Explanation of the experience : The hot
water, colored red, moves in borrowing spreads so the
top tube on the cold water colored blue and shoot down the
tube. The cold water moves via the lower tube and
passes under hot water. Arriving in
the compartment hot,
cold water is warmed gradually and slowly rises up the tube,
driven by cold water coming through the bottom tube.
The witness made at uniform temperature,
but with two different dyes in each compartment shows a lack of
movement of water, which shows that water movements observed are indeed due to a
thermal gradient.
Water weighing and calculating their density also shows that the difference in temperature ultimately results in a difference in water density.
Conclusion : Hot
water is less dense than cold water, this difference in density causes a flow of water.
Photos from our own experience
The hot
water circulates well colored red by the
top tube.
The hot
water, less dense colored in
red moves and pushes the cold water down.
We performed the
same experiment by exchanging dyes, ie hot
water is now colored blue and red with cold water.
Regarding the Gulf Stream, the warm equatorial water moves poleward at
the surface and cold polar water runs deep towards the
equator.
b) What is
the influence of salinity?
Hypothesis : The salinity of the water plays a
role in the
movement of oceanic water masses.
Verifiable consequence : If the
hypothesis is correct then we should observe a movement of water along a salinity gradient.
It performs the following experience :
Photos from our own
experience:
The colorful saltwater moves through the tube bottom.
We performed the
same experiment but changing colors. The water is colored blue freshwater colorless and water is salt water :
Regarding the Gulf Stream, making sea
ice causes an increase in salinity, so the density of ocean water around the sea
ice of this, the
pole, the
very cold temperatures cause the formation ice in
winter. This ice is
not salty, so the
more ice, more ocean water around the sea
ice is salty. The water that reaches the pole from the
equator, so cool and will be increasingly saline thus becoming more dense, which makes his dive.