Long-term global ocean salinity variation provides an insight into water cycle change. This connection reflects changes to the evaporation and precipitation (E–P) fields along with terrestrial runoff, which comprises the global water cycle and sets the spatial pattern of salinity on the ocean surface. The dynamic nature of the global ocean ensures that along with E–P, temperature and circulation changes also play a role in driving patterns of salinity change. This chapter provides an introduction to the global water cycle, briefly outlines the history of ocean salinity observation, and introduces results that relate resolved salinity change to water cycle change. Because of sparse observational coverage, the use of climate models are necessary to investigate these relationships. Long-term changes to global ocean salinity suggest that an unambiguous and coherent water cycle change has occurred over the twentieth and early twenty-first centuries. Climate model simulations project that such changes will intensify in the twenty-first century in response to continued greenhouse gas emissions.
Frankignoul C, Sennéchael N. Observed influence of North Pacific SST anomalies on the atmospheric circulation. J Clim. 2007;20:592–606. ... Fratantoni DM, Bower AS, Johns WE, Peters H. Somali Current rings in the eastern Gulf of Aden.
OpenAD/F: a modular, opensource tool for automatic differentiation of Fortran codes. ACM Trans Math Softw. ... Vinogradova NT, Ponte RM, Tamisiea ME, Quinn KJ, Hill EM, Davis JL. Selfattraction and loading effects on ocean mass ...
The book represents all the knowledge we currently have on ocean circulation.
In: Goni, G.J., Malanotte-Rizzoli, P. (Eds.), Interhemispheric Water Exchange in the Atlantic Ocean. Elsevier Oceanogr. Ser., vol. 68. Elsevier, Amsterdam, pp. 411–442, Chapter 16. Johnson, G.C., Zhang, D., 2003.
An inherent feature of the climate is its strong variability on a vast range of timescales, from seasonal to multimillennial and beyond.
The Southern Ocean circulation connects the ocean basins as well as the upper and deep layers of the ocean. As a result, the region has a profound influence on the global ocean circulation and climate.
How do ecosystems react to anthropogenic pressure? This text gives a simple introduction to the concepts, the methods and the applications of marine geochemistry with a particular emphasis on isotopic tracers.
The book comprises chapters covering distinct aspects of contrasting ocean currents: broad and slow, deep and shallow, narrow and swift, large scale and small scale, low latitudes and high latitudes, and moving in horizontal and vertical ...
In The Great Ocean Conveyor, Broecker introduces readers to the science of abrupt climate change while providing a vivid, firsthand account of the field's history and development.
This is the first book to deal with all aspects of the ocean's large-scale meridional overturning circulation, and is a coherent presentation, from a mechanistic point of view, of our current understanding of paleo, present-day, and future ...