Stratification Flashcards

1
Q

What mathematical concept is used to describe stratification?

A

Stratification is described mathematically through density differences (∆ρ = ρ1 - ρ2).

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2
Q

What happens when stratification increases?

A

adds stability to water column.

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3
Q

What does stable mass distribution do in a stratified ocean?

A

resists vertical motion.

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4
Q

What is Brunt-Väisälä frequency (N) used for?

A

N quantifies stratification by measuring natural oscillation resulting from vertical displacement.

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5
Q

What indicates strong stratification according to Brunt-Väisälä frequency?

A

A large N indicates strong stratification and high stability.

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6
Q

What occurs during the mixing process in the ocean?

A

Mixing raises center of mass of water column and converts kinetic energy into potential energy.

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7
Q

What are the main layers mentioned in the ocean’s vertical structure?

A

The main layers are the thermocline, halocline, pycnocline, and mixed layer.

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8
Q

What is the importance of the surface mixed layer?

A

crucial for air-sea exchange and tropical cyclone development.

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9
Q

What characterizes the typical vertical structure of the open ocean?

A

It features a warmer, lighter upper mixed layer and a cooler, heavier lower stratified layer.

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10
Q

What can stratification block from mixing?

A

gases, nutrients, and heat between surface layer and deep ocean.

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11
Q

How does solar heating affect stratification?

A

Increased solar radiation reduces surface density, leading to increased stratification.

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12
Q

What seasonal changes impact mixed layer depth?

A

Winter leads to maximum mixed layer depth due to wind stirring and cooling, while summer results in thinner mixed layers.

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13
Q

What does the density anomaly in mixed layer depth refer to?

A

It refers to long-term averages of density differences in the mixed layer.

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14
Q

What role does wind mixing play in the mixed layer?

A

deepens mixed layer by entraining fluid from below.

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15
Q

How does buoyancy loss due to cooling/evaporation affect the mixed layer?

A

causes dense water at the surface to become unstable, leading to mixing.

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16
Q

What happens when buoyancy gain from heating/precipitation occurs in the mixed layer?

A

stabilizes surface water, can make the mixed layer shallower.

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17
Q

Why does mixing create a stair-step pattern in density and temperature profiles?

A

Multiple episodes of heating, cooling, and mixing contribute

18
Q

What is an effect of tropical cyclones on the mixed layer?

A

significant storm-driven mixing, which deepens the pycnocline.

19
Q

How can long-term seasonal stratification affect biological production?

A

Seasonal stratification controls biological production cycle due to impact on temperature and density gradients.

20
Q

What happens to the mixed layer at the end of winter?

A

deepens to maximum thickness due to erosion of stratification.

21
Q

What are the characteristics of an unstable density distribution?

A

vertical motion within water column.

22
Q

What is a key characteristic of the neutral state in stratification?

A

density has no influence on vertical motion.

23
Q

How is the mixed layer affected by diurnal heating?

A

Diurnal heating can lead to variability in mixed layer depth due to the difference between daytime heating and nighttime cooling.

24
Q

What is the effect of storm timing on mixing efficiency?

A

The timing of storms, especially in seasonally stratified shelves, can affect the efficiency of storm-driven mixing.

25
Q

How is density difference quantified in ocean studies?

A

Density difference is quantified using the equation ∆ρ = ρ1 - ρ2, which describes layers.

26
Q

What is indicated by a small Brunt-Väisälä frequency (N)?

A

A small N indicates weak stability and a small vertical density difference.

27
Q

What physical process is involved in vertical motion within stratified layers?

A

The distribution of density within the layers causes vertical motion.

28
Q

How does mixing in the mixed layer affect maximum chlorophyll levels?

A

by affecting nutrient availability and primary productivity.

29
Q

What seasonal phenomenon leads to the creation of the thermocline?

A

The seasonal warming of surface layers creates a temperature gradient that forms the thermocline.

30
Q

What is the significance of the nutricline in stratification?

A

The nutricline marks a region of rapid change in nutrient concentrations, which can be crucial for marine productivity.

31
Q

How does seasonal evolution affect the mixed layer?

A

Seasonal evolution impacts growth and decay of thermocline, affecting depth of mixed layer.

32
Q

What is the outcome of increased solar heating on water density stratification?

A

Increased solar heating results in reduced density at the surface, enhancing stratification.

33
Q

What do measurements of mixed layer depths often rely on?

A

temperature and density thresholds to define mixed layer properties.

34
Q

What is an example of a local factor impacting solar-driven stratification?

A

Local time variations can significantly affect spatial gradients of solar heating and stratification.

35
Q

What does the term ‘pycnocline’ refer to in ocean stratification?

A

a layer in the ocean where there is a rapid change in density with depth.

36
Q

How does the concept of kinetic energy relate to mixing in water columns?

A

Kinetic energy from mixing is converted into potential energy, facilitating the lifting of mass against gravity.

37
Q

What factors can influence the spatial footprint of river plumes?

A

Wind, river discharge, and initial shelf water conditions

38
Q

What does the mixed layer allow for in terms of bio-chemistry?

A

facilitates crucial processes for gas exchange and presence of photosynthesizers.

39
Q

What conditions characterize neutral stratification?

A

implies that density neither resists nor promotes vertical motion.

40
Q

How does the concept of stratification intersect with global climate?

A

Stratification is significant in the ocean as it affects gas and heat exchange, influencing global climate systems.

41
Q

What role does the atmosphere play in stratification dynamics?

A

surface layer’s contact with atmosphere facilitates gas and heat exchange crucial for stratification dynamics.