The difference in temperature patterns between Lihue and Kilauea is because of altitude. Kilauea is 364m above mean sea level and Lihue is 31m above mean sea level.
Given the elevations of the two location, the phase difference can be calculated by the average lapse rate of 6.5oC to every 1000m (.0065oC to 1m). The difference between both cities is 364m - 31m = 333m. Using the phase difference calculation, the difference of 333m would lead to a temperature difference of (333 * .0065) 2.1645oC.
The temperature difference between Lihue and Kilauea can be attributed to their different elevations and proximity to the ocean. Kilauea is located at a higher elevation, which generally results in cooler temperatures, while Lihue is closer to the ocean, which tends to moderate temperatures due to the maritime influence. Additionally, local weather patterns and microclimates can also play a role in temperature variability between the two locations.
The temperature difference between the equator and poles is mainly due to the Earth's tilt and curvature. The equator receives more direct sunlight year-round, leading to warmer temperatures, while the poles receive less direct sunlight, leading to colder temperatures. This temperature difference drives atmospheric and oceanic circulation patterns, influencing global climate.
The temperature difference between 74°F and 63°F is 11°F.
To calculate the delta temperature, you will take the difference between the final and initial temperature.
The difference in temperature between a warm tube misfire and a warm tube misfire in hot weather is the temperature that resulted in the hot weather .
Aldebaran has a surface temperature of around 3,900 Kelvin, while Algol has a surface temperature of around 5,500 Kelvin. The temperature difference between Aldebaran and Algol is approximately 1,600 Kelvin.
To find the difference in temperature between two values, subtract the smaller temperature from the larger temperature. The result will give you the difference in temperature.
There is no difference between "Temprature" and "Temperature." "Temprature" appears to be a misspelling of "Temperature," which refers to the degree of hotness or coldness of an object or environment.
A conclusion explains what you found out by your research. An evaluation explains what went well and what could have been improved and how.
Different Patterns
A degree is a unit of temperature.
The difference in temperature refers to the variation in temperature between two points, objects, or times. It indicates the degree of variation in heat energy between the two points, with a larger temperature difference indicating a greater contrast in temperature.
Creating a bigger temperature difference between the poles and the equator leads to a stronger pressure gradient force in the atmosphere, driving stronger winds. This temperature difference causes air to move from high pressure to low pressure areas, resulting in faster wind speeds. The Coriolis effect also plays a role in shaping wind patterns based on the Earth's rotation.
The difference between two temperatures is the numerical value that represents how much one temperature is larger or smaller than the other. To calculate the temperature difference, you subtract the lower temperature from the higher temperature.
The annual range of temperature may be described as the difference between the average of the highest and lowest temperatures recorded during a year.
The main difference between heat and temperature is that temperature measures the average kinetic energy of the particles in a substance, while heat is the transfer of energy between two substances due to a temperature difference. Temperature is a scalar quantity, while heat is a form of energy.
The difference between the hottest temperature of 134F and the coldest temperature of -128F is 262 degrees Fahrenheit. This represents the range of temperatures between the two extremes.
The difference in temperature between the ocean and the sand is primarily due to the difference in their heat absorption capacities. Water has a higher specific heat capacity compared to sand, so it heats up and cools down more slowly. As a result, the ocean retains heat for longer periods of time compared to sand, leading to differences in temperature between the two.