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2007, Piran, Slovenia

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Environmental Ergonomics XII<br />

Igor B. Mekjavic, Stelios N. Kounalakis & Nigel A.S. Taylor (Eds.), © BIOMED, Ljubljana <strong>2007</strong><br />

526<br />

A BIOMETEOROLOGICAL PROCEDURE TO DETERMINE THE<br />

OPTIMAL OUTDOOR CLOTHING INSULATION FOR THE<br />

FORECASTED WEATHER<br />

Marco Morabito 1 , Alfonso Crisci 2 , Lorenzo Cecchi 1 , Pietro Amedeo Modesti 1,3 ,<br />

Giampiero Maracchi 2 ,Gian Franco Gensini 1,3 , Simone Orlandini 1<br />

1 Interdepartmental Centre of Bioclimatology - University of Florence, Florence, Italy<br />

2 Institute of Biometeorology, National Research Council, Florence, Italy<br />

3 Clinica Medica and Cardiologia, University of Florence, Italy<br />

Contact person: marco.morabito@unifi.it<br />

INTRODUCTION<br />

The impact of climate change on human health and on general biological systems has been<br />

widely described and most of the observational data series are consistent with the direction of<br />

change expected as a response to warming. The rapidity of this climate change requires that<br />

policymakers are kept informed of the manner in these changes can impact on human<br />

adaptation and behavior, to ensure thermal comfort and avoid or reduce risks. For this reason<br />

there is an increasing demand to assess the thermal climate in a human-biometeorologically<br />

manner. Clothing represents an important variable directly involved in the estimation of<br />

thermal load in relation to the physical activity and environmental parameters. Most studies<br />

focused on the estimation of general thermal comfort of people for indoor thermal<br />

environments and the Predict Mean Vote (PMV) (Fanger, 1972) represents the standard<br />

method based on the steady state energy-balance model used by the International<br />

Organization for Standardization (ISO 7730, 1994). On the other hand, relatively few studies<br />

have investigated outdoor thermal comfort, because of the great complexity of the outdoor<br />

environment. Recently we reported that the association of German engineers considered<br />

stationary models, such as the PMV and similar thermal indices, useful to facilitate the<br />

thermophysiological acquisition of thermal conditions even of surrounding outdoor air as<br />

point layers. In several studies, thermal indices were employed, taking into account solar<br />

radiation parameters, to improve the assessment of outdoor comfort, even creating bioclimatic<br />

maps useful for urban planners, human health and helpful for saving energy. Dressing<br />

properly for the outdoor environment is a component of thermoregulatory behavior, and it is<br />

well known that ample outdoor clothing can contribute to the prevention of excess winter<br />

mortality typical of populations living in temperate countries. The aim of the present work<br />

was to investigate the clothing factor related to climate changes, retrospectively evaluating<br />

the seasonal trend of the minimum clothing insulation value necessary to maintain the thermal<br />

neutrality in outdoor spaces in three major Italian cities over the second half of the last<br />

century. Subsequently an operational biometeorological procedure was developed to provide<br />

72-hour forecast maps concerning the optimal outdoor minimum clothing insulation value to<br />

maintain thermal neutrality over Tuscany and all of Italy.<br />

METHODS<br />

Preliminary analysis<br />

Daily meteorological data of air temperature (°C), relative humidity (%), wind speed (m s -1 )<br />

and cloud cover (in eighths) were measured at 04:00 (night), 10:00 (morning), 16:00<br />

(afternoon) and 22:00 (evening) hours in three weather stations managed by the Italian<br />

Meteorological Service for the period 1951-2000. These were located in three Italian<br />

geographical areas: Northern Italy, Turin, λ = 11°11' E; Φ = 43°22' N; Central Italy, Rome, λ<br />

= 12°58' E; Φ = 41°80' N; Southern Italy, Palermo, λ = 13°32' E; Φ = 38°12' N. In addition,<br />

mean radiant temperature (Tmrt, °C), defined as the uniform surface temperature of an

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