Global warming simulations suggest that wet regions (where precipitation exceeds evaporation) will become wetter and dry regions drier by the end of the 21st century (e.g., Held and Soden 2006), with larger contrasts expected between dry and wet seasons (Chou et al., 2013). This ‘rich-get-richer’ behavior is consistent with a large increase in the moisture content of atmosphere, leading to enhanced horizontal moisture fluxes across regions.
(CNN) Most of us can appreciate that the world is an ancient place and that a lot has changed in the almost 4.6 billion years since it took its shape.
It’s not easy to have a feel for the amount of time that has passed, but grappling with deep time helps you understand why an atmospheric carbon dioxide concentration (CO2) of 400 parts per million (ppm) is meaningful.
Deep time is geologic time and the scale needed to fathom the evolution of life, mountains, oceans, and Earth’s climate.
YCEI Postdoctoral Fellow, Jessica Barnes, will be leaving New Haven to take up a position at the University of South Carolina as an Assistant Professor in the Department of Geography and Environment and Sustainability Program.
Subpolar ocean gyres (large systems of rotating ocean currents) in the Southern Hemisphere are found poleward of the Antarctic Circumpolar Current near the Weddell and Ross Sea. They play a key role in the global energy and water budgets. These gyres are crucial for the transport of heat around the planet, as well as the distribution of nutrients and marine species. Thus, the subpolar gyres are important in the mixing and transformation of water masses.
Earth’s climate is characterized by persistent westerly jets (eastward flow) in the upper troposphere, located in the mid-latitudes of the Northern and Southern Hemisphere, which are associated locally with strong weather systems. The location of these jets is of paramount importance to human societies, as these are collocated with maximum in precipitation rates and surface winds in the extratropical regions.
Venkatachalam Ramaswamy, Director, Geophysical Fluids Laboratory, Princeton University, delivers a lecture entitled, “Understanding Trends and Extremes in Climate”.
Carbon sequestration, the removal of CO2 from combustion exhausts and its geological storage, is one of the major thrusts to reduce global warming. The only cost-effective, and commercially-available technology to remove CO2 from power plant flue gases for carbon sequestration relies on chemicals call amines to bind the CO2. Unfortunately, preliminary research has indicated that nitrogen oxides (NOx) in flue gases react with amines to form potent carcinogens called nitrosamines and nitramines.
Public discussions of climate change often focus on greenhouse gases and rising temperatures, but the most severe and immediate societal impacts of global warming are likely to be associated with changing hydrological conditions. Disruptions in water supply, extreme storms and record droughts may impact every aspect of rural and urban society: from agriculture and manufacturing to housing, energy and human health.