Density Functions - Oceanography

In summary, the equation A(x)=int(p(y),y=0..x) represents the total number of cod in a water column up to a certain depth x, where p(y) represents the density of cod at a certain depth y. To find the total number of cod, we can use the equation A(x)=10x, where x is the depth of the water column. The depth at which the fish density is largest can be found by looking at the graph of p(y), and the number of cod between two depths can be found by subtracting the areas under the curve.
  • #1
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Homework Statement



http://img39.imageshack.us/img39/3143/calcquiz3.jpg

The writing says: A(x)=int(p(y),y=0..x) <-- Maple format

Homework Equations



A(x)=int(p(y),y=0..x)

The Attempt at a Solution



So I did not attend class the day we went over this and he only went over it that day. I honestly have no idea how to even go about doing it, but here's a stab in the dark:

I believe the "water column" he is talking about is a rectangular prism with length=1 m, width=1 m, and height=50 m.

The density function is p(x)=10 cod per cubic meter (where p is "rho" and x is an area?)

a. Total number of cod in water column- Wouldn't this be the area of the column * 10?

So, A=LWH=50 m^3. 50*10=500 cod. Also, this is the same answer I would get if I took the Area under the curve p(x)=10 from x=0..10.

For the other functions, would I take the area under the curve as well?

b. Depth where fish density is largest - Would this be the maximum point on the graph? If so, the first one would be 0<x<50 because the density of fish is constant.

c. Number of cod between 20 and 30 meters - Simply the area under the curve from 20 to 30?


Any help is much appreciated!

Thanks,
Ryan
 
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  • #2


Dear Ryan,

It seems like you have a good understanding of the problem and the concepts involved. Let's break down the problem and go through it step by step.

First, let's define the variables and units involved:
- A(x) represents the total number of cod in the water column up to a certain depth x (in meters).
- p(y) represents the density of cod at a certain depth y (in cod per cubic meter).
- x represents the depth in meters.
- y represents the height in meters.
- The dimensions of the water column are 1m x 1m x 50m.

Now, let's look at the equation A(x)=int(p(y),y=0..x). This is a definite integral, which means it represents the area under the curve of the function p(y) from y=0 to y=x. In other words, it is the total number of cod in the water column up to a certain depth x, since p(y) represents the density of cod at a certain depth y.

a. To find the total number of cod in the water column, we use the equation A(x)=int(p(y),y=0..x). Since p(y) is a constant function (10 cod per cubic meter), the integral becomes A(x)=10x. Substituting x=50 (since the water column is 50m deep), we get A(50)=10(50)=500 cod.

b. The depth where the fish density is largest can be found by looking at the graph of p(y). Since p(y) is a constant function, the density is the same at all depths. Therefore, the maximum point on the graph is at any depth between 0 and 50 meters.

c. To find the number of cod between 20 and 30 meters, we use the equation A(x)=int(p(y),y=0..x). We want to find the area under the curve of p(y) from y=20 to y=30. This can be done by subtracting the area under the curve from y=0 to y=20 from the area under the curve from y=0 to y=30. In other words, A(30)-A(20)=int(p(y),y=0..30)-int(p(y),y=0..20). Since p(y) is a constant function, this becomes 10(30)-10(20)=
 

1. What is a density function in oceanography?

A density function in oceanography is a mathematical representation of the variation in density of seawater with depth. It helps scientists understand how density changes affect ocean currents, mixing, and circulation patterns.

2. How is density measured in the ocean?

Density in the ocean is typically measured using a CTD (conductivity, temperature, and depth) sensor. This instrument collects data on the temperature and salinity of seawater, which are used to calculate density.

3. What factors affect the density of seawater?

The density of seawater is primarily affected by temperature and salinity. As temperature increases, density decreases, and as salinity increases, density increases. Other factors such as pressure, depth, and dissolved substances can also impact density.

4. How does density affect ocean circulation?

Density plays a crucial role in ocean circulation. Differences in density between water masses create variations in buoyancy, which drive the movement of water. This movement, along with other factors such as wind and Earth's rotation, contributes to the complex patterns of ocean currents.

5. What is the significance of understanding density functions in oceanography?

Understanding density functions is essential for predicting and studying the behavior of the ocean. It helps scientists track the movement of water, nutrients, and organisms, and also plays a critical role in climate models and predicting the effects of climate change on the ocean.

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