By David W. Sims (Eds.)
Advances in Marine Biology has been supplying in-depth and updated reports on all features of Marine Biology considering that 1963 -- over forty years of exceptional assurance! The sequence is famous for either its excellence of experiences and enhancing. Now edited by means of D.W. Sims (Marine organic organization Laboratory, Plymouth, UK), with an the world over well known Editorial Board, the serial publishes in-depth and up-to-date content on quite a lot of themes that allows you to entice postgraduates and researchers in marine biology, fisheries technology, ecology, zoology, and organic oceanography. * Rated "Number 1" within the hugely aggressive type of Marine & Freshwater Biology by way of ISI within the 2000 ISI journals quotation record * continues an impression issue of 3.37, the top within the box * sequence positive factors over 35 years of assurance of the study
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Ocean heat content The ocean’s main role in climate variability and change is its huge capacity for the transport and storage of heat. , 2007). 06 W mÀ2. This large increase in heat storage has implications for seasonal and decadal variability in climate, transport and circulation by ocean currents, stratification, biology and biogeochemistry. All of these factors can lead to feedbacks to climate change. Because of its fundamental importance, there have been many studies of changes in ocean heat content.
2008). 2. Meridional overturning circulation in the Southern Ocean/Antarctica The Southern Ocean is a key region in the THC/MOC where the products of deep convection in the North Atlantic are upwelled and mixed into shallower layers. These waters are then converted into shallow and deep return flows to complete the overturning circulation (see Section 7). Profound physical changes have been observed in the water masses of both the shallow and deep return flows. The shallow limb of the MOC is sourced towards the northern flank of the Antarctic Circumpolar Current (ACC).
Because of its fundamental importance, there have been many studies of changes in ocean heat content. These have revealed deficiencies in both historical and recent global ocean datasets. Analyses have demonstrated significant time-dependent biases in the expendable bathythermograph (XBT) data that dominates the historical archive since the early 1970s until the recent advent of Argo profiling floats. Wijffels et al. (2008) have shown that biases in the fall rate of XBTs are the dominant source of error and that they can be reduced substantially.
Advances in Marine Biology by David W. Sims (Eds.)