Increased frequency of extreme Indian Ocean Dipole events due to greenhouse warming
Wenju Cai (),
Agus Santoso,
Guojian Wang,
Evan Weller,
Lixin Wu,
Karumuri Ashok,
Yukio Masumoto and
Toshio Yamagata
Additional contact information
Wenju Cai: CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195 Australia
Agus Santoso: Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, The University of New South Wales, Sydney, 2052 Australia
Guojian Wang: CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195 Australia
Evan Weller: CSIRO Marine and Atmospheric Research, Aspendale, Victoria, 3195 Australia
Lixin Wu: Physical Oceanography Laboratory, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China
Karumuri Ashok: Centre for Climate Change Research, Indian Institute of Tropical Meteorology Pashan, Pune 411 008, India
Yukio Masumoto: Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan
Toshio Yamagata: Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Kanazawa-ku, Yokohama 236-0001, Japan
Nature, 2014, vol. 510, issue 7504, 254-258
Abstract:
Extreme positive-Indian-Ocean-dipole events cause devastating floods in eastern tropical Africa and severe droughts in Asia; increasing greenhouse gas emissions will make these dipole events about three times more frequent in the twenty-first century.
Date: 2014
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DOI: 10.1038/nature13327
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