Global Change

There is more carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) in the atmosphere today than there has been for 3 million years. These greenhouse gases trap heat in Earth’s atmosphere, triggering worldwide changes in climate.

Earth’s climate has always changed, but the changes today are occurring at a faster rate than at any time in the planet’s history. Before the Industrial Revolution, atmospheric concentrations of CO2 hovered around 280 parts per million. In 2013, they passed 400 parts per million. The greenhouses gases CH4 and N2O have risen even faster over the same period of time. Globally, the decade from 2001 to 2010 was the warmest decade on record since thermometer-based measurements started. And climate isn’t the only thing that’s changing. Nutrient pollution, ultraviolet radiation and the spread of invasive species are all transforming the planet.

Global change is a reality, not only of the future, but of the present moment. Here at SERC, ecologists are investigating its impacts today and making projections to the end of the twenty-first century. The Global Change Research Wetland seeks to uncover the fate of wetlands into the year 2100. The Forest Global Earth Observatories (ForestGEO) track how forests across the world are responding now. Other researchers delve into the impacts of coastal acidification, low oxygen, sea-level rise, nutrient over-enrichment and other symptoms of global change. Explore the topics below to learn about some of the latest discoveries, and what areas remain to be explored.