Which mechanism amplifies the initial Milankovitch cycle forcing on global temperatures?

💡 Explanation

When initial Milankovitch cycles induce slight warming, ice-albedo feedback occurs because melting ice exposes darker surfaces that absorb more solar radiation, amplifying the initial warming. Therefore ice-albedo feedback increases solar absorption, rather than rebound, dust changes, or circulation shifts, each needing independent forcing scenarios.

• Which effect commonly arises where a transform fault connects two divergent plate boundaries on the ocean floor?
• Which outcome occurs when thawing overburden destabilizes Arctic slopes?
• Which slope stability risk increases when repeated freeze-thaw cycles affect shale bedrock underlying a tundra region with solifluction?
• Near active stratovolcanoes, which consequence results when pyroclastic flows encounter a large body of water?
• Which pedogenic effect follows enhanced chemical weathering by increased acidity?
• Which outcome results when a glacial cirque degrades?