The Effects of Green Spaces (Palme Trees) on the Microclimate in Arid Zones, Case Study: Ghardaia, Algeria

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Architecture Research 1, (5): 6-67 DOI: 1.593/j.arch.15.1 The Effects of Green Spaces (Palme Trees) on the Microclimate in Arid Zones, Case Study: Ghardaia, Algeria Hamida bencheikh 1,*, Ame ur Rchid 1 Genie civil laboratory Amar Telidji University Laghouat Algeria Depatement of architecture Amar Telidji University Laghouat Algeria Abstract The microclimate and air quality in urban spaces are of a great interest for the well-being of citizens. Mitigating urban heat island is a ma jor concern for human health by improving comfort especially in desert regions. While the therma l comfo rt is relatively easy to obtain in indoor spaces, it is more difficult to provide in outdoor ones. It is often sought by passive means. Vegetation could play an important role in ameliorat ing urban microclimates. It should be used judiciously in urban planning and designing outdoor spaces. The objective of this work is to exp lore the influence of green cover during summer on microclimate in the region of Ben-Isguen, a city of a hot-arid climate in the M zab valley, Ghardaïa (Algeria). Many studies have proved that vegetation can produce a cooling effect of to 3 on average. Gardens and urban parks in particular, in and around cities contribute to alleviating heat stress by creating the so-called "oasis effect" through public spaces. They improve therma l co mfort and reduce cooling energy consumption. The microclimate of different locations, in both green and built-up areas (old town, palm grove, etc.) was characterized with the help of field measurements carried out during summe r days. The results confirmed the presence of an important cooling effect of vegetation (PCI). It was shown that it is essentially a nocturnal phenomenon by displaying a ma ximu m value of 1. This result is very important regarding the results of similar studies. The research demonstrated that the oasis effect is best developed around dawn in calm and clear sky conditions. Maximu m daytime cooling effect of the green cover was.5 in reference to old town. Nevertheless this effect showed fluctuation so that it displayed negative values by mo ments. The cooling effect of the palm grove is due to shade foliage, evapotranspiration, low heat capacity of vegetation and high aerodynamic roughness. In fact the oasis acts as a "heat sink". The old town of Ben-Isguen presented a diurnal heat island and a nocturnal cool island with ma ximu m intensity of 3.5 and respectively. The investigation of the oasis microclimate revealed that densely vegetated areas display higher cooling effect. The latter varied among different areas due to shade conditions, density of vegetation, sky view factor (SVF), soil characteristics and water surface availability. Keywords Microclimate, Urban Space, Heat Island, Green Space, Arid Zone 1. Introduction In the past, Mzab settlements (the ksurs and their cities gardens) were developed in response to both cultural and climatic needs of their inhabitants[1], the inhabitants of Mzab site use detached houses in Pa lme trees gardens for day liv ing and the ksurs for night living (due to security problems) and now they use garden houses for day and night living during summe r period. Our study investigates the effects of vegetations on the outdoor temperatures in hot arid zones, and Ghardaia in the south of Algeria was taken as a case study. * Corresponding author: hamida.bencheikh@gmail.com (Hamida bencheikh) Published online at http://journal.sapub.org/arch Copyright 1 Scientific & Academic Publishing. All Rights Reserved Vegetation cover has positive effects on the microclimate[], it can lower the outdoor temperature[3--5]. Many studies on urban tree cover like green CTTC (cluster therma l time constant) model have indicated a very high correlation between daily outdoor temperature and consumption of space conditioning energy[6-7-8]. It is assumed that a tree has a pro jection area of shading and a reduction of sky view factor, in the air surrounding a tree always has a high humidity due to tree irrigations system. The surrounding space between detached houses in Palme trees are well protected fro m solar radiations and the surrounding air is usually saturated with humidity, wh ich can affect directly the outdoor temperature. M. Santumouris[9] shows that trees with a crown of 8m could reduce the peak cooling load by to 1%. A kbari[7], found that trees reduce the cooling load by 1-53% in Californ ia. This paper studies the effect of Palme trees on microclimate in arid

61 Architecture Research 1, (5): 6-67 zones, and Ghardaia in the south of Algeria (3.3 N 3.9 E) was taken as a study case.. Study Area Ghardaia is located in the south of Algeria, which is well known by its hot arid climate, its ksurs (dense old buildings), its river, and its detached houses surrounded by Palme trees as shown in figure (1). The climate of Ghardaia is characterized by a very hot dry summer, the mean summer temperature in July is 36.8 and the ma ximu m absolute temperature is 6. The outdoor temperatures were recorded in four different sites in addition to the reference point; Figure () shows the different sites where field measurements were recorded. The reference point is situated at the frontier of Pa lme trees site on the top of the local radio build ing and the first site, detached houses in Palme trees (Oasis) is situated at the bottom of the valley as shown in figure (3). The second site called Beni Ezgen ksur, the old part of the city (high density buildings and partially covered narrow streets as shown in figures (, 5). The third site the new city extension called Tafilalt and the forth site is the new detached houses in open area without vegetations. Fi gure 3. Weather station in P alme trees zone at low level Fi gure. Weather station in the st reet of the old ksur Beni Ezgen Fi gure 1. Houses surrounded by Palme trees Fi gure. The different zones where field measurement s were recorded Fi gure 5. Weather station on the top of houses roof in the old ksur Beni Ezgen

Hamida bencheikh et al.: The Effects of Green Spaces (Palme Trees) on the 6 Microclimate in Arid Zones, Case Study: Ghardaia, Algeria 3. Measurement Instrumentations Ten weather stations type HOBO where planted in five different points; A reference weather station was planted on the top the local radio station in open area. In point one, the o ld ksur of Beni Ezgen, two weather stations were planted, one on the top of houses and the other one in 1.3m wide street. In point two, Tafailelt, two weather stations were planted, one on the top of houses and the other in 6 m W ide Street. In point three, Palme trees houses, two weather stations were planted, one at human height above the soil, the second at canopies level on the top of houses. In Point four, new detached houses in open area, one weather station was planted on the top and the second in.7m wide street. In point five, at the bottom of the valley one station was planted on the top of one level building. The streets weather stations were m height fro m the ground for security raisons and the period of measurements was from the 16 th until th of august. Figures (3 to 5) show the station at each site. In addition to the weather stations, three same model testometers were used to measure the outdoor temperatures, relative hu mid ity and wind speed in Palme trees zone. Two of them were placed in the Palme trees center (high density and continues canopies), the first one at 1.m of height and the second one at 5.5m just below canopies, these measurement help in studying the temperature stratifications above the ground and at canopies level. The Palme trees were irrigated once a day at 18h 3. The third testometer was placed in the outer Palme trees site (less density and discontinues canopies). The testometers measurements were taken fro m th until nd August.. Results and Discussion Ghardaia a hot arid city situated in the south of Algeria, the outdoor temperatures were recorded by fixed weather stations at two level points, street level and canopies level (roof of building and bottom of bu ild ing) for the four mentioned sites and the reference weather station site. Figure (6) presents the outdoor temperature variat ion at building roof level in the four sites in comparison with the outdoor reference site. Figure (7) presents the outdoor temperature variation for the same sites at street level. Figures (6, 7) show that the high difference in outdoor temperatures between sites were recorded during night time at canopies level in palm trees site. At canopies of Pa lme trees the outdoor temperatures were higher by.5 than the reference site in two times, early in morning and at midday due to solar radiation. Under the canopies, in the Palm trees site and in the open site, the lower outdoor temperatures were recorded during night, which also cited by, Shashua-Bar and Hoffman[1], Bacci and al.[11] and S. Spronken and Oke[1]. The Oasis presents the lower outdoor temperature due to the intense evaporation and the low therma l capacity of the vegetations. The night outdoor temperatures recoded were lower by than the ones recorded in the open site, which was similar to the results in many bibliographical references such as; Correa & al.[13] and Up manis & al.[1]. Figure (8) presents the heat-island and the cool island (the negative values present the heat island and the positive one present the cool-island) at the top of buildings and in the street of Beni Ezgen ksur compared to the reference point. The ma ximu m cool-island was recorded at. 1 Am and the ma ximu m heat-island was 3.5 recorded at 13. pm. Figure (9) presents the heat-island and the cool island at the top and the bottom of buildings of Tafilelt ksur compared to the reference point. The ma ximu m cool-island was 3.8 recorded at. 1 Am and the ma ximu m heat-island was 3 recorded at 13. pm. Figure (1) presents the heat-island and the cool island at the top and the bottom of buildings of Pa lme trees site compared to reference point and the ma ximu m cool-island was 1 recorded twice and minimu m value was. Figures (11, 1) present the cool-island in Pa lme trees site at the top and the bottom of buildings compared to the other three sites, Beni Ezgen ksur, Tafilelt ksur and open site houses. The ma ximu m cool-island at the bottom of buildings level recorded during night time were 7., 9. and 7.1 compared to Ben i Ezgen ksur, Tafilelt ksur and open site houses respectively. The ma ximu m cool-island at the top of buildings level were recorded during night time, 5.1, 7.8 and.5 compared to Ben i Ezgen ksur, Tafilelt ksur and open sit houses respectively. The outdoor air temperatures during day Time in Pa lme trees site were lower by, than the reference weather station, 3 to than the ones in Beni Ezgen site, and by 5 to 8 lo wer than Tafilelt, and the open site houses as shown in figure (11). During night time the outdoor temperatures in Palme trees site were lower by 5 to 8 than the Beni Ezgen site, and by 1 lower than Tafilelt, and the open site houses as shown in figure (1). Two other measurements were taken at street level in two different points in Palme trees site, the fist one at the center of the vegetations and the other at the outer limit of the vegetations. From figure (13), at the outer limit of the vegetation, the outdoor air temperature is higher by to than the temperature in the center of the vegetation, due to the density of Palme trees which gives well shaded area.

63 Architecture Research 1, (5): 6-67 7.5 T air Palm (niv haut) T air toit Ksar T air toit Tafilelt T air toit Extens T air Réf 5.5 37.5 T air ( ) 35 3.5 3 7.5 5.5 Fi gure 6. Out door temperat ure recorded in different zones at canopies level 7.5 T air Palm (niv haut) T air toit Ksar T air toit Tafilelt T air toit Extens T air Réf 5.5 37.5 T air ( ) 35 3.5 3 7.5 5.5 Fi gure 7. Out door temperat ure recorded in different zones at st reet level

Hamida bencheikh et al.: The Effects of Green Spaces (Palme Trees) on the 6 Microclimate in Arid Zones, Case Study: Ghardaia, Algeria ΔT Kt - Réf ΔT Kr - Réf 3 1 T -1 - -3 - -5 Time in hours Fi gure 8. Temperat ure difference at roof and street level bet ween reference weather station and old ksur ΔT Taf t-réf ΔT Exten t-réf 3 1-1 - -3 - -5 T Time in hours Fi gure 9. Temperat ure difference at roof l level bet ween reference weather station and Tafilelt, and open sit e

65 Architecture Research 1, (5): 6-67 1 ΔT Réf -Pb ΔT Réf -Ph 1 8 6 T - - Fi gure 1. Temperature difference at roof and street level between reference weather station and P alme trees sit e 1 ΔT Kr - Pb ΔT Taf r - Pb ΔT Exten r - Pb 9 8 7 6 5 T 3 1-1 - Fi gure 11. Temperat ure difference at st reet level between Palme trees sit e and old ksur, tafilelt, open sit e

Hamida bencheikh et al.: The Effects of Green Spaces (Palme Trees) on the 66 Microclimate in Arid Zones, Case Study: Ghardaia, Algeria 8 ΔT Kt - Ph ΔT Taf t- Ph ΔT Exten t - Ph 7 6 5 T 3 1-1 - Time in hours Fi gure 1. Temperat ure difference at roof level between Palme trees sit e and old ksur, tafilelt, open sit e 6 T air Pt périph T air Pt central-sup T air Pt central-inf 38 36 3 3 3 8 6 19:53 :53 1:53 :53 3:53 :53: 1:53: :53: T ( C) 3:53: :53: 5:53: 6:53: 7:53: 8:53: 9:53: 1:53 11:53 1:53 13:53 1:53 15:53 16:53 17:53 18:53 19:53 :53 1:53 :53 3:53 :53: 1:53: :53: 3:53: :53: 5:53: 6:53: 7:53: 8:53: 9:53: 1:53 11:53 1:53 13:53 1:53 15:53 5. Conclusions Fi gure 13. The outdoor air t emperat ure at soil level in the middle and extremities of the P alme t rees sit e The study shows that the outdoor temperatures in center of Palme trees site were lower by 5 to1 in comparison to the other studied sites. The old ksur characterized by its compact buildings with narro w streets and its surrounding ramparts was designed to offer a good therma l co mfort and security fro m enemies, however in our days the security problems does not exist. A second ksur called tafilelt was designed in 199 in the same shape as the old one but with larger streets, for cars and technique equipments to get inside, but our study shows that the outdoor temperatures in the ks ur of tafilelt were greater than the outdoor temperatures in Palme trees site. Therefore we suggest a new urbanization method, which g ives the vegetations (Palme trees) great space in all buildings design. For further studies it is recommended to find the optimum vegetation surface percentage in the new extension of Ghardaia city. The existence of Palme trees surrounding houses offer a better microclimate, protection fro m hot wind, sand and also Palme trees fruits (dates) for the inhabitants.

67 Architecture Research 1, (5): 6-67 REFERENCES [1] A. Bouchair, A. Dupagne, Building traditions of Mzab facing the challenges of re-shaping of its built form and society, Building & Environment 3, 38 135-136. [] R. Giridhagan & al, Lowering the outdoor temperature in high-rise-density residential developments of costal Hong Kong: The vegetation influence, Building & Environment, 8, 3 1583-1595. [3] B. Givoni, Climate considerations in building and urban design. U SA Wiley, 1998 [] R. Emmanuel, Summertime heat island effects of urban design parameters, PhD thesis, The University of Michigan, 1997. [5] L. Shashua-Bar & al, Integrated thermal effects of generic built forms and vegetation on the UCL microclimate, Building & Environment, 6, 1 33-35. [6] YJ. Huang & al, The potential of vegetation in reducing the cooling loads in residential buildings, Climate and Applied Meteorology, 1987, 6 113-16. [7] H. Akbari & al, Peak power and cooling energy savings of shade trees, Energy and Buildings, 1997, 6 139-18. [8] L. Shashua-Bar, ME. Hoffman, Geometry and orientations aspects in passive cooling of canyon streets with trees, Energy and Buildings, 3, 35 61-68. [9] M. Santamouris, editer, Energy and Climate in the urban built environment, UK, James & James, 1 (chapters 1, 3-7,1,11). [1] L. Shashua-Bar, ME. Hoffman, Vegetation as climatic component in the design of an urban street, Energy and Buildings,, 31 1-35. [11] L. Bacci and all, Thermo-hygrometric conditions of some urban parks of Florence, Italy and their effects on human well-being, Proceedings 5th international conference on urban climate, 3 1-5 September, Lodz, Poland. [1] R. A. Spronken-Smith and T. R. Oke, The thermal regime of urban parks in two cities with different summer climates, International Journal of Remote Sensing, 1998, 19 85-1. [13] E. Correa and al, Impact of urban parks on the climatic pattern of Mendoza s metropolitan area, in Argentina, the 3th conference on passive and low energy architecture, PLEA Geneva Switzerland, 6 b. [1] H. Upmanis and al. The influence of green areas on nocturnal temperatures in high city (Goteborg, Sweden), International Journal of climatology, 1198, 18 681-7.