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Landscape Planning for Climatic Adaptation in hot arid climatic zones

 Imad Kayyali

 Preface:

 There are not different “kinds” of architecture, but only different situations, which
 require different solutions in order to satisfy man’s physical and psychic needs.

 Man dwells when he can orient himself within and identify himself with an
 environment, or, in short, when he experiences the environment as meaningful.
 Dwelling therefore implies something more than “shelter”. It implies that the spaces
 where life occurs are places, in the true sense of the word. A place is a space, which
 has a distinct character. Since ancient times the genius loci, or “spirit of place”, has
 been recognized as the concrete reality man has to face and come to terms with in
 his daily life.

                                                            Christian Orberg-Schultz


 This article summarizes a project research that has been conducted in some Gulf country. The site was
 distinguished with its extreme dry and hot climate, in addition to the dust storms, which blow in spring
 and summer each year, resulting sand erosion and very uncomfortable weather conditions. These
 conditions may cause some problems for the labors that will be in site during construction.

 Our team’s idea was to protect the site through the landscape planning, before any construction works
 being curried out on site. Our main target that could become our main achievement was to minimize the
 effects of the harsh climate generators, in addition to increase all those elements that may beco- me
 moderating factors and provide comfort for the work site.

 In response to Dubai Municipality’s plan on the continuous training program, this study has been enriched
 recently, with additional text on the climate that distinguishes Dubai and a high percentage of the UAE
 area while still part of the hot arid climate area, this climate witnesses high humidity.

 The article manifests two parts: The first part demonstrates in summary the general topics of landscape
 architecture. The second sheds lights on landscape planning for climatic adaptation, with special emphasis
 for the hot arid climate zone.

                                                                 Imad M. Kayyali
                                                                 Dubai, 1999.

 Part One:          Landscape Architecture:

1.1 Introduction:

 While architects are involved with the design of buildings and their immediate surroundings, landscape
 architects are concerned with the design and preservation of the whole outdoor natural elements:
 topography, vegetation, water surfaces, Ecology, etc, that should make man’s outdoor life more
 comfortable, & afford him with means that help him to resist natural dangers such as: frost, floods, dust &
 precipitation, etc. as well as man-made effective elements, such as: pollution & noise, land forms & water
 features, beside facilitating man with recreational areas, pathways, street furniture & others.




                                                       1
Landscape architecture has been developed through history, in parallel with architecture. Landscape
 styles were related to regions, cultures or historical eras, such as: Ancient Egypt, Mesopotamia, Greece,
 Romans, Islamic World, middle Ages, Renaissance, Baroque, China, Japan, India, etc.

 New movements have appeared in the late 1960s in several regions, that concluded landscape types into
 the following defined categories.

        a- Formal Geometric Landscape            b- Rustic Landscape
         c- Natural and Desert Landscape. d- Transitional Landscape
         e- Tropical Landscape                     f- Oriental Landscape.
         g- Woody Landscape.

          Eventually, Landscape Architecture comprises the following two parts:

        a- Hard Landscape: which is concerned with man-made elements, such as paving, sidewalks,
             streets, parapets, decks, gazebos, etc.
        b-   Soft Landscape: Which deals with plant materials and vegetation: trees, shrubs, vines, ground
             covers, etc.

 1.2      Plants:

 The Plant Kingdom is usually categorized into the following:

a- Annuals,           b- Non-flowering (ferns) & Herbaceous perennials (Bulbs) c- Biennials.
       d- Woody Perennials- Flowering plants (Permanent).

 For landscape purpose, plant materials are sorted out into:

 a- Trees         b- Shrubs                                       c-Bushes
 d- Vines e- Ground Covers and Lawns           f- Bulbs, Ferns & Annuals.

 Trees and shrubs are usually either Deciduous or Evergreen, where deciduous stands for those species
 which loose their leaves in winter.

 1.3      Site Analysis:

 Prior to the design process get started, a full site analysis shall be conducted, comprising site geology,
 slopes, ecology, soil, vegetation, climate, aquifers & infrastructure. Analyzing this information shall lead to
 the best adaptation to site restrictions, potentials & requirements.

 Part Two:          Landscape Planning for Climatic Adaptation in Hot Arid Climate.

          2.1       Introduction:

          In the ancient times, it was said that man’s life pattern is dependent upon the climatic conditions
          in which he finds himself. Environment dictates man’s means of livelihood, home, food and
          clothing

          People believe that the proper climatic conditions were the main stimulus for the development
          of civilizations, also it is believed that workers productivity declines in climates of excessive heat
          or cold.




                                                        2
Hence, we are getting closer to the question: can man control his environment? In spite of the
    great choices offered by modern technology in order to facilitate man with means so as to
    sustain excessive climatic conditions, it became quite improper to rely on those artificial means
    that have side effects upon man’s environment. Beside, communities are loosing natural
    resources through the extensive use of modern technology.

    During last decades, man began to look for natural elements those can modify his micro-climate.
    The relatively new expression of “micro-climate” describes the climatic conditions of a very local
    area or place, such as a hillside or an in-house courtyard, which are smaller in scale than the
    Mesoclimate and the Macroclimate scales. The micro-climate shall not confuse the reader with
    the microclimate expression, which describes the microscopic scale of climatic conditions.

    The following table illustrates the principal climatic scales:
               Climate                            Scale                         Example
     Macro-climate                    Extremely Large                Continent, Country
     Meso-climate                                                    Country, City
                                      Moderate
     Micro-climate                    Small                          City block, Lot, Garden
     Microclimate                     Extremely small                Leaf, sidewalk crack

    2.2      Climatic Impact of Natural and Man-made Elements:

           2.2.1. Climate Generators:

             Before discussing the natural elements affecting micro-climate areas, it’s quite helpful
             to have a look on the main generators of climate affecting man’s comfort. These
             generators are:

            i- Solar Radiation: moving through the atmosphere, solar radiation may:
           a- Reflected back into space.
           b- Dissipated within the atmosphere.
           c- Diffused through the atmosphere.
           d- Strikes the earth’s surface.

Energy is transferred through, Radiation, Conduction

and Convection. Radiated Heat transfers at the

speed of light in the form of electromagnetic waves.

The other forms of heat transfer are much slower

and need a media to transfer.


The dynamics of the solar movement shall be

analyzed for best shading.




                                                  3
ii- Winds: Moving over the earth’s surface, they encounter of impediments which:
              detract, deflect, obstruct and lessen the impact of speed of the flow of the
              unobstructed wind.

            Wind movement can be (a) Laminar (Steady), (b) Turbulent (Random Pattern and
            unpredictable) or (c) Separated. Air movement is affected by its inertia, friction with
            surrounding elements and differences in pressure and temperature.

            The major groups of winds are:
                      a- Tropical Easterly of Trade Winds.
                      b- The Mid-latitude Westerly.
                      c- Polar Winds.

           iii- Precipitation and Humidity: Rain, Snow, Moisture, Evaporation, Dew and Frost.
              Atmospheric Humidity can be measured in three different ways:
                     a- Absolute Humidity: g/m3 of air
                     b- Specific Humidity: g/kg of air.
                     c- Vapor Pressure: Bars of Water Weight.
                     d- Relative Humidity RH: Actual/ Saturated %

           2.2.2     Man Made Elements (Hard Landscape Materials)

           Different Materials have variable responses to sun radiation, in what we call “Specific
           Heat”. On the other hand, some of the material’s properties may alter the material’s
           response against sun radiation. Those properties are, Mass, color, texture, exposed area,
           location, orientation, etc.
           Therefore, our landscape materials are categorized according to their abilities to reflect,
           radiate and transmit solar radiation.

           We hereby list some selected materials together with their relative reflectivity % of sun
           radiation, taking into consideration that these figures may vary as mentioned above in
           connection with other parameters such as color and texture:


            Asphalt                            12%               Brick
                   50%

            Concrete                  40%                Dark Forest                05%

Desert                     25%               Dry Grass                   30%
            Green Forest              09%                Oak woodland      17%
            Green Leaves              30%                Green Fields               12%
            High Fresh Grass          25%                Rock                       12%

Dry Sand            27%

           2.2.3.    The Natural Elements:

           Landforms and vegetation are considered to be the major natural elements that may
           affect the micro-climate:




                                              4
a-         Landforms: Landforms can be either of large, medium or small scale.
Landforms may affect air movement through deflection, impeding airflow pattern, velocity, quality
and quantity.




                   b-          Vegetation: The effectiveness of special plant materials in climate
                               control depends upon the forms and character of the plant, the climate
                               of the region and the specific requirements of the site.

                         Vegetation may absorb 90% of the light falling on it.
                         Vegetation can filter, guide, obstruct, reduce or accelerate winds.
                         The optimum density of vegetation for wind control (by ASLA) is 50-60%
                         Vegetation may reduce wind speeds in an area to less than 10% of that in
                          the open, or increase them, reduce day time temperature by as much as
                          8.5°C, and in certain situations, raise night time temperature.
                         The main uses of vegetation of special importance to the energy- conscious
                         designers are:

             1- Large trees and shrubs: screen out undesirable winds and evergreen trees of high
                dense leaves should be used to control winter winds.
             2- Trees: channel winds to increase ventilation.
             3- Plantings: Reduce snow accumulations on ground.
             4- Vegetation: Especially needle leave trees: capture fog, increase sunlight reaching
                ground.
             5- Deciduous Trees: Screen sunlight in summer, then reduce required cooling loads and
                allow it to pass in winter, then reduce required heating loads.
             6- Planted Areas: Will be cooler during day, then heat loss at night will be less, then
                razing specific heat of area.
             7- Precipitation increases in forest areas.


                                                 5
2.3 Temperature Control:
a- Solar Radiation Control:

Vegetation provide solar radiation control through:
Absorbing, Reflecting, Radiating and Transmitting.

The Major effect of the forest on any climatic factor is
reduction of short wave radiation by 73-80%. The forest
can reduce monthly maximum air temperature in the
summer by 6.5°C, reduce annual rain fall (through
interception) by 15-30% and wind velocity by 20-60%.

b- Wind Control:

The most interest wind is that blowing at 1.8-2.5 m High.
But it is effective up to 18 m.

Planting affect air flow in the following ways:

     1-   Affecting Wind Movement.
     2-   Affecting amount of airflow.
     3-   Changing air direction.
     4-   Has no effect on lees side of a building, but may perform as an obstacle when applied on an
          outlet opening.

          Wind velocity control is a principal factor that needs to be modified so as to reduce energy used
          in either heating or cooling. For example, heating load with a 36-km/h wind is 2.4 times as 10-
          km/h wind (without protection). When protected, it would be twice only. For hot humid climate,
          wind control is the vital factor that has to be considered for ventilation.

          Notes on wind breaker trees and hedges:

             The taller the trees are, the more raws
              required, as tree gets naked trunk taller as it is
              taller, which allow for low height streams of
              wind.
             Width affects only penetrability.
             Irregular windbreakers (mixture of trees) are
              more effective.
             Trees of pitched edges are less effective.
             The most effective ratio of height to protected
              length is 1:11.5.
             The optimum density for a shelter belt is about
              50-60%.
             Parallel shelterbelts, spaced widely apart, have no acomm-ulative effect on reducing wind
              velocity. But closer ones do.
             Plants should be located to protect buildings from expected directions.

          2.4      Water




                                                        6
Seas, Lakes and Rivers are preferable for people... for amusement, picnics, recreations and
adventures, in addition to transportation.

People like to be near water surfaces because they can enjoy skating, sailing, fishing, swimming,
sinking, etc. However, they like it also because of the cooling effect that water bodies provide in
the surrounding area.

Old Arabs have practiced another experience with water features, such as: fountains, ponds,
channels, etc. In order to modify the micro- climate of places like the “Dorqua” by adding
humidity to the dry air in summer and cooling it by investing the high specific heat of water,
which cause less variation of pattern of temperature between day and night, summer and
winter.

Therefore, it would be a right decision to use water bodies in the hot arid climate zones, so as to
modify the climate and reduce its extremes through the cooling effect of water and moisture.
Add to that, a small percentage of the solar radiation is radiated off water bodies, that is because
solar radiation is stored deeply underneath surface. Water bodies cause evaporation that would
reduce temperature in the surrounding space.

Airflow in day blows from cooled sea towards warmed land, and at night, from cold land to
cooled sea.

2.5 Hot Arid Climate and Human Adaptation

         2.5.1 - Hot Dry Climate:

         The main macro features of the hot arid climate are: Clear sky, dry atmosphere, extends
         periods of overheating & high diurnal temperature range. Among the principle
         parameters of overhea- ting is the formation of the dust particles in the air that absorb
         solar radiation & radiates heat through atmosphere.

         2.5.1.1 Objectives of Adaptation

       1- Block dry dusty wind. Vegetation can clear air through reducing the formation of
          clouds of dust and smoke by preventing formation of rising air due to reducing
          overheating.
       2- Maximize filtered air movement in summer.
       3- Maximize humidity.
       4- Provide maximum shade, especially in late morning and all afternoon.
       5- Create cool and dark micro-climate.
       6- Vegetation is desirable as a radiation absorbent surface and for it has evaporative and
          shade giving properties.
       7- Increase building density.

         2.5.1.2 Adaptation

         1-       Building shouldn’t be sited in narrow valleys, but at lower hillside for maximum
                  cool airflow.
         2-       Use decks, as they are less reflective, less hot and allow air circulation
                  underneath.
         3-       Winds are to be modified rather than blocked.
         4-       Streets should be East-West oriented and located to the building’s north side.
                  For ventilation, Streets shall be perpendicular to winds direction


                                             7
5-        Orient active living areas to the southeast to collect early morning sun.
             6-        Optimum orientation is east of South.
             7-        Glass areas should face south with properly designed overhangs.
             8-        East and West windows should be avoided to minimize radiation with low sun
                       angles.
             9-        Cluster buildings and utilize solar panels for shade.
             10-       Use deciduous trees in southern elevation.
             11-       Minimize paved areas, abandon and locate them on the lee side. Color and
                       texture should be studied.
             12-       Use vines in south and west walls for shade.
             13-       Use north and east areas for outdoor activities.
             14-       Use low conductive, high reflective materials of light color in sun-exposed
                       surfaces & dark color in shaded surfaces
             15-       Use water body and locate buildings on the lee side.
             16-       Use balconies, overhead canopies, courtyards & canopy trees to slow
                       evaporation.
             17-       Use ground covers and extensive irrigation.
             18-       Use dust and draught resistance vegetation.

             2.5.2 - Hot arid Climate with high humidity:

           It should be understood that this clause sheds light on the Hot Arid Climate that
           witnesses high humidity, which can’t be categorized under the Hot Humid (Wet). The
           reason behind this confusion is that among the basic principles of climate classification
           is the precipitation rates that categorize our two types of dry and humid arid zones
           under Hot Arid.
The Main Macro Features that are to be added here are the Humid Atmosphere, Light Winds and Still

Air, Extends Periods of Even Overheating and low diurnal temperature range.


The high amount of water vapor in this climate absorbs more of solar radiation that causes the

uncomfortable feeling. Man can bear a much higher air temperature in the dry weather than he can

do in the humid weather.


             2.5.2.1 Objectives of Adaptation

             1- Maximize filtered air movement, Speed up Winds.
             2- Minimize humidity.
             3- Provide maximum shade, especially in late morning and all afternoon.
             4- Create cool and dark micro-climate.
             5- Vegetation is desirable as a radiation absorbent surface and for it has evaporative
                 and shade giving properties.
             6- Low building density for better air movement.

             2.5.2.2 Adaptation


             1-    Use decks, as they are less reflective, less hot and allow air circulation underneath.
             2-    Winds are to be modified rather than blocked.




                                                  8
3-    Orient active living areas to the southeast to collect early morning sun. For a
                      particular site, wind direction shall be considered.
                4-    Winds shall be enhanced through the use of natural and man-made forms, to
                      create air pressure differences, thus air movement.
                5-    Streets shall coincide with wind direction.
                6-    Optimum orientation is east of South, exact angle shall be studied for the particular
                      site, taking into consideration the breeze direction. This degree of deviation is
                      12º-25º.
                7-    Glass areas should face south with properly designed overhangs.
                8-    Avoid locating your structures in the low lands, as breeze can be stopped by
                      windbreakers.
                9-    East and West windows should be avoided to minimize radiation with low sun
                      angles. Wind direction shall be considered to catch the breeze.
                10-   Separate buildings and utilize solar panels for shade.
                          Use deciduous trees in southern elevation.
                11-   Streets should be East-West oriented and located to the building’s north side.
                12-   Minimize paved areas, abandon and locate them on the lee side. Color and texture
                      should be studied.
                13-   Use vines in south and west walls for shade.
                14-   Use north and east areas for outdoor activities.
                15-   Use low conductive, high reflective materials of light color in sun-exposed surfaces
                      & dark color in shaded surfaces.
                16-   Air should enter the building through shaded outdoor areas, avoiding passing
                      through heated surfaces.
                17-   Use overhead canopies and canopy trees for shaded pathways. Trees shall be of
                      high canopy to allow airflow for proper ventilation, as low canopy trees prevent
                      cooling breeze and trap humidity in pockets of dead air. Trellis has some
                      advantages on trees, as they don’t need to grow to give the full shade.
                18-   Use ground covers.
                19-   Shading Vegetation should not block ventilating winds. Trees shall be located in
                      parallel to wind direction.
                20-    Provide Parks in the downtown to reduce concentration of heated air.
                21-   Equilibrium shall be achieved between the desire of softening the heat load and to
                      provide unobstructed ventilation of a plot or building.
                22-   In sloped areas, High positions are more desirable to receive winds. Skyline of
                      Buildings formation shall be coping with the natural form of the hill that may allow
                      for a smoother air movement.
                23-   Parking lots shall be covered with pergolas and deciduous trees.
                24-   In flat areas, provide more building’s separation for free wind movement.

Bibliography and References

1-      Alpern. Andrew. AIA, “Handbook of specialty Elements in Architecture”. Mc Graw-Hill. New York.
        1982.
2-      Booth, Norman K. “Basic Elements of Landscape Architecture Design”.
3-      Boutet, Terry S. “Controlling Air Movement”. Mc Graw-Hill, New York, 1987.
4-      Cejka, Jan & Al Amiry, Suad. “Trees & Shrubs for Landscape Use in Jordan and Neighboring
        Countries”. Selden Und Tamm, Wiesbaden, West Germany, 1982.
5-      Davis, A. J. & Schubert R. P. “Alternative Natural Energy Sources”. Van Nostrand Reinhold, New
        York, 1981.
6-      Givoni, B. “Man, Climate & Architecture”. Van Nostrand Reinhold, New York, 1976.
7-      Konya, A. “Design Primer for Hot Climates”. Architectural Press, London, 1980.



                                                    9
8-    Meteorological Summaries, Kuwait International Airport. 1962- 1982.
9-    Olgyay, Victor. “Design with Climate”, Bioclimatic Approach to Architectural Regionalism.
      Princeton University Press, Princeton, New Jersey, 1973.
10-   Rimsha, A. “Town Planning in Hot Climates”.
11-   Robinette, Gary O. & McClennon, Charles. “Landscape Planning for Energy Conservation”. Van
      Nostrand Reinhold, New York, 1983.
12-   Saini, Balwat. “Building in hot dry climates”, John Wiley & Sons, 1980.
13-   Simonds, John Ormsbee. “Earth Landscape, A Manual of Environmental Planning & Design”. Van
      Nostrand, New York, 1983.
14-   Simonds, John Ormsbee. “Landscape Architecture”. Mc Graw-Hill, 1983.




                                              10

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Landscape Planning for Climatic Adaptation

  • 1. Landscape Planning for Climatic Adaptation in hot arid climatic zones Imad Kayyali Preface: There are not different “kinds” of architecture, but only different situations, which require different solutions in order to satisfy man’s physical and psychic needs. Man dwells when he can orient himself within and identify himself with an environment, or, in short, when he experiences the environment as meaningful. Dwelling therefore implies something more than “shelter”. It implies that the spaces where life occurs are places, in the true sense of the word. A place is a space, which has a distinct character. Since ancient times the genius loci, or “spirit of place”, has been recognized as the concrete reality man has to face and come to terms with in his daily life. Christian Orberg-Schultz This article summarizes a project research that has been conducted in some Gulf country. The site was distinguished with its extreme dry and hot climate, in addition to the dust storms, which blow in spring and summer each year, resulting sand erosion and very uncomfortable weather conditions. These conditions may cause some problems for the labors that will be in site during construction. Our team’s idea was to protect the site through the landscape planning, before any construction works being curried out on site. Our main target that could become our main achievement was to minimize the effects of the harsh climate generators, in addition to increase all those elements that may beco- me moderating factors and provide comfort for the work site. In response to Dubai Municipality’s plan on the continuous training program, this study has been enriched recently, with additional text on the climate that distinguishes Dubai and a high percentage of the UAE area while still part of the hot arid climate area, this climate witnesses high humidity. The article manifests two parts: The first part demonstrates in summary the general topics of landscape architecture. The second sheds lights on landscape planning for climatic adaptation, with special emphasis for the hot arid climate zone. Imad M. Kayyali Dubai, 1999. Part One: Landscape Architecture: 1.1 Introduction: While architects are involved with the design of buildings and their immediate surroundings, landscape architects are concerned with the design and preservation of the whole outdoor natural elements: topography, vegetation, water surfaces, Ecology, etc, that should make man’s outdoor life more comfortable, & afford him with means that help him to resist natural dangers such as: frost, floods, dust & precipitation, etc. as well as man-made effective elements, such as: pollution & noise, land forms & water features, beside facilitating man with recreational areas, pathways, street furniture & others. 1
  • 2. Landscape architecture has been developed through history, in parallel with architecture. Landscape styles were related to regions, cultures or historical eras, such as: Ancient Egypt, Mesopotamia, Greece, Romans, Islamic World, middle Ages, Renaissance, Baroque, China, Japan, India, etc. New movements have appeared in the late 1960s in several regions, that concluded landscape types into the following defined categories. a- Formal Geometric Landscape b- Rustic Landscape c- Natural and Desert Landscape. d- Transitional Landscape e- Tropical Landscape f- Oriental Landscape. g- Woody Landscape. Eventually, Landscape Architecture comprises the following two parts: a- Hard Landscape: which is concerned with man-made elements, such as paving, sidewalks, streets, parapets, decks, gazebos, etc. b- Soft Landscape: Which deals with plant materials and vegetation: trees, shrubs, vines, ground covers, etc. 1.2 Plants: The Plant Kingdom is usually categorized into the following: a- Annuals, b- Non-flowering (ferns) & Herbaceous perennials (Bulbs) c- Biennials. d- Woody Perennials- Flowering plants (Permanent). For landscape purpose, plant materials are sorted out into: a- Trees b- Shrubs c-Bushes d- Vines e- Ground Covers and Lawns f- Bulbs, Ferns & Annuals. Trees and shrubs are usually either Deciduous or Evergreen, where deciduous stands for those species which loose their leaves in winter. 1.3 Site Analysis: Prior to the design process get started, a full site analysis shall be conducted, comprising site geology, slopes, ecology, soil, vegetation, climate, aquifers & infrastructure. Analyzing this information shall lead to the best adaptation to site restrictions, potentials & requirements. Part Two: Landscape Planning for Climatic Adaptation in Hot Arid Climate. 2.1 Introduction: In the ancient times, it was said that man’s life pattern is dependent upon the climatic conditions in which he finds himself. Environment dictates man’s means of livelihood, home, food and clothing People believe that the proper climatic conditions were the main stimulus for the development of civilizations, also it is believed that workers productivity declines in climates of excessive heat or cold. 2
  • 3. Hence, we are getting closer to the question: can man control his environment? In spite of the great choices offered by modern technology in order to facilitate man with means so as to sustain excessive climatic conditions, it became quite improper to rely on those artificial means that have side effects upon man’s environment. Beside, communities are loosing natural resources through the extensive use of modern technology. During last decades, man began to look for natural elements those can modify his micro-climate. The relatively new expression of “micro-climate” describes the climatic conditions of a very local area or place, such as a hillside or an in-house courtyard, which are smaller in scale than the Mesoclimate and the Macroclimate scales. The micro-climate shall not confuse the reader with the microclimate expression, which describes the microscopic scale of climatic conditions. The following table illustrates the principal climatic scales: Climate Scale Example Macro-climate Extremely Large Continent, Country Meso-climate Country, City Moderate Micro-climate Small City block, Lot, Garden Microclimate Extremely small Leaf, sidewalk crack 2.2 Climatic Impact of Natural and Man-made Elements: 2.2.1. Climate Generators: Before discussing the natural elements affecting micro-climate areas, it’s quite helpful to have a look on the main generators of climate affecting man’s comfort. These generators are: i- Solar Radiation: moving through the atmosphere, solar radiation may: a- Reflected back into space. b- Dissipated within the atmosphere. c- Diffused through the atmosphere. d- Strikes the earth’s surface. Energy is transferred through, Radiation, Conduction and Convection. Radiated Heat transfers at the speed of light in the form of electromagnetic waves. The other forms of heat transfer are much slower and need a media to transfer. The dynamics of the solar movement shall be analyzed for best shading. 3
  • 4. ii- Winds: Moving over the earth’s surface, they encounter of impediments which: detract, deflect, obstruct and lessen the impact of speed of the flow of the unobstructed wind. Wind movement can be (a) Laminar (Steady), (b) Turbulent (Random Pattern and unpredictable) or (c) Separated. Air movement is affected by its inertia, friction with surrounding elements and differences in pressure and temperature. The major groups of winds are: a- Tropical Easterly of Trade Winds. b- The Mid-latitude Westerly. c- Polar Winds. iii- Precipitation and Humidity: Rain, Snow, Moisture, Evaporation, Dew and Frost. Atmospheric Humidity can be measured in three different ways: a- Absolute Humidity: g/m3 of air b- Specific Humidity: g/kg of air. c- Vapor Pressure: Bars of Water Weight. d- Relative Humidity RH: Actual/ Saturated % 2.2.2 Man Made Elements (Hard Landscape Materials) Different Materials have variable responses to sun radiation, in what we call “Specific Heat”. On the other hand, some of the material’s properties may alter the material’s response against sun radiation. Those properties are, Mass, color, texture, exposed area, location, orientation, etc. Therefore, our landscape materials are categorized according to their abilities to reflect, radiate and transmit solar radiation. We hereby list some selected materials together with their relative reflectivity % of sun radiation, taking into consideration that these figures may vary as mentioned above in connection with other parameters such as color and texture: Asphalt 12% Brick 50% Concrete 40% Dark Forest 05% Desert 25% Dry Grass 30% Green Forest 09% Oak woodland 17% Green Leaves 30% Green Fields 12% High Fresh Grass 25% Rock 12% Dry Sand 27% 2.2.3. The Natural Elements: Landforms and vegetation are considered to be the major natural elements that may affect the micro-climate: 4
  • 5. a- Landforms: Landforms can be either of large, medium or small scale. Landforms may affect air movement through deflection, impeding airflow pattern, velocity, quality and quantity. b- Vegetation: The effectiveness of special plant materials in climate control depends upon the forms and character of the plant, the climate of the region and the specific requirements of the site.  Vegetation may absorb 90% of the light falling on it.  Vegetation can filter, guide, obstruct, reduce or accelerate winds.  The optimum density of vegetation for wind control (by ASLA) is 50-60%  Vegetation may reduce wind speeds in an area to less than 10% of that in the open, or increase them, reduce day time temperature by as much as 8.5°C, and in certain situations, raise night time temperature. The main uses of vegetation of special importance to the energy- conscious designers are: 1- Large trees and shrubs: screen out undesirable winds and evergreen trees of high dense leaves should be used to control winter winds. 2- Trees: channel winds to increase ventilation. 3- Plantings: Reduce snow accumulations on ground. 4- Vegetation: Especially needle leave trees: capture fog, increase sunlight reaching ground. 5- Deciduous Trees: Screen sunlight in summer, then reduce required cooling loads and allow it to pass in winter, then reduce required heating loads. 6- Planted Areas: Will be cooler during day, then heat loss at night will be less, then razing specific heat of area. 7- Precipitation increases in forest areas. 5
  • 6. 2.3 Temperature Control: a- Solar Radiation Control: Vegetation provide solar radiation control through: Absorbing, Reflecting, Radiating and Transmitting. The Major effect of the forest on any climatic factor is reduction of short wave radiation by 73-80%. The forest can reduce monthly maximum air temperature in the summer by 6.5°C, reduce annual rain fall (through interception) by 15-30% and wind velocity by 20-60%. b- Wind Control: The most interest wind is that blowing at 1.8-2.5 m High. But it is effective up to 18 m. Planting affect air flow in the following ways: 1- Affecting Wind Movement. 2- Affecting amount of airflow. 3- Changing air direction. 4- Has no effect on lees side of a building, but may perform as an obstacle when applied on an outlet opening. Wind velocity control is a principal factor that needs to be modified so as to reduce energy used in either heating or cooling. For example, heating load with a 36-km/h wind is 2.4 times as 10- km/h wind (without protection). When protected, it would be twice only. For hot humid climate, wind control is the vital factor that has to be considered for ventilation. Notes on wind breaker trees and hedges:  The taller the trees are, the more raws required, as tree gets naked trunk taller as it is taller, which allow for low height streams of wind.  Width affects only penetrability.  Irregular windbreakers (mixture of trees) are more effective.  Trees of pitched edges are less effective.  The most effective ratio of height to protected length is 1:11.5.  The optimum density for a shelter belt is about 50-60%.  Parallel shelterbelts, spaced widely apart, have no acomm-ulative effect on reducing wind velocity. But closer ones do.  Plants should be located to protect buildings from expected directions. 2.4 Water 6
  • 7. Seas, Lakes and Rivers are preferable for people... for amusement, picnics, recreations and adventures, in addition to transportation. People like to be near water surfaces because they can enjoy skating, sailing, fishing, swimming, sinking, etc. However, they like it also because of the cooling effect that water bodies provide in the surrounding area. Old Arabs have practiced another experience with water features, such as: fountains, ponds, channels, etc. In order to modify the micro- climate of places like the “Dorqua” by adding humidity to the dry air in summer and cooling it by investing the high specific heat of water, which cause less variation of pattern of temperature between day and night, summer and winter. Therefore, it would be a right decision to use water bodies in the hot arid climate zones, so as to modify the climate and reduce its extremes through the cooling effect of water and moisture. Add to that, a small percentage of the solar radiation is radiated off water bodies, that is because solar radiation is stored deeply underneath surface. Water bodies cause evaporation that would reduce temperature in the surrounding space. Airflow in day blows from cooled sea towards warmed land, and at night, from cold land to cooled sea. 2.5 Hot Arid Climate and Human Adaptation 2.5.1 - Hot Dry Climate: The main macro features of the hot arid climate are: Clear sky, dry atmosphere, extends periods of overheating & high diurnal temperature range. Among the principle parameters of overhea- ting is the formation of the dust particles in the air that absorb solar radiation & radiates heat through atmosphere. 2.5.1.1 Objectives of Adaptation 1- Block dry dusty wind. Vegetation can clear air through reducing the formation of clouds of dust and smoke by preventing formation of rising air due to reducing overheating. 2- Maximize filtered air movement in summer. 3- Maximize humidity. 4- Provide maximum shade, especially in late morning and all afternoon. 5- Create cool and dark micro-climate. 6- Vegetation is desirable as a radiation absorbent surface and for it has evaporative and shade giving properties. 7- Increase building density. 2.5.1.2 Adaptation 1- Building shouldn’t be sited in narrow valleys, but at lower hillside for maximum cool airflow. 2- Use decks, as they are less reflective, less hot and allow air circulation underneath. 3- Winds are to be modified rather than blocked. 4- Streets should be East-West oriented and located to the building’s north side. For ventilation, Streets shall be perpendicular to winds direction 7
  • 8. 5- Orient active living areas to the southeast to collect early morning sun. 6- Optimum orientation is east of South. 7- Glass areas should face south with properly designed overhangs. 8- East and West windows should be avoided to minimize radiation with low sun angles. 9- Cluster buildings and utilize solar panels for shade. 10- Use deciduous trees in southern elevation. 11- Minimize paved areas, abandon and locate them on the lee side. Color and texture should be studied. 12- Use vines in south and west walls for shade. 13- Use north and east areas for outdoor activities. 14- Use low conductive, high reflective materials of light color in sun-exposed surfaces & dark color in shaded surfaces 15- Use water body and locate buildings on the lee side. 16- Use balconies, overhead canopies, courtyards & canopy trees to slow evaporation. 17- Use ground covers and extensive irrigation. 18- Use dust and draught resistance vegetation. 2.5.2 - Hot arid Climate with high humidity: It should be understood that this clause sheds light on the Hot Arid Climate that witnesses high humidity, which can’t be categorized under the Hot Humid (Wet). The reason behind this confusion is that among the basic principles of climate classification is the precipitation rates that categorize our two types of dry and humid arid zones under Hot Arid. The Main Macro Features that are to be added here are the Humid Atmosphere, Light Winds and Still Air, Extends Periods of Even Overheating and low diurnal temperature range. The high amount of water vapor in this climate absorbs more of solar radiation that causes the uncomfortable feeling. Man can bear a much higher air temperature in the dry weather than he can do in the humid weather. 2.5.2.1 Objectives of Adaptation 1- Maximize filtered air movement, Speed up Winds. 2- Minimize humidity. 3- Provide maximum shade, especially in late morning and all afternoon. 4- Create cool and dark micro-climate. 5- Vegetation is desirable as a radiation absorbent surface and for it has evaporative and shade giving properties. 6- Low building density for better air movement. 2.5.2.2 Adaptation 1- Use decks, as they are less reflective, less hot and allow air circulation underneath. 2- Winds are to be modified rather than blocked. 8
  • 9. 3- Orient active living areas to the southeast to collect early morning sun. For a particular site, wind direction shall be considered. 4- Winds shall be enhanced through the use of natural and man-made forms, to create air pressure differences, thus air movement. 5- Streets shall coincide with wind direction. 6- Optimum orientation is east of South, exact angle shall be studied for the particular site, taking into consideration the breeze direction. This degree of deviation is 12º-25º. 7- Glass areas should face south with properly designed overhangs. 8- Avoid locating your structures in the low lands, as breeze can be stopped by windbreakers. 9- East and West windows should be avoided to minimize radiation with low sun angles. Wind direction shall be considered to catch the breeze. 10- Separate buildings and utilize solar panels for shade. Use deciduous trees in southern elevation. 11- Streets should be East-West oriented and located to the building’s north side. 12- Minimize paved areas, abandon and locate them on the lee side. Color and texture should be studied. 13- Use vines in south and west walls for shade. 14- Use north and east areas for outdoor activities. 15- Use low conductive, high reflective materials of light color in sun-exposed surfaces & dark color in shaded surfaces. 16- Air should enter the building through shaded outdoor areas, avoiding passing through heated surfaces. 17- Use overhead canopies and canopy trees for shaded pathways. Trees shall be of high canopy to allow airflow for proper ventilation, as low canopy trees prevent cooling breeze and trap humidity in pockets of dead air. Trellis has some advantages on trees, as they don’t need to grow to give the full shade. 18- Use ground covers. 19- Shading Vegetation should not block ventilating winds. Trees shall be located in parallel to wind direction. 20- Provide Parks in the downtown to reduce concentration of heated air. 21- Equilibrium shall be achieved between the desire of softening the heat load and to provide unobstructed ventilation of a plot or building. 22- In sloped areas, High positions are more desirable to receive winds. Skyline of Buildings formation shall be coping with the natural form of the hill that may allow for a smoother air movement. 23- Parking lots shall be covered with pergolas and deciduous trees. 24- In flat areas, provide more building’s separation for free wind movement. Bibliography and References 1- Alpern. Andrew. AIA, “Handbook of specialty Elements in Architecture”. Mc Graw-Hill. New York. 1982. 2- Booth, Norman K. “Basic Elements of Landscape Architecture Design”. 3- Boutet, Terry S. “Controlling Air Movement”. Mc Graw-Hill, New York, 1987. 4- Cejka, Jan & Al Amiry, Suad. “Trees & Shrubs for Landscape Use in Jordan and Neighboring Countries”. Selden Und Tamm, Wiesbaden, West Germany, 1982. 5- Davis, A. J. & Schubert R. P. “Alternative Natural Energy Sources”. Van Nostrand Reinhold, New York, 1981. 6- Givoni, B. “Man, Climate & Architecture”. Van Nostrand Reinhold, New York, 1976. 7- Konya, A. “Design Primer for Hot Climates”. Architectural Press, London, 1980. 9
  • 10. 8- Meteorological Summaries, Kuwait International Airport. 1962- 1982. 9- Olgyay, Victor. “Design with Climate”, Bioclimatic Approach to Architectural Regionalism. Princeton University Press, Princeton, New Jersey, 1973. 10- Rimsha, A. “Town Planning in Hot Climates”. 11- Robinette, Gary O. & McClennon, Charles. “Landscape Planning for Energy Conservation”. Van Nostrand Reinhold, New York, 1983. 12- Saini, Balwat. “Building in hot dry climates”, John Wiley & Sons, 1980. 13- Simonds, John Ormsbee. “Earth Landscape, A Manual of Environmental Planning & Design”. Van Nostrand, New York, 1983. 14- Simonds, John Ormsbee. “Landscape Architecture”. Mc Graw-Hill, 1983. 10