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Showing 1–4 of 4 results
Advanced filters: Author: Andreas Lückge Clear advanced filters

  • The hydrological response to climate forcing during the past 25,000 years varied throughout the Indo-Pacific warm pool region. Marine sediment records suggest that during the Last Glacial Maximum, drying in northeast Borneo did not result in a vegetation shift, whereas the development of a severe dry season on Sumba led to water stress and the expansion of herby vegetation.

    • Nathalie Dubois
    • Delia W. Oppo
    • Braddock K. Linsley
    Research
    Nature Geoscience
    Volume: 7, P: 513-517

  • The last glacial period was marked by dramatic climate fluctuations. Sediment records from the Cariaco Basin and the Arabian Sea suggest that cooling in the North Atlantic region was tightly coupled with a southward displacement of the intertropical convergence zone and a weakening of the Indian summer monsoon.

    • Gaudenz Deplazes
    • Andreas Lückge
    • Gerald H. Haug
    Research
    Nature Geoscience
    Volume: 6, P: 213-217

  • The Australian–Indonesian monsoon is an important component of the climate system in the tropical Indo-Pacific region. High-resolution records of monsoon-controlled austral winter upwelling during the past 22,000 years reveal that glacial–interglacial variations in the Australian–Indonesian winter monsoon have been in phase with the Indian summer monsoon system.

    • Mahyar Mohtadi
    • Delia W. Oppo
    • Andreas Lückge
    Research
    Nature Geoscience
    Volume: 4, P: 540-544

  • New sea surface temperature and oxygen isotope records, combined with climate modelling experiments, show that slowdowns of the Atlantic meridional overturning circulation during Heinrich stadials and the Younger Dryas stadial affected the tropical Indian Ocean hydroclimate through changes to the Hadley circulation.

    • Mahyar Mohtadi
    • Matthias Prange
    • Andreas Lückge
    Research
    Nature
    Volume: 509, P: 76-80