Water is very unusual in that it's solid density is lower than that of it's liquid state (hence ice floats). As such when you increase the temperature of solid water (ice) and cause it to melt, it's volume will decrease and so it will become more dense. Increasing the temperature of the water continues to increase the density and decrease it's volume until around 4 degrees Celsius where it's density reaches a maximum (and so it has a minimum volume).
This fact allows bodies of fresh water such as lakes and ponds to freeze at the surface and remain fluid underneath as the warmer water is actually at a higher density and sinks to the base of the pond or lake.
Above this temperature, water begins to expand as it is heated resulting in a decrease in density and an increase in volume.
100 degrees Fahrenheit = 37.78 degrees Celsius
At 1 degree Celsius, water is in its liquid state. This is because it is above its freezing point of 0 degrees Celsius but below its boiling point of 100 degrees Celsius at standard atmospheric pressure.
100.5 degrees Fahrenheit = 38.06 degrees Celsius.
170 degree Celsius = 338 degree Fahrenheit
25 degrees Celsius is equal to a temperature of 77 degrees Fahrenheit.
17 degrees Celsius is colder than 30 degrees Celsius. The lower the temperature in degrees Celsius, the colder it is.
-5 degrees Celsius is 6 degrees colder than 1 degree Celsius.
18 degrees Celsius is colder than 20 degrees Celsius.
At 100 degree celsius water starts boiling. It starts changing into water vapour. 100 degree celsius is the boiling point of water.
0.6 degree Celsius = 33.08 degrees Fahrenheit,
0.9 degree Celsius = 33.62 degrees Fahrenheit.
14 degree Fahrenheit = -10 degree Celsius
0 degrees Celsius is equal to 32 degrees Fahrenheit.
28 degree Celsius = 82.4 degree Fahrenheit
100 degrees Fahrenheit = 37.78 degrees Celsius
42 degrees Celsius = 107.6 degrees Fahrenheit
400 degree Celsius = 752 degree Fahrenheit.