Climate Lecture 5- Oceans and Climate Flashcards

1
Q

What can the ocean store?

A

Heat, water and carbon dioxide and this storage is greater than the atmosphere

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2
Q

How does global scale oceanic circulation transport water, heat and co2?

A

Horizontally over large distances at rates comparable to atmospheric rates.

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3
Q

Discuss the relation between oceanic and atmospheric exchange.

A

They exchange as much heat, water and carbon dioxide between them as each transports horizontally.

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4
Q

What is specific heat?

A

The amount of heat it takes to raise or lower the temperature of a kilogram of a substance by 1 degree.

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5
Q

Are oceans thermally conservative compared to land?

A

Yes, there are no large variations in temperature.

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6
Q

How much more heat is required to raise the temperature of water compared to air?

A

4x

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7
Q

What is specific heat capacity of water?

A

4180 J/Kg

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8
Q

What is specific heat capacity of air?

A

1005 J/Kg

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9
Q

What is specific heat capacity of dry soil?

A

800 J/Kg

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10
Q

What is specific heat capacity of wet soil?

A

1480 J/Kg

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11
Q

Discuss oceanic-atmospheric exchange in terms of mass.

A

Precipitation, evaporation and gases.
Salinity, cloud cover and ocean productivity

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12
Q

Discuss oceanic-atmospheric exchange in terms of heat.

A

Temperature and evaporation

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13
Q

Discuss oceanic-atmospheric exchange in terms of momentum (wind).

A

Currents

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14
Q

Does latent heat vary seasonally?

A

Yes, higher in NH in January and higher in SH in July

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15
Q

Discuss oceanic CO2 uptake (biological pump).

A

Biologically driven sequestration of carbon from the atmosphere to the ocean interior and seafloor sediments.
It is responsible for transforming dissolved inorganic carbon (DIC) into organic biomass and pumping it in particulate or dissolved form into the deep ocean.
There, carbon is stored for millions of years.
It is the part of the oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis, as well as the cycling of calcium carbonate (CaCO3) formed into shells
by certain organisms such as plankton and molluscs.

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16
Q

Discuss ocean acidification.

A

Oceans currently absorb approximately half of the CO2 produced by burning fossil fuel; put simply, climate change would be far worse if it were not for the oceans.
However, there is a cost; when CO2 dissolves in seawater it forms carbonic acid and as more CO2 is taken up by the oceans surface, the pH decreases, moving towards a less alkaline and therefore more acidic state.

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17
Q

Discuss the role of phytoplankton, DMS and CCN.

A

DMS= dimethyl sulphide
CCN= cloud condensation nuclei

Phytoplankton in the ocean produce DMS which rises into the atmosphere and can lead to the production of CCN which cause cooling (indirect light scattering by clouds)

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18
Q

Is the CLAWS hypothesis negative or positive feedback?

A

Negative

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19
Q

What is the CLAWS hypothesis?

A
  • Warmer temperatures mean higher phytoplankton growth and more DMS
  • More DMS means more CCN
  • Lots of cloud means that sunlight is reflected back into space, leading to cooling
  • Cooler temperatures mean lower phytoplankton growth and less DMS
  • Less DMS means less CCN
  • Fewer clouds means more sunlight reaches the earth which causes warming
  • Warmer temperatures mean higher phytoplankton growth and more DMS, etc.
20
Q

What does CLAWS stand for?

A

Charlson, Lovelock, Andreae and Warren

21
Q

Discuss the key components and changes of the ocean.

A

Key components and changes of the ocean and cryosphere, and their linkages in the Earth system through the global exchange of heat, water, and carbon in the ocean include sea
level rise, increasing ocean heat content and marine heat waves, increasing ocean oxygen loss and ocean acidification.
Climate change-related effects (increase/decrease) indicated by arrows in pictograms. Changes in the cryosphere include
the decline of Arctic sea ice extent, Antarctic and Greenland ice sheet mass loss, glacier mass loss, permafrost thaw, and decreasing
snow cover extent.

22
Q

How have observations of the ocean been completed over the years?

A

Historical sampling from buckets - evaporation on the dock could cause bias, only first few metres

Since 20th century more engine room intake temperatures- warming in room can cause bias, deeper sample than buckets

Hull mounted sensors- more accurate than engine room intake, depth of sensor depends on if the ship is light or loaded

23
Q

Is there a bias in voluntary observing ships collecting sst data?

A

Yes, NH bias

24
Q

What are argo floats?

A

Argo floats measure salinity to monitor the changing hydrological cycle and global volume of ice in our oceans.

Descend to drift depth for up to 3 hours, drift for around 3 days, descend to profile depth for up to 3h then behin profile than begin their ascent and then at surface interval collect GPS data and transmit data. Them repeat until battery death.

25
Has average SST increased?
Yes, most drastic in the top 700m
26
Has ocean heat content increased?
Yes, more profound closer to the surface. Some areas have lost heat however as seen in N Atlantic.
27
How much of warming which happened between 1971 and 2010 ocurred in the ocean?
More than 90%
28
What is increasing ocean heat content associated with?
Sea level rise Ocean heat waves Coral bleaching Melting of ocean-terminating glaciers and ice sheets around Greenland and Antarctica
29
Will heat stored in the ocean eventually be released?
Yes
30
What is heat-gain between 1993-2019 averaged over the full depth of the ocean?
0.55-0.79 watter per square metre (over 360 million square km)
31
Discuss surface ocean circulation patterns.
Warm currents in ocean circulation patterns occur to the west and flow anticlockwise in the SH and clockwise in the NH.
32
What are ocean gyres?
A gyre is a large system of rotating ocean currents.​​
33
Discuss equatorial and counter-currents?
The North and South equatorial currents are largely driven by the trade winds. The counter-current (CC) tends to return in the doldrums between the two trade wind belts where there is no wind resisting it. The location of the doldrums and counter-current (CC) varies somewhat with the season, but it's always north of the equator, between about 5º N and 15º N. Equatorial currents tend to flow westward.
34
What is Ekman's spiral?
Ekman's spiral indicates that each moving layer is deflected to the right of the overlying layer's movement; hence, the direction of water movement changes with increasing depth. As depth increases, the force transmitted from the driving wind declines and thus the speed of the resultant steady current decreases, hence the tapered spiral or Ekman Spiral.
35
Discuss Ekman current.
Ekman current is the surface current that develops from steady wind at the ocean surface. As wind blows over the ocean a surface current develops due to the drag at the wind-water interface. The surface current, under the Coriolis effect is deflected to the right (northern hemisphere). The Ekman current is transmitted to greater depths by viscous forces, each subsequent layer is forced by viscous forces (internal friction) to flow in the direction of the layer above. The Coriolis force will cause the deflection of the current to the right; thus, each subsequent layer as we go deeper is deflected even further to the right compared to the initial wind direction.
36
Discuss ET and upwelling.
Water transported away from the coast because of ET : a removal of mass Surface water replaced by upwelling of cold water
37
Where are areas of major upwelling?
Onshore dry climates Areas of upwelling cold water = stable atmosphere
38
Name three currents.
Canary current Humboldt (Peru) current Beneguela current - Africa
39
What can upwelling impact?
Temperature Salinity Phosphate concentrations Nitrate concentrations
40
What does MOC stand for?
Meridional overturning circulation
41
What produces North Atlantic Deep Water (NADW)?
Temperature and salinity differences
42
What are climatic impacts of Atlantic MOC shutdown?
The Atlantic Meridional Overturning Circulation (MOC) helps to maintain relatively mild temperatures in north- west Europe. Some observations suggest that the MOC has reduced in strength by up to 30% since the early 1990s. However, other studies disagree with this interpretation. Most climate models anticipate some reduction in strength of the MOC due to increased freshwater influence in high latitudes, but continue to show overall future warming of the UK climate. An abrupt MOC shutdown leading to rapid cooling remains a high-impact, low- probability event. There is low confidence that this will be an outcome of climate change
43
What produces deep ocean thermohaline circulation?
Contrasts in salinity and temperature Exerts a fundamental control on the climate of W Europe
44
What does global ocean circulation reflect the pattern of?
Global atmospheric circulation
45
How are ocean currents created?
Wind transfering kinetic energy to the ocean surface.
46
Does climate change alter the global mass balance of water?
Yes
47