Which mechanism amplifies CO₂ sequestration when increased wind stress drives ocean circulation change?

💡 Explanation

When winds intensify, upwelling circulation increases leading deeper, nutrient-rich waters to surface because of Ekman transport, stimulating algal blooms. Therefore amplified CO₂ sequestration by algae results, rather than increased stratification, methane release, or reduced runoff, which don't directly increase CO₂ absorption.

• Which outcome occurs when prolonged warming increases active layer depth on a tundra slope subject to solifluction?
• Which outcome occurs when coastal upwelling is disrupted by increased freshwater runoff?
• Which land deformation results when thawing permafrost causes widespread ground subsidence?
• Which mechanism dictates fjord sill depth controlling deep water renewal in a stratified fjord?
• Which resulting ground feature indicates intense solifluction due to thawing permafrost on gentle alpine slopes?
• Which mechanism causes increased anchovy populations following strong coastal upwelling events?