Prof. Dr. Ingo Grevemeyer, 91探花: "L眉cken in der Theorie der Plattentektonik 鈥 warum ist der Meeresboden an Transformverwerfungen in der Mitte der Ozeane tiefer als in den benachbarten Tiefseebecken?""
Prof. Jonathan Gregory, National Centre for Atmospheric Science University of Reading & Met Office Hadley Centre, Reading, UK: "A new conceptual model of global ocean heat uptake"
Dr. Richard Seager, Lamont-Doherty Earth Observatory, Columbia University, New York, USA: "Persistent discrepancies between modeled and observed trends in upper tropical Pacific Ocean temperature and a few implications for regional climate projections"