Authors: Ethan Coffel*, Syracuse University, Corey Lesk, Columbia University, Jonathan M Winter, Dartmouth College, Erich C Osterberg, Dartmouth College, Justin S Mankin, Dartmouth College
Topics: Climatology and Meteorology, Coupled Human and Natural Systems, Agricultural Geography
Keywords: climate change, agriculture
Session Type: Virtual Paper
Start / End Time: 8:00 AM / 9:15 AM
Room: Virtual 46
Presentation File: No File Uploaded
Crop yields have grown rapidly over global breadbaskets since 1960. Higher yields mean that crops produce more evapotranspiration (ET), pumping water into the lower atmosphere and modifying the surface energy balance. In some high yielding regions like the central U.S., maximum temperatures have cooled over the past four decades despite rising greenhouse gas concentrations, an effect which has benefited yields. We show that this cooling has been driven by crop ET growth raising the evaporative fraction, increasing latent heating and reducing sensible heating during the growing season. This crop-driven cooling results in a positive feedback that we call the crop-climate feedback: crop yield growth modifies the local climate in a way that benefits crops and promotes further yield growth. In some regions, the feedback can account for nearly 15% of maize yield growth since 1980, and across the U.S., we find that the feedback has entirely balanced out the detrimental effects of warming over that time period. Here we analyze how the crop-climate feedback modifies the surface energy balance, assess the feedback’s strength and variability, and project how it may evolve as greenhouse gas forcing increases and yield growth potentially slows in the coming decades.