// lecture 04 Flashcards

1
Q

sea level rise since 1880 has been about:

A

225 mm (22 cm or ~9 in)

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2
Q

these don’t contribute to sea level rise:

A

sea ice and ice shelves (connected to ice sheets, but floating on ocean).

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3
Q

these contribute to sea level rise:

A
  • thermal expansion of sea water - water expands when it warms and is the main contributor of sea level rise so far.
  • mountain glaciers.
  • ice sheets (Greenland and Antarctica).
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4
Q

contribute only a tiny amount to sea level rise:

A

permafrost and snow cover.

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5
Q

natural influences on sea level:

A

tides, ocean currents, winds, tectonic activity (some are rising/falling).

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6
Q

tide gauges

A

are measuring sticks or sometimes floats in wells. always coastal and few long records.

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7
Q

TOPEX

A

Poseidon Radar Altimetry - instruments emit a short radar flash and measures the time-of-flight of its reflection from Earth 1,000 times per second. Measures sea level and ice sheet height.

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8
Q

addition of heat and addition of freshwater (land ice melting mostly) =

A

total sea level rise.

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9
Q

sea level rise 1993-2010 IPCC AR5:

A

thermal expansion 39%, mountain glaciers 27%, Greenland 12%, Antarctica ice sheet 9%, land water storage 13%, total 100%.

thermal expansion and mountain glaciers account for 2/3 of total sea level rise for this year period as well.

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10
Q

measuring the global oceans:

A

addition of heat (Argo) + addition of freshwater (Grace) = total sea level rise (Jason).

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11
Q

Exendable Bathyermographs (XBT)

A

helps monitor the ocean heat content. about 70 voluntary ships toss them overboard, about 14,000 each year. they measure down to 1500 m and have been in use since 1962.

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12
Q

the base of much of Greenland’s ice is

A

below sea level. was ice free about 15 million years ago when CO2 was 400-500 ppm.

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13
Q

Greenland ice is equivalent to a

A

~7 m rise in global sea level.

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14
Q

Mountain glaciers currently contribute

A

27% to rising sea levels. Greenland and Antarctica currently contribute 21%.

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15
Q

Recent estimates of sea level rise including increases in calving:

A
  • 0.5 - 1.4 m by considering past SLR to past warming dependence and used IPCC estimate of future warming.
  • accelerated but plausible dynamic thinning could give 0.8 - 2 m.
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16
Q

current best estimate for 2100 global sea level

A

will rise by 0.8 m. assumes business as usual, depends on location, and has an uncertainty of 30% or so.

17
Q

sea level rise is a very slow process.

A

takes an extremely long time to melt Greenland/Antarctica. In the long term, ice sheets will be the main problem, but this will take centuries to happen completely. In some places it has already started.

18
Q

11 of the 15 largest cities are

A

along coasts or estuaries.

19
Q

Population of people living with 1 m of sea level:

A

around 150 million.

20
Q

costs of sea level rise:

A

wetland loss, salinization of aquifers/crops, constructing barriers, and relocation.