Construct · 1 fields · 1 citations

41-kyr problem: a standalone construct

One name. One construct. A landmark on the map.

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Paleoclimatology

the puzzle that early Pleistocene ice volume varied at the 41,000-year obliquity period with little precession signal despite strong precession forcing of insolation.

In paleoclimatology, 41-kyr problem refers to the puzzle that early Pleistocene ice volume varied at the 41,000-year obliquity period with little precession signal despite strong precession forcing of insolation. This meaning comes from Raymo (2003) in Paleoceanography.[1]

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Nearby constructs

forcing3 fields · 4 citationsjingle · one word, three constructs period1 fields · 1 citationsanchor · a standalone construct precession3 fields · 7 citationsinvariant · one construct, three systems

References

Raymo, M. E., & Nisancioglu, K. H. (2003). The 41 kyr world: Milankovitch's other unsolved mystery. Paleoceanography, 18(1). https://doi.org/10.1029/2002pa000791

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