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The physics and dynamics of the atmosphere and atmosphere-ocean interactions provide the foundation of modern climate models, upon which our understanding of the chemistry and biology of ocean and land surface processes are built. Originally published in 2006, Frontiers of Climate Modeling captures developments in modeling the atmosphere, and their implications for our understanding of climate change, whether due to natural or anthropogenic causes. Emphasis is on elucidating how greenhouse gases and aerosols are altering the radiative forcing of the climate system and the sensitivity of the system to such perturbations. An expert team of authors address key aspects of the atmospheric greenhouse effect, clouds, aerosols, atmospheric radiative transfer, deep convection dynamics, large scale ocean dynamics, stratosphere-troposphere interactions, and coupled ocean-atmosphere model development. The book is an important reference for researchers and advanced students interested in the forces driving the climate system and how they are modeled by climate scientists.
In a career that spans over four decades, Robert D. Cess has pioneered the study of diverse topics and disciplines. He first attacked problems dealing with conductive, convective, and radiative heat transfer in engineering systems and his contribution to these topics culminated in a classic text book on radiative transfer. The hallmark of this early work is the successful application of singular peturbation techniques to solve complex radiative heat transfer problems. His intellectual curiosity took him to the study of thermal structure of planetary atmospheres. He is one of the very select few (if not the only one) who has solved the thermal structure of almost all of the inner and outer planets of the solar system including Mercury, Mars, Earth, Venus, Jupiter, Saturn, and others, including study of the satellites. He was probably the first to obtain an analytical solution for the radiative-convective equilibrium-temperature structure of the troposphere-stratosphere of Mars and Venus.
The latter part of his career has been focused exclusively on Earth, where he has made fundamental contributions to our understanding of the physics of climate with a particular focus on processes that regulate the Earth's radiation budget and the mechanisms of cloud feedback processes. He obtained worldwide recognition for a comprehensive comparative study of the nature of water-vapor and cloud feedback processes of over 15 three-dimensional climate models, and brilliantly demonstrated that cloud feedback is the major source for the wide range in climate sensitivity of climate models.