climate change final exam Flashcards
what word must you put before sea levl rise relating to water
eustatic sea levelrise
whats another word for flooded
inunduated
when is the maldives expected to be mostly inunduated + AO2
- 2100
- this is significant as its a rapid change / near future
what % of toruist go for its white sand beaches
60%
whats teh highest point in the maldives
2.4 m above sea level
whats teh average height above sea levl in teh maldives
1.2 m (4 feet)
how muc are sea levls expected to rise by 2100 due to eusttic change
- 0.8m - 2m
what % of the maldives GDP is tourism
- 70%
whats teh maldives population + AO2 comment
- 600,000 - small compared to other countries but significant if all made refugrees by 2100
whats the median age in the maldives + AO2 coment
30 years - significant as young working age popualtion
how many air portis in the maldives are within 50m of the coast
3
how to spell primarily
primarily
what is the fact that teh artci is walming quicker tahn teh rest of teh world called
artic amplification
what has been the significance of sea level rise on the holderness coast in england ? + link
- coastal retreat from increse storm events has becoem rapid
- fasted retreating coastline in europe
- 2m / yr
- 29 villages have been lost to the sea - ( libks to place and coats)
how much is global water vapor expeceted to increse besue of cliamte change and what doe sthis link to
- 1%-2% a decade
- the water and carbon cycle cretig a possitive feedback loop with climate cahbeg as its a GHG
whats a significnat thing did brazil agree to at cap 26
to end defforestaion by 2030
1. already rates have decresed from 17,500 from 1870-23013 to 7,500 in 2017-18
list teh ways we can measure/reconstruct past climate change
- ice cores
- lake sediment ( pollen and beatals)
- fossils
- dendrochronography
- marine sediment
what are tree rings to reconstruct climate change also known as
dendro chronography
expalin demdrochronography + give advantages and limitations
- a tree grows a ne wring every year
- the rings are the cambian layer ( th elayer between teh bark and the wood and the bark
- the conditions of the enviroment determine how big the cambrian layer wil grow each year
- for exaple walmer and wetter years the tree will growmore and there will be more cell growth in this layer and a larger ring
- this means that by cutting trees down we are able to tell what time climate was like anually and how it has changed dating back a rellativly long time,
AO2
* despite this, not all trees form regualr rings annualy ( e.g troppical and evergreenrings grow very irregualrly). this means we are only able to take readigns from certain areas and we arent sure if past readings are entirly accurate)
* the readings also dont date abck that long ( the oldest trees are just short of 5000 years old.
how do fossils tell us about
- corral
- coralls are very pasticular as to were tehy grow. they need walm consitions and sun light. if the temperture or dept of the water changes jsut a fraction they canot survive.
- if corral fossils are found in a particular regin we are able to estimate pretty presisely the conditions of the enviroment by dating teh fosill as well as the ight of sea levels.
AO2
* however this is assueming they need the same conditions as today
* movement: fossils can be moved both above ground and under the sea by a variety of methods such as tides, aeolian processes etc.
* they give us reading streching far far back into the pasts, hundreds of millians of years
1. the oldest chorla fossil record is 485 million years old
* loctaion specific - benifit and negtive
what is a tree ring also known as
cambiun layer
how does lake sediment (pollen and spores) tell us about past cliamtic conditions
- layers of sediment retreved from the bottom of lakes
- pollen is produced by palnts by teh millions and it has a hard outer shell so it fossalised easilly and covered by mud quickly
- differnt polen spores of plants are differnt and therefore we can trase differnt plants that grew at differnt times during the earths climatic history
- the type of plants that grow depend on the type of climatic condition eg aridity and temperture
- sicentist figure thsi out by looking at teh spores under a microsope
- ( the same applies for beatles as they fossalise well due to their hard outer shell), they are also very sensative to their enviromntal conditions
AO2
* there records date back around 100- millions of years
* rellatvly acurate
* may be hard to reteave
* loctaion specific - benifit and negtive
how can sea floor / marien sediemnt tell us about past climatic conditiosn
- Isotopes
- the ocean contains both oxogen 18 and 16 isotopes and oxogen 18 isotopes are heavier
- because of this when water evapertes of the ocean it contains the 0xegen-16
- therfore rain and snow also contain this isotope
- in colder conditions more presipitation falls as snow and gathers and remains at the polls.
- this means there is a much greater consentration of the isotope oxgen 18 in the ocean.
- (organismds that grow in the oceans during times like there absorb this isotope)
- now shells and sediment that formed during these times have higher consentrations of the element. as this is rellated to there being more ice and snow we know conditions where colder.
- therefore by dating these records we can take a pretty good guess at how past climatic condiiiiiitionds were
AO1
* can date back hundreds of millions of years
* hard to retreave
* presise
explain how we can recreate past climatic conditions through the use of icee cores
- ice in near the polls contains higher numbres of O16 iotopes in colder periods
- This is because havier O-18 water vapour condenses over mid walmer latitudes where as O16 condenses over latitudes frther noth and that are coller. thus water napour at the polls in increasingly depleeted of O18 in higheer latitudes so so is the ice as it freeses.
- the ices cores also contain a varriety of other records such as gass bubles that have the atmopheric compoition of the atmophere, blown ans and radeo active substances
- its easy to count shallow course by visable layers
AO2
* the numbre of climatic proxies s greater than in any other type of natral record (blown as, bubbles of atmospheric gass (carbon indicator) and raideoactive substancres)
* these date back along time ( 800,000 years ago is our oldest) ( this is still significnatly old)
* it is regular and presise
give an exaple of an ice cores record
- europen prodject
- atlantc ice core
- dating 800,000 years
- revealed the earth has expirences 8 glacial cycles in that time
whats teh oldest dendro chronography record we ahve
- “Methuselah,” which is estimated to be over 4,800 years old
what is the study of past climates known as
Paleoclimatic refers to the study or analysis of past climates
list teh natural forces that have driven past climate change
- milankovitch Cycles and orbital change
- solar outputs ( sun spots)
- natural greehouse gasses change
- plate tectonics ( continetal drift) ( volcnaic erruptions)
expalin milankovich cycles
- this is esentually orbital change that effects teh amount of solar radeoation reaching teh earths surface
Eccentricity (orbital variation) 100,000
* the amount the eaths orbit changes from circular
* the more eliptical the longer the earth stays away from the sun and the colder the cliamte becomes)
* glacials and interglacials - why they follow 100,000 year cycles
Obliquity (tilt) 41,000
* the more the tilt the more seasonal variation and the more ice will acumuate - more ice accumulation at the polls IN WINTER
Pressesion (wabble)22,000
* gradual movemnet of the earths axis in space ( affects seasonal variation)
explain the role of palet tectonics
- currents
- volcanic activerty
- movement in the earths tectonic plates ( specifically on convergent and divergent boundaries) causes magma, ash and gasses to be vented into the atmosphere.
- ash clouds case tempory blocking out of the sun - this is partyly responcible for the mini ice age in the 1800s
- sulfure dioxide gass also may be released, this rects with water in the atmophere to become an arosols which absorb sunlight and cause a cooling effect of the earths surface. ( however this is an effect that doesnt tend to last for more than a few mounths
- in the long term more CO2 and other green house gasses may be released ( however in rellativly small amounts) but this can cause walmoiing if there is signifiant tectonic activerty)
- Ocean circulation (Currents)
- contiental dirfit ( the seration of pangea) has caused currents to change as the hae to move arounf landmasses
- this effects the circulation of heat and moisture
- 5 million years ago N and S ameica joined where panama is today ( the isthmus). this closed of circulation between the atlantic and pacific oceans dirrecting heat towars the N hemousphere ( the gulf stream)
- Continental drift
- convergent plate bpundaries force land up and causes mountain rages to form. Continental drift has also resulted in more land acumulation in nothern regions
- the higher altitudes mean that tehse regions are cooler and precipitation will fall as snow and settle
- this snow collects over tiem and compresses causing polar ice caps and glaciers to form
- then an incresed abedo from these ice masses can cause a PME where the is more golabl cooling and ice formation
on an essay about past factors effectogn climate change whata re your paragraphs
- nagural green house gasses
- milakovitch cycles
- plate tectonics
- conclusion: milkovitch cycles as significant effct and significant without interdepences on other factors
what is human climate change known as
anthropogenic cliamte change
what is natural climate chnage often called
“natural variability”
what is the point where N and S america are joined called
- the isthmus
- where panama is today
how have natural GHG effect the earth’s climate in the past
- natural GHG in the atmophere liek carbon and methane fluctuate
- this is is actuly thought to be a product of tectonic activerty
- in the terntiary era tectonic movment cretaed extenive fold mountains such as teh rockies.
- the uplift caused incresed rainfall and chemical wethering. (the rain fall was charged with CO2). however it was the carbon in the runoff that incresed carbon in the oceans. this caused carbon fertalistaion of pytoplankton that removed carbon from the atmophere via photosynthesis
- when they died they world fall to the floor and carbon would be stored for the long term as see florr sediemn
- futhermore tectonic activerty can cause phtoplankton blooms though chnging currenst, this can dirrect heat and being up nutrients.
how is it thought that solar outputs are menat to have caused natural climatic changes
- 11 year cycles of sun spots
- there is a possitive correlation between the numbre of sun spots and solar output ( this means the earths climate will be walmer when there are more)
- 1800s mini ice age lines up with this
AO2
* minimal varation
* short term
what are ice house and greenhouse periods
- span over millions of years
- ice house- when there is ice overing the planet to a degree and coller tempertures ( now)
- hot house- usually high levels of CO2, walm climate and conditions and no ice.
what era are we in
Cenzoic( started 66 million years ago )
what epoch are we in + what acme before
- the holocine ( still ice house but much walmer)
- ( before - Pleistocene) ( ice house (lasting 2.6 million years)
what period are we in
- quaternary and what catorgrises it
1. The Quaternary is known for its fluctuating climate, with repeated cycles of glacial advances and retreats
2. contains teh pliestoncene and holocne
3. started 2.6 mill years go to now
what periods became before the quaternary
- neogene
- paleogene
when was the last glacial maxumum
- 20,000 years ago
- ( during the riss ( in europe around 108,000 years ago
when did the holocene inter glacial start
- 11,000 years ago
- rapid change during flandran transgression 6000 years ago
what era was before the quaternary
- Tertiary
- 66 million to 2.6 million years ago
- irregular
what was thougth to have causes the holocene
- pecifically variations in the tilt of Earth’s axis (obliquity), the shape of its orbit (eccentricity)
what islargly attributed to triggering teh quaternary period
- plate tectonics ( isthus of panama N and S america joinign)
what was thought to have triggered the last glacial period
photo plankton bloom and carbon firtlisation removing natural atmopheric gasses from the atmophere ( CO2) + obital change
whats teh consentration of carbon in the atmophere glacials vs interglacials
- 180ppm ( glacials )
- 280ppm
without GHG how much cooler would the earths surfce be on average
- the average surface temp would be -18C’
- now its 14C’
what cuased the glaciation of antartica primarily
- tectonic movemetn- continental drift
- movemt of land down under
- changing on curents
- 35 million years ago
how green house gasses cause walming
- ( must explain if your talking about GHG as a natural factor envolved inclimate change)
- short wave radeation from the sun
- soem radeation is refelcted back by the earths atmospheric albedo ( short wave)
- some is refected by the earths suface albedo ( short wave)
- most is absorbed by the surface and remitted
- most is re-radeated back to space as long wave radeation
- alot is absorbed by the atmosphere / GHG heating the atmophere and the suface of the earth further
whats teh most prominant GHG
water
what are the differnce sources of evidence that the world has walmed since the 19th centuary ?
- increse in surface and atmopheric tempertures
- shrinking of glaciers and ice sheets
- rising sea levels
- increaisng atmopheric water vapour
- decresing snow cover and sea ice
explain and evidence hwo glacial records provide evidence of climate change since the 19th centuary
- glaciers are retreating and disapearing
- more than 110 glaciers have disapeared from montanas glacier national park
- we also have historical records evidence of glacial retreat dating back to the 1850s
- sattelight images aslo can show this
- though these methods its clear that the rate as to wihc glaciers are meting is speeding up
- Muir Glacier in Alaska extensive studies and has seen massive retreat in recent years
evidence and explain how riding sea evels evidence climate change since the 19th centuary
- on average sea levls have risen 1-2.5 mm per year in the 1900 suggesting melting and lessrefreesing of the ice caps and well as more thermal expension
- recently this has risen to 3mm/ yr suggetsing the cliamte is even walming fatser and ice is melting faster and there is more thermal expansion of the oceans
- however this is not consistent. some places expirece isostaic reboun meanign that norways sea levels are actully decreasing. this has the potencial t make readings had
by whta means can sea levels rise
- thermal expension
- ice melting
how is decreasing snow and sea ice coverage evidence of global walming since the 19th centuary
- acoring to satteligth images artic sea ice is decreasing at around 13% a declaid acording from 1979-2020 this is up from 8% prior
- snow coverage in the NH has decresed 2% since 1966
how is increaed atmopheric water vapour a sign of increased walming in the 19th centuary + evidence
- increased temp - more evapotranspiration + rates of absolute humidity
- NASA’s NOAA polar orbiters - detected general increase in last few declaids 1-2% increase a decaid
how do sea, atmopheric and surface temperture evidence climate change
- NASA NOAA sattelight reads radeo waves emitted of the seas urface
- NASAs orbiting carbon observtry measures the effectivness of CO2 absorbtion from palnts by meausring changes in radeation
- atmophere has incresed 1 degrees since pre indutrial levels
list the reasons that anthroprogenic GHG emissions have incresed since the preindustical era
- land use change
- welth/ life style change
- populaton growth
- demand for energy
how mcuh GHE come from land use change
- 1/3
how much of the worlds forrests have been lost since 1700
25%
how does land use change contribute to a surge in emmisons
- 1/3 of all fossil fules released a year - scale
- defforestion
1. was a atural cardon sink that kep the caron cycle in a state of dynamic equalibrium ( 120 GT sequestrated each year to the 120 released via respirationa nd natural combustion) however now there is a satte of disequlibrium with far fewer orrest and much more carbon emitted = incresed GHE
2. man made forrest fires - huge emissions of COS - 1300ha in 2020 due to out of controle ones
1. 25% of forrests deforrested since preindustrail era - scale - farming
1. cattle ranching methain - x25 worse than carbon as GHG - urbanisation
1. more cars releasign CO2 and poltencially methain
2. urban heat iland effect
in any question about cliamte chamge what should you expalin once in your intro ?
the GHE ( once in intro)
how has demand for energy caused anthropogenic emission to tincrese
- there is a huge global demand for energy and buring fossil fuels is the cheapest msot effetcive way to produce this
- the demand is also growing and LIDC’s and EDC’s develope
- in 2019 around 34 Gt of Co2 was produced from burning fossil fuels soly for energy (73% of all GHG emitted that year came from this) - scale
expalin how rapid population growth is causign a spike in anthropogenic emissions
- 1 bill in 1800 to 8 bill today
- one of the main driving factors behind other resons
1. Increased energy consumption
2. Urbanization to house
3. Changes in land use and deforestation: As the population expands, there is a growing need for agricultural land, housing, and infrastructure
4. Increased waste generation: A growing population produces more waste, including municipal solid waste and industrial waste
5. Agricultural practices: Meeting the food demands of a growing population often requires changes in agricultural practices. Intensive agricultural methods, such as large-scale livestock production and increased use of synthetic fertilizers, can result in higher emissions of methane and nitrous oxide (N2O), both potent GHG - on average golbally a perso produces 5 metric tons of CO2 a year
explain how wealth and change inliving standard has lead to more anthropogenic emissions
- as LIDC’s and EDC’s develope there is a rise in consumer demands and globalisation, industry, urbanisation, farming and land use change to support that
- more meat consumption = more CH4 to the atmophere for instance
- more air travel besuse of bussiness expaning and more vactioing
- planes hav avery high foot print as they polute rigth in to the upper atmophere ( its hard to tell exectly how much)
- in teh us a house hodld produces around 50 tones of cO2 per year x5 higher than the golbal average
- more countries are begining to look more likly the us
the key this is that the rate of anthropogenic emissions are ……
anthropogentic emisiions have compounded since the 19th centuary and are oly just starting to slow
whats the ballence of anthropogenic emissions around the owrld and how has this changed inrecent history
- during industrialistion of the west from the 1800s to up to 1900 the NW specifically europe and north america dominated in terms of emissions
1. in 1960 europe produced around 4000MT of Co2 a year and in the same year NA produced 3000MT - in around the 1990s asia took over as the dominant poluters with their contrabutions rising expernentially
1. in 1990 their emission were around 6000MT compared to 8000 for europe and 4500T for NA
2. in 2011 their emission where 16,500MT compared to europes who had decresed to 4500MT adn NA at at 6000MT
3. africa and SA had also incresed to produce aorund 3000MT comined from basiclly non in 1960
4. now europe produce arounf 4000Mt a year vs asia 16,000MT ( srounf the same as 2011) = 48% of emission and NA 5500Mt
5. in teh uk in 2019 we produces 351.5 million tonnes (Mt), 3.9 per cent lower than 2018 (365.7 Mt)
6. 2,110.00 was the Maldives carbon (co2) emissions for 2019 was 2,110.00, a 0.48% increase from 2018.
how much is the earths albedo
- 1/3
what is outputted radeation called
terrestrail long wave
what % of suface radeoation is radeated abck to the surface
84%
what is global dimming
Global dimming is a phenomenon that refers to the gradual decrease in the amount of sunlight reaching the Earth’s surface. It is caused by an increased albedo in the atmosphere of light from Clouds and aerosols = colling effect
in 2016 how much did teh Uks GHG emissions fall
- 6%
- 52% drop in emissions from coal and 52% by fossil fuels
- however from natural gass emissions rose 12.5%
what are your case study countries for an AC and EDC’s contrabution to GHG emissions
- The Uk
- China
when will all teh uks coal power sations close
2025