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Authoritative facts about the skin from the New Zealand Dermatological Society Incorporated.

Basic photobiology

Learning objectives
Electromagnetic spectrum
Ultraviolet radiation on earth
Optics of the skin
The biological effects of light on normal skin
Photoprotection
Activity

Learning objectives

Electromagnetic spectrum

The electromagnetic spectrum emitted from the sun includes:

Name Wavelength (nm) Comments
X-rays 0-200
UVC 200-290 Not present at Earth's surface as removed by ozone layer. Germicidal band used in labs for sterilization. Very damaging to superficial skin.
UVB 290-320 Sunburning rays. Main cause of sun damage and skin cancer.
UVA 320-400 Long-wave black light tanning rays. Can penetrate into dermis. Contributes to erythema, skin aging and skin cancer.
Visible light 400-760 Does not significantly damage skin.
  • Violet 400-440
  • Blue 440-500
  • Green 500-550
  • Yellow 550-590
  • Orange 590-650
  • Red 650-760
Infra-red 760-1000 Heat
Microwave/
Radiowaves
>1000

Ultraviolet radiation on earth

Most UVR is absorbed by the ozone layer or reflected back into space; in New Zealand, ozone (O3) is maximum in spring and minimum in early autumn. According to the National Institute of Water & Atmospheric Research (NIWA) ozone declined by 8% over New Zealand between 1980 and 1990. This has resulted in a summer-time increase in UV of approximately 9% per decade and is thought related to chlorine in the stratosphere.

Ultraviolet (UV) levels at ground level are greater when the sun is higher in the sky, as it passes through thinner atmosphere than when the sun is at a greater angle:

About 30% of the daily amount of UVB is received between 12.30 & 2.30pm and 78% is received between 10.30 & 4.30pm.

There is also greater total UV:

Variation is greater for UVB than for UVA.

Only 10% of the sunburning UVR is transmitted through standard window glass.

A UV on a clear day B Seasonal UV
Measurements of UVR at Waikato Hospital in 1989

A: The difference in UVR on a clear day compared with a cloudy day, by time of day.
B: The difference in UVR in different seasons, by time of day.

Optics of the skin

UVR incident on the skin may be:

The total quantity of UVR transmitted through skin depends on:

UVR and the skin
UVR and the skin

The biological effects of light on normal skin

UVR causes biological effects when it is absorbed. Target biomolecules are:

There are several repair mechanisms to UVR damage.

Acute response of skin to exposure to UVR

The acute response of the skin to exposure to UVR has rapid onset (minutes to days) and short duration (hours to weeks).

Erythema mainly results from UVB i.e. wavelengths <320nm. It arises from dilation of the superficial blood vessels. Solar-induced erythema is delayed by a few hours after exposure.

The mechanism that results in erythema is unknown. Possibilities include:

Skin phototypes 1 to 6 are used to classify the effect of sun exposure on an individual's skin.

Type 1 Very fair. Burns easily, doesn't tan
Type 2 Fair. Burns easily, tans lightly
Type 3 Olive. Burns somewhat, tans readily
Type 4 Light brown. Burns rarely, tans well
Type 5 Dark brown. Doesn't burn, tans deeply
Type 6 Black

In skin types 4-6, immediate tanning may arise within minutes of exposure to long wave ultraviolet radiation (UVA) or visible light and is due to oxidation of pre-formed melanin in basal keratinocytes.

Delayed tanning is noticeable two days after exposure and most intense a week afterwards. It is due to melanogenesis and distribution of melanin to keratinocytes throughout the epidermis. UVA and even visible radiation may cause melanogenesis, but UVB is the most effective in initiating it.

Further exposure to UVR causes less damage:

UVB converts precursors in the skin into vitamin-D. The liver then the kidneys change vitamin-D into calcitriol (1,25 dihydroxycholecalciferol), which is required for calcium homeostasis.

Immune response

UVR results in profound alterations of both local and systemic immune responses.

Chronic response to exposure to UVR

Sun damage (photoaging) includes:

Thin Skin Furrows Bruising Solar keratoses
Thin skin Furrows Aging skin bruises easily Solar keratoses
Basal cell carcinoma Squamous cell carcinoma Melanoma
Basal cell carcinoma Squamous cell carcinoma Melanoma
Long term effects of exposure to UVR

Skin cancers are induced by:

A 5% increase in erythemally effective global UVR may result in a 15% increase in skin cancer in a susceptible population after about 60 years.

Photoprotection

The best protection from sun damage is to stay indoors. If outside, then protection from directly incident light can be obtained by seeking shade: trees, verandas, and umbrellas.

As much skin as possible should be covered with densely woven darkly coloured clothing.

Children with hats
Clothing as sun protection

Apply sunscreen to all uncovered skin liberally. Reapply after half an hour to ensure an even coating soaks into the skin, and then follow the instructions on the container. These generally advise reapplication 2-hourly and after bathing.

Sun protective factors (SPF) are calculated from in-vivo testing, and are the ratio of the time for the skin to burn when exposed to solar simulating UVR with the sunscreen compared without the sunscreen. Thus white skin that normally burns in 10 minutes will burn in 150 minutes (2 1/2 hours) with SPF 15 sunscreen however often it is reapplied. In general, sunscreens are much less effective than predicted by their SPF number as they are applied significantly less thickly than is tested and are rubbed, sweated or washed off.

Desirable properties of the sunscreen include:

Activity

What are the required criteria for a sunscreen to comply with the Australian & New Zealand Standard?

 

Page 3 of 8. Next topic: Indications for phototherapy. Back to: Phototherapy course contents.

Related information

References:

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Author: Clin Assoc Prof Amanda Oakley

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If you have any concerns with your skin or its treatment, see a dermatologist for advice.