QUESTION IMAGE
Question
analysis of data
- describe the general shape of the temperature - depth curve:
a) at low latitudes
b) at mid latitudes in winter
c) at mid latitudes in summer
d) at high latitudes
- label the three temperature layers for each location: surface layer, thermocline, deep and bottom layer. on graph
- which two locations indicated by your graphs might require the use of a wetsuit (or drysuit) to prevent hypothermia when swimming in the ocean? why?
- approximately where (at what depth) is the primary thermocline:
a) at low latitudes
b) at mid latitudes in winter
c) at mid latitudes in summer
d) at high latitudes
Brief Explanations
- a) Low latitudes: The temperature - depth curve at low latitudes typically shows a warm surface layer, a well - defined thermocline where temperature drops rapidly with depth, and a cold deep and bottom layer.
- b) Mid - latitudes in winter: The surface layer is cooler due to colder air temperatures. The thermocline is less pronounced compared to summer, and the deep and bottom layers are cold.
- c) Mid - latitudes in summer: There is a warm surface layer heated by the sun. A distinct thermocline separates the warm surface from the cold deep and bottom layers.
- d) High latitudes: The surface layer is cold, and there is little to no well - defined thermocline as the water column is relatively uniformly cold, with the deep and bottom layers being only slightly colder.
- On graph: For each location, label the uppermost layer as the Surface Layer (where temperature is most affected by the atmosphere), the layer with a rapid temperature change as the Thermocline, and the lower, colder layers as the Deep and Bottom Layer.
- Locations for wetsuits/drysuits: High latitudes and mid - latitudes in winter. In high latitudes, the water is cold throughout the water column due to the low solar input. In mid - latitudes in winter, the surface water is cold from the cold air temperatures, and swimming without proper protection can lead to hypothermia.
- Depth of primary thermocline:
- a) Low latitudes: Usually between 100 - 1000 meters.
- b) Mid - latitudes in winter: May be around 50 - 200 meters or less distinct.
- c) Mid - latitudes in summer: Around 100 - 500 meters.
- d) High latitudes: May be very shallow or non - existent, but if present, less than 50 meters.
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1.
- a) Warm surface layer, distinct thermocline, cold deep and bottom layer.
- b) Cooler surface layer, less pronounced thermocline, cold deep and bottom layer.
- c) Warm surface layer, distinct thermocline, cold deep and bottom layer.
- d) Cold surface layer, little to no distinct thermocline, cold deep and bottom layer.
- Label on graph as described above.
- High latitudes and mid - latitudes in winter. Reason: Cold water temperatures can cause hypothermia.
4.
- a) 100 - 1000 meters.
- b) 50 - 200 meters or less distinct.
- c) 100 - 500 meters.
- d) Less than 50 meters or non - existent.