Sharp
slopes are not inhabitable?
A
bioclimatic answer
Fausto
Simões
Introduction
It
is somewhat easy to understand and modify microclimatic conditions, as we can
see and feel in an air-conditioned, artificial-lighted
room. But what are the side-effects on environment, of our mechanized buildings
and towns?
It seems very
dificult indeed, to understand antropogenic climate change at the global and at
regional scales… But it is likely that the antropogenic signal will emerge more
and more convincingly with time, in model simulations, as says the IPCC
[1]. So it seems well justified to
design, build and use our setlements WITH CLIMATE, and not against it, applying
scientific research.
Sharp
slopes are not inhabitable? This is perhaps a provocative question to those who
intend to design with climate, and broadly, with nature.
Design
with nature, that´s to say: WHERE and HOW to build our setlements following local liabilities and assets, within a
holistic approach. All this, in order to satisfy our needs and to do NO HARM to
man and to NATURAL ENVIRONMENT. This is precisely what is NOT done, when hills
and valleys are covered by the same concret-and-asphalt receipt, be it the
high-rise or the detached house one. Natural diversity and complexity are
reduced to a boring sameness (see Figure 1).
Side
effects of this current pratice can imply high costs, even life costs, not
accountable in the financial system.
So, intending to design with
nature, one should not, of course, build on poorly drained, flooded, unhealthy
or rich topsoil valleys, but on well
drained plain land and on slopes…even on steep slopes?
Building on slopes
Even
on steep slopes? That´s a good question to answer, intending to enhance the
relationship between WHERE and HOW, and
to show that rigid, stringent rules should be rejected.
So,
what are the suitable slopes for
residential areas?
In
the sunny Mediterranean fringe, solar space heating and cooling, solar water
heating and daylighting can give more comfort with less pollution by energy
plants.
Passive and
active solar require a free solar access in a South exposure, more or less 15
degree, for maximum efficiency.
Microclimatic
conditions related to solar radiation have a better equilibrium between winter
and summer on steep slopes up to
fifty-sixty degree, with a south exposure, in the case of Lisbon.
This can be
seen in the graphic of solar radiation against slope for Eastward slopes and
Sowthward slopes, blue and red curves, in winter and summer, lower and upper
curves (see Figure 2).
How to build on
steep slopes?
Building
on steep slopes is an old story. Hilltop villages were a strategic rule, during
the primeval age of “castros”, in what is now Portugal.
This,
long time before they came downslope to
the valleys, clearing the primeval forest.
The
URBAN MORFOLOGY suited to steep
slopes is LOW RISE GROUP HOUSING descending the hillside (see Figure 3). The
hilltop must be THERE, not built.
With Low Rise Group Housing can be attained
the Human scale in buildings and
in a positive open space and also, a low-energy
profile considering transport, comfort and construction demands.
The
ARCHITECTURAL TYPOLOGY suited to steep
slopes is TERRACED HOUSING, following a natural slope. Terraced housing is the
urban counterpart of rural terracing. The terrace of one house is over the roof
of the other downwards. With terraced or diagonal housing one can attain a free
solar access, large views, privacy staying outdoors in secluded terraces and a
desirable urban density. This main requirements and its relationships can be
translated in a terraced-housing set of equations.
In
the graphic form of these equations, one can see that the Floor Space Index
(IC) can be a little over 1.5, allowing a density higher then 500 p.p.h.,
suitable for a good balance between
community and privacy (see Figure 4). FSI is represented by the lower red curve
in the graphic.
Sensible
creativity is needed, in order to give form to this terraced-housing formulary.
The terraced housing landscape asset of a modern example on a 35 degree slope
is shown in Figure 5.
CONCLUSIONS
1. Non speculative terraced housing on steep,
brownfield, stable southward slopes, from 10º up to 40º (nearly) can enhance
life, dealing with the problems of energy use, flood control and erosion.
Portuguese recommendations based on the UN convention against desertification
consider terraced housing on steep slopes [4], but current interpretation of
the Portuguese environmental regulation (REN) forbids residential areas on
slopes greater than 17º [5].
2. Conception and evaluation methods of urban
design following local geo-climatic suitabilities, should be supported by
scientific modelling.
REFERENCES
1.
Intergovernmental
Panel on Climate Change 1996. Climate
Change 1995 – The science of Climate
Change. Cambridge University Press (Cambridge 1996).
2.
Mata, L.;
Marques, C.; Totais Diários da Radiação
Global Recebida por Superfícies com Diversas Orientações e para Diferentes
Ângulos de Inclinação. INMG (Lisboa 1981).
3.
Schwagenscheidt,
W.; Ein Mensch Wandert Durch die Stadt.
H. Müller- Wellborn. (Bad Godsberg – Mehlen, 1957).
4.
Ministério da
Agricultura, do Desenvolvimento Rural e das Pescas. Convenção das Nações Unidas de Combate à Desertificação.
Organização Nacional para a Aplicação da CCD (Lisboa 1997).
5.
Pereira,A.;
Bento, J.; Gomes,M.; e N. Cerejeira. Metodologias de Avaliação da Reserva
Ecológica Nacional (MAREN). Ambiente,
Ordenamento, Gestão do Território e Sistemas de Informação Geográfica.
Faculdade de Letras da Universidade de Lisboa, (33-41). (Lisboa 1995).