Chapter 6: climate change and oceans Flashcards

1
Q

concentration of deissolved salts in water

A
  • NaCl (sodium chloride)
  • magnesium
  • calsium
  • potasium
  • sulfate
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2
Q

the average salinity of ocean is

A

35 ppt (parts per thousand)

35 grams of salt dissolved in 1000g of sea water

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3
Q

properties of water that are changed by

A

having salt in it

  • salt makes sea water more dense than fresh water
  • salty water needs to be colder than fresh water before it freezes
    • freezing point of fresh water is 0c
    • freezing point of sea water is -2 c
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4
Q

ocean salinity change due to climate change:

impacts on anthropogenic CC on ocean

A
  • rise in sst
  • sea level rise
  • acidification
  • salinity variations (indirect impact of CC)
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5
Q

cause of changed salinity

A
  • evaporation (inc)
  • precipitation (dec)
  • fresh water from river discharge (dec)
  • ocean currents
    • from less saline oceans (dec)
    • from saline oceans (inc)
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6
Q

global salinity is effected by

A
  • hydrological cycle
    • evaporation rates
    • precipitation rates
    • river discharge
  • ocean currents

climate change will result in stronger hydrological cycle

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7
Q

how global warming effects salinity

A
  • global warming
    • stronger hydrological cycle
      • arid regions
        • become dryer
          • more evaporation
            • salinity increase
      • wet regions
        • become wetter
          • more precipitation
            • salinity decrease
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8
Q

ocean acidification

A

oceans take up CO2 from the atmosphere (absorb 1/3 of the atmospheric CO2) since the industrial revolution

  • reduce global warming
  • cause changes in ocean chemistry (carbonate chemistry)
    • ocean acidification
    • DIC (dissolved inorganic carbons)
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9
Q

Carbonate chemistry of sea water

A
  • atmospheric CO2 dissolve in sea water
    • aquous CO2
      • carbonic acid
        • rapidly dissociate to produce photons and
        • bicarbonate ionns
          • dissociate into
            • carbonate ions and photons
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10
Q
  • atmospheric CO2 dissolve in sea water
    • aquous CO2
      • carbonic acid
A

CO2 (aq) + H2O –> H2CO3

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11
Q

carbonic acid

  • rapidly dissociate to produce photons and
  • bicarbonate ionns
A

H2CO3 <—> HCO3- + H+

(carbonic acid) <—–> (bicarbonate ions) + (photons)

GIVE RISE TO PHOTONS

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12
Q
  • bicarbonate ionns
    • dissociate into
      • carbonate ions and photons
A

HCO3- <——> CO32- + H+

(bicarbonate ions) <—–> carbonate ions + photons

GIVE RISE TO PHOTONS

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13
Q

PH is defined as

A

PH= -log10 [H+]

the increase in H+ photons will reduce the PH value of the sea water making it more acidic when (PH value <7)

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14
Q

compare the PH values from the past and now

A

over the past 300 million years = 8.2

current value of PH = 8.1

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15
Q

for a reduction of 0.1 in PH value, what is the corresponding change in [H+] photons

A

H+ = antilog10 (PH)

H+= 108.1

H+ 8.1 = 125892541.2

H+ 8.2= 158480319.2

( (H8.2 - H8.1)/H8.1 )x 100 = 25.9% (increasing acidity)

this is becaue PH sscale is not linear

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16
Q

the total DIC in sea water is defined as

A

DIC = [CO2] + [HCO3-] + [CO3 2-]

carbon dioxide + bicarbonate + carbonate

17
Q

distribution of DIC

A

the distribution between the three species varies between PH of sea water

18
Q

for PH = 8.1

A

[CO2] : [HCO3-] : [CO32-]

1 : 100 : 10

19
Q

as more CO2 is added to sea water

A
  • PH decreases
  • the balance between the three carbonate species also change
    • CO2 (aq) and HCO3- increase
    • CO32- decrease

(this is an indication of anthropogenic ocean acidification

20
Q

projected ocean acidification

A
  • anthropogenic CO2 emissions cause
    • warming of oceans
      • 2 to 4 c by the end of 21st century
    • increase in ocean carbon content
      • ocean acidification
        • reduction in marine carbonate
      • reduction of dissolved neutrients in the surface
21
Q

sea level rise is caused by

A
  • thermal expansion
  • additional water flow from ice melting
22
Q

sea level rise consequence

A

due to increase of sea level rise

  • low lying areas will have more frequent flooding
  • very low lying areas could be submerged campletely
  • wil change coastal wet lands and harm coastal ecosystems
    • mongroov forests
    • coral refs
23
Q

sea level rise projection

A
  • over the past 100 years average sea level rise in 7 inches
  • by the end of 21st century, 7-23 inches additional rise expected