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a body of knowledge and is what we know about the natural world |
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A proposed explanation for a narrow set of phenomena |
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Broad explainations for a wide range of phenomena |
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Plate tectonics is a ____ _____ |
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What is the mechanism behind plate tectonics
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-Changes density of the substance -Substances expand as they're heated -convection currents within the substance arise from differences in density |
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how does density relate to convection currents |
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slab pull- -Denser oceanic crust pulling lighter (& newer) crust down into mantle
less dense plates float on more dense plates
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What is the difference between exponential growth model and logistic growth model?
Exponential |
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is the graph showing population growth growing endlessly at the point of ideal living conditions
screen shot in folder |
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uses the exponential growth model but has a function in it that makes the grapgh platu when it reaches K, which is the maximum population the environment can withhold |
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3 periods of human population growth |
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preagricultural period
agricultural period
industrial period
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this was caused by human migration
slowly over 1 million years
humans expanded into new territories and created tools |
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caused by the introduction of agriculture
stimulated human population growth
population grew rapidly over 7000 years
domestication of plants and animals
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caused by industrial revolution
increased food production
better sanitation and health
population grew rapidly in 3 centuries
our current period
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Main problem with rapid human population growth: |
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Area of land needed to supply resources consumed to absorb waste |
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how do ecological footprints vary between countries |
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size varies greatly between countries
compare US and Haiti US footprint is massive compared to Haiti (screenshot in folder) |
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what porportion of the average us citizen ecological footprint comes from food and energy |
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-Made up of elements -Anything that takes up space and has mass |
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-Formed when two or more atoms join together chemically -Elements properties depend on the structure of its atoms
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Two atoms of an element that differ in number of neutrons |
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Smallest unit of matter that still retains the properties of an element |
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column (number of electron is outer shell)
row (number of shells) |
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atoms share the electron equally |
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unequal sharing of electron
the atoms that has a higher electronegativity holds electron more |
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is an atom’s attraction for the electrons in a covalent bond
The more electronegative an atom, the more strongly it pulls shared electrons toward itself
An atom is more electronegative the more electrons it has in its outer shell |
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A covalent bond is the sharing of a pair of valence electrons by two atoms, the shared electrons count as part of each atom’s valence shell |
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Valaence electrons are those in the outermost shell (valence shell) |
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single and double covalent bonds |
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a single covalent bond or single bond is the sharing of one pair of valence electrons a, c and d
a double covalent bond double bond is the sharing of two pairs of valence electrons
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(between atom) atoms sometimes strip electrons from their bonding partners |
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•Ionization energy – amount of energy required to remove an electron from an atom |
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•Electron affinity – amount of energy released when an electron is added to form a negative ion |
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left side of periodic table
(screenshot in folder) |
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right of periodic table
Screenshot in folder |
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after the transfer of an electron in the ionic bond what happens |
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the atoms have a charge and become either a cation or a anion |
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the atom that loses a electron becomes a |
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the atom that loses a electron becomes a |
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•Form when a hydrogen atom covalently bonded to one electronegative atom is also attracted to another electronegative atom (between polar molecules)
example is between water and ammonia (H2O and NH3) |
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what percentage of earths water in in ocean seas and bays |
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% of freshwater in ice caps glaciers and permanent snow |
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% of freshwater in groundwater |
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% of freshwater in freshwater lakes
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% of freshwater in atmosphere |
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% of fresh water in rivers |
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water is most dense in what state |
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water that fills open spaces and cracks in the soil, sediment, and rocks beneath earth’s surface |
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level of ground water where below is 100% saturated
look at screenshots
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Permeable layer transporting groundwater |
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what affects infiltration rate |
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porosity-percentage of material pore space
permeability- how well pore space is connected
shape of material- angular or rounded
sorting of material- well or poorly sorted
packing of the material- loosely or tightly packed |
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discharge is greater than recharge |
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how have we modified the groundwater and implications from this |
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pulling out drinking water from groundwater
contamination- surface run off point source pollution
subsidence- Combination of excessive withdrawal and poorly consolidated sediment
saltwater intrusion- salt water gets into groundwater
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flowing water Begin at high elevation point (mountain, hill)
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Type of pollution where you can trace it back to source |
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Type of pollution where you cannot tract it back to source(s) |
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Useful indicator species bc: -they are critical components of the food web -the community reflects cumulative impacts of pollution -easy to sample and identify |
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Tolerance values reflect an invertebrates tolerance of organic ___________ |
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BI is 0-10 0 is (least/most) tolerant to pollutants 10 is (least/most) tolerant to pollutants |
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Established the basic structure for regulating pollutant discharges into the waters of the United States. |
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what Decrease with stream order/longitudinal flow |
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what Increases with stream order/longitudinal flow |
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Channel width, discharge, sediment storage |
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amount of nutrients stored
theyre all nutrient pools |
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movement of nutrients between pools (transfer) |
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more nutrients coming in than out |
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more nutrients leaving than coming in |
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first law of thermodynamics |
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Energy is neither created nor destroyed, it changes from one form to another |
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second law of thermodynamics |
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Energy transformations are not 100% efficient |
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flicking a light switch loses energy along the process |
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stored energy and the energy of position |
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environmental costs with mountain top mining and valley fills
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Loss of topsoil, decreased infiltration
burial of headwater streams
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What proportion of US energy consumption is renewable energy? |
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Why do we not use renewables to a greater extent? |
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unfamiliar technologies
economies of scale
externilized costs if fossil fuels result in low prices
limited consumer knowledge
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advantages and disadvantages of wind energy |
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a-No fuel CO2 emission free Domestic
dis- Intermittent, Aesthetics, Impacts to wildlife
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advantages and disadvantages of solar power
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•Advantages –Free –Renewable –Few environmental costs
•Disadvantages –Intermittent –Regional |
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advantages and disadvantages of hydropower |
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Advantages
No Fuel
Relatively inexpensive
Also provides flood control and water storage
Continuous electricity
Disadvantages
Loss of land
Ecosystem disruption
Initial cost |
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Environmental costs associated with natural gas extraction |
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Definition
causes earthquakes
contaminates water
air emissions from equipment
noise pollution
habitat fragmentation
once done plugged and abandoned
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How well a surface reflects solar energy |
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When radiation is sent directly backward from a surface; the fraction of radiation reflected back is ALBEDO |
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Carbon cycle has been altered by |
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the burning of coal oil and natural gas since the industrial revolution |
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combustion reactants and products |
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reactants- hydrocarbon and oxygen
products - carbon dioxide and water
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Short-term changes in the atmosphere (minutes-months) |
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Description of long-term patterns of weather in a particular are |
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tropical zone
temperate zone
polar zone |
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23.5s to 23.5n is the tropical zone warm year round |
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23.5s and n to 66.5 s and n is the temperate zone sunlight not as constant not as hot year round |
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66.5 s and n to 90 s and north polar zone cold year round |
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eccentricity, obliquity, precession |
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earths orbital eccentricity |
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the shape of the orbit around the sun changes which affects the earth-sun distance; the cycle takes about 100000 years |
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changes in the angle the Earth's axis makes with the plane of the Earth's orbit. The cycle that averages about 40000 years |
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Change in direction of Earth's axis or rotation, cycle averages 23,000 years. Current axial tilt is at 23.2 % |
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parts per million
out of a million |
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Nitrogen contains ___% of a dry atmosphere |
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Oxygen contains ___% of a dry atmosphere |
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Carbon dioxide contains ___% of a dry atmosphere |
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Argon contains ___% of a dry atmosphere
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what kind of waves do the sun emit? |
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_____% of incoming short wave radiation is reflected and scattered
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___% of incoming short wave radiation is absorbed |
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Absorbed energy is transformed into _____ energy |
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Most of the emitted long wave radiation warms the lower atmosphere, which in turn warms our planet's surface |
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what the greenhouse effect is difference in short wavelength coming in long wavelength leaving |
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long wavelength goes and gets trapped by a beneficial greenhouse effect life evolved under these conditions much colder without greenhouse effect the problem with it is that we are adding a ton to it so energy is getting trapped and temperatures are getting warmer
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most abundant greenhouse gas in atmosphere |
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albedo effect: indicated how well a surface reflects solar energy
0= everything absorbed
1=everything reflected
earth is at .3
open ocean .06 (it absorbed a lot)
bare sea ice is .5-.7 (reflected a lot)
snow covered sea ice is .9 (90% is reflected |
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make things bigger (warming of climate) |
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tend to minimize the effect of a disturbance and return to the normal state. |
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Do The Math Documentary - Divestment Plan |
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2 components 1. A freeze on new fossil fuel investments 2. Wind down existing fossil fuel investments in 5 years |
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1. How has sea level changed (rate)? |
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up 3.4 millimeters per year |
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3 numbers from do the math documentary |
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2 degrees c
2,795 gigations
565 gigations |
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How much the world has said it would be safe to let the planet warm (only # agreed w/ by politicians, world leaders, etc.)
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How much carbon we can put into the atmosphere and have a reasonable chance of staying below 2 degree change |
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How much carbon the world's fossil fuel industry has in their reserves |
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Represents the change in concentration of CO2 (steady lows and highs throughout the years, until recently it went sky high) |
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1. How much has temperature changed since the late 1800s? |
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1. How much has ocean warmed? |
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Ocean has warmed .302 ºF since 1969 |
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1. What is the trend in average global temperature since the late 1800s? |
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The annual temperature anomaly is ___ (up/down) 1º in comparison to average since 1880 |
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chemical energy from radiant energy (sun) |
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photosynthesis reactants and products |
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carbon dioxide + water >Light energy> carbohydrates + oxygen |
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cellular respiration
and
formula |
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reactions and processes in the cell that create energy and waste
f: C6H12O6 + 6O2 --> 6H2O + 6CO2 + ATP |
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earths orbit in terms of northern hemisphere
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march equinox: nether pole tilts toward sun
June: NH tilts toward sun day longer than nights more sun
september equinox: nether poles tilts
December: winter equinox NH tilts away from sun less sunlight day shorter than night
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precipitacion wet and dry zones with equator
look at screen shot
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how ocean currents can affect climate |
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ocean currents formed by differences of temperature of water and salinity of the water. Salinity changes with amount of sunlight water received and all of this can affect the climate |
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how topography effects climate |
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-topography (mountains) mtn ranges force air to rise along the windward side of the range clouds form and precipitation falls. Little falls on the leeward side, dry air descends and warms, little rain falls here creating a rain shadow |
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what the greenhouse effect is difference in short wavelength coming in long wavelength leaving |
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Definition
long wavelength goes and gets trapped by a beneficial greenhouse effect life evolved under these conditions much colder without greenhouse effect the problem with it is that we are adding a ton to it so energy is getting trapped and temperatures are getting warmer |
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1. Know how greenhouse gasses trap heat (light absorption) |
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there are certain green house gases that absorbed the light and infared radiation and then emit energy back to earth "trapping gasses" warming the climate
these gases are carbon dioxide methane nitrous oxide sulfur hexafloride |
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Know how the average (10 year) growth rate in CO2 levels measured at Mauna Loa has changed since the late 50s |
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about .25 ppm Co2 increase per decade |
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Radiant energy: Chemical energy: |
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Radiant energy: electromagnetic energy that travels in waves of light Chemical energy: energy stored in bonds of atoms and molecules |
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How were atmospheric CO2 levels pre-1958 determined? |
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from air bubble trapped in polar ice cores |
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How are CO2 and global temperatures related? |
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increase in CO2=increase in global temperatures |
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The average (10yr) growth rate in CO2 levels measured at Mauna Loa
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past 10 years the average annual rate of increase is 2ppm, In the 50's it was less than 1ppm
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What does the Keeling curve represent? |
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Graph which plots the ongoing change in concentration of CO2 in Earth's atmosphere since 1958. Based on continuous measurements taken at the Mauna Loa Observatory in Hawaii- overall increasing trend.
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Why does the Keeling curve vary on an annual cycle? |
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Carbon dioxide levels drop during the Northern hemisphere spring and summer, when plants are taking CO2 out of the atmosphere to grow. In fall and winter, plants and leaves die off and decay, releasing CO2 back into the atmosphere causing a small spike. |
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What kinds of effects does ocean warming have on ocean food webs? |
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1. changing temperature affects how ecosystems function by affecting the performance of different species. 2. places where temperature rose are the same places where phytoplankton productivity declined.
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ocean warming effects on ice shelf loss |
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basal melt: melting of ice shelves from underneath. basal melt accounted for 55% of ALL Antarctic ice shelf mass loss form 2003-2008 |
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ocean warming effects on arctic sea ice |
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arctic sea ice is at its minimum during September. September Arctic sea ice is declining by 13.3% per decade |
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What impact might ocean warming have on energy from the sun reaching the earth? |
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open ocean: 94% being absorbed, more energy being absorbed results in more warming (positive feedback), less sunlight is reflected.
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What is ocean acidification and what problems does it pose? |
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increased atmospheric CO2 has led to acidification of surface ocean waters (decrease in pH), more H+ makes the water more acidic, water buffering removed carbonate ions and decrease availability to calcifying organisms that make calcium carbonate shells.
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What proportion of renewables is made up of solar, wind, hydropower, and biomass? |
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Solar: 6%, Wind: 21%, Hydropower: 24%, Biomass: 46%, Geothermal: 2%
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118 gigatonnes per year ice loss rate
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281 gigatonnes per year greenland mass loss rate |
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13.3% decline each decade |
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is it how much heat something can absorb before it raise in temperature by 1 degrees
specific heat of an object regardless of mass
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Heat capacity of water (greater or less than) heat capacity of atmosphere |
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Be able to explain the exchange between groundwater and surface water- |
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knowing that what we do to impact groundwater has an effect on surface water and vice versa |
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Short lived
Only flows during and after precipitation and has very little connection to groundwater
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Has characteristics of both ephemeral flow and perennial |
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Flows throughout the year and is well connected to groundwater
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mechanism behind plate tectonics |
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slab pull thermal convection |
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(Transfer)Movement of nutrients between pools
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