Carbon Cycle and Climate Change Projections + Modelling Flashcards

1
Q

What is the Carbon Cycle?

A

Flow of carbon through the atmosphere, hydrosphere, terrestrial and marine biosphere, and lithosphere (NOT CRYOSPHERE)

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2
Q

Define the difference between a carbon sink and source?

A

A sink is any process that removes a GHG from the atmosphere and a source is any process that releases GHG into the atmosphere

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3
Q

What is a Reservoir of Carbon and what is another word for it?

A

A component of the climate system which has the capacity to store, accumulate, or release a substance
Other term: Pool

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4
Q

The stock is?

A

The absolute quantity of the substance held within a reservoir at a specified time

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5
Q

What are reservoirs measured in?

A

Petagrams (PgC)

1 PgC = quadrillion gC (10 to power of 15)

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6
Q

Since pre-industrial to anthropogenic times (now), what are some reservoirs that are showing changes in their stock levels?

A

Atmosphere: increase carbon stocks
(caused by fossil fuels, net land use change, ocean-atmosphere gas exchange, respiration and fire)
Intermediate and deep sea (LARGEST RESERVOIR): increase carbon stocks
Fossil fuel reserves: decrease carbon stocks
Vegetation: decrease carbon stocks

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7
Q

Finish this statistic: The Co2 emitted from human activities during the decade of 2010-2019 was distributed between three Earth system (reservoir):

A

46% accumulated in atmosphere
23% taken up by the ocean
31% stored by vegetation in terrestrial ecosystems

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8
Q

What are four major sources of global anthropogenic Co2 emissions? (Largest to smallest)
When and where was this statistic released?

A

Land use change
Gas
Oil
Coal

In 2021 in AR6

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9
Q

In 2022, the annual average atmospheric CO2 was:
In 1959, the annual average atmospheric CO2 was:
In 1750, the annual average atmospheric CO2 was:

A

418.57 ppm
315.98 ppm
280.00 ppm

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10
Q

GHGs Co2, Methane, and Nitrous Oxide increased from levels in 1750-2019 by:

A

47%, 156% and 23% respectively

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11
Q

What is a Carbon Cycle feedback?

A

Changes in the properties of the land and ocean carbon cycle in response to climate change, such as to temperature and circulation or photosynthesis and soil microbial respiration

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12
Q

What are shared socio-economic pathways?

A

Illustrative scenarios covering range of possible future development of anthropogenic drivers of climate change

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13
Q

SSPs start in __ and include

A

2015

Scenarios with high and very high GHG emissions, double from current levels (SSP5-8.5 2050 & SSP3-7.0 2100)

Scenarios with intermediate GHG emissions, remaining around current levels (SSP2-4.5)

Scenarios with very low and low GHG emissions, declining to net zero around or after 2050 (SSP1-2.6 around 2050 and SSP1-1.9 after 2050)

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14
Q

What is a climate model?

A

Qualitative or quantitative representation of the climate system - properties of its components, interactions and feedback processes

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15
Q

Projects are computed with the…

A

Aid of a model, conditional on assumptions concerning future developments that may or may not be realised

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16
Q

TEMPERATURE:
Global surface temperatures will increase until ___ under all emission scenarios

A

Mid-century

17
Q

Relative to a 1850-1900 baseline, what are the projected increases in global surface temperature for each scenario at 2100?

A

SSP1-1.9 = 1.5C
SSP1-2.6 = 2C
SSP2-4.5 = 2.5C
SSP3-7.0 = 4C
SSP5-8.5 = 5C

18
Q

Land/ocean warm more than land/ocean and the arctic and antarctica/tropics warm more than the arctic and antarctica/tropics

A

Land
Ocean
Arctic and Antarctica
Tropics

19
Q

Precipitation is likely to decrease/increase over… but increase/decrease over…

A

Increase
- High latitudes
- Equatorial pacific
- Monsoon regions

Decrease
- Subtropics

20
Q

Under scenarios with increasing Co2 emissions, the ocean and land carbon sinks are…

A

projected to be less effective at slowing accumulation of Co2 in the atmosphere

SSP1-1.9 70% taken up
SSP1-2.6 65% taken up
SSP2-4.5 54% taken up
SSP3-7.0 44% taken up
SSP5-8.5 38% taken up

21
Q

What changes are irreversible for centuries to millennia ?

A

Loss of ice sheets, and glaciers
Global sea level