As humans pump carbon dioxide into the atmosphere and global temperatures rise, many questions loom. One major issue is how much fresh water will be available for people, forests and agriculture. A study led by the University of Washington shows that popular long-term drought estimates have a major flaw: They ignore the fact that plants will be less thirsty as carbon dioxide rises.
Read more at UW Today »Long-term Pacific climate cycle linked to expansion of Antarctic sea ice
A new study may resolve a longstanding mystery: Why is Antarctic sea ice expanding despite climate-related global warming?
Read more at UW Today »UW researchers attend sea ice conference—above the Arctic Circle
University of Washington polar scientists are on Alaska’s North Slope this week for the 2016 Barrow Sea Ice Camp. Supported by the National Science Foundation, the event brings together U.S.-based sea ice observers, satellite experts, and modelers at various career stages to collect data and discuss issues related to measuring and modeling sea ice. The goal is to integrate the research community in order to better observe and understand the changes in Arctic sea ice.
Read more at UW Today »Deep, old water explains why Antarctic Ocean hasn't warmed
New research from the University of Washington and the Massachusetts Institute of Technology finds that ocean currents explain why the seawater has stayed at roughly the same temperature while most of the rest of the planet has warmed.
Read more at UW Today »Dennis L. Hartmann elected to National Academy of Sciences
Dennis L. Hartmann, a University of Washington professor of atmospheric sciences, is among 84 new members and 21 foreign associates elected as fellows of the National Academy of Sciences. They were chosen in recognition of their distinguished and continuing achievements in original research, according to a May 3 news release from the academy. Hartmann joined the UW faculty in 1977 after earning his bachelor’s in mechanical engineering from the University of Portland and his doctorate in geophysical fluid dynamics from Princeton University.
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