text: Research Highlights – Page 9 – Geophysical Fluid Dynamics Laboratory
  February 5th, 2015 - Tropical Climate Change Control of the Lower Stratospheric Circulation
  Tropical air has less ozone than polar air, even though the tropical stratosphere is where most atmospheric ozone is produced. The Brewer-Dobson circulation is considered key to understanding this apparent contrast. It also brings water vapor, aerosols and other species from the troposphere up into the stratosphere. The strength of the Brewer-Dobson circulation directly affects the thermal structure of the stratosphere and upper troposphere, and impacts the transport and distribution of important climate-influencing constituents including stratospheric water vapor, ozone, and volcanic aerosols. Read More…
  December 16th, 2014 - Drivers of trophic amplification of ocean productivity trends in a changing climate
  October 12th, 2014 - Karakoram snowfall less sensitive to warming than Himalayas due to a unique seasonal cycle
  September 29th, 2014 - Seasonal- and annual-mean precipitation extremes occurring during 2013: A U.S. focused analysis
  September 17th, 2014 - Retrieval of Tropical Storm Statistics by Combining Data with a High-Resolution Coupled Model
  August 22nd, 2014 - Predicting a decadal shift in North Atlantic climate variability using the GFDL forecast system
  August 13th, 2014 - Seasonal Forecasting of Regional Tropical Cyclone Activity
  July 21st, 2014 - Rapid subsurface warming and circulation changes of Antarctic coastal waters by poleward shifting winds
  July 13th, 2014 - Regional rainfall decline in Australia attributed to anthropogenic greenhouse gases and ozone levels
  June 26th, 2014 - Trajectory sensitivity of the transient climate response to cumulative carbon emission