Thermocline - Wikipedia
A thermocline (also known as the thermal layer or the metalimnion in lakes) is a distinct layer based on temperature within a large body of fluid (e.g. water, as in an ocean or lake; or air, e.g. an atmosphere) with a high gradient of distinct temperature differences associated with depth.
What is a thermocline? - NOAA's National Ocean Service
A thermocline is the transition layer between warmer mixed water at the ocean's surface and cooler deep water below. The red line in this illustration shows a typical seawater temperature …
11.7: The Seasons and the Thermoclines - Geosciences LibreTexts
The warming of the surface waters creates a temperature difference between the uppermost layer and the layer beneath it. The boundary between the now-warmer surface layer and the still-cold layer beneath it represents a different kind of thermocline, the seasonal thermocline.
Understanding Thermoclines In Ocean Waters - Marine Insight
2021年4月7日 · In this article, we will look at thermoclines, the role they play in the marine ecosystem, the various ocean layers, the impact on marine life, and a unique aspect of thermocline impact on the field of naval design and engineering.
Thermocline Graph - College of Exploration
The oceans have a well-mixed surface layer where the water temperatures are relatively constant. Below the mixed layer is the thermocline, a zone where temperature changes rapidly with depth. Below the thermocline the temperature is relatively uniform with depth, showing only a small decrease to the ocean bottom.
Thermocline - an overview | ScienceDirect Topics
The thermocline is defined as a layer within the water column where the vertical gradient of temperature is a local maximum. From: Encyclopedia of Atmospheric Sciences (Second Edition), 2015
Thermocline climatology depicted from March to November in a ...
Thermocline climatology depicted from March to November in a observations (ECMWF) and b March-initialized CFSv2 forecasts. Red oval in panelb highlights the deeper thermocline in SWEIO...
Thermocline - an overview | ScienceDirect Topics
The thermocline is an advective feature formed through the circulation tilting the horizontal contrast in surface density over the subtropical gyre into the vertical. The subducted thermocline extends over the mixed-layer density range within the subtropical gyre.
What Is a Thermocline and How Is It Formed? - thedailyECO
2024年1月30日 · The thermocline, observed in oceans, lakes, and rivers, is a distinctive phenomenon characterized by a vertical layer within the water column, signaling a rapid temperature change. This transition occurs abruptly between two water strata with differing temperatures, typically situated at a specific depth.
THERMOCLINE - thermopedia.com
The thermocline is the layer of sea water in which the temperature changes rapidly (≥1°C/100 m) with distance from the surface. The surface water temperature is controlled by radiative heating (from the sun) or cooling (to the night sky) and convective heating or cooling from/to the atmosphere; currents and wave action keep this layer well ...
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