PTE · Multiple Choice, Single Answer

El Niño Ecological and Regional Impacts

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  • PTE Academic and PTE Core
1

Peatland Fires in Southeast Asia

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During severe El Niño events, descending air over the western equatorial Pacific suppresses convective cloud formation, causing extended dry spells across equatorial Southeast Asia. In drained tropical peatlands, the lowered water table exposes thick layers of organic carbon to atmospheric oxygen. Even minor agricultural clearances can trigger underground smouldering that proves virtually impossible to extinguish by conventional firefighting methods. These subterranean fires burn through ancient biomass for months, releasing vast quantities of carbon monoxide and particulate haze into regional air basins, which severely degrades respiratory health and disrupts international aviation networks.

According to the passage, why are peatland fires particularly difficult to control during El Niño?

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2

Vector-Borne Disease Transmission

Shifts in precipitation patterns orchestrated by El Niño create distinct ecological niches for insect vectors. In normally arid regions of South America, uncharacteristic torrential downpours generate abundant ephemeral pools that accelerate mosquito breeding, precipitating sudden spikes in malaria transmission. Conversely, in humid tropical areas where El Niño induces drought, river beds dry into stagnant pools that serve as ideal breeding habitats for other disease-bearing mosquitoes. Furthermore, elevated ambient temperatures shorten the extrinsic incubation period of pathogens within vectors, quickening the transmission cycle. Consequently, public health agencies increasingly synchronise preventative vector-control measures with seasonal climate anomalies.

Which statement best summarises the central mechanism discussed in the text?

  • APublic health agencies have eradicated vector-borne pathogens by tracking equatorial precipitation anomalies.
  • BSevere droughts in arid zones eliminate insect breeding pools while reducing ambient temperatures.
  • CRising atmospheric moisture uniformly accelerates the lifecycle of mosquitoes across all tropical landmasses.
  • DEl Niño influences mosquito-borne disease risks by altering breeding environments and pathogen incubation speeds.
3

Tropical Coral Bleaching Dynamics

Pronounced warming of equatorial surface waters during El Niño places extreme thermal stress on shallow coral reef ecosystems. When ocean temperatures exceed local summer thresholds by merely one degree Celsius for sustained periods, the symbiotic relationship between corals and photosynthetic dinoflagellates collapses. Corals expel these pigmented microalgae, leaving their translucent calcium carbonate skeletons exposed in a phenomenon known as bleaching. Deprived of the carbohydrates supplied by their endosymbionts, the hosts must rely entirely on heterotrophic feeding. If elevated temperatures persist beyond several weeks, widespread coral mortality ensues, triggering structural degradation that diminishes shelter for thousands of associated marine species.

What can be inferred from the passage regarding bleached corals?

  • AThey rebuild their calcium carbonate skeletons to withstand prolonged heat stress.
  • BThey can survive temporarily by altering their mode of nutritional intake.
  • CThey immediately perish once the symbiotic dinoflagellates are expelled from their tissues.
  • DThey become completely unable to absorb organic nutrients from surrounding water.
4

Central Pacific Modoki Variations

Climate scientists distinguish between canonical El Niño events and Central Pacific variations, frequently termed El Niño Modoki. In traditional episodes, maximum sea surface temperature anomalies develop along the eastern Pacific coast off South America. In contrast, Modoki events feature anomalous warming confined to the central equatorial Pacific, flanked by cooler waters to both the east and west. This unique tri-polar sea surface temperature pattern generates anomalous two-cell atmospheric circulation loops instead of the conventional single-cell shift. Consequently, Modoki events produce teleconnection patterns that diverge radically from classic occurrences, often steering tropical cyclones along unusual trajectories and triggering unexpected rainfall distributions.

How does an El Niño Modoki event differ structurally from a canonical El Niño?

  • AIt generates an uninterrupted single-cell circulation pattern across the entire Pacific basin.
  • BIt suppresses the development of unusual storm trajectories throughout the tropics.
  • CIt concentrates peak thermal anomalies in the central Pacific rather than eastern coastal waters.
  • DIt uniformly warms both the eastern and western margins of the equatorial ocean.
5

Pelagic Seabird Breeding Success

The arrival of an intense El Niño imposes severe nutritional bottlenecks on pelagic seabirds nesting across oceanic islands. As the warm surface layer deepens, small pelagic fish descend beyond the diving depths of surface-foraging seabirds like boobies and frigatebirds. Adult birds are forced to undertake protracted foraging flights over hundreds of kilometres, significantly increasing their energy expenditure. Faced with inadequate provisions, breeding pairs frequently abandon their nests, leading to near-total reproductive failure across entire colonies. By examining these behavioural shifts, ornithologists gain valuable bioindicators that reflect broader ecological restructuring and biomass redistribution within upper trophic levels during major climatic events.

What is the primary purpose of the passage?

  • ATo dispute the reliability of seabird nesting rates as ecological indicators during climatic shifts.
  • BTo explain how El Niño impairs seabird reproduction and serves as an indicator of marine disruption.
  • CTo argue that pelagic seabirds are adapting successfully to changing ocean depths.
  • DTo propose new conservation zones for frigatebirds and boobies across oceanic islands.

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