Lecture iii - Anthropogenic causes of climate change Flashcards

1
Q

Describe natural greenhouse effect

A
  • naturally occurring ghg eg CO2, CH4, nitrous oxides help keep earth warm (maintain avg 15 C)
  • w/o natural ghg, avg temp wld b freezing -18 C
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2
Q

Why is present day climate becoming a concern?

A

-earth is in stage of rapid warming
- rate of increase of surface temp bcome more rapid/ has accelerated, rising on average
- called global warming/contemporary CC

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3
Q

Human-induced global warming of … deg C has…

A

1.1°C

spurred changes to earth’s climate, unprecedented in recent human history

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4
Q

Name characteristics of global warming

A
  • characteristics changing include temp, precipitat n, snow cover & extreme weather events
  • droughts bcome more severe (intense) & frequent in some areas
  • rivers melt earlier in spring
  • ice sheets (Greenland & Antartic) melt earlier in spring
    => extreme flooding events (high magnitude, higher frequency)
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5
Q

Explain enhanced greenhouse effect

A
  • ghg effect oni a problem when there r excessive ghg in troposphere, enhancing ghg effect, raising mean annual temp of world
  • Since 1750s which saw start of IR, man’s intense activities hv accelerated increase of ghg act as thermal blanket re-radiating heat back into earth’s atmos
  • CO2 is principal ghg, provides main warming/ ‘radiative forcing effect’
  • CO2 & other ghg once emitted, can stay in atmos for long time; even if emissions stop today, warming will continue (thermal inertia)
  • bringing anthropogenic carbon emissions to zero WON’T reduce global avg temp NOW - effect oni can b felt years later (in long term)
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6
Q

Define anthropocene

A

idea that humans hv create its own ‘epoch’ beginning when human activities started to hv a significant global impact on earth’s geology & ecosystems

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7
Q

How has atmospheric CO2 concentration changed from pre-industrial times?

A

pre-industrial: 270ppm (b4 1750s)

by 1950s, rose to 310ppm

2022 - abt 418ppm

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8
Q

What can be said about the rapid increase in CO2 levels in the last few centuries?

A
  • argued that human activities since IR ard 1750 hv increased atmospheric trace gases eg CO2
  • human-induced CO2 emissions enhanced edi existing gh effect, causing global warming & fundamental change in climate
    => enhanced gh effect
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9
Q

What are two main ways in which anthropogenic activities have contributed to global warming

A
  1. Increase in emissions of ghg (CO2, CH4, etc.) arising fr human activity
    a. Industrial
    (burn fossil fuel in intense manufacture gds, transport, etc.)
    b. Agricultural
    ( change in landuse eg livestock rearing)
    c. Domestic
    (indiscriminate waste disposal, use transport, natural gas piping, etc.)
  2. Reduct n of carbon sink
    a. large scale, accelerated deforesta n
    b. warming, acidifi n of oceans
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10
Q

Explain how industrial activities increase greenhouse gas emissions

A
  • produce gds, raw materials we use everyday (intense manufacturing activities)
  • emit large qtys of ghg eg CO2, nitrous oxides, etc.
  • emissions can be either direct or indirect
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11
Q

Explain how agricultural activities increase greenhouse gas emissions

A
  • reduce forests (carbon sinks) that absorb CO2 -> more CO2 thus trapped in atmos, re-emit longwave rad n back to earth, warming it
  • use of fertilisers, tilling, increase nitrous oxides in atmos
  • livestock rearing eg cattle ranching produce methane when they belch as part of their digest n
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12
Q

Explain how domestic activities increase emission of greenhouse gases

A
  • eg transport, cook, dispose/recycle waste, refrigerat n, electricity consumpt n
  • transport n: cars trucks, ships, trains, planes
  • CO2 emission fr combust n of petroleum-based products
  • likely increase as we bcome more dvloped (w associated increased affluence) & demand for more energy
  • Growing pop n Pa = growing global demand for more gds, svcs to b produced
  • Increased affluence = higher PP
    => can demand, pay for more gds, svcs
  • Dietary preferences/ lifestyle
    -> prefer meat-based foods
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13
Q

Explain reduction of carbon sinks by deforestation

A

(release of stored carbon)
- deforestat n is generally categorised as long-term/permanent removal of forest cover & convers n to other land uses (non-forested land)
- if not properly managed, can cause permanent destruct n & eventual disappearance of once renewable resource
- Large scale deforestat n increased rapidly in last 50 yr
eg Amazon rainforest (holds 20% of all CO2 in atmos), Congo Basin Rainforest
BUT, rapidly being cleared for agriculture & urban dvlopmt
=> release carbon stored in trees back into atmos
- farming activities may oso increase release of CO2 & CH4 by animals

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14
Q

What are main anthropogenic causes of tropical deforestation

A
  1. Logging (for timber & urban expan n)
  2. Livestock ranching eg cattle ranching
  3. Agricultural expan n eg palm oil
  4. Firewood/fuelwood collect n (for subsistence farmers)
  5. Urban dvlopmt (to accommodate growing global pop n )
  6. Mining for resources

(all these human activities are the reason rainforests r disappearing)

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15
Q

Elaborate on primary losses in tropical rainforests

A
  • 3 countries account for ~ 48% of primary rainforests loss in 2018
  1. Amazon forest in Brazil (1.3ha lost)
    cleared for cattle ranching and timber logging
  2. Africa’s congo rainforest loss due to
    - conversion to agricultural lands, timber exports, increased pop n demand for firewood
  3. Indonesia rainforests (300Kha lost)
    - cut down to make way for palm oil plantat n (palm oil used in shampoos, cleaning pdt, detergents, lotions, lipsticks, etc.)
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16
Q

Explain cattle ranching as a cause of tropical deforestation

A
  • ranching is farming, raising of livestock to produce meat for food product n
  • rise in fast food chains, change in dietry needs (prefer meat) & increasing affluence
    eg large amt beef fr cattle in Amazon greatly demanded by burger chains eg Burger King, McDo, etc.
17
Q

Explain agricultural expansion as cause of tropical deforestation

A
  • globally, large scale commercial agri (cash crops = cultivate for profit) is main cause of deforestat n (up to 75%)
  • In Latin America, deforestat n related to large-scale ranching (beef) & oso soybean product n (large part of GDP for many Latin America countries)
  • In SEA (esp Indonesia), deforestat n related to palm oil agri (palm oil plant n now cover > 27million ha - forests & human settlemt destroyed & replaced by ‘green deserts’ w no biodiversity on area size of New Zealand)
  • In Africa, expan n of small-scale shifting agri (slash-and-burn cultivat n) cause deforestat n
18
Q

Explain urban expansion as cause of tropical deforestation

A
  • increasing pop n & increased affluence will increase demand for land, other forest pdt eg timber, cattle, agricultural produce, etc.
    => all these increased demands cause accelerated rate of deforestat n
    eg In SG, compared to 1800, oni 2.99% of primary forest remains
19
Q

What are underlying drivers of deforestation?

A
  • rapid pop n growth (global)
  • econ dvlopmt -> capitalism (increased affluence causing higher PP & increasing demands)
  • urban n (global)
  • poverty (in LDCs)
  • Low agri productivity (poor qlty of land)
  • unequal distribut n of land
20
Q

Explain reduction of carbon sinks ( oceans)

A
  • ocean is planet’s greatest C sink (vital buffer against impacts of CC, stabilises climate)
  • absorbs 30% of all CO2 emiss n, capture 90 % of excess heat generated by these gas emiss n trapped in earth’s system
  • oceans absorb C 20 times more than trees by:
    i. photosynthesis of phytoplankton
    ii. atmos CO2 dissolving in ocean, esp cold waters

HOWEVER, more ghg emiss n affected ocean health
- human activiteis eg burn FF cause more ghg emis n, cause increase global temp
- as global temp increase, more atmos CO2 dissolved in ocean sink, increase pH lvl (more acidic) - 30% more acidic than pre-industrial period
- warming & acidifying of seawater reduce ocean ability to absorb CO2
- when ocean warm up, ocean C capacity decrease
- more CO2 released into atmos

21
Q

How does ocean acidification harm ecosystems?

A
  • ocean acidifi n can create condit n that eat away minerals used for calcificat n by oysters, clams, lobsters, shrimp, coral reefs, other marine life to build shells, skeletons
  • dissolved CO2 in ocean bcome carbonic acid which react w calcium ion to form bicarbonate, making calcificat n of organisms less available
    => damaging effects to aquatic (lack of nutrients) & terrestrial ecosystems