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Climate
and Design Strategies for Beijing and Shanghai
Paul Rafiuly, Sean Kwok,
Christoph Ospelt
Revised: 10/9/1998
Climate
of Beijing and Shanghai
The analysis of the climate
is the starting point for a design that maximizes comfort and minimizes
the energy consumption for heating and cooling. One possibility
to show the distribution of temperature and humidity over a whole
year is to plot hourly climatic data in a psychrometric chart. The
horizontal axis of a psychrometric chart shows the dry-bulb-temperature.
The vertical axis shows the absolute water content of air in g of
water per kg of dry air. Air can take up water up to saturation.
The 100% relative humidity line corresponds to saturation of air
with water. The warmer air is, the more water it can take up.
The weather data generator
"Medpha" from Tsinghua University creates hourly weather data for
a full year. There is a statistical probability that a year is warmer
or colder than an average year. We used a "high" and a "low" year
to cover a wide range of possible weather situations for Beijing
and Shanghai. However, an extreme year may have "very high" or "very
low" climatic data, but this is statistically a small possibility,
so it is not considered as a scenario in our studies.
For Beijing and Shanghai,
we plot the climatic data into four graphs- Average Hourly Temperature
categorized by months, Average Hourly Horizontal Total Solar Radiation,
Annual Temperature Range and Annual Relative Humidity Range. From
the graphs we are then able to determine the specific climatic characteristic
of Beijing and Shanghai.
BJ-Daily.JPG
- Figure 1 Average Hourly Temperature with Hourly Horizontal Total
Solar Radiation for the months of January and July in Beijing
BJ-Annual.JPG
- Figure 2 Annual Temperature Range and Annual Relative Humidity
Range in Beijing
SH-Daily.JPG
- Figure 3 Average Hourly Temperature with Hourly Horizontal
Total Solar Radiation for the months of January and July in Shanghai
SH-Annual.JPG
- Figure 4 Annual Temperature Range and Annual Relative Humidity
Range in Beijing
To summarize the climatic
data for the whole year, we made a scatter plot with hourly data
into a psychrometric chart for each month. The zones with a high
density of scatters are colored in figures 5 to 8.
The rest of the scatters in each month are contained in the zone
delimited by the solid line.
The determination of comfort
zones (gray area) in figures 5 to 8 is discussed in
detail in chapter Comfort Zones and
Bioclimatic Charts.

Figure 5 Climate and comfort
zones January to July in Beijing (Zoom)

Figure 6 Climate and comfort
zones August to December in Beijing (Zoom)

Figure 7 Climate and comfort
zones January to July in Shanghai (Zoom)

Figure 8 Climate and comfort
zones August to December in Shanghai (Zoom)
It can be seen from the graphs
that in both Beijing and Shanghai, the climates cover
a wide range on the temperature scale. In winter Freezing
occurs in both cities, however, Beijing shows lower temperatures,
down to around -10ºC. Shanghai has only has a few hours of temperatures
below freezing. The summers are hot and humid for
both cities. The maximum temperatures are somehow higher in Shanghai.
Shanghai has a very high humidity level during the summer.
In Beijing humidity can also be quite high. As compared to
Shanghai, Beijing has a higher diurnal temperature
range ( about 10-15ºC ).
Prevailing wind directions
and speed are another important issue for climate directed design
strategies. Wind data will be available on this
page soon.
Comfort
Zones and Building Bio-Climatic Charts
At the state of thermal comfort
there is no perceived discomfort due to neither heat nor cold. The
range of comfortable combinations of air temperature and humidity
can be plotted in a psychrometric chart. ASHARAE has published a
standard for comfort zones. In Figures 5 to 8 AS
represents the ASHRAE comfort zones for summer, AW represents
the comfort zone for winter. The difference in summer and winter
comfort zones is because of seasonal acclimatization and clothing
habits.
Different authors pointed
out that the ASHRAE comfort zones are too narrowly limited. Givoni
gives a good overview on this issue (Givoni 1998). The principal
findings are presented below.
There are two distinct and
independent sources for heat discomfort: the thermal
sensation of heat and discomfort resulting from skin wetness
(sensible perspiration). Depending on the climate
the two sources of thermal discomfort will be felt simultaneously
or one of the discomfort sources is predominant. In Beijing
and Shanghai, where the summer climate is hot and humid,
both sources for discomfort will be felt.
Cold discomfort is
felt when the skin temperature gets below 32-33ºC. Environmental
factors that increase cold discomfort are low air temperatures,
draft and low radiant temperatures. Both cities, Beijing
and Shanghai have outside winter temperatures much lower
than the comfort zone. Different measures for reducing the heat
loss and maximizing the gains are necessary in order to reduce the
energy consumption for heating purposes.
Acclimatization
The comfort standards published
by ASHRAE have been established based on findings for American and
European people living in a region of around 40 degrees latitude
and who are used to mechanically conditioned buildings. People living
in warmer regions generally prefer higher temperatures and often
show no thermal discomfort at temperatures outside the ASHRAE comfort
zone. This is due to physiological and psychological adaptation
to the climate. A rule of thumb proposes to extend the comfort zone
by 1ºC for being 12º latitude closer to the equator. The cultural
background with intensive or little use of HVAC systems has an influence
as well on the feeling for discomfort. This also explains the difference
in comfort zones for developing and developed countries, as they
are proposed by some authors. A recent study of at Tsinghua University
in Beijing confirmed these principles. Temperature measurements
in apartments were accompanied by a survey. The apartments did not
have HVAC systems. Most of the people did not complain about thermal
discomfort even at indoor temperatures of about 30ºC.
The inverse is true for people
that grew up in colder regions. They will generally prefer a colder
environment and might even feel discomfort at temperatures near
the upper end of the ASHRAE comfort zone. Clothing and bedding habits
also have a strong influence on the lower end of the comfort zone.
Zone E in Figures
5 to 8 shows the comfort zone taking into account acclimatization
and standard of living. The zone for hot-developing countries is
shown. For people that grew up in a temperate climate the comfort
zone would be smaller.
Daytime ventilation
Increasing the airspeed
is an effective means to increase the thermal comfort in summer,
as long as the temperature is below 33ºC. It reduces the discomfort
due to thermal sensation and in particular due to perspiration.
ASHRAE guidelines recommend a maximal airspeed of 0.8m/s. In residential
buildings, where no papers fly from desks, the airspeed can be increased
up to around 2m/s. There are two ways to attain higher airspeeds:
The first one is natural
ventilation by opening windows and doors. The indoor surfaces
will then be at a temperature close to the outside temperature.
Therefor it is only reasonable to use daytime natural ventilation
if we also would feel comfortable outside with the same windspeed
that we get in the apartment.
In the case of nocturnal
convective cooling (see below), the building's openings should be
closed during the day. In that case a simple fan can help
increasing the airspeed during the day.
It has been shown that with
airspeed of about 2m/s the comfort zone is extended to the area
V=2 in Figures 5 to 8. Again, the comfort zone
for hot developing countries is shown.
Passive and low energy
cooling systems:
The indoor temperature can
be kept below the outside temperature by passive and low energy
cooling systems. This temperature difference between outside and
inside temperature can also be added to the comfort zone graph,
where the temperature scale represents the outside temperatures.
Nocturnal Ventilation
The Structural mass
of the building can be used for thermal storage together with nocturnal
ventilation (night flushing). The potential for lowering the
indoor daytime temperature below the outside temperature is proportional
to the outdoor diurnal temperature range. For a high-mass, well
insulated and shaded building, closed during the daytime and ventilated
only during the night, a drop of 45 to 55 percent of the outdoor
range is possible (Givoni 1998). At night the indoor temperatures
will be higher than the outside temperatures. Very good ventilation
is necessary to keep this problem under control.
Beijing has a quite
high daily temperature swing of nearly 10ºC during the hot summer
months. There is a large potential for nocturnal ventilation. We
can expect that it is possible to keep the indoor temperature about
5ºC below the outside temperature during daytime. This extends the
comfort zone in Figures 5 to 8 to zone MB.
Again, the comfort zone for hot developing countries is shown.
Shanghai on the other
hand only has a moderate daily temperature swing of around 5ºC.
In addition Shanghai is very humid. Further investigation is necessary
to decide if a strategy with nocturnal ventilation or daytime ventilation
is more promising. The inside temperature is expected to be about
2-3ºC below outside temperature with nocturnal ventilation, which
extends the comfort zone to MS.
Direct and Indirect Evaporative
Cooling
Evaporative cooling can be
very efficient in hot arid climates, which is not the case for Beijing
and Shanghai. With evaporative cooling the comfort range can be
extended to temperatures as high as 45ºC (not shown in figures).
Design Strategies
From our study of the climatic
data generated by "Medpha", we are able to suggest a few design
criteria that aim to enhance the thermal comfort level in buildings
for both Beijing and Shanghai. We divided these design
strategies into four categories: Orientation,
Building Envelope,
Thermal Mass
and Ventilation.
Most of the design strategies suggested are in general applicable
for both Beijing and Shanghai with a few that are
more relevant to one of the cities according to its specific climatic
characteristics (AIA 1978).
Orientation
Building
Envelope
 |
| Relevant to both Beijing
and Shanghai |
| |
 |
| Relevant to both Beijing
and Shanghai |
| |
 |
| Relevant to both Beijing
and Shanghai |
| |
 |
| Relevant to both Beijing
and Shanghai |
| |
 |
| Relevant to both Beijing
and Shanghai |
Thermal
Mass
 |
| This is more particular
for Beijing with its fairly large diurnal temperature range.
The thermal mass created by building material can help to dampen
indoor temperature fluxuation in comparison with outdoor temperature |
Ventilation
 |
| Relevant to both Beijing
and Shanghai |
| |
 |
| Relevant to both Beijing
and Shanghai |
| |
 |
| Relevant
to both Beijing and Shanghai, but may be particularly in Shanghai
with its higher relative humidity all year round |
| |
 |
| Relevant to both Beijing
and Shanghai |
References:
Givoni, Baruch: Climate Considerations
in Building and Urban Design. Van Nostrand Reinhold, 1998.
AIA Research Corporation:
Regional Guidelines for Building Passive Energy Conserving Homes.
US Department of Housing and Urban Development, 1978.
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