Which mechanism inhibits stream formation downstream when continental ice sheets melt?

💡 Explanation

Isostatic rebound causes land uplift because the removal of the ice sheet's mass reduces the downward force, therefore flattening regional geopotential gradients; because of it, streams drain into the sea less effectively, rather than increasing evaporation.

• Which flow pattern change results when a warm ocean stream destabilizes adjacent cold water?
• Which outcome develops when intense tropical rainfall alters surface soil profiles?
• Which risk increases as rising global temperatures accelerate permafrost thaw?
• Which landscape feature primarily results due to solifluction processes in regions with permafrost?
• Which outcome occurs when plate motion stalls following subduction?
• Which risk markedly increases when permafrost thaw intensifies solifluction processes on a sloping tundra landscape?