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GAMMA Project
Vliegverkeer en Het broeikaseffect in
           een notendop
        My Linh Nguyen 3V2
Broeikasgassen

    Atmosfeer
    De atmosfeer is een dunne deken
    van lucht die de aarde bedekt. Deze
    luchtige deken, ook wel dampkring
    genoemd, houdt onze planeet op        Zonnestralen gaan door
    een comfortabele temperatuur          de atmosfeer
    (ongeveer 15 graden).

                                                                      De broeikasgassen
                                                                      laten een deel van
                                                                      de
                                                 Het aardoppervlak
                                                                      infraroodstraling
                                                 neemt de zonne
                                                                      door, maar kaatsen
                                                 energie op, maar
                                                                      ook een deel terug
                                                 stuurt ook
                                                                      naar de aarde. Hoe
                                                 infraroodstralen
                                                                      meer
                                                 terug de atmosfeer
                                                                      broeikasgassen er
                                                 in
                                                                      zijn, hoe meer
                                                                      infraroodstraling
                                                                      en warmte er naar
                                                                      de aarde wordt
                                                                      teruggekaatst.
                                                                      Daardoor warmt
                                                                      de aare op.
Zomersmog
   ontstaat door een combinatie van
  warmte, uitstoot van afvalgassen en
  chemische reacties in de atmosfeer.
Resultaat is een dikke witte mist: smoke-
            and-fog, of smog.

                        Emissie
                       Uitstoot van uitlaatgassen uit de motoren van
                       vliegtuigen, auto`s etc. en de schoorstenen van
                       huishoudens, fabrieken en elektriciteitscentrales.
Ozonlaag
   De laag, hoog in de
    atmosfeer
    (stratosfeer), waarin de
    aanwezige ozon (O3)
    de meeste ultraviolette
    straling van de zon
    absorbeert, waardoor
    het leven op aarde niet
    beschadigd wordt.
Ministerie van VROM




   Het ministerie van Volkshuisvesting, Ruimtelijke Ordening en Milieubeheer (VROM)
    was het Nederlandse ministerie voor zaken betreffende huisvesting, de ruimtelijke
    ordening en het beheer van het milieu.

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Gamma project

  • 1. GAMMA Project Vliegverkeer en Het broeikaseffect in een notendop My Linh Nguyen 3V2
  • 2. Broeikasgassen  Atmosfeer De atmosfeer is een dunne deken van lucht die de aarde bedekt. Deze luchtige deken, ook wel dampkring genoemd, houdt onze planeet op Zonnestralen gaan door een comfortabele temperatuur de atmosfeer (ongeveer 15 graden). De broeikasgassen laten een deel van de Het aardoppervlak infraroodstraling neemt de zonne door, maar kaatsen energie op, maar ook een deel terug stuurt ook naar de aarde. Hoe infraroodstralen meer terug de atmosfeer broeikasgassen er in zijn, hoe meer infraroodstraling en warmte er naar de aarde wordt teruggekaatst. Daardoor warmt de aare op.
  • 3. Zomersmog ontstaat door een combinatie van warmte, uitstoot van afvalgassen en chemische reacties in de atmosfeer. Resultaat is een dikke witte mist: smoke- and-fog, of smog.  Emissie Uitstoot van uitlaatgassen uit de motoren van vliegtuigen, auto`s etc. en de schoorstenen van huishoudens, fabrieken en elektriciteitscentrales.
  • 4. Ozonlaag  De laag, hoog in de atmosfeer (stratosfeer), waarin de aanwezige ozon (O3) de meeste ultraviolette straling van de zon absorbeert, waardoor het leven op aarde niet beschadigd wordt.
  • 5. Ministerie van VROM  Het ministerie van Volkshuisvesting, Ruimtelijke Ordening en Milieubeheer (VROM) was het Nederlandse ministerie voor zaken betreffende huisvesting, de ruimtelijke ordening en het beheer van het milieu.