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H

ealth

is recorded around 13:00 local time (LT) year-round in the whole

country. In northern and central Chile, the period of high-risk expo-

sure (levels above 6) goes from 10:00 to 17:00 LT in summer, while

in the most southern city (Punta Arenas, ~ 53°, 70°W, 39 masl), on

average, the UVI is under level 6 risk year-round; that is, the index

only reaches moderate values which are equivalent to small risk of

damage from unprotected sun exposure. However, during spring,

Punta Arenas and the surrounding areas can experience episodes of

significant UVI increase.

Analysis of the data recorded by stations deployed at different

elevations indicates an increment of UV – and therefore of the UVI

– with altitude. This is due to two factors: first, at higher altitudes

more UV can get to the surface because the atmosphere is thinner.

And second, due to a clearer atmosphere, lower values of aerosol

optical depth are found near the surface atmosphere as compared

with values at lower altitudes.

1

In northern Chile, comparison

between data recorded by the stations located at Antofagasta (~

23°S, 70°W, 115 masl) and San Pedro de Atacama during cloudless

days in summer reveals differences in UVI of five to seven levels,

which correspond to an altitudinal increase of two to three units per

kilometre. However, on average, results from the Chilean stations

concur with the overall altitudinal increment of 10-12 per cent of

the UV levels per kilometre. This altitudinal factor on UV radiation

is not constant throughout the year; significant seasonal variation

is mainly found in winter when the vertical differences at midday

hours are higher due to a greater solar zenith angle.

The incoming UV irradiance is attenuated by clouds, which

depend on both thickness and cloudiness (type and amount). Thin

or scattered cloud can have little effect or even enhance

the UV compared with cloudless skies. On the other

hand, cloudy days can decrease UV irradiance reach-

ing the ground by absorption and scattering through

the water vapour and the aerosols. A good correla-

tion between UV and cloudiness was found at stations

located in northern and central Chile (r = 0.88 for

Santiago), but the correlation is poor in the southern

regions, most probably due to the presence of cumu-

liform clouds as revealed the study done at Valdivia.

2

However, days with a concentration below 250 DU can

correlate with episodes of increased UVI under cloud-

less sky conditions in summer. The impact of this on

human health is documented by a medical study

3

that

found a relation between stratospheric ozone concen-

tration below 260 DU and cases of sunburn in children

due to exposure during January. With regard to the

ozone hole that develops in the southern Polar regions

during the spring season, regions with minimum

concentration eventually reach the Antarctic Peninsula

and the southern tip of South America. Large increases

in UV-B associated with the Antarctic ozone hole have

been measured, with increases up to 38 times those of

similar days with normal ozone.

4

Significant decreases

of stratospheric ozone along with increments of UV-B

occurred during the mid and late austral spring of 1999.

These events caused a significant increase of patients

with sunburn in Punta Arenas.

5

The stratospheric ozone layer is a natural protec-

tive filter for the harmful UV radiation provided by the

atmosphere. Depletion of this layer has negative effects

on flora and fauna, including human health, due to

exposure to higher UV levels. This fact motivated some

senators and the Chilean Government to produce a

law regarding the protection of the stratospheric ozone

layer. The Ozone Law, as it is called, was published in

2006. Its main objectives are to establish control mech-

anisms for substances that deplete the stratospheric

ozone, and to ensure the appropriate implementation

of the Montreal Protocol and the protection of human

health and ecosystems affected by UV. The law gives

responsibility to the DMC as the official source of infor-

mation and public dissemination of the UVI and risk

for human beings. Today, the daily maximum UVI and

the prediction for the next day can be found on the

institutional webpage

www.meteochile.gob.cl

. The law

was later complemented by a Supreme Decree that was

published in 2011, with the purpose of establishing

regulations for health protection and preventions to

be applied at workplaces. This is a pioneer legislation

in Latin America which establishes a precedent in the

prevention of occupational health risk in the country.

In this context permanent monitoring, the addition

of new stations to the URN, climate UV studies and the

daily forecast have become essential information not

only with regard to physical and biological effects over

the territory, but also with regard to supporting deci-

sion-makers within the framework of protecting public

and occupational health.

Skin cancer caused by excessive exposure to UV radiaton

Image: Sociedad Dermatológica de Chile