Lecture 10: Climate Change Flashcards
Loss of Arctic Sea Ice
- Decrease in Albedo (the proportion of light/radiation reflected by a surface) with melting sea ice creates a positive feedback.
- Sea levels rise
- Changing ocean currents
Ocean Acidification
ongoing decrease in the pH of Earth’s oceans, caused by the uptake of CO2 from the atmostpher
Positive Feedback
a process that occurs in feedback loop in which the effects of a small disturbance on a system include an increase in the magnitude of the perturbation.
Ocean Currents Slowing
changing ocean currents equals changing weather and potentially stronger weather systems.
Effects on Biodiversity
- Changing geographical distributions
- Challenging physiological thresholds
- Changing phenologies and biotic interactions
Changing Geographical Distributions
latitudinal expansions/shifts are common: species expand North(or South) as climate becomes more suitable.
- Pathogens and parasites of humans interact
- High alt species vulnerable (nowhere to go to escape temp increases)
- Loss of habitat with sea level rise
- Range shifts may be natural, but habitat loss and fragmentation shifts more difficult.
Challenging Physiological Thesholds
many sensitive species have limited tolerance for changes in temp, water availability, and chemistry.
-Coral bleaching
Biotic Interactions
changes in timing of life histories
- Phenology: study of the timing of life cycle events.
- Timing of events may be based on day length or temp.
- Trophic Mismatch/Decoupling
Trophic Mismatch/Decoupling
between a consumer and its food resource.
- Warbler migration timing is based on photoperiod cues, has not changed
- Eastern Spruce Budworm emergence in spring is based on temp cues, and has shifted to be earlier
- Warblers arrive at stopover too late to make use of peak caterpillar abundance.