Ke Lin
Biographic Data
| ID | 4068944 |
|---|---|
| NAME | Ke Lin |
| GIVEN NAMES | Ke |
| FAMILY NAME | Lin |
| SIGNATURE | LIN K |
| AFFILIATIONS | National Taiwan University, Taiwan |
| ORCID | 0000-0003-3675-9054 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2017 |
| H-INDEX | 0 |
Late Holocene reef ecosystem baseline
Decoupling of the East Asian summer monsoon and Indian summer monsoon between 20 and 17 ka
Marine Oxygen Isotope Stage (MIS) 2, with its profound environmental and climatic changes from before the last glacial maximum (LGM) to the last deglaciation, is an ideal period for understanding the evolution of the East Asian summer monsoon (EASM) and Indian summer monsoon (ISM), two Asian monsoon sub-systems. With 875 stable oxygen isotope ratios and 43 230 Th dates from stalagmites in Sanxing Cave, southwestern China, we construct and interpr…
Mid-Holocene climate conditions and moisture source variations based on stable H, C and O isotope compositions of speleothems in Hungary
Replicated stalagmite-inferred centennial-to decadal-scale monsoon precipitation variability in southwest China since the mid Holocene
A lack of agreement between stalagmite records of the centennial- to decadal-scale Asian summer monsoon (ASM) variability since the mid Holocene limited our understanding of forcings and the possible impacts on culture evolution. Here we present replicated high-resolution stalagmite δ 18 O profiles from Dark Cave in Guizhou province, southwest China, established with 512 oxygen isotope data and 28 230 Th ages, providing a continuous history of th…
No prominent works on this page.
Mid-Holocene climate conditions and moisture source variations based on stable H, C and O isotope compositions of speleothems in Hungary
Replicated stalagmite-inferred centennial-to decadal-scale monsoon precipitation variability in southwest China since the mid Holocene
A lack of agreement between stalagmite records of the centennial- to decadal-scale Asian summer monsoon (ASM) variability since the mid Holocene limited our understanding of forcings and the possible impacts on culture evolution. Here we present replicated high-resolution stalagmite δ 18 O profiles from Dark Cave in Guizhou province, southwest China, established with 512 oxygen isotope data and 28 230 Th ages, providing a continuous history of th…
Decoupling of the East Asian summer monsoon and Indian summer monsoon between 20 and 17 ka
Marine Oxygen Isotope Stage (MIS) 2, with its profound environmental and climatic changes from before the last glacial maximum (LGM) to the last deglaciation, is an ideal period for understanding the evolution of the East Asian summer monsoon (EASM) and Indian summer monsoon (ISM), two Asian monsoon sub-systems. With 875 stable oxygen isotope ratios and 43 230 Th dates from stalagmites in Sanxing Cave, southwestern China, we construct and interpr…
Late Holocene reef ecosystem baseline
Geography (4 works) · Holocene (4 works) · Climatology (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Oceanography (3 works) · Physical geography (3 works) · Stalagmite (3 works) · Archaeology (2 works) · Cave (2 works)