Ice storms happens when a cold mass of air and a warm mass of air combine to create a ice storm
The final temperature of the liquid water after all the ice has melted will be 20 degrees Celsius. This can be calculated using the principle of conservation of energy, where the heat lost by the water in cooling down from 60°C to the final temperature is equal to the heat gained by the ice in melting and then heating up to 20°C.
It takes more thermal energy to raise the temperature of 5 grams of ice by 20 degrees Celsius. This is because you need to first melt the ice, which requires additional energy (the latent heat of fusion) before you can raise the temperature of the resulting water.
According to the law of conservation of momentum, the total momentum before the catch should equal the total momentum after the catch. Since the initial momentum of the ball is 200 kgm/s, the final momentum after the catch will also be 200 kgm/s shared between Jocko and the ball. The final velocity can be calculated using momentum = mass * velocity. Jocko and the ball will move across the ice at the same final velocity.
The potential energy of the safe can be calculated using the formula: Potential energy = mass x gravitational acceleration x height. Plugging in the values, we get: Potential energy = 20 kg x 9.8 m/s^2 x 0.5 m = 98 Joules. Therefore, the potential energy of the safe is 98 Joules.
There is no mass loss (nor gain) in state change, so there would be 100 grams of ice formed.
The heat absorbed by the ice can be calculated using the formula Q = m * L, where Q is the heat absorbed, m is the mass of the ice (20 kg), and L is the latent heat of fusion for ice (334 kJ/kg). Therefore, the ice absorbed 20 kg * 334 kJ/kg = 6680 kJ of heat as it melted.
1. Ice sheets contain enormous quantities of frozen water. If the Greenland Ice Sheet melted, scientists estimate that sea level would rise about 6 meters (20 feet). If the Antarctic Ice Sheet melted, sea level would rise by about 60 meters (200 feet). 2. The Antarctic and Greenland ice sheets contain more than 99 percent of the freshwater ice on Earth. 3. An ice sheet is a mass of glacial land ice extending more than 50,000 square kilometers (20,000 square miles).
Ice storms happens when a cold mass of air and a warm mass of air combine to create a ice storm
The final temperature of the liquid water after all the ice has melted will be 20 degrees Celsius. This can be calculated using the principle of conservation of energy, where the heat lost by the water in cooling down from 60°C to the final temperature is equal to the heat gained by the ice in melting and then heating up to 20°C.
You can tell if ice cubes have reached room temperature by observing if they have completely melted. Once they have melted, the water will reach room temperature. Placing a thermometer in the water can also confirm if it has reached room temperature.
6,660,000 J
Ice has a density of 916,8 kilograms per cubic meter or 0.9128 grams per cubic centimeter. 20 cubic meters of ice weigh then 20 times 916,8 = 18336 kilograms = 18.336 tonnes.
When ice melts, the absorbed heat energy is used to break the intermolecular bonds holding the solid structure of ice together, rather than increasing the temperature of the ice. This is known as the latent heat of fusion, and it occurs at a constant temperature until all the ice has melted.
The thermal power required can be calculated using the formula: Power = (mass * specific heat capacity * change in temperature) / time. Given data: mass = 2.5kg, specific heat capacity of ice = 2100 J/kg°C, specific heat capacity of water = 4200 J/kg°C, change in temperature = 20°C, and time = 2 minutes. First calculate the energy required to melt the ice (from -10°C to 0°C), then to heat the water to 20°C. Finally, divide the total energy by the time in seconds to get the thermal power.
A. 56 j
6,000 J