This heat is: 5 x 4,18 x m = 20,9 x m (in calories) where m is the mass of water.
Get it cold enough, and its state will change from liquid to solid.
To change the temperature of water from 27ºC to 32ºC will depend on the mass of water that is present. Obviously, the more water, the more heat it will take. This can be calculated as follows:q = heat = mC∆T where m is the mass of water; C is sp. heat = 4.184 J/g/deg and ∆T is 5ºC (change in temp).
The cause of evaporation is the continuous movement of molecules at the surface of a liquid; gaining more energy they can escape in the air. Temperature favors this process.
It depends on the material waters freezing point is 0deg celsius(32faren) but any other liquid in the element chart varies on many other things
I know it sounds a little stupid, but supercooling is when water remains a liquid while it is below freezing point. Note, only some waters can do this.
Liquid
Get it cold enough, and its state will change from liquid to solid.
So long as the water remains liquid, the temperature measures between 27 and 32 decrees F.
To change the temperature of water from 27ºC to 32ºC will depend on the mass of water that is present. Obviously, the more water, the more heat it will take. This can be calculated as follows:q = heat = mC∆T where m is the mass of water; C is sp. heat = 4.184 J/g/deg and ∆T is 5ºC (change in temp).
Specific heat
things take extra energy to change states, thus when water reaches boiling point the energy put into it goes into breaking up the bonds and changing it from a liquid to gas form
The Southern Ocean around Antarctica keeps temperatures between about 32 degrees F -- when the surface is frozen, and about 28 degrees F -- when the water is liquid. The water remains liquid below freezing temperature, because of the high saline content.
Sunlight warms the waters on the ocean surface. Some heat energy is transferred to cooler waters through convection.
The cause of evaporation is the continuous movement of molecules at the surface of a liquid; gaining more energy they can escape in the air. Temperature favors this process.
The major seasonal cause of water temperature change is due to the change in solar isolation in addition to currents and local hydrodynamics. Some more specific causes of water temperature variation in coastal waters may include: changes in the amount of river flow, discharges of 'cooling' waters from power plants, and changes in air temperature due to global warming.
warm waters in the summer cold waters in the winter
It can do.