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At high latitudes, the Sun does not warm surface waters like it does in the tropics. Hence, water temperature stays constant with depth In other words, no thermocline exists. This type of water column is said to be isothermal Similar to temperature, density change with depth differs by latitude A pycnocline is a layer of ocean water that changes density rapidly that also exists between 300 and 1000 meters depth. This is similar to the thermocline mentioned in the introduction, but when temperature is high, density is low, and vice versa cline = slope) is a low-latitude feature. .High-latitude ocean waters are isopycnicr constant in density throughout the entire water column, Just as the thermocline prevents mixing of surface waters with the water below, so does the pycnocline. Imagine a researcher aboard an oceanographic vessel collects samples from the water column, extending from the surface to 3000 meters depth. Sample analyses shows that the water is isopycnich of the following statements correctly define wh Select the three statements below that apply. View Available Hint(s) The sample analyses show there is no pycnocline present Isopycniceans the samples of the water column have constant temperature throughout its depth. The temperature of the water column is constant throughout its depth The samples must have been taken from a location in the ocean at high latitude