Air has a heat capacity of 1007 J/(kg K).Water has a heat capacity of 4218 J/(kg K).There is approximately a factor of four difference.
When comparing the effective heat capacities of a column of air and a column of water, the relative masses of the columns must be considered;
A column of air extending to mean sea level (no topography) has a mass of 10^4 kg / m^2 (surface pressure divided by gravity). Thus a column of atmosphere has a heat capacity of about 10^7 J/m^2.
The same mass is found in 10 meters depth of water. Thus, a column of water has a heat capacity of 4*10^7 * (depth / 10 m) J/m^2.
Thus, when comparing the heat capacity of a water column and an air column, there is a factor of four difference for the heat capacity and a factor of water depth / 10 meters for the masses. For example, a 50 meter column of water (typical mixed layer depth) has 4*50/10 = 20 times that of air.
I would love to know some values for the land surface... that's how I ended up here.
The specific heat of soil is 123457 degress celcious.
14256987 degress
specific heat of lpg
Because land needs the sun. Suppose the water was in a frying pan. And then think about land in a frying pan. Land is a solid, water is a liquid thus the molecules are moving around if they are heated. And think about a blacktop if you step barefoot on it it will hurt because the color attracts light and so does land. Water is transparent meaning the color soesnt attract the sunlight as much as land.
By heating and cooling more slowly than land or air
aluminium
specific heat of benzen sulphonic acid
Breezes are created when there are specific heat differences between land and ocean.
their specific heat, the specific heat is the amount of jewls (unit of work) divided by mass (kg). land has an average specific heat of 300-800. water has a specific heat of 4180 which means it takes much more energy to heat up or cool it down
WATER
Specific heat refers to the amount of heat energy required to raise the temperature of a substance. In the context of local winds, specific heat affects the temperature of the land and water. Land has a lower specific heat compared to water, meaning it heats up and cools down faster. This difference in specific heat causes differential heating, leading to temperature differences and the formation of local wind patterns such as sea breezes and land breezes.
Water heats and cools slower than land. It is because the specific heat is the amount of heat that it takes to be raised to a certain temperature. If the heat is higher it would take longer to heat and cool. That is my interpretation anyways.
it heats up much faster, the specific heat value of water is very low, and the specific heat value of land is almost always higher than that of water.
Breezes are created when there are specific heat differences between land and ocean.
Absorption of heat by land(compared to water)Specific heat of land is 0.84J/kg and that of water is 4.2J/Kg.So:-4.2-0.84=3.6Therefore, land gets heated up 3.6 times faster than water.
Water has a higher specific heat, and this is an intensive property of the substance itself.
The land because water takes time to heat and cool. Also if the piece of land is dark colored then it will absorb more solar radiation then the water.
Breezes are created (apex)
Water has a higher specific heat than land.