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Proceedings of 7th
Windsor Conference: The changing context of comfort in an
unpredictable worldCumberland Lodge, Windsor, UK, 12-15 April 2012. London:
Network for Comfort and Energy Use in Buildings, http://nceub.org.uk
1
Significance of air movement for thermal comfort in warm climates:
A discussion in Indian context
Madhavi Indraganti1,*
, Ryozo Ooka1, Hom B Rijal
2
1Institute of Industrial Science, The University of Tokyo, Japan
2Tokyo City University, Japan
*Corresponding Author: [email protected]
Abstract
Thermal comfort research is yet to gain momentum in India. Indian designers
follow verbatim the ASHRAE standard when designing the indoor environments.
This only leads to over design/ energy wastage and in environments inappropriate to
the local climates and customs. Our earlier study in 2008 highlighted the wide gulfbetween the actual comfort temperature recorded on field and that specified in the
National Building Code- 2005. Therefore, comfort studies are exigent in India.
Addressing this need, the authors are conducting a field study in warm-humid and
composite climates of India from January 2012. The current paper highlights the
significance of air movement for comfort at elevated temperatures as observed in our
Hyderabad study. Subjects using fans had higher comfort temperature than those
without. The occupants successfully achieved higher air velocities through the use of
various personal environmental controls in order to comfortably offset the
discomfort during the warm-humid months.
Keywords
Comfort temperature; Air movement; Humidity; Thermal Comfort research in
India; Griffiths Method
Introduction
Thermal comfort research is mainly concentrated in the west and in some parts of
Asia and Africa. This is perhaps one of the reasons why thermal comfort standards are
not defined yet in India. In the absence of comfort standards and very little first- hand
field work (Sharma and Ali, 1986, Indraganti, 2010a), the tendency is to follow the
comfort standards as described in ASHRAE Std-55 (2005) verbatim. However, the
base cases used in the above standard are predominantly based on western climates
and do not necessarily represent the wide ranging tropical climates in India. This
inappropriate standard neither matches the social attitudes nor cultural variety found
in Indian indoor environments. It is thus leading to over specification of air
conditioning systems and an enormous energy misuse.
On the contrary, several studies in the warmer climates have shown that increased
air movement can comfortably offset thermal discomfort at high indoor temperatures
without compromising the overall acceptability of the environment (Mallick 1996,
Nicol 2004, Brager 2000). The present paper discusses the importance of air
movement in Indian context, referring to literature on this, our earlier (Indraganti,
2010a) and present studies in India.
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Ergonomics of thermal comfort
Thermal comfort is a six- dimensional topological solid, having at least six
parameters that give dimensions to any unique thermal condition. Two of these,
activity and clothing are specific to an individual while the other four are the
properties of the environment itself air temperature, humidity air velocity and
radiation. Under isothermal and steady state conditions, the heat balance of the body
can be defined by these vital six variables.
While there are several other minor parameters like health, light etc. which also
influence thermal comfort, Fanger (1972) clarifies that comfort can be achieved by
many different combinations of the above variables. The effect of any of these factors
should not be considered independently as the effect of each of them depends on the
level and conditions of the other factors, and also by the use of many fundamentally
different technical systems (both passive and active). The effect of humidity and air
velocity shall be discussed in detail as under.
Humidity
While conductive heat gain is affected by the air and skin temperature difference,
the rate of heat exchange depends on the air velocity and the clothing. Although
humidity of air does not directly affect the heat load operating on the body, it
determines the evaporative capacity of air and hence the cooling efficiency of
sweating. In extremely hot conditions the humidity level determines the limits of
endurance time by restricting the total evaporation (Givoni, 1969).
Markus and Morris (1980, pp 59) add to this bio physical phenomena that,
evaporation is critical to heat loss from the body at high temperatures (above skin
temperature), and high humidity at this level impedes the rate of evaporation.
Evaporative cooling was exploited in many different ways both indoors and outdoorsin several cultures, since antiquity, for ex. pools in open courts and wind towers with
water sprays or pots in warm climates. There is no evidence that extreme humidities
are undesirable, from thermal comfort stand point. However, it leads to unwanted side
effects, such as wettedness sensation at high humidity (June and July months in
Hyderabad) and dehydration of mucous membranes at low humidity (April and May).
Maroof and Jones (2009) from their Malaysian Mosque study point that humidity
had an overarching influence on thermal comfort than temperature, and that 30C was
tolerable, with even a minor increase in the humidity adversely effecting the comfort
than temperature. Literature indicates that, relative humidity as low as 9 % is judged
comfortable over long periods of time. However, an acceptable range extends from 30
% to 65 %, with the optimum at about 50 %. High relative humidity, together withhigh air temperature, increases heat stress because the body cannot be cooled by
evaporation.
Airvelocity
Air velocity (VA) has little effect on evaporation at low humidity, as it takes place
readily. However it is of great importance in hot- dry conditions in affecting the
convection transfer. Though its effect is limited at high humidity, it is vital, as the
atmospheres ability to absorb moisture is limited. At increased air velocities, most
people remain comfortable even at higher relative humidity.
Nicol (1993) reports that, the effect of air movement is generally considered to beroughly proportional to the square root of the air velocity. He has identified in his
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Baghdad and Roorkie studies (Nicol, 1974) that there is little difference in the comfort
vote with VAin the range of 0.5 to 1.0 (m/s) and when VA
exceeds 1.0, i.e., the
major effect on comfort is observed than when VAexceeded 0.5. He has also noted
that air movement has reduced discomfort from heat at temperatures above 31 C; at
temperature exceeding 40 C discomfort from heat is experienced whatever the air
velocity. The ISO - 7730 recommends that the mean indoor air velocity should be lessthan 0.25 m/s for moderate thermal environments with light, mainly sedentary activity
during cooling season, and in winter it should be less than 0.15 m/s.
It is worth noting that acclimatised populations in warm humid climates report
comfort even at air velocities above 1.5 m/s, when air temperature is well above the
skin temperature and humidity is high (Krishnan, 2001). Nicol (1974) has similar
findings to present; in the range of 32- 40 C, moderate air movement (VA > 0.25 m/s)1 reduced both thermal discomfort and skin moisture in hot climates
2. However, air
velocities above 2 m/s are undesirable for prolonged periods because of other
inconveniences, (papers flying off, window shutters fluttering etc.). Thus, comfort can
be achieved over a much wider range of conditions than present standards recognize,necessitating the need for less conservative comfort standards.
Role of clothing in warm climates
While buildings are our third skin, clothing forms the second skin.
Clothing and buildings are similar in that, both use passive devices to
control natural flows of heat, air, and moisture vapor for the increased
comfort of the wearer or occupant- Olgyay.
As Olgyay (1963) says, clothing forms a barrier to the convective and radiant
heat transfer between the body and the environment, as it interferes with the process
of sweat evaporation. It reduces the bodys sensitivity to variations in air temperatureand velocity, forming a protective layer.
At air temperatures below 35 C the effect of clothing is always to reduce the
dry heat loss from the body, producing a heating effect. At air temperature above 35
C (the case in Hyderabad Summer) the effect of clothing is quite complicated.
Clothing reduces the dry heat gain from the environment on one hand; it increases
the humidity and reduces the air velocity over the skin on the other hand. It results in
a reduction of the cooling obtained from sweat evaporation. In this case the
evaporation takes place mostly from the clothing and not from the skin, reducing the
cooling efficiency of evaporation. The net resultant evaporative cooling depends on
the metabolic rate, humidity and air motion (Givoni, 1969).Significance of Air Movement and Ventilation in warm environments
Areas with poor thermal comfort conditions are mainly due to the poor natural
ventilation (Wang and Wang, 2005). Both natural and mechanical ventilation serve
the dual purpose of eliminating indoor surplus heat and contaminants in time. In fact,
air movement is the only way to achieve physiological comfort at high temperatures,
as it affects both evaporative and convective heat losses from the human body. Air
exchange efficiency and ventilation efficiency can both reflect the capacity for
eliminating indoor contaminants of ventilation system (Su et al. 2009). Holm and
1 These can be easily achieved with the use of a ceiling fan.2 The humidity is too low to affect the sensation of warmth.
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Engelbrecht (2005) maintain that air movement at a temperature below 37 C cools
the body, while heating it at an air temperature above 37 C.
The frequency distribution of wind velocity in natural ventilation is skew, and
people enjoy the fluctuations and remain comfortable, while that of mechanical
ventilation system is normal and has an unfavourable effect on thermal comfort. It is
well known that the fluctuation of natural wind can make people more comfortable3
and closer to nature. Furthermore, the airflow of natural ventilation moves at a low
speed for long time which can reduce the feeling of tiredness. The larger turbulence
intensity of natural wind is also believed to enhance the feeling of comfort, for it
intensifies the heat convection between people and the environment. Therefore,
natural ventilation is better than mechanical ventilation on the whole (Su et al. 2009).
ASHRAE (Std-55, 2004) indicates that acceptable indoor air speed in warm
climates should range from 0.2 to 1.50 m/s; yet 0.2 m/s for air conditioned
environments. These ranges specified by ASHRAE do not explicitly address air
movement acceptability, but focus mainly on overall thermal sensation and comfort.
Zain et al. (2007)4 find that in warm humid climes an increase in air movement from0.0 m/s to 0.7 m/s has substantially increased the PPS from 44% to 100% at
temperatures around 28.69 C. Maarof and Jones (2009) point out that at high
temperature (>30 C) and high humidity (>70%), continuous air moment is important,
rather than spasms of air drafts.
While investigating the relation between air movement acceptability and thermal
comfort inside buildings, Cndido et al., (2010)5 have found that, at operative
temperatures above 24 C, building occupants preferred mean air speeds up to 1m/s. It has also been observed that complaints of draft did not occur in significant
numbers until air speeds exceeded 1 m/s; and natural ventilation combined with solar
protection, is the most efficient building design strategy to achieve thermal comfortwithout (Stein and Reynolds, 2000, p. 57) resorting to mechanical cooling in warm
humid climes.
Similarly, Cheng and Ng (2006) reported that, when airspeed was increased to
about 1.5 m/s, the upper comfort temperature limit further moved up by 1.5 degC to
about 33.5 C and the predicted comfort range far above the maximum outdoor air
temperature. This study suggested that, indoor natural ventilation of airspeeds up to
1.0 - 1.5 m/s is likely to be satisfying the thermal comfort requirement of 80% of the
occupants in hot summer period. Interestingly, Heidari (2008) found increased air
movement above 37 C to be counterproductive, resulting in heating sensation.
Brager et al. (2004), report from their field study of NV office buildings thatpeoples preferences for higher air movement have increased with increase in thermal
sensation. They also show that people consciously recognize air movement as having
a direct impact on their thermal comfort, and that their air movement preferences are
for a change of air movement as needed to return to comfort quickly, especially in
warm humid climates (Feriadi et al., 2004).
It well accords with the 1/f rhythm of body also
4 Thermal comfort field study of residential environments in Malaysia5Studied the effects of natural ventilation on thermal comfort and air movement acceptability of a
large number of university students inside naturally ventilated buildings in Brazilian hot humid zone
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Perception of Air Movement
It is based on several parameters such as air velocity, air velocity fluctuations, air
temperature, and personal factors such as overall thermal sensation, clothing
insulation and physical activity level (metabolic rate) (Toftum, 2004). Even for the
same individual, sensitivity to air movement may change from day to day as a result
of, e.g., different levels of fatigue.
Draught is defined as an unwanted, local cooling of the body caused by air
movement. Toftum (2004) reports that, at temperatures up to 22-23 C, at sedentary
activity and with occupants feeling neutral or cooler, there is a risk of air movement
being perceived as unacceptable, even at low velocities. Supplementing this, he points
that, a cool overall thermal sensation negatively influences the subjective perception
of air movement. When occupants feel warmer than neutral, at temperatures above 23
C or at raised activity levels, humans generally do not feel draught at air velocities
typical for indoor environments (up to around 0.4m/s). In the higher temperature
range, very high air velocities up to around 1.6m/s have been found to be acceptable
at air temperatures around 30C. However, at such high air velocities, the pressure onthe skin and the general disturbance induced by the air movement may cause the air
movement to be undesirable (Toftum, 2004).
Cena and de Dear (1999) have observed in their Karlgoorlie study that 40% of the
occupants who preferred higher temperatures also asked for more air movement
regardless of the fact that this would make them feel even cooler. This may indicate
that field study respondents find it difficult to balance and express their thermal
preferences. Thus, in field settings, the interaction between draught and thermal
sensation is not as clear as in the laboratory studies, but a warmer thermal sensation
results in a preference for higher air velocities, as also found in other studies (Toftum
2004).While Cena and de Dear (1999) point out the incongruence between draught and
thermal sensation in a field study, and recommend a climate chamber for better
results, Toftum (2002) finds that climate chamber studies for activity and air
movement interaction do not yield realistic results. He notes that subjects in real
environments are exposed to interrupted exposure to air movement and non-sedentary
tasks without any stabilization of metabolic rate. These occupants activity level is
higher than the level corresponding to stationary, seated work in a climate chamber.
Methods
The hot- humid climate and the composite climate (experienced in Chennai and
Hyderabad respectively) represent about 80% of the geographic area in India. Theauthors are conducting a thermal comfort research in offices in these climates after
Indraganti (2010b) has identified the vital absence of thermal comfort field work in
India.
Indragantis (2010a) residential buildings field study was conducted in
Hyderabad (1727 N, 78 28 E). This study involved over 100 occupants of
naturally ventilated (NV) apartment buildings in summer, monsoon and post-monsoon
period. Hand-held digital instruments were used to measure the environmental
variables while the questionnaires recorded clothing, activity, sensation, preference
and adaptation in both longitudinal and transverse surveys, yielding about 4000 data
sets. Table 1 presents the scales used in this study.
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Methodology adapt
The hot humid clima
Hyderabad respectively)
authors are conducting a
Indraganti (2010a) identif
About 20 office build
cities (Chennai and Hyd
buildings have air condi
majority of them. The su
While the former is done
sample, the latter is cond
total buildings and a limit
All the four environ
globe temperature) cou
adaptation are recorded
standard Class I protoc
conjunction with the air/
both environmental and b
Results
Outdoor mean tempe
the survey period, with i
relative humidity varied s
quite dry. Thermal sensat
comfort equation of TS
presented in Indraganti (velocity in achieving com
Effect of Air Velocity
Air velocity is one of
the thermal comfort of oc
it varied significantly dur
more tolerant of high air
The requirement of air m
Figure 1: Linear regress
6
d for further studies in India
te and the composite climate (experienced
represent about 80% of the geographic are
thermal comfort research in offices in thes
ed the vital absence of thermal comfort field
ings are selected for yearlong comfort studi
rabad) from January 2012- January 2013.
ioning, although its use is limited to the
rvey is planned in two levels: transverse a
once a month in all the offices involving
cted throughout the year and is limited to a
d number of occupants in each of these buil
ental variables, (viz: temperature, humidit
led with CO2 levels, clothing, metaboli
through field measurements and data lo
ls. We expect to analyse the change in c
globe temperature, humidity, air movement
havioural.
ature during the study ranged between 27.4-
ndoor temperature ranging between 26.6
ubstantially (15 76%) as the summers in
ion (TS) varied with globe temperature (Tg 0.31Tg - 9.06 (r= 0.61, p
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As seen in figure 2, in May, air velocity at neutrality (median VA= 0.27 m/s, n=
108) is low, with a slow increase in air velocity as the TS increases to 1 (median VA=
0.3 m/s n= 438), to 2 (median VA= 0.4 m/s n= 480) and 3 (median VA=0.41 m/s,
n=361), which is achieved by using fans most of the time.
This is equivalent to an increase in comfort temperature by about 2-3 C (Nicol
and Roaf, 1996). It is also important to note that in May at thermal sensation of 2 and
above, higher air velocities have caused discomfort, as the humidity is very low and it
produced undesirable effects like dryness etc. A few votes in May could be recorded
when people sitting in front of a high efficiency air cooler had experienced cold
discomfort i.e. at thermal sensation -1 at slightly higher velocity (median VA= 0.3 m/s
n= 14) and at -2 (median VA=0.58 m/s n=4), i.e. air movement requirement increases
at TS 2 and 3 in June, in July higher air velocity at TS - 2 is not desired.
The requirement for higher air velocities significantly increased as the humidity
increased from May to June. This is due to the fact that mean indoor temperature is
around average skin temperature (32 34 C) and humidity is also high (mean 55%).
The only way subjects can achieve physiological comfort under these conditions
is through increased ventilation. This is achieved by using the ceiling fans and a few
subjects have also used air coolers, in roof exposed flats where the radiant heat from
ceiling at midday caused most discomfort than high humidity. High air velocity is no
longer required as mean thermal sensation (and Tg) falls down in July, although the
humidity is still high (~72%).
As the room temperature is below the skin temperature in July, air velocity
beyond 0.2 m/s induces drafts and causes cold discomfort (see figure 2) at normal
activities . Conversely, at high metabolic rates (>1.7 met) and at TS (2 and 3) higher
air velocities are preferred for short periods to provide physiological comfort through
increased ventilation.
Air Movement Sensation (AMS) and Preference and Preference (AMP)
Air movement sensation and preference were evaluated based on the responses to
the questions How do you find the air movement and How would you prefer to
have? (Refer Table 1). AMS correlated well with TS (r= 0.43) and with OC (r= -
0.42). It has correlated robustly with median of square root of air velocity (r= 0.87)
and with AMP (r= 0.71). Peoples preferences for higher air movement increased with
increase in thermal sensation (Brager et al., 2004). Toftum (2002) found clear impact
of activity and overall thermal sensation on human sensitivity to air movement.
Figure 2: Relationship between thermal sensation and air velocity (May, June and July - all data)
0.30.4
0.5
0.6
0.7
0.8
0.9
1.0
-3 -2 -1 0 1 2 3Median
squarerootofair
velocityinm/s
Thermal sensation (TS)
May
June
July
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The subjects voted the air movement low when voting hot on TS scale (mean
AMS vote = -1.42). When the AMS vote was 1 and above the subjects preferred the
air movement to be lesser. Similarly the subjects voted in the comfort range on the
overall comfort (OC) scale (OC = 4, 5 and 6 on a scale 1 to 6) when the AMS was
between 0 and lower coinciding with neither high nor low, high, very high
sensations.
Air movement sensation correlated positively with the thermal effect on
productivity (r= 0.15). When the air movement sensation vote was low, the self
declared productivity vote was also low. The air movement sensation correlated
well with globe temperature (r= -0.35) and with relative humidity (r=0.23). June and
July recorded very high relative humidity coupled with moderate temperatures. This
allowed the occupants to adaptively open the windows, promoting cross ventilation.
Moreover, high humidity prompted the subjects to use the fans more, increasing
indoor air velocities. As a result, AMS vote moved up with the relative humidity.
Conversely, at high indoor temperature most of the natural cross ventilation ceased,
due to the adaptive closure of windows. This prompted most of the subjects to give a
low AMS vote, even when the percentage of subjects with fan onwas high. This
was due to the fact that, at high levels of thermal distress, the air movement
requirements of the subjects could not be satisfactorily met by the ceiling fans alone.
Figure 3 shows the distribution of AMS vote and its relationship with median of
square root of air velocity. Understandably, as air velocity reduced, AMS vote has
also reduced indicating a need for higher air movement. Conversely, 27% of the
subjects voted -2 and -3 (low and very low), on the AMS scale even when the
recorded (median) air velocities were between 0.4~ 0.7 m/s.
The highest percentage of subjects has felt the air movement to be neither high
nor low (38%). Similarly, Ogbonna (2008) found a weak relationship between the
actual vote and the air-velocity in his Jos, Nigeria study.
It is essential to note that, the air movement sensation related strongly with
thermal discomfort. Only when a subject was under thermal distress, he/she gave a
very low air movement sensation vote (-3). At all other times, the majority (52%)
found the air movement lower, but voted in the central zone, with a skew towards
the right side of AMS scale. This was partially due to the fact that, the air movement
induced by the natural ventilation in summer was less dependent and was variable.
Table 1: Thermal comfort Scales employed (Transverse and longitudinal surveys)
Scale value Description of scale
ASHRAE 's Thermalsensation (TS)
Air movementsensation (AMS)
Air movement preference (AMP)
3 Hot Very high
2 Warm High Much less air movement
1 Slightly Warm Slightly high A bit less air movement
0 Neutral Neither high nor low No change
-1 Slightly Cool Slightly low A bit more air movement
-2 Cool Low Much more air movement
-3 Cold Very low
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Moreover, the efficacy of the ceiling fans also was non-uniform, resulting in
inconsistent levels of satisfaction (Indraganti, 2010c). Therefore, the subjects always
desired cooler air movement in hot summer rather than just increased air
movement. The ceiling fans or natural wind drafts in hot weather could not provide
this. The ceiling fans re- circulated the hot air around, causing further discomfort to
the subjects.
Correlation between air movement preference, temperature and relative
humidity
Interestingly, peoples preferences for air movement (AMP) changed with the indoor
globe temperature (r = -0.25) and relative humidity (r = 0.17). The correlation figures
indicate that at higher temperature, the subjects desired increased air movement (refer
Figure 5: Influence of Fan on the comfort temperature
y = -0.0955x + 2.3848
(AMP) R = 0.0618
y = -5.7881x + 230.03
(RH) R = 0.57240
20
40
60
80
100
-3
-2
-1
0
1
2
3
25 30 35 40 45
Rela
tiveHum
idity
(%)
AirMovemen
tP
reference
(AMP)
Indoor Globe Temperature ( C)
AMP
RH
Linear (AMP)
Linear (RH)
Figure 4: Distribution of AMS and its relationship with median of square root of air velocity
1 2
7
38
25
19
8
0
10
20
30
40
0
0.1
0.2
0.30.4
0.5
0.6
0.7
0.8
0.9
1
Veryhigh
High
Slightlyhigh
Neitherhighnor
low
Slightlylow
Low
Verylow
Freq
uency(%)
Medianofsquarerootofairvelocity
(m
/s)-1
Air movement sesnation (AMS)
Frequency (%)
Median of square rootof air velocity (m/s)-1
Trend line
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Figure 4). On the contrary, increased humidity had little effect on the air movement
preference, which returned a low positive correlation value (r = 0.17).
The positive trend reflects a desire for reduced air movement during period of
moderate temperatures experienced by the subjects in the humid season. It is
imperative to note that higher temperature in Hyderabad is usually associated with
low humidity (hot-dry season), while humid periods have moderate to low
temperature.The following observations prove the existing standards redundant: the subjects
voted neutral on much wider higro-thermal regime. When voting neutral, the indoor
globe temperature varied between 26.6 36.9 C, while the relative humidity ranged
17% - 76% and the air velocity was in between 0.00 m/s to 2.8 m/s. This can be
attributed to very high levels of adaptation (through reduced clothing and metabolism)
and acclimatisation coupled with moderate expectations from the domestic
environments.
Effect of air movement (ceiling fan) on comfort temperature
Comfort temperature is a simple consequence of people optimizing
comfort under the various constraints of fashion, fuel, costs, climate,available technology, climate, cost of clothing, etc. Humphreys (2008)
In naturally ventilated buildings, comfortable indoor temperatures are shown to
follow the seasonal shifts in outdoor climate and often fall beyond the stipulated
comfort zones of ASHRAE Standard-55. Steady state comfort theory based on human
physiology cannot completely account for this. Griffiths (1990) method is suggested
as an alternate method in the literature to evaluate comfort temperature when the field
data constitutes a smaller sample (Nicol, 1995 p. 151, Rijal et al., 2008, 2010). A
detailed discussion on the Griffiths method can be found in (Rijal et al., 2008).
Equivalence between changes in comfort vote and the measured temperature areassumed first. Nicol (1995) modifies this method further by applying it to the centroid
Figure 6: Influence of Fan on the comfort temperature
Fan on: y = 0.2303x + 23.543
R = 0.5363
Fan off: y = 0.3309x + 20.345
R = 0.59329.0
29.5
30.0
30.5
31.0
31.5
32.0
25 26 27 28 29 30 31 32 33 34 35 36 37
Gri
ffith'scom
fort
tempera
ture
C
Mean out door temperarure (binned data) C
Fan on
Fan off
Linear (Fan on)
Linear (Fan off)
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of the body of data instea
equivalence coefficient o
(1972), who through cli
comfort vote, a three degr
However, as we hav
study, we used the same
temperature obtained in th
beyond the comfort zon
invalid (Nicol et al, 1995
analysis (for ex: cases wh
thermal sensation is clo
results. This is due to t
population hovers around
and Humphreys, 2002).
Brager et al. (2004)
temperatures are not onlySubjects who have mor
particular, the operable
warmer than subjects wit
thermal environments and
Griffiths comfort tem
evaluated for all the mea
their corresponding ther
categories: fan on and fan
and the mean outdoor tem
As the outdoor tempe
the cases. More importawithout any significant
Figure 7: NBC (India
11
d of applying it to the individual votes. He
0.33 in his Pakistan studies, which is deriv
ate chamber experiments deduced that, fo
e rise in temperature is needed.
obtained an equivalence coefficient of 0.3
in the Griffiths method. It is important to n
is method may not be valid if the mean ther
(i.e. beyond -1.5 to +1.5) where Fanger
- pp 152). Hence we have eliminated the o
n the TSmeanwas 1.5 and more). In addition,
e to zero, Griffiths comfort temperature
he fact that the mean thermal sensation
the neutral point on the sensation scale of A
in their California study have noticed tha
influenced by season but by the degree of pcontrol over thermal conditions of their
indow) have a neutral temperature that is
minimal control, even though they experi
exhibited no differences in cloor met.
perature (TnG= T g_mean+ (0 TSmean/ R),
n outdoor temperature bins at one degree
mal sensation votes. The data is grou
off. Figure 5 shows the variation in the com
perature (To_mean).
rature increased, the comfort temperature is
tly, the use of fan pushed the comfort tncrease in clothing etc, although the sub
) and the comfort zone of Hyderabad juxtaposed on
ada tive model
uses a Griffiths
d from Fanger
r a unit rise in
in the present
ote that neutral
al sensation is
s prediction is
tliers from the
when the mean
shows realistic
f acclimatised
HRAE, (Nicol
t ideal comfort
ersonal control.workplace (in
1.5 C (2.7 F)
nced the same
ith R = 0.31) is
eriodicity with
ed under two
ort temperature
increased in all
emperature up,jects are more
the ASHRAEs
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sensitive to the changes in the temperature (slope = 0.23), than the subjects without
the use of fans (slope = 0.33). This clearly renders support to the argument that the
use of fans not only provides comfort at elevated temperatures but also without the
escalation of energy bills emanating from the use of air-conditioning.
The findings recorded by Sharma and Ali (1986) and Nicol (1974) in office
buildings of Roorkie in North India, are particularly interesting in this context. While
Nicol (1974) reported reduced skin moisture when the indoor temperature ranged
between 31-40 C, Sharma and Ali observed a decrease of 1.4 to 3.2 degC in the
Tropical Summer Index (TSI)6, (a measure for indoor comfort) for an increase in air
velocity from 0.5 to 2.5 m/s, all else remaining unchanged in addition.
Rijal et al., (2008) analysed the Pakistan data (Nicol 1996) separately for cases
withfan onandfanoff. They corroborated the earlier findings, in addition to defining
equations for estimating the indoor comfort temperature with ceiling fan in use. They
used the concept of running mean temperature for factoring in the outdoor conditions
in their equations. When the running mean temperature was 30 C, the indoor comfort
temperature withfan onwas 31 C, which is 2.2 degC more than when thefan wasoff(Rijal, 2012).
It is important to note that the comfort temperatures to the tune of 31.5 C with
or without the use of fan were achieved in indoor environments in our Hyderabad
study, as against the stipulated standard comfort zone of (23-26 C)(refer Figure 6).
This finding calls for a revision of standards.
Conclusions
This paper discusses in detail the relevance of increased air movement at elevated
indoor temperatures and humidity, usually encountered in warm climates in the
tropical subcontinent. A thermal comfort field study in residential buildingsconducted by the authors in India revealed the following:
(1) Higher comfort temperatures are successfully obtained through the use of
fans,
(2) The subjects are comfortable at much higher indoor temperatures than those
specified in the standards (NBC, 2005),
(3) They achieved higher indoor air velocities in the months when the humidity
was very high, through the use of many adaptive controls (fans, air-coolers, windows
and balcony doors and
(4) The residents displayed a proclivity for higher air movement indoors.(5) The air movement preference varied with temperature, while humidity had a
little effect on the air movement preference.
These findings call for the development of thermal comfort standards custom-
made to in Indian subjects and climates. The authors are now conducting a thermal
comfort survey in the composite and warm-humid climates of India from Jan 2012 to
Jan 2013.
The tropical summer index is defined as the air/globe temperature of still air at 50% relative
humidity which produces the same overall thermal sensation as the environment under investigation.
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Acknowledgements
We wish to profoundly thank Michael Humphreys and Fergus J Nicol, who
advised, e-mailed and generously sent papers and books during our Hyderabad survey
in 2008. The present thermal comfort research in Indian offices is funded by the
Japanese Society for Promotion of Science, Japan and The University of Tokyo,
Tokyo, Japan. The authors sincerely thank these two institutions.
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