Climate Change Flashcards

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1
Q

What is global warming?

A

Increase in global temperatures through natural response or human activity e.g. industrialisation, caused by GHG emissions

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2
Q

How does GHG contribute to the greenhouse effect & global warming?

A
  • GHG allow short-wave radiation from sun to pass through & heat the earth sf→ heated sf radiate out-going, long-wave radiation/infrared which is absorbed and re-emitted by GHGs into atmosphere
  • Increased conc of GHG→ increased trapping of radiation/heat
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3
Q

How does combustion of fossil fuels contribute to global warming?

A

Combustion of fossil fuels for increasing energy usage: electricity, transport, production of chemicals etc. –> CO2, a GHG

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4
Q

Explain how forests and peatlands are carbon sinks

A
  • CO2 absorbed stored as organic material in plants (biological carbon sequestration)
  • Undisturbed waterlogged peatlands store large amts of C (small net sinks).
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5
Q

How does the clearing/drainage of forests/mangroves/peatlands contribute to global warming?

A
  • Reduces net photosynthesis, reduce amt of C sinks available
  • Drainage of peatlands–> increased decomposition rates, risk of peatland fires–> more CO2 and N2O
  • Burning of forests –> CO2
  • Conversion to agriculture further increases GHG emissions
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6
Q

How does the growth in meat consumption (due to rising incomes) contribute to global warming?

A
  • Beef produces the highest GHG emissions compared to other foods
  • Source of GHG from raising livestock
    > Enteric fermentation: carbohydrates digested by microorganisms into simple mlcs for absorption into bloodstream of animal ⇒ methane
    > Nitrogenous fertilisers:
    –> increases production of animal feed for livestock⇒ N2O
    –> production of chemical N fertilisers⇒ CO2 + N2O
    > Manure
    –> Stored manure from livestock⇒ methane
    –> Used as fetilisers⇒ N2O
  • Deforestation and conversion of grassland into agricultural land: decomposition of N-rich humus⇒ CO2 + N2O
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7
Q

With reference to biochemical details, explain how planting young trees helps to counteract CO2 emissions

A
  • Photosynthesise to produce sugars for their growth and survival
  • LD: Light energy→ ATP and NADPH
  • LID: CO2 combines with RuBP to form GP, catalysed by enzyme, RuBP carboxylase→ GP (in the presence of ATP and NADPH) reduced to triose phosphate (G3P)* and subsequently to RuBP;
  • G3P used in the formation of other carbohydrates/proteins/fatty acids, which can be used to form structural tissues that is incorporated into the growing trees;
  • G3P also converted into storage molecules like starch or structural materials like cellulose
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8
Q

Explain why stations should include CCS or CCU facilities

A
  • CO2 is a GHG→ global warming
  • CCS and CCU limits CO2 emissions→ mitigate the effect of global warming
  • To prevent coral bleaching/more extreme weather conditions (AVP: any other environmental effects of high CO2 concentration)
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9
Q

Describe the impact of global warming on frozen organic matter

A
  • Permafrost stores immense amt of C (frozen organic matter) and methane (methane hydrates)
  • Thawing of permafrost/warming→
    > Organic matter in permafrost starts to decompose→ CO2
    > Organic matter decomposes at a faster rate→ CO2
    > Methane released directly or broken down into CO2 by bac before being released
    > Increased microbial activities (even in winter; thawed regions between frozen layers) → new methane produced
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10
Q

What causes the rise in sea levels?

A
  • melting of land ice: polar ice caps, glaciers, ice sheets

- thermal expansion of water

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11
Q

Describe the impact of global warming on freshwater supplies

A

Stress on freshwater supplies
1. Higher temp→ melting of ice sheets, glaciers and polar ice caps (land ice) → increase flood risk during rainy seasons, depletion of glaciers (water source)
2. Higher sea level→ saltwater intrusion into streams/lakes (increase salt conc in groundwater, extending areas of salinity, less freshwater)
3. Wetter rainy seasons
> more runoff→ more sedimentation→ contaminate freshwater supplies⇒ decline in water quality
> Flooding→ streams cannot contain water, wasted when water drains into sea⇒ depletes freshwater
4. Dryer dry seasons/drought→
> depletes groundwater and -vely affects replenishment of groundwater
→ ↑ evaporation and transpiration removes water from water from lakes/ground water
→ More pumping of groundwater for irrigation
→ Shorter duration of rainfall
> decline in water quality
→ More areas affected by drought, which depletes groundwater reserves→ residual water of inferior quality: leakage of saline/contaminated water from land sf/adj water bodies that are contaminated
→ Higher conc of pollution and nutrients in water→ increase load of microbes in waterways & drinking water reservoirs
5. Increase in temp→ Increased microbial growth

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12
Q

Describe the impact of climate change: change in weather, heatwaves, heavy rainfall

A
  • Rise in temp and warmer air→ more evaporation of water into atmosphere→ more water vapour in air→ increased precipitation, but distribution of precipitation around the world is uneven
  • Higher precipitation in tropics: Increased freq and intensity of rainfall / wetter rainy seasons
    > → more pollution e.g. erosion and sedimentation due to run-off→
    –> Water-borne diseases
    –> More runoff→ more sedimentation→ contaminate freshwater supplies (e.g. drinking reservoirs)⇒ decline in water quality
    –> Flooding→ streams cannot contain water, wasted when water drains into sea⇒ depletes freshwater
    –> Eutrophication of water→ more algae→ less light/O2 → death of fish and other plants
    > Increased risk of flooding in urban area
  • Lower precipitation in already dry subtropics / Dryer dry seasons: during drought/periods w less rainfall→
    > Depletes groundwater & -vely affects replenishment of groundwater
    > Flooding→ streams cannot contain water, wasted when water drains into sea⇒ depletes freshwater
    4. Dryer dry seasons/drought→
    > depletes groundwater and -vely affects replenishment of groundwater
    → ↑ evaporation and transpiration removes water from water from lakes/ground water
    → More pumping of groundwater for irrigation
    → Shorter duration of rainfall
    > decline in water quality
    → More areas affected by drought, which depletes groundwater reserves→ residual water of inferior quality: leakage of saline/contaminated water from land sf/adj water bodies that are contaminated
    → Higher conc of pollution and nutrients in water→ increase load of microbes in waterways & drinking water reservoirs
  • Less amount and duration of snowcover→ affect timing of ice melting & water flowing into waterways→ less groundwater
  • Less frost days at high latitudes→ increasing growing season and food production
  • More freq & intense heatwaves→ more heat-related deaths
  • Stronger storms and hurricanes: top layer of ocean gets warmer→ hurricanes and tropical storms grow stronger, w faster winds and heavier rain
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13
Q

What are the negative effects of rise in sea levels?

A
  • Higher projected storm surge (less protection by seawalls)
  • Infrastructure and sewers compromised
  • Coastal areas high enough to avoid flooding still affected
    > Saltwater intrusion→ increase soil salinity/reduce freshwater sources/ changing soil pH
    > Colonisation of habitats by displaced populations of animals
    > Increased coastal erosion/shoreline erosion
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14
Q

Explain how a positive feedback mechanism may affect global climate change.

A
  • (defn) initial change results in further change of same factor
  • Higher temperature will lead to increased CO2 in atmosphere in these activities→ more GHG→ more infrared radiation absorbed→ further increase in temperature
    > Increased decomposition of organic matter in soil→ increased CO2 in atmosphere
    > Reduced CO2 solubility in oceans and seas→ increased CO2 in atmosphere
    > Melting of permafrost → increase of CH4 in atmosphere
    > Melting of land and sea ice→ less radiation from sun is reflected (less albedo) → more sunlight & heat absorbed→ increase temperature
    > Drier climate→ more forest fires→ more CO2 released in atmosphere
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15
Q

Describe the physiological/morphological changes in plants under water stress (drought, high temp)

A
  • Reduction of water content and turgor→ cell expansion slows/ceases
  • Less/no photosynthetic pigment
  • Less RuBisCO→ less carbon fixation
  • Incresed ratio of roots to shoots
  • Stomatal closure & less stoma per leaf → reduce water loss through transpiration
    ⇒ photosynthetic rates decrease→ plant growth is retarded; dehydrate and die
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16
Q

What are the morphological adaptations of plants in response to high temp/water stress?

A
  • Small sf area to vol ratio of leaf
  • Thick waxy cuticle and epidermis
  • Stomata only on bottom of leaf; only in grooves and surrounded by hair → high humidity at stomata opening→ reduce evaporation and water loss through transpiration
  • Leaves that curl up on dry days e.g. marram grass using “hinge”/bulliform cells
17
Q

Explain why during high temperatures, there is low CO2: O2 ratio in the airspaces of the leaves

A
  • High temp→ significant transpiration→ water loss→ stomata closes to reduce transpiration→ prevent gaseous exchange
  • Rate of photosynthesis is higher than rate of respiration
  • LD rxn of photosynthesis continues→ photolysis of water, more O2 gas produced & accumulates
  • Available CO2 is used up during carbon fixation
18
Q

What problem occurs when there’s a low CO2: O2 ratio in the airspaces of the leaves?

A

Photorespiration: RuBisCO fixes O2 (competitive inhibitor of RuBisCO) instead of CO2 → less photosynthesis

19
Q

How do C4 and CAM plants adapt to high daytime temp and intense sunlight (photorespiration)?

A

C4 plants: CO2 converted to 4C compounds by enzyme that doesn’t bind O2 → 4C goes to deeper tissue layer where less O2 is present → CO2 released and enters Calvin cycle

CAM plants: CO2 converted to 4C in the day. CO2 released, C fixation at night

20
Q

How do high temp affect physiology of plants?

A
  • drought and water stress–> C4 and CAM plants
  • reproduction of plants: high temp→ reduced pollen viability, disrupt flowering process, affects seed production
  • smaller body size of animals–> large sf area to v ratio–> efficient heat loss
  • Body temp of ectoderms fluctuates w env temp. Higher temp→ faster rate of enzyme-catalysed biochemical rxn→ faster metabolism rate→ less time to maturity
  • Higher temp→ affect fitness of insects
    > Decrease relative fitness of tropical insects: small thermal safety margins as their envs are already close to their physiological optimum→ approach physiological optimum temp faster and risk extinction
    > Increase relative fitness of temperate insects: larger thermal safety margins as their envs are on average cooler than their physiological optimal→ broader thermal tolerance→ warming enhances fitness
  • Change in timings of seasonal life cycle events: mismatch in timing of migration, hibernation, breeding, food availability, flowering timings etc.→ species out of synch with other species /impt natural events in ecosystem
21
Q

What is a thermal safety margin

A

Diff between thermal optimum and current climate

22
Q

Describe the effect of global warming on plant and animal distribution

A

To stay within their ideal temp range→ move to areas with cooler temp
Shift to higher elevations and northern latitudes

23
Q

What is the life cycle of Aedes aegypti?

A
  • Egg (1-2 days): can survive very long in dry ststae, and hatch almost immediately when water appears
  • Larva (4 days): 1st to 4th instars
  • Pupa (2days)
  • Adult
24
Q

Describe how global warming affects the transmission of dengue virus

A
  • Mosquito vector, Aedes aegypti, lives and breeds in moist tropical regions.
  • Dengue virus spread through human-to-mosquito-to-human cycle

Virus reproduces within mosquito. ↑ mosquito vector which transmits dengue→ higher transmission of dengue
- Higher temp in temperate regions/higher altitudes→ conditions more suited for survival of mosquitoes→ mosquitoes move to higher latitude, expanding their distribution + colonise higher altitudes
- Higher temp
→ Shorter life cycle (first instar to emergence shorter): ↑ rates of enzyme-catalysed rxns→ ↑ metabolism→ faster development, decreasing length of reproductive cycles→ stimulate hatching of eggs
→ more rainfall → more pools of stagnant water for mosquito breeding
⇒ more mosquitoes→ more transmission of dengue fever

Higher temp→ shorter extrinsic incubation period in mosquito

25
Q

Describe the development and virulence of dengue in humans

A
  • DENV infects Langerhans cell (dendritic cell), which secrete cytokines and limit spread of infection and travel to lymph nodes-> display viral antigens on sf–> activate monocytes and macrophages–> instead of ingesting and destroying pathogens, they are targeted and infected by virus
  • Infected monocytes and macrophage travel through lymphatic system→ virus spreads and infects more cells→ Viremia: high lvl of virus in bloodstream
  • Infected cells secrete cytokines (interferons) → activate innate and adaptive immune system
26
Q

Describe the symptoms of dengue

A

DF: Viraemia, headache/pain, fever, rash

Severe dengue: DHF (lowered blood pressure) DSS (death)

27
Q

Why is there a higher risk of severe dengue upon infection from 2nd serotype?

A
  • antibody-dependent enhancement of infection: antibodies from 1st infection bind to infecting virus particle, cannot neutralise virus→ higher overall replication of virus; non-neutralising ab facilitates virus entry into host cells→ increasing viremia
  • cytotoxic T cells provide only partial immunity against new serotype/don’t effectively clea virus + release excess cytokines→ serious inflammation and tissue damage
    > ↑ vascular permeability→ leakage of plasma, fluids collect in body cavities; severe bleeding: stomach and intestinal bleeding→ death
    > Loss of plasma and protein→ shock: lack of blood circulation, undetectable blood pressure and pulse
28
Q

Suggest why it may be difficult for species displaced by a rise in sea level to colonise new habitats–> unable to adapt, higher risk of extinction

A
  • No other suitable habitat/not able to adapt
  • No biological corridor for species to move from one habitat to another
  • Rate of sea rise too high, time taken for colonisation is insufficient
  • Lack of other species for its survival e.g. prey / New predators
  • Niches already filled
  • Compete with native species for food & resources
  • Exposure to new forms of disease
29
Q

How does climate change affect corals?

A
  • Higher
    > thermal stress on corals
    > more bac multiplication and infection of corals by bac–> stress
    > zooxanthellae leaves corals–> coral bleaching etc.
  • More CO2 and acidification of oceans–> calcification rates and growth rates of corals reduce
  • Over-fishing of herbivorous fish that eat macroalgae→ corals under more threat from macroalgae
  • ↑sea level and sedimentation→ smothering of coral
  • Stronger and more freq storms→ destory coral reefs
  • ↑ runoff of freshwater, sediment, pollutant→ algae bloom→ blocks light
    ⇒ loss of coral reefs = loss of habitats for marine organisms, disrupt ecosystem, loss of diversity
30
Q

Describe the benefits to zooxanthellae of the coral-algae symbiotic rs

A
  • CO2 from coral respiration can be used for photosynthesis
  • nitrogenous waste from corals–> nutrients for algae
  • Physical support and shelter provided by corals
31
Q

Describe the benefits to corals of the coral-algae symbiotic rs

A
  • Algae photosynthesise, produce food for corals

- Algae absorb light light energy, protecting corals from harmful effects of sunlight

32
Q

Why does the loss zooxanthellae lead to coral death?

A
  • As zooxanthellae produce food, no algae–> less source of food
  • Loss of inorganic ions for deposition of skeleton
  • loss of protective algal layer
33
Q

How does climate change affect salmon?

A
  • Warmer water temp
    → affects life cycle of salmon
    → ↓ cardiovascular capacity→ more vulnerable to disease & predators→ death
  • Expanded industrial activities→ decline in salmon populations
  • Loss of snowpack, shrinking glaciers→ ↓ stream flows in summer & fall
    → water levels in rivers and streams ↓→ bears snap at spawning salmon more easily→ ↓ survival of salmon
    → more difficult to return to spawning grounds/juvenile fish to enter ocean in summer
  • Intense spring floods→ wash away salmon eggs laid in stream beds
  • Salmon return to native rivers to spawn, don’t migrate to cooler waters to spawn
34
Q

What are the effects of the loss of biodiversity?

A
  • Loss of biomedicines
  • Loss of genetic diversity in food
    > Without genetic diversity in crop production/consistent mutation→ species cannot continue to thrive in face of disease and pestilence→ ↓sustainability of food source
35
Q

Describe the impact of climate change on global food supply: crops

A
  • reduce crop yield:
    > droughts, change in ppt–> less water
    > High temp–> poor anther dehiscence, low pollen production→ sterility and no seeds
    > Warming→ shorter periods of low winter temp→ low flower bud initiation
  • Alter patterns of weeds, plant pests and pathogens/diseases
    > high temp–> more pests and weeds
    > new pests
  • Loss of arable land
    > high ppt and flooding–> soil erosion–> destroy veg plots–> lower yield
36
Q

Describe the impact of climate change on global food supply: fisheries

A
  • Migration towards poles
    > → catches more dominated by warm-water species
    > Tropics: less catches→ ↓ food security
  • Acidification of ocean
    > → death of coral reefs, the foundation of many fisheries
    > Harm shellfish by weakening their shells
37
Q

Describe the impact of climate change on global food supply: livestock

A
  • High temp→ heat stress in animals→ vulnerable to disease, reduced fertility & milk production, high mortality
  • High temp→ drought→ loss of pasture grazing land (food) for livestock