ISOBATHYTHERM Meaning and
Definition
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An isobathytherm is a term used in oceanography to describe a line or contour on a map that connects points of equal water temperature at a specific depth within the ocean. The prefix "iso-" means equal, "bathy-" refers to depth, and "therm" pertains to heat or temperature. Therefore, an isobathytherm represents a line of constant temperature at a particular depth.
Isobathytherms are created by collecting temperature measurements from various points in the ocean and then plotting them on a map. By connecting points with the same temperature at a specific depth, a visual representation of the temperature distribution within the ocean can be obtained. Isobathytherms are often used in conjunction with other oceanographic data, such as isotherms (lines of constant temperature at the surface), to analyze and understand the thermal structure of the ocean.
The presence and shape of isobathytherms provide valuable information about ocean circulation patterns, heat distribution, and the formation of various oceanic features like currents, eddies, and upwelling zones. They are also useful for studying changes in ocean temperature over time and identifying areas of vertical mixing within the water column.
In summary, isobathytherms are contour lines representing equal temperatures at a specific depth within the ocean and are essential tools for analyzing and visualizing the thermal characteristics of the world's oceans.
Common Misspellings for ISOBATHYTHERM
- usobathytherm
- jsobathytherm
- ksobathytherm
- osobathytherm
- 9sobathytherm
- 8sobathytherm
- iaobathytherm
- izobathytherm
- ixobathytherm
- idobathytherm
- ieobathytherm
- iwobathytherm
- isibathytherm
- iskbathytherm
- islbathytherm
- ispbathytherm
- is0bathytherm
- is9bathytherm
- isovathytherm
Etymology of ISOBATHYTHERM
The word "isobathytherm" is derived from two Greek roots: "iso" meaning equal, and "bathys" meaning depth. The term "isobathytherm" is commonly used in oceanography and refers to a line on a map that connects points of equal depth.
