Global trends in oceanic wind speed and wave height. This project will determine whether winds and waves over the world's oceans have changed over the past 30 years. Such information is critically important in understanding global climate change, evaporation, air-sea interaction and to safely design and operate coastal and offshore facilities.
Carbon sequestration by mineral surface area as a feedback to climate warming in a greenhouse ocean. The project will investigate a previously unrecognised negative feedback to global warming resulting from sequestration of carbon to marine sediments by soil-formed clay minerals. By studying the past transitions to greenhouse periods, this project will assess the likely influence of this feedback in the present transition to a warmer climate.