Moisture transport in warmer climates

Map of all authigenic carbonate and tooth oxygen isotope data from Quaternary Europe. We use spatial compilations, such as these, to understand changes in water transport during colder and warmer climates.

Global warming is likely to substantially alter the water cycle. While some changes in the water cycle are well-understood, other components remain difficult to predict because they involve a large number of small-scale processes operating across the globe to generate change. For example, how much rain is converted into runoff depends upon how much water plants will use in the future, how quickly storms produce precipitation, and how temperature and relative humidity change over land. We use a combination of data collection and modeling to understand how the terrestrial water cycle operated during past greenhouse episodes. 

Relevant Publications: