Final answer:
The strong trade winds cause the thermocline to be (b) shallower in the eastern tropical Pacific compared to the western Pacific.
Step-by-step explanation:
The strong trade winds in the tropical Pacific Ocean create significant differences in the thermocline between the eastern and western parts of the ocean. Due to the piling up of warm surface waters in the western tropical Pacific caused by these winds, the thermocline in the eastern tropical Pacific becomes shallower compared to the western Pacific.
This is because the transport of surface waters toward the west intensifies the slope of the thermocline, causing it to dip deeper in the west and rise closer to the surface in the east, thereby making it shallower in the eastern tropical Pacific.