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The _____ method studies currents by travelling with their flow. the ______ methdo studies currents by measuring the water that flows by a fixed point
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
the primary source of deep and bottom water is from
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
without current the world's climates would be
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
thermohaline circulation is water movement caused by
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
during a warm phase ENSO event, warm water ____________. this event causes ___________
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
The test is on what chapter
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
the ocean conveyor belt is improtant because
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
based on density stratification, the primary water mass classifications include
accumulaties in the Eastern Pacific, near South America, dramatic weather changes
Chapter 8 and 9
central water, intermediate water, and deep water
it redistributes heat and moderates the Earth\\\'s climate
more extreme
high latitudes due to freezing and cooling raising the salinity and density
Lagrangian, Eularian
water density differences
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