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Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition
The Indonesian Throughflow (ITF) controls the oceanic flux of heat and salt between the Pacific and Indian Oceans and therewith plays an important role in modulating the meridional overturning circulation and low latitude hydrological cycle. Here, we report new sea surface temperature and aridity re...
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| Foilsithe in: | Sci Rep |
|---|---|
| Main Authors: | , , , , , , , , , |
| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe: |
Nature Publishing Group UK
2019
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| Ábhair: | |
| Rochtain Ar Líne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6861309/ https://ncbi.nlm.nih.gov/pubmed/31740711 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-53382-0 |
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