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A study led by Brown researchers showed how melting ice water from massive glaciers can ultimately lead to droughts and flooding in East Africa and Indonesia. PROVIDENCE, R.I. [Brown University] — Wi...
Climate change is approaching a tipping point that, during this century, could reawaken an ancient climate pattern in the Indian Ocean similar to the Pacific Ocean El Niño, new National Scie...
We know a lot about how carbon dioxide (CO2) levels can drive climate change, but how about the way that climate change can cause fluctuations in CO2 levels? New research from an international te...
The global climate is a complex machine in which some pieces are separate yet others are connected. Scientists try to discover the connections to predict what will happen to our climate, especially in...
The Chinese-American Oceanic and Atmospheric Association (COAA) and the China Meteorological Society (CMS) are pleased to announce their cooperation in organizing the 7th International Conference on A...
Ocean/atmosphere dynamics result from flow interactions on a wide range of time and space scales. The representation of such complex scale interactions is a key challenge for numerical modeling, reg...
The waters surrounding Antarctica may be one of the last places to experience human-driven climate change. New research from the University of Washington and the Massachusetts Institute of Technology ...
Advances in nucleic acid sequencing technology are removing obstacles that historically prevented use of genomics within ocean change biology. As one of thefirst marine calcifiers to have ...
Researchers are struggling to solve the challenge of predicting climate change impacts on marine environments.
University of Queensland researchers have found physical evidence in Great Barrier Reef corals of a little-known, long-term climate pattern in the Pacific Ocean.
There is considerable evidence in support of Milankovic's theory that variations in high-latitude summer insolation caused by Earth orbital variations are the cause of the Pleistocene ice cycles. The ...
Sediments from the Southern Ocean reveal a meridional divide in biogeochemical cycling response to the glacial-interglacial cycles of the late Neogene. South of the present-day position of the Antarct...
Using a 3-dimensional climate model of intermediate complexity we show that the overturning circulation of the Atlantic Ocean can vary at multicentennial-to-millennial timescales for modern boundary c...
This study analyses the response of the Atlantic meridional overturning circulation (AMOC) to LGM forcings and boundary conditions in nine PMIP coupled model simulations, including both GCMs and Earth...

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