By Jochen Kämpf, Piers Chapman
ISBN-10: 3319425226
ISBN-13: 9783319425221
ISBN-10: 3319425242
ISBN-13: 9783319425245
Upwelling structures are exact locations within the oceans the place nutrient-enriched water is introduced into the euphotic region to gasoline phytoplankton blooms that, through marine food-web interactions, create the world’s richest fish assets. This ebook introduces the reader to the interdisciplinary technological know-how of upwelling and gives a accomplished review of the world’s most efficient marine ecosystems within the context of weather variability, weather switch and human exploitation. This fabric provided is appropriate for undergraduate and postgraduate examine or simply for somebody to profit in regards to the construction of lifestyles within the oceans and the way this can be compromised by way of human activities.
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Additional info for Upwelling Systems of the World: A Scientific Journey to the Most Productive Marine Ecosystems
Example text
1971; Wyrtki 1973) and many other legacies such as the first comprehensive description of the Somali Current coastal upwelling system (see Chap. 8). Data from IIOE still underpin current scientific research half a century later, such as research on upwelling in the Arafura Sea (see Sect. 3). These early expeditions set the foundation for our understanding of upwelling systems. , was pivotal to the understanding of processes involved in the biological pump (Ducklow et al. 2001). 26 1 Preliminaries Fig.
R. 1974. The oceans food web: a changing paradigm. BioScience 24: 409–504. Redfield, A. 1958. The biological control of chemical factors in the environment. American Scientist 46: 205–221. , R. Murnane, and C. LeQuere. 1995. Air-sea CO2 transfer and the carbon budget of the North Atlantic. Philosophical Transactions of the Royal Society London (B Biological Science), 348: 211–219. A. 2007. Introduction to ocean sciences, 2nd ed. W Norton & Company. 581 pp. , and G. Hempel. eds. 2008. The UNEP large marine ecosystem report: a perspective on changing conditions in LMEs of the world’s Regional Seas.
Although the Coriolis force vanishes at the equator it comes into full swing at relatively short distances (>50 km) from it. Due to this spatial variation of rotational effects, the dynamical role of the equator in the upwelling process is similar to that of coasts. Ice‐edge upwelling is created via a substantial dampening of the effect of wind stresses on currents under the sea ice. Depending on typical wind conditions in a region, coastal upwelling can be either a quasi‐permanent feature in so‐called major coastal upwelling systems or a seasonal feature in seasonal coastal upwelling systems.
Upwelling Systems of the World: A Scientific Journey to the Most Productive Marine Ecosystems by Jochen Kämpf, Piers Chapman
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