Introduction

By Sheila Xu and Costa Christopoulos

There are two "ingredients" needed for weather on Earth:

1) Temperature Gradient

The Earth receives more sunlight at the equator than anywhere else. Hence, the equator receives the most net energy gain and loses the energy at the Poles. Temperature gradient is created through this process of the heat transfer. 

2) Rotation

Rotation can have an effect on the circulation of the atmosphere. In the tropics (Equator), the Coriolis force (due to rotation) is small, so the Earth's rotation has less effect on the tropics. On the other hand, Coriolis force has more effect in the the middle and higher latitudes. 

Hadley Circulation

The process of the gain and loss of solar heat sets up a general circulation pattern where the warm air parcels rises near the equator, flows away from the equator until the 30 degrees latitude, sinks near the poles, and the flows back to the equator.This process is called Hadley Circulation. 

The air parcels are not able to move beyond the 30 degrees latitude due to the conservation of angular momentum, especially the zonal velocity of the air must increase. The Coriolis effect is small. 

(Source: http://www.cotf.edu/ete/modules/elnino/cratmosphere.html)

Tank Experiment of Hadley Circulation

In order to visualize the Hadley Circulation, a rotating tank experiment was set up. We define Hadley Circulation as a "low rotation" experiment since the effect of Earth's rotation is small. Place a bucket of ice in the center of the tank, which will represent the cold poles. Make sure to measure the mass of the ice beforehand (Our mass of ice was 675 grams). The equator will be represented at the edge of the tank, since it is warmer than in the center of the tank. Then, place eight thermometers in the tank to get data on temperature gradient inside of the tank. The set-up is shown as below:

(Top-view of the tank set-up)

(Side-view of the tank and thermometers placement) (Christopoulos, 2014)

The tank was rotated at 1 revolution per minute (rpm). Place permanganate potassium crystals and the blue dye in the tank to observe the motion of the dye and crystals. The crystals are used to observe the motion of the fluid at the bottom while the dye is for motion within the fluid. Place black paper dots on the surface of the water to observe the motion at the surface. Use the overhead camera to record the evolution of the tank.

Note that the tank moves in counterclockwise motion in the image below. The crystals move in clock-wise motion, opposite of the tank rotation, but the blue dye moves in the direction of the tank rotation. The crystals represent "Easterly wind" and the blue dye the "Westerly wind." 

Note how the cold water would slowly move out from the center at the bottom (such as Blue #1, #2) and the eventually, the temperature of the outermost thermosisters would drop. The trend of the graph clearly decreases over time. There are minor "bumps" in the graph, which could be attributed to the rotation of the tank. 

Then, we used the thermal wind equation for water, since water in the tank is an incompressible fluid:

where Ω = 0.1046 rad/sec, α = 207 * 10^-6^ K^-1, and dT/dr = 35.7 C/m. du/dz ended up to be 0.34 s^-1 from those values. The surface velocity was 0.054 m/s. The Hadley circulation is axisymmetric, especially in due to thermal wind balance with the radial temperature gradient. 

(Costa……not sure what else to say from those numbers above…)

Atmospheric Examples

We have evidences the circulation from climatological plots of February: 

(insert plots) 

Eddy Circulation

Eddies are formed at high rotation rates and at middle to high latitudes. Coriolis forces have more effect, in this case. Due to the rotation, the Coriolis forces overpower pressures from temperature gradients, so the Hadley circulation breaks down. However, the heat must be transported from the tropics to the sub-tropics and the poles:

(Source: http://paoc.mit.edu/12307/gencirc/climatology_lab.pdf)

This can be explained by the conservation of angular momentum. When air parcels move to the higher latitudes, their zonal velocity must increase and their radius of their paths must decease to conserve angular momentum. 

Tank Experiment of Eddy Circulation

The tank experiment of eddy circulation is similar to the set-up of Hadley circulation. We define eddy circulation "fast rotation." Thermometers are placed a little differently than the set-up of Hadley circulation: 

(Side-view of the tank and thermometers placement) (Christopoulos, 2014)

Another difference is that red and blue dye are used to observe the motion of cold and warm water in the tank. Blue dye is placed closer to the ice bucket while red dye is placed closer to the edge of the tank ("equator"). A series of images below show an evolution of the eddy circulation:

The rotation rate was set to 10 rpm. The bucket of ice contained a mass of 1200 g. Note that the red currents transport energy to the center.

The results from the thermometers are shown in the graph below:

There are larger temperature fluctuations, much more than the graph of the Hadley circulation tank experiment. This can be explained by the currents of the cold and warm water mixing. We estimated the fluctuation in the graph to be of an amplitude of 1 Celsius. Then, we calculated the radial heat flux so we can see the flow of heat into ice:

The power required to melt the ice is the latent heat of the ice times the amount of ice, divided by the amount of time it took for the ice to melt. L = 333 KJ/kg, m = 1.2 kg, t = 27 min (1624 sec), which came out to 0.246 kJ/s (246 Watts). 

However, we also want to see how much of heat was transported by the eddies: 

The area of the cylindrical surface at radius of 10 cm was 0.1 m^2. The velocity was .005 m/s. Using those values, the heat flux came out to 0.277 kJ/s (277 Watts). 

The values of the fluxes, 246 Watts and 277 Watts, are close to each other even though the values are different (as long they are in the same order of magnitude). 

Atmosphere

Two Regimes of Heat Transport