Difficulty: Easy
Correct Answer: Kuroshio Current
Explanation:
Introduction / Context:
Ocean currents redistribute heat and influence climate. Western boundary currents in subtropical gyres are typically warm and swift, carrying heat from low to higher latitudes. Recognizing these currents is central to physical geography and climatology.
Given Data / Assumptions:
Concept / Approach:
Western boundary currents (e.g., Gulf Stream, Kuroshio, Agulhas) are warm; eastern boundary currents (e.g., Benguela, Canary) are cold due to upwelling. Subpolar currents like the Labrador are cold. The basin-scale “South Pacific Current” label is ambiguous, but the canonical warm choice among the options is the Kuroshio off Japan.
Step-by-Step Solution:
Identify Kuroshio (western North Pacific) → warm, poleward, fast.Benguela (SE Atlantic, eastern boundary) → cold upwelling.Labrador (NW Atlantic) → cold subpolar flow.South Pacific Current — mid-latitude eastward flow; not the classic warm boundary current.Therefore select Kuroshio Current.
Verification / Alternative check:
Climatology texts pair Kuroshio with Gulf Stream as archetypal warm western boundary currents influencing East Asian and North American climates.
Why Other Options Are Wrong:
Benguela — cold, nutrient-rich upwelling along SW Africa.Labrador — cold current from the Arctic–Greenland region.South Pacific Current — not a boundary current classified as “warm” in the same sense.Canary — cold eastern boundary current.
Common Pitfalls:
Confusing current names or assuming all “western” currents are warm without checking basin location. Remember: Kuroshio = warm Japan current.
Final Answer:
Kuroshio Current
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