Treibhauseffekt und Ozonloch

Patch Quartermain
18 Nov 201817:12

Summary

TLDRThis script delves into the phenomena of the greenhouse effect and ozone depletion, explaining their distinct roles in global warming. It describes how sunlight interacts with Earth's atmosphere, highlighting the protective role of the ozone layer in filtering harmful UV radiation. The script also discusses the natural greenhouse effect, essential for maintaining Earth's temperature, and contrasts it with the anthropogenic effect exacerbated by human activities. It emphasizes the impact of greenhouse gases like carbon dioxide, methane, and chlorofluorocarbons (CFCs), which not only contribute to global warming but also deplete the ozone layer. The script concludes by pondering the future implications of these human-induced changes on our planet and the potential measures to mitigate them.

Takeaways

  • 🌞 All living beings on Earth use sunlight for life and growth, with light traveling in electromagnetic waves of varying lengths and energies.
  • 👀 The human eye can only see a certain range of solar radiation, but we can perceive the effects of ultraviolet (UV) radiation, such as sunburns.
  • ☀️ UV radiation is divided into three categories: UVA, UVB, and UVC, with UVA reaching the Earth's surface largely unimpeded, UVB being mostly absorbed by the atmosphere, and UVC being almost entirely filtered out by the ozone layer.
  • 🌁 The Earth's atmosphere consists of different layers, including the troposphere and the stratosphere, where the ozone layer is located at an altitude of 20 to 30 kilometers.
  • 🔁 The ozone layer plays a crucial role in filtering out harmful UVC and a significant portion of UVB radiation, protecting life on Earth.
  • 🌡️ The Earth's average surface temperature is +15 degrees Celsius, thanks to the natural greenhouse effect, which compares to a hypothetical average temperature of -18 degrees Celsius without the atmosphere.
  • 🌍 The natural greenhouse effect is caused by greenhouse gases like water vapor, carbon dioxide (CO2), methane, and ozone, which trap heat in the atmosphere.
  • 🚫 The anthropogenic greenhouse effect, caused by human activities, has intensified the natural greenhouse effect, leading to global warming and climate change.
  • 🔝 Carbon dioxide (CO2) is the primary contributor to the anthropogenic greenhouse effect, released through activities such as deforestation and the burning of fossil fuels.
  • 🈲️ The production and use of fluorocarbons (FCKW), which were used in refrigerants and aerosols, have been banned worldwide since 2010 due to their high greenhouse potential and ozone depletion.
  • 🔄 The ozone hole over Antarctica forms due to the reaction of ozone with chlorine atoms released from FCKW molecules, but the ban on these substances has led to a slow recovery of the ozone layer.

Q & A

  • What is the greenhouse effect and how is it related to global warming?

    -The greenhouse effect is a natural process where certain gases in the Earth's atmosphere trap heat, preventing it from escaping into space, which contributes to the warming of the planet. This effect is related to global warming as it is the primary cause of the increase in Earth's average temperature.

  • What are the different layers of the Earth's atmosphere mentioned in the script?

    -The script mentions two main layers of the Earth's atmosphere: the troposphere, which is the lowest layer and contains the ozone layer, and the stratosphere, which is located above the troposphere and contains a significant amount of ozone.

  • What is the role of the ozone layer in the stratosphere?

    -The ozone layer in the stratosphere plays a crucial role in filtering out the majority of the sun's harmful ultraviolet (UV) radiation, specifically UVC and a large part of UVB, protecting life on Earth from their damaging effects.

  • How does the ozone layer form and what maintains its natural cycle?

    -The ozone layer forms when UVC radiation in the stratosphere encounters oxygen molecules, splitting them into individual atoms. These reactive oxygen atoms can then react with other oxygen molecules to form ozone molecules. The bonds within ozone molecules are weaker than those in oxygen molecules, allowing them to break down again upon absorbing UVB radiation, maintaining a natural cycle.

  • What is the significance of UVA, UVB, and UVC radiation?

    -UVA radiation reaches the Earth's surface relatively unimpeded and is less harmful, though it can cause sunburn if exposed for long periods. UVB radiation, which is more energetic, is mostly absorbed in the Earth's atmosphere, with only about 10% reaching the surface and causing sunburn and increasing skin cancer risk. UVC radiation is the most harmful and is almost entirely filtered out by the atmosphere before reaching the surface.

  • What is the average surface temperature of the Earth and how does the atmosphere contribute to it?

    -Without the atmosphere, the Earth's average surface temperature would be minus 18 degrees Celsius. However, thanks to the atmosphere and the natural greenhouse effect, the actual average surface temperature is plus 15 degrees Celsius, creating a more habitable environment.

  • What are the five most important naturally occurring greenhouse gases mentioned in the script?

    -The five most important naturally occurring greenhouse gases mentioned are water vapor (H2O), carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and ozone (O3).

  • How does carbon dioxide contribute to both the greenhouse effect and the anthropogenic (human-induced) greenhouse effect?

    -Carbon dioxide contributes to the natural greenhouse effect by being a part of the Earth's atmosphere and playing a role in maintaining the planet's temperature. In the anthropogenic greenhouse effect, human activities such as deforestation and the burning of fossil fuels release large amounts of CO2, which significantly enhances the greenhouse effect and leads to global warming.

  • What are the main sources of methane and how does it compare to carbon dioxide in terms of greenhouse potential?

    -Methane is produced in the digestive tracts of ruminants, during wet rice cultivation, in landfills, and in wastewater treatment plants, as well as through the burning of fossil fuels. Methane has a much higher greenhouse potential than carbon dioxide, with a single methane molecule having the same warming effect as about 20 CO2 molecules.

  • What are fluorocarbons (FCKW) and why were they banned worldwide?

    -Fluorocarbons (FCKW) are a group of chemically similar molecules that are produced exclusively by humans and do not occur naturally in the atmosphere. They were used in applications such as propellants in spray cans. They were banned worldwide since 2010 due to their high greenhouse potential and their destructive effect on the ozone layer.

  • How does the depletion of the ozone layer affect human health and the environment?

    -The depletion of the ozone layer allows more harmful UVA and UVB radiation to reach the Earth's surface, increasing the risk of skin cancer and other health issues. It also has broader environmental implications, such as affecting the balance of ecosystems and contributing to climate change.

  • What is the connection between the ozone hole and the greenhouse effect?

    -Both the ozone hole and the greenhouse effect are influenced by human-produced gases. While the ozone hole is primarily caused by the release of chlorofluorocarbons (CFCs), which deplete ozone, the greenhouse effect is exacerbated by gases like carbon dioxide and methane, which trap heat in the atmosphere. Both phenomena involve gases that have a significant impact on the Earth's climate and atmospheric composition.

Outlines

00:00

🌿 Understanding the Greenhouse Effect and Ozone Layer

This paragraph delves into the phenomena of the greenhouse effect and global warming. It explains how all living beings on Earth utilize solar energy for life and growth, and how different wavelengths of electromagnetic waves, including visible light and invisible ultraviolet (UV) radiation, interact with the Earth's atmosphere. The text highlights the importance of the ozone layer, located in the stratosphere, which filters out harmful UV radiation, particularly UVC, and plays a crucial role in maintaining the balance of life on Earth. The natural greenhouse effect is also introduced, which is essential for maintaining Earth's average surface temperature at a hospitable level.

05:00

🌍 The Impact of Human Activities on the Greenhouse Effect

This section discusses the human-induced enhancement of the natural greenhouse effect, known as the anthropogenic greenhouse effect. It identifies carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and fluorinated gases (FCKW) as the primary greenhouse gases emitted by human activities, with CO2 being the most significant contributor. The paragraph also explains how these gases, especially FCKW, have a long atmospheric lifetime and high global warming potential, leading to an increase in global temperatures and significant environmental changes. The role of methane in agriculture and other human activities is also highlighted, emphasizing the need for sustainable practices to mitigate climate change.

10:03

🌡️ The Ozone Layer Depletion and Its Consequences

This paragraph focuses on the depletion of the ozone layer, particularly over the Antarctic, and the role of human-produced chlorofluorocarbons (CFCs) in this process. It describes how CFC molecules, once in the stratosphere, are split by UV radiation, releasing reactive chlorine atoms that catalyze the breakdown of ozone molecules. The formation of the ozone hole and its seasonal recovery are explained, illustrating the global transport of ozone and CFCs by wind systems. The paragraph also connects the depletion of the ozone layer to increased harmful UV radiation reaching the Earth's surface, which poses risks to human health and the environment.

15:04

🔗 The Interconnection Between Ozone Depletion and Greenhouse Effect

The final paragraph explores the commonalities between ozone depletion and the greenhouse effect, emphasizing that both phenomena are significantly influenced by human activities. It points out that while the ozone layer protects us from aggressive UV radiation, the greenhouse effect, exacerbated by human-produced gases, leads to global warming. The paragraph concludes by posing questions about the future impact of the anthropogenic greenhouse effect on life on Earth and the potential actions that can be taken to reduce emissions and mitigate these environmental challenges.

Mindmap

Keywords

💡Greenhouse Effect

The greenhouse effect is a natural process that warms the Earth's surface. It is likened to the function of a greenhouse, where certain gases in the Earth's atmosphere trap heat, preventing it from escaping into space. In the video, it is explained that without this effect, Earth's average temperature would be much colder at minus 18 degrees Celsius, whereas it is actually plus 15 degrees Celsius. The script also discusses the anthropogenic (human-induced) greenhouse effect, which is exacerbating this natural process due to activities like burning fossil fuels and deforestation.

💡Global Warming

Global warming refers to the long-term increase in Earth's average surface temperature due to human activities, primarily the emission of greenhouse gases. The script mentions that the anthropogenic greenhouse effect leads to a rise in global temperatures, causing significant changes to the environment and human life, such as shifts in climate zones.

💡Ozone Layer

The ozone layer is a region of the Earth's stratosphere that contains a high concentration of ozone (O3) molecules. It plays a critical role in absorbing the Sun's ultraviolet (UV) radiation, particularly the harmful UVC rays. The script explains that the ozone layer filters out UVC and a large part of UVB radiation, allowing only the less energetic UVA radiation to reach the Earth's surface. It also discusses the depletion of the ozone layer, particularly over the Antarctic, due to human-made chemicals like CFCs.

💡Ultraviolet Radiation (UV)

Ultraviolet radiation is a part of the electromagnetic spectrum with wavelengths shorter than visible light but longer than X-rays. The script divides UV radiation into three types: UVA, UVB, and UVC. UVA reaches the Earth's surface with minimal harm, UVB can cause sunburn and increase skin cancer risk, and UVC is the most harmful but is almost entirely absorbed by the atmosphere.

💡Troposphere

The troposphere is the lowest layer of Earth's atmosphere, where weather phenomena occur. It is mentioned in the script as the layer through which sunlight passes, and where UVC and much of the UVB radiation are filtered out by the ozone layer.

💡Stratosphere

The stratosphere is the second layer of Earth's atmosphere above the troposphere, extending from about 10 to 50 kilometers above the Earth's surface. The script highlights the stratosphere as the location of the ozone layer and the place where the ozone molecules form and protect the Earth from harmful UV radiation.

💡Infrared Radiation

Infrared radiation is a type of electromagnetic radiation with wavelengths longer than visible light. The script explains that the Earth's surface absorbs shortwave UVA radiation and visible light and re-emits it as longwave infrared radiation, which is trapped by greenhouse gases, contributing to the warming of the atmosphere.

💡Carbon Dioxide (CO2)

Carbon dioxide is a greenhouse gas that contributes to the greenhouse effect. The script states that CO2 is released through processes like volcanic eruptions, wildfires, and metabolic processes of humans and animals, and it makes up about 22% of the natural greenhouse effect. It is also the primary greenhouse gas contributing to the anthropogenic greenhouse effect, released through activities like burning fossil fuels.

💡Methane (CH4)

Methane is another potent greenhouse gas that is formed in the digestive tract of ruminants and also during the decay of organic matter in wetlands, landfills, and anaerobic digestion in sewage treatment plants. The script mentions that methane has a much higher global warming potential than CO2, with one methane molecule having the same warming effect as about 20 CO2 molecules.

💡Chlorofluorocarbons (CFCs)

Chlorofluorocarbons, or CFCs, are synthetic compounds that were historically used as refrigerants and propellants in aerosol products. The script explains that CFCs are not naturally occurring and have a significant impact on both the greenhouse effect and the depletion of the ozone layer. They release highly reactive chlorine atoms in the stratosphere, which can destroy up to 100,000 ozone molecules each.

💡Ozone Hole

The ozone hole refers to the significant depletion of the ozone layer above Antarctica, which allows more harmful UV radiation to reach the Earth's surface, increasing the risk of skin cancer. The script describes how CFCs contribute to the formation of the ozone hole and how the ban on CFCs is helping the ozone layer to slowly recover.

Highlights

All living beings on Earth use the energy of sunlight to live and grow.

The eye can only see a certain range of solar radiation, but UV radiation can be perceived through effects like sunburn.

UV radiation is divided into three regions, with UV A reaching the Earth's surface relatively unimpeded and being less dangerous.

The ozone layer, located in the stratosphere, filters out harmful UV C radiation and most of the UV B radiation.

Without the atmosphere, Earth's average temperature would be -18 degrees Celsius, but it is actually +15 degrees Celsius due to the greenhouse effect.

The natural greenhouse effect is compared to the functioning of a greenhouse, maintaining a life-friendly average temperature on Earth.

The top five naturally occurring greenhouse gases are water vapor, carbon dioxide, methane, nitrous oxide, and ozone.

Water vapor contributes the most to the natural greenhouse effect at around 66%.

Carbon dioxide contributes approximately 22% to the natural greenhouse effect, released by volcanic eruptions, wildfires, and metabolic processes.

Ozone in the stratosphere does not affect the greenhouse effect but plays a role in the natural greenhouse effect at around 6%.

Human activities have disrupted the natural warming system, causing an artificially intensified greenhouse effect known as the anthropogenic greenhouse effect.

The five most common greenhouse gases released by humans into the troposphere are carbon dioxide, methane, nitrous oxide, hydrofluorocarbons (HFCs), and perfluorocarbons (PFCs).

Carbon dioxide is released particularly through deforestation and the burning of fossil fuels, contributing the most to the anthropogenic greenhouse effect.

Methane is produced in the digestive tract of ruminants, in rice paddies, landfills, wastewater treatment plants, and from burning fossil fuels.

Nitrous oxide, also known as laughing gas, is released mainly through fertilization in agriculture and has a greenhouse potential 300 times higher than carbon dioxide.

Fluorocarbons (FCKW) are produced solely by humans and were used as propellants in spray cans; their production and use have been banned worldwide since 2010.

Ground-level ozone irritates human mucous membranes, especially on hot summer days, and can lead to health warnings about high ozone levels.

The anthropogenic greenhouse gases also contribute to the warming of the atmosphere, leading to a rise in global average temperatures and significant environmental changes.

In the 1980s, researchers discovered a significant depletion of the ozone layer over Antarctica, largely due to long-lived fluorocarbons (FCKW).

FCKW molecules in the ozone layer are split by UV B radiation, releasing highly reactive chlorine atoms that accelerate ozone depletion.

The ban on FCKW has shown its effect, with the ozone layer slowly recovering, although it will take many decades for the long-lived FCKW gases to fully decompose.

Both the greenhouse effect and ozone depletion are phenomena that FCKW gases play a significant role in, affecting both ozone protection and atmospheric warming.

The impact of the anthropogenic greenhouse effect on our future life on Earth remains uncertain, and efforts to reduce or prevent the emission of greenhouse gases and ozone are crucial.

Transcripts

play00:06

treibhauseffekt globale erwärmung wozu

play00:10

noch schlagworte die wir immer wieder

play00:13

was genau verbirgt sich hinter diesen

play00:16

phänomenen

play00:18

verursacht der treibhauseffektes

play00:20

ozonloch oder umgekehrt

play00:22

haben sie überhaupt etwas miteinander zu

play00:24

tun bringen wir licht in die

play00:27

angelegenheit

play00:30

alle lebewesen auf der erde nutzen jeden

play00:32

tag die energie des sonnenlichtes um zu

play00:35

leben um zu wachsen

play00:42

licht bewegt sich in elektromagnetischen

play00:44

wellen fort diese sind unterschiedlich

play00:47

lang

play00:47

je kürzer die wellenlänge desto höher

play00:50

die energie der strahlung

play00:54

unser auge kann nur einen bestimmten

play00:57

bereich der sonnenstrahlung sehen

play00:59

doch auch unsichtbare bereiche wie die

play01:02

ultraviolette strahlung die uv strahlung

play01:05

können wir wahrnehmen wenn wir etwa zu

play01:08

lange in der sonne liegen und einen

play01:10

sonnenbrand bekommen

play01:13

die uv strahlung wird in drei bereiche

play01:16

unterteilt die uv a strahlung gelangt

play01:20

relativ ungehindert zur erdoberfläche

play01:23

sie ist für uns kaum gefährlich die

play01:29

energiereiche uv b strahlung wird in der

play01:32

erdatmosphäre größtenteils abgeschwächt

play01:34

nur noch circa zehn prozent der

play01:37

strahlung erreichen die erdoberfläche

play01:38

sind wir der uvb-strahlung längere zeit

play01:42

ausgesetzt bekommen wir einen

play01:44

sonnenbrand und hautkrebs risiko steigt

play01:50

die besonders kurzwellige und sehr

play01:53

schädliche uv b strahlung wird in der

play01:56

atmosphäre fast vollständig

play01:58

herausgefiltert und kann nicht bis zur

play02:01

erdoberfläche durchdringen wo in der

play02:12

atmosphäre wird der schädliche uv anteil

play02:14

der sonnenstrahlung herausgefiltert

play02:17

facebook zu

play02:21

die erdatmosphäre setzt sich aus

play02:23

unterschiedlichen schichten zusammen

play02:26

die unterste schicht bezeichnen wir als

play02:29

troposphäre

play02:30

[Musik]

play02:37

[Applaus]

play02:39

hoch über den wolken folgt die

play02:41

stratosphäre

play02:43

[Musik]

play02:47

hier in einer höhe von 20 bis 30

play02:49

kilometern stoßen wir auf eine besondere

play02:52

schicht die ozonschicht in ihr

play02:56

konzentrieren sich etwa 90 des gesamten

play02:59

atmosphärischen und ewig was aber ist um

play03:02

zu

play03:04

in der stratosphäre trifft die besonders

play03:06

energiereiche uvc strahlung auf

play03:09

sauerstoff moleküle und spaltet sie in

play03:12

einzelne atome diese sauerstoff atome

play03:16

sind sehr reaktionsfreudig und können

play03:19

mit anderen sauerstoff molekülen zu ozon

play03:22

molekülen weiter reagieren die

play03:25

bindungskräfte innerhalb von ozon

play03:27

molekülen sind geringer als die

play03:29

innerhalb von sauerstoff moleküle schon

play03:32

bei der aufnahme von uv b strahlung

play03:34

können sie wieder zu fall

play03:36

er wird nie der gesamte sauerstoff in

play03:39

der atmosphäre in ozon umgewandelt es

play03:42

besteht ein natürlicher kreislauf

play03:43

[Musik]

play03:50

auf diese weise filtert die ozonschicht

play03:53

die uv c strahlung sowie einen großteil

play03:56

der uvb strahlung aus der

play03:57

sonnenstrahlung heraus lediglich die

play04:00

energie ärmere uva strahlung kann

play04:02

ungehindert zur erdoberfläche gelangen

play04:10

höhe von wir mit unserem wetterballon

play04:12

leider nicht

play04:19

[Musik]

play04:35

ohne die atmosphäre hätten wir auf

play04:38

unserem planeten eine

play04:39

durchschnittstemperatur von minus 18

play04:42

grad celsius

play04:43

tatsächlich beträgt die

play04:44

durchschnittliche oberflächentemperatur

play04:47

der erde aber plus 15 grad celsius

play04:50

dies verdanken wir einem phänomen das

play04:53

vereinfacht mit der funktionsweise eines

play04:55

treibhauses verglichen wird

play04:57

man spricht auch von natürlichen

play05:00

treibhauseffekt das licht der sonne

play05:03

passiert auf seinem weg zum erdboden

play05:06

unserer atmosphäre in der ozonschicht

play05:09

werden die uv c strahlung und ein

play05:12

großteil der uvb-strahlung

play05:13

herausgefiltert die uv a strahlung und

play05:17

die sichtbare strahlung hingegen

play05:18

gelangen relativ ungehindert zur

play05:20

erdoberfläche nur ein gewisser teil wird

play05:25

an allen oberflächen wie zum beispiel

play05:27

den wolken reflektiert und

play05:29

zurückgeworfen

play05:31

die erdoberfläche nimmt die kurzweilige

play05:34

uv a strahlung auf und gibt sie in form

play05:37

von langwellige wärmestrahlung der

play05:40

infrarotstrahlung wieder ab doch so

play05:42

einfach wie die strahlung in die

play05:44

troposphäre gelangt ist kommt zu ihm

play05:47

nicht mehr heraus dafür sorgen die

play05:49

sogenannten treibhausgase

play05:55

der moleküle sind zwar durchlässig für

play05:57

kurzweilige sonnenstrahlung für

play06:00

langwellige infrarotstrahlung allerdings

play06:02

nicht sie nehmen diese auf und strahlen

play06:06

anschließend wieder wärmestrahlung in

play06:08

alle richtungen ab auch zurück zu ehren

play06:11

diese gegen strahlung erwärmt die

play06:14

atmosphäre zusätzlich

play06:20

die fünf wichtigsten der natürlich

play06:22

vorkommenden treibhausgase sind

play06:24

wasserdampf kohlenstoffdioxid co2

play06:28

lachgas und methan das bedeutendste

play06:32

treibhausgas ist wasser h2o in form von

play06:36

wasserdampf

play06:37

es trägt mit circa 66 zum natürlichen

play06:41

treibhauseffekt bei co2

play06:46

kohlenstoffdioxid das etwa bei

play06:48

vulkanausbrüchen

play06:51

weit bränden und stoffwechselprozessen

play06:54

von menschen und tieren freigesetzt wird

play06:56

macht etwa 22 aus dass ozon der

play07:02

ozonschicht hat keinen einfluss auf den

play07:04

treibhauseffekt aber in geringer

play07:06

konzentration bildet sich ozon o3 auch

play07:11

in geltow bus wäre zum beispiel bei

play07:13

waldbränden und ist mit rund sechs

play07:15

prozent an natürlichen treibhauseffekt

play07:17

beteiligt die übrigen anteile entfallen

play07:20

auf lachgas n2o und methan ch4 dank des

play07:39

natürlichen treibhauseffekt es herrscht

play07:41

bei uns auf der erde eine

play07:42

lebensfreundliche durchschnitts

play07:44

temperatur von 15 grad celsius

play07:47

seit einigen jahrhunderten greift der

play07:49

mensch das natürliche system der

play07:52

erderwärmung ein und sorgt für einen

play07:55

künstlich verstärkten treibhauseffekt

play07:58

wir bezeichnen diesen als anthropogenen

play08:01

treibhauseffekt nach dem altgriechischen

play08:04

wort im anthroposophisch

play08:09

die fünf häufigsten von menschen in die

play08:11

troposphäre gebrachten treibhausgase

play08:14

sind kohlenstoffdioxid methan lachgas

play08:19

fckw und wozu kohlenstoffdioxid wird

play08:25

insbesondere durch die brandrodung

play08:27

großer waldflächen freigesetzt ebenso

play08:30

durch das verbrennen fossiler rohstoffe

play08:32

mit circa 66 prozent leistet

play08:35

kohlenstoffdioxid den größten beitrag

play08:37

zum anthropogenen treibhauseffekt im

play08:41

verdauungstrakt von wiederkäuern wird

play08:44

das treibhausgas methan gebildet welches

play08:47

die nahezu in minuten takt auf dem ein

play08:50

oder anderen weg

play08:54

aber auch beim nass reisanbau

play08:57

mülldeponien oder in klärwerken sowie

play09:01

beim verbrennen fossiler energieträger

play09:03

wird methan erzeugt metall moleküle sind

play09:08

in der troposphäre zwar nicht so häufig

play09:10

vertreten wie kohlenstoffdioxid moleküle

play09:12

besitzen allerdings ein höheres

play09:15

treibhauspotenzial ein einziges methan

play09:18

molekül trägt so stark zur globalen

play09:21

erwärmung bei wie etwa 20 co2 moleküle

play09:28

das treibhausgas die stickstoffmonoxid

play09:31

auch lachgas genannt gelangt

play09:34

insbesondere durch düngung in der

play09:35

landwirtschaft in die atmosphäre

play09:38

lachgas hat sogar einen rund 300 mal

play09:41

höheres treibhauspotenzial als

play09:44

kohlenstoffdioxid fluor chlor

play09:50

kohlenwasserstoffe oder kurz fckw bilden

play09:55

eine gruppe von ähnlich aufgebauten

play09:57

molekülen

play09:58

sie werden allein von menschen

play10:00

produziert und kommen anders als die

play10:02

anderen treibhausgase nicht von natur

play10:05

aus in der atmosphäre vor

play10:07

früher dienten sie zum beispiel als

play10:10

treibmittel in spraydosen

play10:11

seit 2010 sind die herstellung und der

play10:14

einsatz von fckw gasen weltweit verboten

play10:17

weil sie jeden ihrer treibhauswirkung

play10:20

auf die ozonschicht zerstört

play10:26

[Musik]

play10:29

fckw gase sind extrem langlebig ihr

play10:34

treibhauspotenzial entspricht sogar dem

play10:36

bis zu 14.000 fachen von

play10:38

kohlenstoffdioxid auch die

play10:43

treibhauswirkung von bodennahem ozon hat

play10:46

durch den menschen an bedeutung gewonnen

play10:51

autos blasen stickstoffdioxid moleküle

play10:54

in die atmosphäre welche durch

play10:57

sonnenstrahlung in stickstoffmonoxid

play10:59

moleküle und sauerstoff atome gespalten

play11:02

werden

play11:03

dieser atomare sauerstoff verbindet sich

play11:07

mit molekularen sauerstoff wiederum zu

play11:09

ozon moleküle ozon wirkt bei uns

play11:13

menschen schleimhaut reizen

play11:15

besonders an heißen sommertagen wird

play11:17

daher manchmal vor zu hohen ozonwerten

play11:20

gewarnt

play11:22

diese durch den menschen produzierten

play11:24

treibhausgase sorgen dafür dass

play11:27

zusätzlich zum natürlichen

play11:29

treibhauseffekt noch mehr wärmestrahlung

play11:32

in der atmosphäre gehalten

play11:34

das zu einem weltweiten anstieg der

play11:37

durchschnittstemperaturen und zu

play11:39

schwerwiegenden veränderungen für mensch

play11:42

und umwelt wie zum beispiel der

play11:45

verschiebung von klimazonen

play11:48

[Musik]

play11:55

in den 1980 er jahren haben forscher

play11:58

festgestellt dass sich die ozonschicht

play12:01

über der antarktis so stark ausgedünnt

play12:04

hatte dass man erstmals von einem

play12:07

erzieher sprache schuld an dessen

play12:10

entstehung war und ist vor allem die

play12:12

gruppe der langlebigen

play12:14

fluorchlorkohlenwasserstoffen fckw

play12:18

gelangen fluorchlorkohlenwasserstoff

play12:21

moleküle in die ozonschicht werden sie

play12:24

durch die energiereiche uv b strahlung

play12:26

der sonne gespalten

play12:28

dadurch werden hoch reaktive chlor atome

play12:31

freigesetzt

play12:32

sie verstärken den ozonabbau um ein

play12:35

vielfaches

play12:36

denn ein chloratum kann bis zu 100.000

play12:41

ozon moleküle spalten ohne dabei selbst

play12:44

verbraucht zu werden

play12:45

je stärker die sonneneinstrahlung desto

play12:49

mehr ozon wird in der stratosphäre

play12:50

gebildet über dem äquator ist die

play12:53

sonneneinstrahlung und somit auch die

play12:56

ozonbildung besonders hoch

play12:58

überschüssiges ozon und auch fckw werden

play13:02

über globalen zirkulierende windsysteme

play13:04

in richtung der pole transportiert

play13:07

aufgrund der sehr unterschiedlichen

play13:09

landwasser verteilungen auf beiden

play13:12

erdhalbkugel bildet sich in den kalten

play13:14

wintermonaten jedoch über der antarktis

play13:17

ein riesiger stabiler greifen

play13:21

dieser isoliert ozon reiche luftmassen

play13:23

in seinem inneren und blockiert die

play13:26

zufuhr weiterer ozon haltiger luft aus

play13:29

den tropen die perfekten

play13:31

ausgangsbedingungen für einen

play13:32

ungebremsten ozonabbau durch die fckw

play13:36

gase erst im antarktischen frühjahr wenn

play13:40

der kite luftwirbel schwächer wird und

play13:42

frische ozon heilige luft aus den tropen

play13:44

nach strömt kann sich das ozonloch

play13:47

wieder schließen

play13:49

auch das weltweit der fckw verbot zeigt

play13:52

wirkung die ozonschicht erholt sich

play13:55

langsam

play13:56

trotzdem wird es noch viele jahrzehnte

play13:57

dauern bis die langlebigen fckw gase in

play14:01

der stratosphäre vollständig abgebaut

play14:03

sein werden

play14:11

treibhauseffekt

play14:13

noch sind zwei sehr unterschiedliche

play14:15

phänomene durch ein ozonloch kann die

play14:20

schädliche uv a und uv b strahlung der

play14:23

sonne ungefiltert bis zur erdoberfläche

play14:25

gelangen

play14:27

das hautkrebsrisiko steigt

play14:30

vom treibhauseffekt hingegen spricht man

play14:33

wenn sich die erdatmosphäre dank der in

play14:36

ihr enthaltenen treibhausgase erwärmt

play14:39

die von der sonne entsendete kurzweilige

play14:42

uv a strahlung unter sichtbare licht

play14:45

werden vom erdboden aufgenommen und in

play14:48

form von langwellige wärmestrahlung

play14:50

wieder abgegeben

play14:51

die treibhausgas moleküle nehmen diese

play14:54

wärmestrahlung auf und geben sie

play14:56

anschließend wieder in alle richtungen

play14:58

ab

play14:59

die wärme bleibt so etwas länger in der

play15:01

troposphäre erhalten und die

play15:03

temperaturen steigen an

play15:07

doch trotz dieser unterschiede haben

play15:09

beide phänomene zumindest eine

play15:11

gemeinsamkeit sowohl wohn als auch die

play15:15

ozon abbauen denn fckw sind

play15:17

treibhausgase und spielen bei beiden

play15:20

phänomenen eine wichtige rolle für ozon

play15:24

kann man deshalb zusammenfassen oben hui

play15:27

das uns vor der aggressiven uv strahlung

play15:30

schützt und um das hier den

play15:33

treibhauseffekt verstärkt und beim

play15:35

einatmen unsere atemwege schädigen

play15:38

wie stark der anthropogenen

play15:41

treibhauseffekt und das so tun noch

play15:43

unser leben auf der erde in zukunft

play15:46

beeinflussen werden bleibt offen

play15:47

[Musik]

play15:49

können wir den ausstoß von

play15:50

treibhausgasen und ozon kielern weiter

play15:53

senken oder sogar ganz verhindern

play15:59

[Musik]

play16:04

[Applaus]

play16:09

[Musik]

play16:16

[Musik]

play16:18

[Gelächter]

play16:18

[Musik]

play16:52

[Musik]

Rate This

5.0 / 5 (0 votes)

Related Tags
Global WarmingOzone LayerClimate ChangeAtmospheric ScienceUV RadiationInfrared RadiationEnvironmental ImpactAnthropogenic EffectsNatural Greenhouse EffectOzone Depletion