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 difference in precipitation in different regions is mainly influenced by variations in atmospheric conditions such as temperature, air pressure, wind patterns, and humidity. Other factors like topography and proximity to large water bodies can also play a role in determining precipitation patterns.
The average temperature in the winter of 2011 was slightly higher compared to the winter of 2010. This difference could be due to fluctuations in global weather patterns or other climatic factors.
It is more COLDER in the POLES and it is more WARMER by the EQUATOR.So therefore the temperature by the equator is warmer and the temperature by the poles is much colder.
Climate refers to the long-term patterns of weather in a particular region, including factors such as temperature, precipitation, and wind patterns. Temperature, on the other hand, specifically measures the degree of hotness or coldness in the atmosphere at a given time and place. Temperature is just one component of climate.
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winds patterns
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.
When the temperature on the ground is different from the temperature high in the atmosphere, it creates a difference in air density. This difference can lead to the formation of weather patterns such as wind, clouds, and precipitation as the air tries to equalize the temperature difference.
Scientific Law
The Coriolis effect explains this phenomenon clearly. Pressure belts and wind belts differ in patterns depending on certain atmospheric factors like temperature.
Desceibe some of the general patterns you observe for temperature and salinity
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temperature
Narration that tries to imitate the patterns of real thought.
The difference in precipitation in different regions is mainly influenced by variations in atmospheric conditions such as temperature, air pressure, wind patterns, and humidity. Other factors like topography and proximity to large water bodies can also play a role in determining precipitation patterns.
The average temperature in the winter of 2011 was slightly higher compared to the winter of 2010. This difference could be due to fluctuations in global weather patterns or other climatic factors.