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layers of atmosphere
troposphere → stratosphere → Mesosphere → Thermosphere → Exosphere
Tropospheric Ozone
VOC’s + NOx
cause of Earth’s seasons
the Earth’s tilt and the angle of the sun
stratospheric ozone
highly beneficial gas in the stratosphere
shields Earth’s surface from harmful UV radiation
UV-C
completely blocked by ozone layer
constructs Ozone from oxygen gas & oxygen
UV-B
majority absorbed by ozone layer
breaks ozone back to oxygen gas & oxygen
UV-A
UV that makes it past the ozone layer
harmful to skin
chlorofluorocarbons (CFCs)
type of halocarbon
nontoxic, nonflammable chemicals containing atoms of carbon, chlorine, and fluorine
refrigerators, fire extinguishers, propellants for spray cans, and cleaners for electronics
halocarbons
synthetic compounds derived from hydrocarbons where hydrogen atoms are replaced by atoms of chlorine or bromine
polar stratospheric clouds
clouds of ice crystals
provide surface for chemical reaction that changes chlorine in molecules into more active forms that do destroy ozone
Antarctic Spring
October
when ozone depletion is most evident
polar vortex
region in pole with intensified winds and cold temperatures
Process of CFCs in atmosphere
rise into stratosphere over 11-20 yrs
break down under high-energy UV radiation (activator)
each CFC molecule can last 65-385 yrs
Montreal protocol
allowed regulations on amounts of ODS’s (Ozone Depleting Substances) released
successful
Copenhagen Protocol
aiming to address climate change and reduce global greenhouse gas emissions, recognizing the need to limit global temperature rise to no more than 2 degrees Celsius
HFCs (hydrofluorocarbons)
created to replace CFC’s
saves ozone layer but acts as a greenhouse gas
drastic warming of the atmosphere
Kyoto Protocol
international treaty trying to reduce greenhouse gases
stricter regulated on developed countries
Paris Agreement Accord
international treaty trying to reduce greenhouse gases
same thing as Kyoto Protocol but it is more even/fairer between countries
Albedo Affect
white/light colors reflect heat/light
Oceans Role in Global Warming
oceans heating up =increased global warming
hotter oceans absorb less CO2
Clouds Role in Global Warming
warmer temps. create more clouds
thick, low clouds decrease surface temp.
thin, high clouds increase surface temp.
absorption/reflection of solar radiation (albedo affect)
Intergovernmental Panel on Climate Change (IPCC)
body that assesses the scientific basis of climate change, providing regular, comprehensive, and authoritative assessments on climate science knowledge for policymakers and the public
HIPPCO
Habitat destruction, degradation, and fragmentation
Invasive (nonnative) species
Population and resource use growth
Pollution
Climate change
Overexploitation
Ocean Acidification
carbonic acid “steals” carbonate needed by marine organisms for their shells
ocean absorbs heat & CO2
Colony Collapse Disorder
a phenomenon where the majority of worker bees in a honeybee colony disappear, leaving behind a queen, plenty of food, and a few nurse bees to care for the remaining immature bees
Bust meat
meat from poached animals
Convention on International Trade in Endangered Species (CITES)
an international agreement that aims to ensure international trade in wild animals and plants does not threaten their survival in the wild
Convention on Biological Diversity (CBD)
international legal instrument for "the conservation of biological diversity, the sustainable use of its components and the fair and equitable sharing of the benefits arising out of the utilization of genetic resources" that has been ratified by 196 nations
Endangered Species Act (ESA)
A U.S. law passed in 1973 designed to protect species that are at risk of extinction and the ecosystems on which they depend. The ESA allows the federal government to list species as endangered or threatened, prohibits the harming or trading of these species, and requires the development of recovery plans to help populations recover.
Weaknesses of ESA
mainly popular animals saved
funding pays for bureaucracy, not recovery
Accomplishments of ESA
Species listed only when in serious danger
takes decades to help endangered species
conditions for more than half of listed species are stable or improving
2010: spend only 9 cents per American
What ozone is created primarily by & equations
sunlight
O2 + UV-C → O + O
O + O2 → O3 + heat
ozone-oxygen-cycle
A natural process in the stratosphere where UV radiation breaks down O₂ into individual oxygen atoms, which then combine with O₂ to form ozone (O₃), and ozone is later broken down again by UV light, maintaining a balance.
continuous process because there is so much oxygen
“Leaky Bucket” of ozone creation
rate of creation = rate of destruction
long lasting effect of one atom of chlorine
one atom repeats reactions with all the oxygen, destroying many molecules of O3
when scientists started measuring ozone
1920’s
“ozone hole”
thinning of the ozone layer over the south pole
what happens when sun rises in Antarctic Spring (September)
light releases Cl atoms into stratosphere and ozone depleting begins
Primary Air pollutants
CO2
SO2
NOx
VOC
Secondary Air Pollutants
NOx + VOC →(sun) O3
SO2 + H2O → H2SO4 (sulfuric acid)
NO2 + H2O → HNO3 (nitric acid)
primary ozone depleting substances
CFCs
halons/halocarbons
bromide
chlorine
in stratosphere
greenhouse gases
gases that trap heat
gases that absorb heat radiated by the earth and then emit Infared radiation that warms the atmosphere
HCFC/CFC/HFC
CO2
H2O (vapor) - short residence in atmosphere
CH4
O3
N2O
Positive Feedback Loop
effect that increases/worsens the cause
ex. ice melting → reduced albedo effect → heating of ocean/water absorbs more heat → leads to more ice melting
Negative Feedback Loop
effect negates the cause
ex. homeostasis in the body
cold —(shaking)→ normal
hot —(sweating)→ normal
Global Warming Potential (GWP)
the ability to trap heat
heat from sun
infrared radiation trapped/retained in troposphere
biosphere
living part of Earth (all living things)
aerosols
causes global cooling
They reflect sunlight back into space and increase cloud formation, both of which reduce the amount of solar energy reaching Earth's surface.