naturally in a
region. Vegetation patterns are
identified on the basis of the
ecosystems they support. An
ecosystem is an interdependent
community of plants and animals.
The ecosystem of a region is referred
to as a biome. Biomes are further
divided into forest, grassland,
desert, and tundra.
*chuman existence in many ways. The
world’s food supply depends greatly on
the top six inches of soil (sometimes
called topsoil). Such factors as depth,
texture, and humus content of the soil
determine the type of vegetation that
can be supported in a region. That, in
turn, helps to influence which human
activities may take place there. As you
study the chart below, notice the
relationship of climate to the
characteristics of the soil. Soil
characteristics and climate are major
influences in vegetation regions.
COLD AND DRY
*WIKIPEDIA.ORG
*GOOGLE IMAGES
*www.nrel.gov
COLD AND DRY

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COLD AND DRY

  • 1. ARCHITECTURE IN COLD & DRY REGIONS SUBMITTED BY:- SARTHAK GOYAL SAYAN MUNSHI SHARDUL GARG SHUBHAM KUMAR RADHIKA PURU SHARMA VANSHIKA TYAGI SWATI SHABNAM SUBMITTED TO:- Ar.GAURAV RANA
  • 2. CLIMATEININDIA India is home to an extraordinary variety of climatic regions, ranging from tropical in the south to temperate and alpine in the Himalayan north, where elevated regions receive sustained winter snowfall. The nation's climate is strongly influenced by the Himalayas and the Thar Desert.
  • 4. Regions that lie in the cold climate zone are situated at high altitudes. The temperatures range between 20–30 ºC in summers; while in winters, it can range from -3 ºC to 8 ºC, making it quite chilly.
  • 5. Humidity Avg - 76% Max - 0% Min - 0% Wind: 3 km/h ↑ from NorthwestVisibility: 4 km Ladakh’s climate is a little extreme – the summers can get a little harsh with direct sunlight falling at such a high altitude and winters can be really cold, with temperatures dropping below freezing point. Pressure: 1007 mb. Cloud Cover: 57 %. Solar radiation- 5530 whr/sq m/ day at 35°south facing
  • 6. Climate data for Leh (1951–1980) Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Record high °C (°F) 8.3 (46.9) 12.8 (55) 19.4 (66.9) 23.9 (75) 28.9 (84) 34.8 (94.6) 34.0 (93.2) 34.2 (93.6) 30.6 (87.1) 25.6 (78.1) 20.0 (68) 12.8 (55) 34.8 (94.6) Average high °C (°F) −2.0 (28.4) 1.5 (34.7) 6.5 (43.7) 12.3 (54.1) 16.2 (61.2) 21.8 (71.2) 25.0 (77) 25.3 (77.5) 21.7 (71.1) 14.6 (58.3) 7.9 (46.2) 2.3 (36.1) 12.8 (55) Average low °C (°F) −14.4 (6.1) −11.0 (12.2) −5.9 (21.4) −1.1 (30) 3.2 (37.8) 7.4 (45.3) 10.5 (50.9) 10.0 (50) 5.8 (42.4) −1.0 (30.2) −6.7 (19.9) −11.8 (10.8) −1.3 (29.7) Record low °C (°F) −28.3 (−18.9) −26.4 (−15.5) −19.4 (−2.9) −12.8 (9) −4.4 (24.1) −1.1 (30) 0.6 (33.1) 1.5 (34.7) −4.4 (24.1) −8.5 (16.7) −17.5 (0.5) −25.6 (−14.1) −28.3 (−18.9) Average rainfall mm (inches) 9.5 (0.374) 8.1 (0.319) 11.0 (0.433) 9.1 (0.358) 9.0 (0.354) 3.5 (0.138) 15.2 (0.598) 15.4 (0.606) 9.0 (0.354) 7.5 (0.295) 3.6 (0.142) 4.6 (0.181) 105.5 (4.154) Avg. rainy days 1.3 1.1 1.3 1.0 1.1 0.4 2.1 1.9 1.2 0.4 0.5 0.7 13.0
  • 7. January, February and December: One of the coldest times of the season. The nights are chilling and temperatures hover around -20°C. Days are still bearable with 2°C as average temperature. March and April: March is colder than April. Temperatures hover between 6°C in the day and -5°C in the night. April is still better and day temperatures go up as much as 12°C. There is still the occasional snowfall that further dips the mercury down. May, June, July and August: Temperatures are a pleasant 16°C during the day and a barely manageable 3°C in the night. The breeze still carries the winter chill and one may feel the bite if sitting in shade for too long. June is when the mercury really kicks up and temperatures soar up to 21°C (day).
  • 8. September, October and November: All through September, the weather is somewhat similar to that in May. The days are a lovely 20-22°C and all of Ladakh is rinsed by ample sunshine. The nights are back to being bitterly cold the months of October and November that Ladakh goes back to its gloomy self.
  • 9. ESSENTIALFEATUREINTHEDESIGNINGOF HOUSE BUILDING WILL HAVE SLOPING ROOF. WINDOWS WILL HAVE WOODEN PANNEL. TIMBER PANNELED WALL WILL BE USED INSTEED OF BRICK OR STONE MASONRY. THICK WALL WILL BE USED WITH SOUND INSULATION. BEDROOM WILL BE ON SOUTH WEST OF THE BUILDING. KITCHEN WILL BE ON SOUTH EAST OF THE HOUSE. DINNING WILL BE ON THE SOUTH. BATHROOM WILL BE ON THE NORTH WEST OF THE HOUSE.
  • 10. ESSENTIALFEATUREINTHEDESIGNINGOF HOUSE Natural light is important in the house. Flooring of the house must be of timber . Noisy place is avoided for building. Living area should be in the north of the building. Utility rooms [washing and domestic works] should be in the south. Cross ventilation is very important for healthy living. Trees can be planted near windows to block cold air.
  • 11. The sun’s movement through the day and through the year is one of the most crucial environmental factors to understand when designing high performance buildings. Altitude is the vertical angle the sun makes with the ground plane (0° < alt < 90°). Azimuth is the horizontal angle between the sun and true north (–180° < azi < 180°, positive in a clockwise direction from north)
  • 12. Resist heat loss Decrease exposed surface area Increase thermal resistance Increase thermal capacity Increase buffer spaces Decrease air exchange rate Increase absorptivity.
  • 14. Gable roofs are used in hilly areas, as these roof types are able to shed snow in hilly areas. The main used material for roofing in hilly areas is timber, as it is locally available from trees. Trees which are used for this purpose are: cedar.
  • 15. Vegetation regions are natural environments that provide the stage for human activities such as farming, raising livestock, and producing timber. Soil, temperature, and moisture influence the type of vegetation that thrives naturally in a region. Vegetation patterns are identified on the basis of the ecosystems they support. An ecosystem is an interdependent community of plants and animals. The ecosystem of a region is referred to as a biome. Biomes are further divided into forest, grassland, desert, and tundra.
  • 16. *chuman existence in many ways. The world’s food supply depends greatly on the top six inches of soil (sometimes called topsoil). Such factors as depth, texture, and humus content of the soil determine the type of vegetation that can be supported in a region. That, in turn, helps to influence which human activities may take place there. As you study the chart below, notice the relationship of climate to the characteristics of the soil. Soil characteristics and climate are major influences in vegetation regions.