Course review

D4.3 Climate change

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Learning objective

D4.3.1—Anthropogenic causes

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• Human activities increase atmospheric CO₂, methane, and other greenhouse gases • Fossil fuels, cement, agriculture, deforestation, and land-use change are major sources

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Learning objective

D4.3.2—Positive feedback cycles

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• Positive feedback amplifies warming after an initial climate change • Examples include ice-albedo loss, permafrost methane, ocean CO₂ release, and wildfire feedback

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Learning objective

D4.3.3—Boreal forest tipping point

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• Boreal forests can shift from carbon sinks to carbon sources • Warming, drought, reduced snowfall, browning, insects, and fire increase tipping-point risk

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Learning objective

D4.3.4—Polar habitat changes

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• Melting landfast ice and sea ice alters breeding, feeding, and resting habitat • Emperor penguins and walruses illustrate species dependent on ice timing and extent

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Learning objective

D4.3.5—Ocean current changes

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• Ocean warming strengthens stratification and can reduce nutrient upwelling • Reduced upwelling lowers phytoplankton productivity and food supply

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D4.3.6—Range shifts

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• Species ranges can shift poleward, upslope, or contract as climate zones move • Montane birds and North American tree species show changing distribution limits

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Learning objective

D4.3.7—Coral reef threats

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• Warming causes coral bleaching by disrupting coral-zooxanthellae mutualism • Ocean acidification suppresses calcification, threatening reef biodiversity and collapse

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Learning objective

D4.3.8—Carbon sequestration approaches

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• Carbon sequestration captures and stores atmospheric carbon dioxide • Afforestation, agroforestry, forest regeneration, and peatland rewetting increase carbon stores

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Learning objective

D4.3.9 (HL)—Phenology

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• Phenology studies timing of seasonal biological events • Events include flowering, budburst, migration, nesting, breeding, and insect emergence

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Learning objective

D4.3.10 (HL)—Disruption of phenological synchrony

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• Climate change can desynchronize interacting species that rely on matched timing • Arctic plant-reindeer migration and great tit-caterpillar peaks are key examples

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Learning objective

D4.3.11 (HL)—Increased insect life cycles

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• Warmer temperatures can shorten insect development and add generations per year • Spruce bark beetles can shift from one to two annual attack periods

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D4.3.12 (HL)—Evolution from climate change

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• Climate change alters selection pressures and can shift phenotype frequencies • Finnish tawny owl colour change links milder winters, snow cover, and survival

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