North Atlantic cooling triggered a zonal mode over the Indian Ocean during Heinrich Stadial 1
North Atlantic cooling during Heinrich Stadial 1 triggered an east-west precipitation dipole over the tropical Indian Ocean.
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- Award ID(s):
- 2202746
- NSF-PAR ID:
- 10437099
- Date Published:
- Journal Name:
- Science Advances
- Volume:
- 9
- Issue:
- 1
- ISSN:
- 2375-2548
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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