The layer in the oceans that undergoes heating and cooling as seasons change is the mixed layer, approximately 100-200 meters thick, followed by the thermocline.
The layer in the oceans subject to heating and cooling as the seasons change is the mixed layer. This layer is typically around 100-200 meters thick in mid-latitude regions. Below the mixed layer, there is a rapid decline in temperature known as the thermocline, where the temperature decreases with depth.
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