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