Atmosphere, Ocean and Climate Dynamics : John Marshall :Lecture notes by Aarnout van Delden home. IMAU , a. These lecture notes are work-in-progress, i. If you have any comments or critiscm, please feel free to tell me. Science is never finished!
For advanced undergraduate and beginning graduate students in atmospheric, oceanic, and climate science, Atmosphere, Ocean and Climate Dynamics is an introductory textbook on the circulations of the atmosphere and ocean and their interaction, with an emphasis on global scales. It will give students a good grasp of what the atmosphere and oceans look like on the large-scale and why they look that way. The role of the oceans in climate and paleoclimate is also discussed. The combination of observations, theory and accompanying illustrative laboratory experiments sets this text apart by making it accessible to students with no prior training in meteorology or oceanography. Undergraduate or master-course students in meteorology, oceanography and climatology are the main target. The book begins with a discusssion of atmospheric characteristics; the final chapter on climate and climatic variability nicely leads into the subject of global warming, and should be read by anyone with an interest in the future of the planet. Highly recommended.
Wiegand, K. Geophysical Research Letters, 46 1 , Badin, G. Multi-scale Methods for Geophysical Flows. Iske Eds. Cham: Springer. Wahl, E.
For advanced undergraduate and beginning graduate students in atmospheric, oceanic, and climate science, Atmosphere, Ocean and Climate Dynamics is an.
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My research focuses on the dynamics of the climate system. The main emphasis of my work is to study the influence of the ocean on local and global scales, through the analysis of observations and a hierarchy of numerical simulations. Recently, I have worked on a wide range of topics including ocean redistribution of heat and carbon under climate change, regional sea level rise, air-sea coupling and predictability in mid-latitudes, ocean turbulence in climate models, and uncertainty quantification. More Posts. Some links press and radio related to our study on quantifying ocean warming over the historical record. More Publications. PDF Bibtex Project.
The large-scale oceanic currents that redistribute heat, salt and momentum in the top kilometer of water are driven by the mechanical stress exerted by the winds at the air-sea interface. In turn, the surface winds are shaped by the north-south temperature differences in the atmosphere. The temperature gradients in the atmosphere, largely determined by the sun's differential heating, are mitigated by the poleward heat transport due to the oceanic currents and the atmospheric flows. Thus, the ocean and the atmosphere work together to make our planet livable. Understanding the partitioning of heat transport between atmospheric and oceanic components, and how fluctuations arise because of the mutual interaction of the two systems, is a crucial aspect of climate dynamics. One approach is to construct simple models based on fundamental conservation principles of heat, salt and momentum. An example of oceanic and atmospheric fields resulting from one such model is shown in figure 1.