In oceanography, an overflow is a type of deep-water circulation in which denser water flows into an adjacent basin beneath lighter water. This process is significant in thermohaline circulation, contributing to the global ocean's deep water mass formation.[1] Overflows influence global climate by transporting heat and salt, impacting sea levels, and affecting marine ecosystems.
Overflows are driven by differences in water density, usually due to variations in temperature and salinity. A classic example is the Denmark Strait overflow, where cold, dense water from the Nordic Seas flows into the North Atlantic Ocean.[2]
References[edit]
- ^ Kida, Shinichiro (2006). Overflows and upper ocean interactions: a mechanism for the Azores current (Ph.D. Thesis). Joint Program in Oceanography/Applied Ocean Science and Engineering, Woods Hole Oceanographic Institution and Massachusetts Institute of Technology. Department of Ocean Engineering.
- ^ Käse, R. H.; Girton, J. B.; Sanford, T. B. (June 2003). "Structure and variability of the Denmark Strait Overflow: Model and observations". Journal of Geophysical Research: Oceans. 108 (C6). doi:10.1029/2002JC001548. ISSN 0148-0227.
Well, that’s interesting to know that Psilotum nudum are known as whisk ferns. Psilotum nudum is the commoner species of the two. While the P. flaccidum is a rare species and is found in the tropical islands. Both the species are usually epiphytic in habit and grow upon tree ferns. These species may also be terrestrial and grow in humus or in the crevices of the rocks.
View the detailed Guide of Psilotum nudum: Detailed Study Of Psilotum Nudum (Whisk Fern), Classification, Anatomy, Reproduction