climate change Flashcards
(140 cards)
lec 1: RESPONSES OF ORGANISMS
Atmospheric CO2 through geological time:
ice ages (low CO2), warmer interglacial (higher CO2) for 800,000 years never higher than 300ppm (NOAA 2008).
lec 1: RESPONSES OF ORGANISMS
Atmospheric CO2 in recent time
: large growth in CO2 emissions. Levels stable until 18th C (industrial revolution 1850s), current 427ppm (NOAA daily measurements since 60s)
lec 1: RESPONSES OF ORGANISMS
Rubisco:
important enzyme in fixing carbon, dual catalytic nature, carboxylation vs. oxygenation is largely dependent on CO2/O2 ratio. CO2 is key (O2 considered constant). The higher the temp the more difficult for rubisco to distinguish CO2 and O2 (higher energy, faster particles) DIAGRAM
lec 1: RESPONSES OF ORGANISMS
Change in net photosynthesis with changing [CO2]
- C4 plant
minimising amount of photorespiration happening while photosynthesis is happening (higher C uptake)
lec 1: RESPONSES OF ORGANISMS
Change in net photosynthesis with changing [CO2]
- C3 VS C4
DIAGRAM. Carbon pump costs energy, if enough CO2 better to be used to photorespire, if not enough worth investing as increases CO2 available.
Caemmerer 2012
- C3: struggle at low CO2 but keep increase in biomass (RICE)
- C4: fair well at low concs. Reach max growth earlier, more likely to find in warmer environ. Investment worth it (SETARIA VIRIDIS)
lec 1: RESPONSES OF ORGANISMS
Interactions between CO2 and temperature
CO2 fertilisation effect (plants grow better under higher CO2). In C3 plants this depends on temp (higher CO2 concs at higher temp to observe same growth rate) (Campbell 2005)
lec 1: RESPONSES OF ORGANISMS
Stomatal conductance and increasing CO2
: rising CO2 induces partial stomatal closure therefore decreases transpiration.
- C3+C4 respond differently. C4 close their stomata more under all circumstances (impacts water loss and carbon gain) (Sage 2003)
- FACE experiments (BIFoR)
lec 1: RESPONSES OF ORGANISMS
Water dynamics in response to CO2 gradient
if stomata close more, loose less water, can see water efficiency increases with high CO2 (Polley 2002)
lec 1: RESPONSES OF ORGANISMS
High CO2 effects during heat and drought
enhancement of plant performace at high CO2 reduced during extremes (no cooling) (Osborne 2016)
lec 1: RESPONSES OF ORGANISMS
Effect of CO2 variation: growth responses of plants to past CO2 change when soil fertility is adequate:
- growth responses
high carb level in plants cause feedback signals that reduce expression of photosynthetic genes (ABA high, cytokinin low, nutrients low
lec 1: RESPONSES OF ORGANISMS
Effect of CO2 variation: growth responses of plants to past CO2 change when soil fertility is adequate:
- in absence of phosphate fertalizer
- In absence of phosphate fertiliser plants do not respond to CO2 (white lupine, Campbell 2002) (45 studies have shown this)
lec 1: RESPONSES OF ORGANISMS
Effect of CO2 variation: growth responses of plants to past CO2 change when soil fertility is adequate:
- in absence of N
- In absence of enriched N growth insensitive to increased CO2 (need N to process C)
lec 1: RESPONSES OF ORGANISMS
Response of photosynthesis
variation between species, enhancement or downregulation, limiting factors (soil)
lec 1: RESPONSES OF ORGANISMS
Biological nitrogen fixation:
N2 –> CHN2, main natural source of N for ecosystems,
principle source from root nodules of higher plants (legumes, tropical grasses) dependent on carbon status of plant.
lec 1: RESPONSES OF ORGANISMS
EFFECT OF CO2 ON N FIXATION
dependent on plant, some decrease fixation with long exposure to increased CO2 (nutrient deficiency) (Reich 2006)
lec 1: RESPONSES OF ORGANISMS
INSECT SENSITIVITY:
: months can sense CO2, more difficult to find food source (prickly pear) in high CO2
lec 1: RESPONSES OF ORGANISMS
OCEAN:
rising CO2 lowers pH and carbonate supply (IPCC, 2013
lec 1: RESPONSES OF ORGANISMS
CORALS
reach saturation of carbonate
(orr, 2005).
lec 1: RESPONSES OF ORGANISMS
MARINE ANIMALS
marine animals problems with building skeletons (orr, 2005
lec 1: RESPONSES OF ORGANISMS
SEA URCHINS
sperm production and motility harmed (Haverhand, 2008)
Lec 2: overview
weather
is the current atmospheric condition
Lec 2: overview
climate
general weather condition over a long period of time
Lec 2: overview
climate change
changes in behaviour of the weather (+ climate) over longer time scales
climate has shown rapid warming trend in last decade (NOAA)
warming evident from several observations
Lec 2: overview
increasing temp. early evidence
1st described by g.s. callendar (1898-1964)
already ascribed it to CO2 from fossil fuel combustion
amateur but formulated coherent theory of IR absorption by trace gases