different temperatures. A machine that converts
thermal energy to mechanical energy, such as a
steam engine or turbine.
Heat exchanger A device that transfers heat
from one material to another. Usually con-
structed to transfer heat from a fluid (liquid or
gas) to another fluid where the two are physi-
cally separated. In phase-change heat exchan-
gers, heat transfers to or from a solid to a fluid.
See also:
Heat recovery ventilator
Heat gain In buildings, the amount of heat
introduced to a space from all heat-producing
sources, such as building occupants, lights, and
appliances, and from the environment, mainly
solar energy.
Heat gain from bulbs Electrical light bulbs
generate heat according to the wattage consumed
by the light bulb (power = current voltage).
As long as the light is absorbed in the space, the
light bulb electrical power equals the heat gain
in the space. This can be converted to Btu by
multiplying the wattage by 3.42 Btu/h (3.42 Btu/
h = 1 watt). For example, a 100 W bulb 3.4 =
340 Btu/h.
Heat island Urban air and surface tempera-
tures that are 2–10 °F (1–6 °C) higher than nearby
rural areas. Elevated temperatures can affect
communities by increasing peak energy demand,
air-conditioning costs, air pollution levels, and
heat-related illness and mortality. Heat islands
form as cities replace natural land cover with
pavements, buildings, and other infrastructure.
These changes contribute to higher urban tem-
peratures by i) displacing trees and vegetation,
minimizing the natural cooling effects of shad-
ing and evaporation of water from soil and
leaves (evapotranspiration); ii) tall buildings and
narrow streets heating air trapped between them
and reducing air flow; iii) waste heat from
vehicles, factories, and air conditioners adding
warmth to their surroundings, further exacerbat-
ing the heat island effect. In addition to these
factors, heat island intensities depend on an
area’s weather and climate, proximity to water
bodies, and topography. Heat islands can occur
year-round during the day or night. Urban– rural
temperature differences are often largest on
calm, clear evenings, because rural areas cool
off more quickly at night, whereas cities retain
heat stored in roads, buildings, and other struc-
tures. As a result, the largest urban–rural tem-
perature difference, or maximum heat island
effect, is often 3–5 hours after sunset. During the
winter, some cities in cold climates may benefit
from the warming effect of heat islands. Warmer
temperatures can reduce heating energy needs
and may help melt ice and snow on roads. In
the summer, however, the same city will experi-
ence the negative effects of heat islands. In
general, the harmful impacts from summertime
heat islands are greater than the wintertime ben-
efits, and most heat island reduction strategies
can reduce summertime heat islands without
eliminating wintertime benefits.
While they are distinct phenomena, summer-
time heat islands may contribute to global
warming by increasing demand for air con-
ditioning, which results in additional power
plant emissions of heat-trapping greenhouse
gases. Strategies to reduce heat islands therefore
can also reduce the emissions that contribute to
global warming.
Heat island effect The increased temperatures
of urban heat islands have a direct influence on
the health of residents, such as heat strokes or
respiratory problems from impure air. Other
effects of heat islands are an increase in energy
use for cooling buildings, changes in local wind
patterns, development of clouds, fog, smog,
humidity, and precipitation. Heat island effects
can be mitigated by using white or re flective
materials to build houses, pavements, and
roads, thus increasing the overall albedo of the
Heat island effect 117