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Ozone Skin Cancer CFC UV-Radiation. The „bad“ ozone on the ground is very different from the „good“ ozone up high in the Stratosphere !!!!!!!!! Too much.

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Presentation on theme: "Ozone Skin Cancer CFC UV-Radiation. The „bad“ ozone on the ground is very different from the „good“ ozone up high in the Stratosphere !!!!!!!!! Too much."— Presentation transcript:

1 Ozone Skin Cancer CFC UV-Radiation

2 The „bad“ ozone on the ground is very different from the „good“ ozone up high in the Stratosphere !!!!!!!!! Too much ozone in the Troposphere (on the gournd) has a very different effect and can cause severe ailments: Respiratory diseases (e.g. asthma); especially endangered are children, the elderly and people under severe physical strain Inflammation Nausea Changes in blood count Effects on the nervous system (exhaustion, decline in performance). Damage to forests Corrosion of metallic items Deterioration of buildings (monuments)

3 1. UV - Radiation 2. Skin Cancer 3. Skin Structure 4. The Ozone Layer 5. CFC and Alternatives Contents

4 What is UV-Radiation?  Visible light ranges between 390nm - 770nm.  UV – light is located below 390nm.  UV-B and UV-C are more harmful; they do not penetrate the skin very deeply, but rather react in the Epidermis and Dermis.

5 52% visible light 44% invisible Infrared radiation 4% UV - radiation (These are the most dangerous to skin!) The Spectrum of Sunrays

6 1.Skin cancer 2.Examples of other illnesses 3. Effects on nature Consequences of Increased UV- Radiation

7 The major dangers are inflammatory reactions (sunburn) and damages to the DNA of the skin cells, which can lead to skin cancer. Benign melanomata Benign melanomata and malignant melanomata malignant melanomatamalignant melanomata are the two possible types of skin cancer that can develop. The malignant melanomata are also called black skin cancer. Damage caused by radiation

8 Benign melanoma Malignant melanoma Superficial spreading melanoma (SSM) Nodular melanoma (NM) Nodular melanoma (NM).

9 Very harmful tumour Place of development: It develops in the cells that give the skin its color (melanocytes) Development: On normal skin or allready existing cellular nevus (mole, birthmark) Development: On normal skin or allready existing cellular nevus (mole, birthmark) Starting point: Basal cells; At first it usually grows in a horizontal direction being rather superficial but depending on the type of melanoma it may start growing rapidly in a vertical direction at an early stage. At first it usually grows in a horizontal direction being rather superficial but depending on the type of melanoma it may start growing rapidly in a vertical direction at an early stage. The malignant melanoma - black skin cancer -

10 Ca. 20% of all melanomata belong to the so called nodular melanoma (NM). The NM varies in colour from blue to dark brown. Melanoma is so dangerous, because once it grows to a certain thickness, it metastasizes or spreads throughout the body. After melanoma has spread to the internal organs there is little that can be done and death follows shortly after.

11 The superficial spreading melanoma (SSM) accounts for about 60% of all melanomata and is the most common type. SSM undergoes two growth phases. During the "radial" phase, the lesion expands through the epidermis (upper skin layer). In the early radial phase, which may last months or years, the lesion is thin. After the radial phase, a "vertical" growth phase begins. It may contain areas of tan, brown/black, red, dark blue/purple, or white coloration. This melanoma often appears as a flat „spot“ with regular borders.

12 The structure of the skin

13 The impact of UV - radiation

14 Because of the advancing loss of Ozone within the stratosphere, the intensity of the UV-radiation increased noticeably. The sensitivity towards UV-A-radiation depends on the skin type. We all react alike towards UV-B and UV-C, because those rays were not planned to reach the earth at all. Do we all react alike?

15 The 4 different skin types Skin type 2 Skin: Fair Hair: Blond to brown Eyes: Grey, blue, green Reaction to sun: Mostly, severe Tan : Moderate tan Sunburn after: 15 min. Skin type 1 Skin: Strikingly fair, pale Hair: Fair blonde to reddish Eyes: Green, blue Reaction to sun: Always, severe, painful Tan: No tan Sunburn after: 10 min.

16 The 4 different skin types Skin type 3 Skin: Light tan, olive Hair: Deep blonde, brown Eyes: Grey, brown Reaction to sun: Rarely, moderately Tan: Good tan Sunburn after: 20-30 min. Skin type 4 Skin: Brown Hair: Deep brown, black Eyes: Brown Reaction to sun: Hardly any Tan : Fast and deep; very good tan Sunburn after: 40-60 min.

17 Examples for other illnesses Damage to the eyes  Damage to the eyes General weakening of the immune system  General weakening of the immune system

18 Effects on nature A permanent damage to the environment leaves broad features on plants:  Retrenchment of the photosynthesis  Shorter sprouts  Decrease of the average leaf surface  Alterations within the plant communities These alterations could lead to extensive crop loss and to changes within the food chain or could contribute to forest dieback.

19 Effects on nature The nutrient-rich phytoplankton (e.g. Algaes) decline in the seas. As the process develops the following tendencies become apparent:  Lack of food for fish and changes in the composition of species composition of species  Loss of the greatest producer of oxygen, as well as less conversion of CO 2 conversion of CO 2  Increase of the greenhouse effect

20 Situation and structure The Ozone Layer

21 General information about the Ozone layer The Ozone layer is located in the stratosphere. The Ozone layer is located in the stratosphere. The highest concentration of Ozone exists at a height from 20 to 25km and serves as a shield against UV-B and UV-C radiation. The highest concentration of Ozone exists at a height from 20 to 25km and serves as a shield against UV-B and UV-C radiation. This is the only way life on earth, as we know it today, is possible. This is the only way life on earth, as we know it today, is possible.

22 Structure of the Atmosphere Our habitat is situated in the Troposphere Our habitat is situated in the Troposphere

23 The Arctic Hole in the Ozone Layer

24 Why above the Antarctic? The graph to the right shows the measured total ozone above the Halley Bay station in Antarctica. Halley Bay stationHalley Bay station

25  Owing to temperatures of - 80° C water vapour condensates in the stratosphere. PSCs form and are made of ice, nitric acid and sulphuric acids.  The HCl and ClONO 2 molecules are able to react with the ice crystals of the PSCs.  HCl is tied to the surface of the ice crystals and reacts with the ClONO 2 molecule. Thereupon, molecular Chlorine (Cl 2 ) is released. (PSC = Polar Stratospheric Clouds). Why above the Antarctic?

26 The descent of the cooling airmasses causes a cyclical, circumpolar votex. It encloses the cool air above the poles and prevents the warmer, more ozoniferous airmasses from reaching the lower latitudes. The descent of the cooling airmasses causes a cyclical, circumpolar votex. It encloses the cool air above the poles and prevents the warmer, more ozoniferous airmasses from reaching the lower latitudes. Why above the Antarctic?

27 The Future of the Ozonehole Due to the long lifespan of CFC it will take approximately 50 years before the already released CFCs in the stratosphere are removed. Due to the long lifespan of CFC it will take approximately 50 years before the already released CFCs in the stratosphere are removed. Furthermore, the use of CFC did not completely stop in spite of agreements such as the Montreal Protocol and succeeding protocols. Furthermore, the use of CFC did not completely stop in spite of agreements such as the Montreal Protocol and succeeding protocols.

28 1. CFC – Where are they found? 2. Climate friendly alternatives and their disadvantages CFC

29 What are CFC‘s? What are CFC‘s? CFC is an abbreviation for Chlorofluorocarbons. They were used in fire extinguishers, aerosol sprays and refrigerators. They can exist in the environment for 45- 300 years, as they are generally non- reactive.

30 Why does CFC destroy the ozone?  UV-radiation breaks off the chlorine atom of the CFC.  The chlorine atoms and Ozone react. Ozone is destroyed  At the same time Chloroxide develops and reacts with the Ozone.  Ozone is destroyed, and the chlorine atoms are released again.  This continuous chain reaction destroys the Ozone.

31 Climate friendly alternatives Refrigerants (since the 30s) have been replaced by the following: Refrigerants (since the 30s) have been replaced by the following: Since January 1st, 1995 CFC is no longer used in car air conditioners and refrigerators. Since January 1st, 1995 CFC is no longer used in car air conditioners and refrigerators. Instead of CFC, Isobutane is used in today‘s refrigerators. Instead of CFC, Isobutane is used in today‘s refrigerators. Ammonia and Propane are used in commercial new construction. Ammonia and Propane are used in commercial new construction. Also used, is H-FC, which is harmless to the Ozone. Also used, is H-FC, which is harmless to the Ozone.

32 Prohibited in foam plastics, pentane or cabondioxide are used instead. Prohibited in foam plastics, pentane or cabondioxide are used instead. Prohibited in insulation since 1994, glas-/ rock wool, animal or herbal fibres are used instead. Prohibited in insulation since 1994, glas-/ rock wool, animal or herbal fibres are used instead. Prohibited since 1992 in detergents and solvents, water-based detergents are increasingly used. Prohibited since 1992 in detergents and solvents, water-based detergents are increasingly used. Prohibitied in fire extinguishers since 1994, carbon dioxide, water, foam and powder are used instead. Prohibitied in fire extinguishers since 1994, carbon dioxide, water, foam and powder are used instead. Prohibited early in aerosol sprays, they are still used in special applications (antiasthmatic sprays). Prohibited early in aerosol sprays, they are still used in special applications (antiasthmatic sprays).

33 Further climate friendly alternatives and their disadvantages Hydrocarbons (propane, isobutane, pentane)  flammable Hydrocarbons (propane, isobutane, pentane)  flammable Carbon dioxide  harmful to the environment and climate: greenhouse effect. Carbon dioxide  harmful to the environment and climate: greenhouse effect. Water  some substances lose their attributes by reacting with water. Water  some substances lose their attributes by reacting with water. Ammonia  could transform into ammonium compound, that could lead to an eutrophication of bodies of water and vegetation. Additionally, ammonia is very toxic. Ammonia  could transform into ammonium compound, that could lead to an eutrophication of bodies of water and vegetation. Additionally, ammonia is very toxic.

34 Thank You


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