Downscaling global ocean climate models improves estimates of exposure regimes in coastal environments

validation of global ocean tide models in coastal regions of persian gulf and oman sea using coastal tide gauge observations

in recent years, several ocean tide models have been used to calculate tides using data of satellite and tide gauges data. global ocean tide models have many applications in various sciences such as geophysics, geology and geodesy and oceanography. considering­ the existence of many models, a quantitative evaluation of research, and ranking and selecting the best model of the global ocean tide ...

Fundamentals of Ocean Climate Models Fundamentals of Ocean Climate Models

Microbial biogeochemistry of coastal upwelling regimes in a changing ocean

711 The coastal upwelling regimes located along the eastern boundaries of the Pacific and Atlantic Ocean basins are small in size, but make a disproportionate contribution to the productivity and microbial biogeochemistry of the ocean. These regimes include the California and Peru/Humboldt current systems in the Pacific, and the Canary and Benguela current systems in the Atlantic. Their charact...

Modelling the global coastal ocean.

Shelf and coastal seas are regions of exceptionally high biological productivity, high rates of biogeochemical cycling and immense socio-economic importance. They are, however, poorly represented by the present generation of Earth system models, both in terms of resolution and process representation. Hence, these models cannot be used to elucidate the role of the coastal ocean in global biogeoc...

Estimates of Cabbeling in the Global Ocean

Owing to the larger thermal expansion coefficient at higher temperatures, more buoyancy is put into the ocean by heating than is removed by cooling at low temperatures. The authors show that, even with globally balanced thermal and haline surface forcing at the ocean surface, there is a negative density flux and hence a positive buoyancy flux. As shown by McDougall and Garrett, this must be com...