Stalagmite-inferred variability of the Asian summer monsoon during the penultimate glacial–interglacial period
The orbital-timescale dynamics of the Quaternary Asian summer monsoons (ASM) are frequently attributed to precession-dominated northern hemispheric summer insolation. However, this long-term continuous ASM variability is inferred primarily from oxygen isotope records of stalagmites, mainly from Sanb...
Gorde:
| Egile Nagusiak: | , , , , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Copernicus Publications
2014-06-01
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| Saila: | Climate of the Past |
| Sarrera elektronikoa: | http://www.clim-past.net/10/1211/2014/cp-10-1211-2014.pdf |
| Etiketak: |
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