9 - links between the water and carbon cycle ✅ Flashcards

1
Q

what is NOAA

A

US National Oceanic and Atmospheric Administration

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

what is the evidence for climate change (2)

A
  • In 2015, global mean surface temperature (GMST) was at a record +0.87 degrees C above the 1951-80 avg.
  • The 10 warmest years since 1880 have all been since 1998.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

what are scientific views of climate change (2)

A
  • Most climate scientists believe that global warming is caused by increasing greenhouse gas emissions. Humans are the main cause of this.
  • In the 5th climate change assessment of 2013, the IPCC scientists reported they were “virtually certain” that humans are to blame for “unequivocal” global warming.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

how have CO2 levels changed over time

A

rising since 1750 from a level of 280ppm to 406ppm at the start of 2017. This is a 45% increase.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

what human activities threaten the planet (3)

A

Population growth + economic development have led to a worldwide use of carbon-rich fossil fuels as an energy source
widespread deforestation, cement flatulence
the decomposition of organic wastes in landfill sites.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

what evidence has there been at real life places (3)

A
  • CO2 measurements have been taken every year at Mauna Loa since 1950 that show a 1-2ppm rise every single year.
  • Cores between 3 + 4km long extracted from the Vostok ice sheet in Antarctica contain air bubbles over half a million years old.
  • CO2 + methane concentrations are the highest for over 800,000 years.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

why has temperature (GMST) risen

A

Rising GMST (global mean surface temperature) is believed to be a product primarily of increases in the atmospheric carbon store

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

what is the impact of rising temperatures

A

has impacted on the Earth’s energy budget:

the state of balance between incoming solar radiation received by the atmosphere + Earth and the re-radiated heat, or reflected energy.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

what is the earth’s energy budget comprised of

A

of incoming solar energy, 6% is reflected by atmosphere, 20% reflected by clouds and 4% reflected from earth’s surface

16% is absorbed by atmosphere
3% is absorbed by clouds
and 51% is absorbed by land and oceans

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

explain shortwave solar radiation composition (3)

A
  • Approximately 31% is reflected by clouds, aerosols + gases in the atmosphere + by the land surface.
  • The remaining 69% is absorbed (50% by the Earth’s surface, especially by oceans).
  • 69% of this surface absorption is re-radiated as longwave radiation.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

what is longwave radiation

A

A large proportion of the longwave radiation emitted by the surface is absorbed by the atmosphere (clouds + greenhouse gases), where it is re-radiated back to the surface + into space.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

what is the impact of longwave radiation

A

By trapping longwave radiation the “natural greenhouse effect” gives a life-supporting average 15 degrees C temp. Without it the earth would average -18 degrees C.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

what is the effect of increasing carbon emissions (2)

A
  • Increasing carbon emissions (CO2 + methane) means more heat is being radiated back towards the surface, changing the energy budget.
  • More heat is being retained, resulting in a warmer, more energetic climate system.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

how do greenhouse gas emissions affect the water cycle

A

There are signs the world’s water cycle + oceans have already been affected by recent increases in the atmospheric carbon store:
The cryospheric storage has shrunk dramatically.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

how has precipitation changed (3)

A
  • warmth = more evaporation. Rainfall patterns change as the oceans warm up.
  • UK average rainfall has not changed since the 18th Century, but in the last 30 years more winter rainfall has fallen in heavier events.
  • Climate change predictions suggest UK total precipitation remains stable, but with more winter frontal rain + summer drought.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

how has high rainfall damaged the UK

A

Extreme high intensity rainfall in the UK in 2007 led to £3 billion worth of damages in floods. Higher temperatures may well mean more high intensity rainfall events.

17
Q

have extreme weather events changed (2)

A
  • Some scientists believe the probability of extreme weather events has significantly increased.
  • The 2012 “State of the Climate” report by the AMS showed an increasing consensus amongst leading scientists.
18
Q

what is the effect of higher precipitation on discharge

A
  • IPCC climate change predictions + UK meteorologists predict more intense winter floods with increased heavy rainfall events.
  • Lower river discharge levels may be seen in southern UK rivers in the summer.
  • As the soil water and groundwater stores may not fully recharge, river discharge may return to normal quicker after flood events in the future.
19
Q

how have sea levels changed over time (synoptic link!)

A
  • Sea levels have historically been higher in warmer periods due to thermal expansion. !Eustatic sea level rises are predicted!
  • Global sea levels have risen 200mm since 1900 at about 3mm per yr.
  • IPCC projections suggest a further global sea level rise of 260-820mm by the year 2100.
20
Q

what are the reasons for sea level rise

A

Glacier melt + permafrost meltwater will produce another metre of sea level rise by 2200 (even if CO2 emissions are cut dramatically).

21
Q

what would be the result of ice sheet melting in areas of the world
(synoptic)

A

The complete loss of the Greenland + Antarctic ice sheets would result in a Eustatic sea level rise of nearly 70 metres.

This will take hundreds or even thousands of years.

22
Q

how have carbon stores changes oceans

A
  • Estimates suggest a third of carbon released by humans into the atmosphere has already been absorbed by oceans.
  • Since 1750 the pH of the ocean’s surface has dropped by 0.1, a 30% change in acidity.
23
Q

how have oceans impacted carbon stores

A

If the oceans had not absorbed this carbon concentrations in the atmosphere would be even higher today.

24
Q

what are the effects of carbon in oceans

A

Increasing acidity could have potentially harmful effects on different marine species.

This might include impacts on metabolic rates, reproduction and immune systems.

25
Q

what has already occurred and what is projected to occur with precipitation

A

ALREADY- annual amount of precipitation unchanged, but more winter rainfall since 1980s.
PROJECTED- precipitation will become even more seasonal, but annual total will stay about the same.

26
Q

what has already occurred and what is projected to occur with UK runoff

A

ALREADY- annual runoff has increased in most parts of the UK, except the SE of England since the 1960s.
PROJECTED- uncertain due to debate about both rainfall and evaporation totals and balances.

27
Q

what has already occurred and what is projected to occur with UK runoff

A

ALREADY- increased frequency + magnitude of winter flooding since the 1980s.
PROJECTED- some studies project slightly increased flows + increased winter flooding, but not all.

28
Q

what has already occurred and what is projected to occur with evaporation

A

ALREADY- little reliable evidence to show how evaporation + transpiration have changed.
PROJECTED- potential evaporation will increase due to higher air temperatures this century.

29
Q

what are links between water and carbon cycles at the local scale

A
  • Carbon is transported in solution by rivers
  • Ecosystems function as stores of both water and carbon, influencing carbon transfers and water flow
  • Deforestation leads to increased overland flow, causing soil erosion and the loss of carbon storage capacity
  • Increasing atmospheric carbon concentrations are changing global climate and water cycle flows and stores.
30
Q

what are factors contributing to desertification

A

CLIMATE CHANGE FACTORS:
- rising carbon emissions and rising temps
- naturally occurring cyclical drought bringing lower and less reliable rainfall

LAND-USE FACTORS:
- over-grazing by cattle
- more wood biomass used for fuel and shelter by growing populations
- over-use of aquifers

PROCESS INTERACTIONS:
- vegetation loss
- reduced soil health
- overland flow and gullying
- soil removal
- NPP reduction

31
Q

how does desertification link the two cycles

A
  • Reduced vegetation cover may lead to reduced carbon sequestration in biomass (due to lower photosynthesis fixation of carbon) + reduced soil carbon.
  • Less vegetation cover may reduce the infiltration capacity of the remaining soil as it becomes crusted or compacted.
  • Excess run-off will occur in heavy rain, resulting in soil erosion and gullying.
  • Accelerated soil erosion will reduce soil carbon storage even more.
  • With less soil cover, ecosystem net primary productivity (NPP) will fall further
32
Q

how can cycle linkages be explored in the UK

A
  • Water and carbon cycles links can be explored at the local scale on floodplains, parks, small gardens or even patches of wasteland.
  • In autumn + winter, fallen leaves can be washed by heavy rainfall into gutters and sewers. You might investigate the approximate carbon content in an area.
33
Q

how can cycle linkages be explored within rivers

A
  • In drainage basins, overland flow and channel flow in the water cycle is responsible for transporting a large volume of carbon (stored as leaf litter biomass + soil organic matter) away from the land.
  • At Malham Cove, limestone pavements are weathered by carbonation and solution, with the released carbon being transported away by rivers.