Weeks 6 & 7 - Sea level change Flashcards

1
Q

What is coastal squeeze?

A

the loss of natural habitats or deterioration of their quality arising from anthropogenic structures or actions, preventing the landward transgression of those habitats that would otherwise naturally occur in response to sea level rise in conjunction with other coastal processes

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2
Q

what are the terrestrial factors that influence sea level rise

A

terrestrial water storage, extraction of groundwater, building of reservoirs, changes in runoff, and seepage into aquifers

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3
Q

what are the factors that influence sea level rise at the shore

A

subsidence in river delta region, land movements, tectonic displacements

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4
Q

what are the factors that influence sea level rise in the ocean

A

surface and deep ocean circulation changes, storm surges
as the ocean warms, the water expands
exchange of the water stored on land by glaciers and ice sheets with ocean water

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5
Q

what is ocean thermal expansion

A

The warming of Earth is primarily due to accumulation of heat-trapping greenhouse gases, and more than 90 percent of this trapped heat is absorbed by the oceans. As this heat is absorbed, ocean temperatures rise and water expands.

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6
Q

how does Greenland and Antarctica contribute to sea level rise

A

Greenland and Antarctica contain giant ice sheets that are also considered glaciers. As temperatures rise, glaciers melt faster than they accumulate new snow. As these ice sheets and glaciers melt, the water eventually runs into the ocean, causing sea level to rise.

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7
Q

where can we get data on sea level rise?

A

instrumental data - tidal gauges which are located at the shoreline which measure the average level of the sea each year
proxy records - e.g., sedimentary records of coastal change and sea level from which we can get quantitative info on sea level
more recent data from satellites - geostationary satellites which are able to regularly measure the level of the sea
future projections - from global atmospheric models and global climate models where we have looked at how temperature leads to ice melt and thermal expansion of the oceans

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8
Q

describe the general trend in SLR across the late Holocene period

A

up to about the mid 1800s, SL was oscillating - it was variable but not increasing significantly (less than 1mm per year)
mid 1800s - present day: acceleration from about 1mm per year to about 3mm per year
future projections: potential for an acceleration in the rate of rising even further (4-6mm per year). there are IPCC projections for very high emissions (RCP8.5 scenario) and very low emissions (RCP2.6 scenario)

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9
Q

why is SLR a risk to infrastructure?

A

so much of the worlds population located around the coastline
majority of large mega-cities are at the coast

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10
Q

why are cities drawn to the coast?

A

international travel possible
exchange of goods via shipping
lots of flat land for agriculture or industry development
fisheries
tourism

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11
Q

what paper suggests ‘realistic’ statistics of the % of world population affected by SLR?

A

Lichter et al. (2011):
12/13% of worlds population would be effected by SLR and increased storm surges
however, w/ todays population numbers, that is still over 1 billion people

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12
Q

what happens as a result of using sea defences in terms of coastal squeeze?

A

as sea level rises, our salt marshes and mangroves start to disappear as a result of the increasing hydroperiod that takes place
normal process would be: there would be inland migration of these environments therefore no net loss of biodiversity (enables the shoreline to be dynamic)
however, by protecting low lying infrastructure using sea defences: lose marine wetlands, reed swamps, salt marshes - left w mud flats and sand flats.

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13
Q

hurricanes cause storm surges of around 5/6 m whereas predictions of SLR show an increase of 4-6mm per year. why is SLR seen as such as big problem if these numbers are small in comparison to storm surges?

A

SLR is a permanent phenomena that will lead to permanent change whereas storms, whilst still damaging, are only temporary
therefore coastlines have a recovery time in between storms
but no such recovery time in terms of SLR

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14
Q

what is Reverse Uniformitarianism?

A

where we look into the past to provide context for what can happen in the future

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15
Q

what are tide gauges?

A

instruments that are located at the shoreline
made up of a vertical tube which sits between the range of the high tide and the low tide
within the tube, the water level can rise and fall w the tide, and there is a float which is connected to a recorder
as the tide rises and falls, the level of the sea is recorded
average sea level per year
can plot yearly trends

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16
Q

what is a pressure gauge?

A

sits below the water level and measures how much water is above it
from that we can get the tidal level

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17
Q

what is a radar gauge?

A

sits above the water level and takes measurements of how close the tidal level is to the instrument

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18
Q

what is an advantage of using tidal gauges?

A

give us extremely accurate measurements of sea level across a period of time

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19
Q

what are the limitations of using tidal gauges?

A

we have lots of them to measure current SL but as we move further into the past there is less and less data because fewer were used
most tide gauge records are less than about 30-50 yrs in duration
therefore data from it is not uniformly distributed
most of the data comes from the mid latitudes because until recently that’s where most of tidal gauges where located
therefore data in inconsistent on a global scale (spatial limitation)

20
Q

data from tidal gauges in ports around the world show variability. what causes this variability?

A

tide gauge might be close to a big river - if there is a lot of rainfall that year, sea level will appear higher due to high levels of river discharge, true for the opposite (dry year = local sea level lower)
oceanographic effects - e.g., El Nino can influence sea level
storms - stormy year = low pressure systems = less atmospheric pressure pushing down on sea = higher sea level

21
Q

what paper shows evidence of accelerated sea level rise using tide gauges?

A

Woodworth et al., 2011:
evidence from ports such as Amsterdam, Liverpool, Stockholm
acceleration visible from mid-1800s
consistent w effects from the industrial revolution (increased co2 conc in atmosphere)
industrial revolution was a bit earlier (start mid-1700s) therefore this is evidence of a response time: response of sea level system to global atmospheric co2 levels and temperature rise has a delay (~30yrs) because ice melt and thermal expansion has to occur first

22
Q

what paper shows an inconsistency in SLR from tidal gauge data?

A

Wahl et al. (2013)
SL in North Sea has been rising however, Stockholm: SLR is decreasing
because: land can undergo uplift or subsidence as a result of tectonic movements or ice loading
tide gauge only gives us relative sea level - level of the sea relative to the land
land can move as well as the sea - this is what is happening here
Stockholm is undergoing uplift as a result of Last Glacial Maximum
rate of glacial isostatic rebound is faster than the rate of SLR (therefore looks like SL is falling)

23
Q

what is Satellite Altimetry?

A

satellites can measure the level of the sea without experiencing problems from land level movements (as they are not tethered to the land)

24
Q

what is the difference between data of SLR from tidal gauges and satellites?

A

Satellites give us data on eustatic SLR whereas tide gauges give us data on relative SLR which can sometimes result from isostatic land level change

25
what type of change do future projections (global climate models) of SLR show?
eustatic
26
why are tide gauges helpful when we collect eustatic data from other sources e.g., satellites?
eustatic data needs to be downscaled to explain what it means locally e.g., if eustatic sea level rise is predicted to be 4-6mm per year what we see at the coastline will also be influenced by what the land is doing therefore, tide gauges are helpful at telling us what the land is doing relative to the sea
27
what is a problem with satellite data?
it is only ~30yrs in duration so if we want to use reverse uniformitarianism, we need to use other data sources
28
what are deep sea sediment records?
things that have been deposited below the level of the sea consistently for a significant period of time
29
what is morphological evidence of SLR?
raised beaches, raised marine terraces these used to be at sea level but have become raised as a result of either sea level change or land level change
30
where does morphological evidence of SLR come from?
as the coast erodes, cliff lines erode backwards and shore platforms extend in a landward direction if sea level falls, the shore platforms are covered by beach/dune sediments above the present sea level each shore platform can be related to a specific sea level at some time in the past i.e., we use the elevation of these platforms and date them dating used from: shell material (radio-carbon dating), mineral matter (luminescence dating)
31
what is sedimentary evidence of SLR?
pattern of sediments below the surface (stratigraphy) different layers of sediment can see if sediments have changed from terrestrial (e.g., peat deposits) to sediment found at marine sites (e.g., mud flats) each change in sediment represents a change in sea level
32
what paper is an example of using stratigraphy as evidence of SLR?
Shennan 1986: changes in stratigraphy from terrestrial to marine represent different tidal levels he said: if you looked at the overall transition between the coastal muds and the coastal peats (i.e., mineral matter to organic matter), that takes place at a tidal level which is somewhere half way between the mean high water spring tide and the highest astronomical tide (M') so the measurement of M' gives us the altitude of former sea level age: take organic matter above and use radio-carbon dating or mineral matter below and use luminescence dating
33
what did Fairbridge (1961) do?
created a 'eustatic curve' from sedimentary data of M' and other types of data to show past changes in SL important as it extended our knowledge on past SL from a few years ago to hundreds of thousands of years ago good example of reverse uniformitarianism
34
how are corals used as evidence SLR?
deep sea sediment records of coral fossils can be used altitude and age of the fossil determined collect many of these data to reconstruct past sea levels e.g., Fairbanks (1989)
35
what is a limitation of using reverse uniformitarianism of the early Holocene period to predict shoreline responses to future sea level rise?
past responses of the shoreline are entirely natural - shorelines can shift as a result of sea level rise whereas now, there is significant human imprint on our coastlines our coastlines may not have the same response to SLR because they are defended, inhabited etc
36
what is a problem of using data from sources that provide reverse uniformitarianism?
evidence from stratigraphic and geomorphic information stops at about 3000 yrs before present how do we connect the geological record to instrumental (present-day) record? i.e., data is missing
37
how can we fill the gap in data between the geological and instrumental record of SLR?
Ecological transfer functions: come from the presence of different foram and diatom species preserved in saltmarshes their distribution depends on: salinity, substrate type, hydroperiod taking a core sample of the sediment and looking at the distribution of species within the sample, we can see what type of an environment used to be there and from this can infer the tidal level example: Mills et al (2013) - using diatoms in the Mersey estuary to reconstruct past sea levels
38
how can global warming cause sea level to fall?
every mass has some kind of gravitational effect if we have a lot of mass in terms of an ice sheet sitting on the coastal bit of the crust, it will cause subsidence (glacio-isostatic loading) at the same time, that mass is attracting the ocean up towards it so, the ocean surface is higher because of the ice mass when the ice mass is lost, there will be a rebound response and less gravitational effect from that ice so, sea level will fall
39
in close proximity to ice masses, when the ice mass is lost - what will happen in terms of sea level?
loss of gravitational pull loss of loading on crust sea level will fall
40
what paper shows different scenarios of ice sheets melting and their effect on SLR?
Mitrovica et al (2001): 3 scenarios - Antarctica, Greenland, melting of mountain glaciers and ice sheets e.g., Antarctica melts: lose gravitational pull, lose glacial isostatic loading - close proximity to Antarctica = SL falls, higher rate of SLR further away i.e., local sea level fall but SLR further away
41
What do we have to take into account when we look at local SLR?
the land is it experiencing subsidence or uplift? example - North of UK is experiencing uplift whereas South is experiencing subsidence as a result of ice loading and rebound from 18,000 yrs ago e.g., we have 3mm SLR per year but Scotland also experiencing 1mm of uplift per year = rate is 2mm (rate of SLR is reduced) Shennan et al. (2012)
42
what factors are considered in future sea level rise models?
ocean thermal expansion glaciers and small ice caps Greenland Antarctica
43
What are uncertain contributions to sea level rise?
Groundwater extraction vs recharge - more is being taken out than being added Reservoirs and lakes – dams - adds to evaporative losses from the earth surface Deforestation & Wetland loss - less capacity for water to be held on earth surface Permafrost - changing frozen ground to water + slush which can then be added to sea level
44
what is the H++ scenario?
the IPCC projections of climate change and sea level rise have been accused of being conservative therefore the H++ scenario came about it is used to put forward unlikely scenarios that could still happen (i.e., extreme but plausible) UK: 93cm - 1.9m SLR by the end of 21st century
45
what is an alternative way of projecting sea level rise instead of climate models?
use trends that we have observed from data (semi-empirical projections) e.g., trends in tide gauge data can be projected example - Grinsted et al. (2015) use semi-empirical methods for 21st century RSL projections in northern Europe