Rainfall and Evaporation - Essay Example

Introduction

In the comparison of temperature rainfall and evaporation under the per cent of the normal index for Nakhon Swan. Regarding temperature, the SPI relation shows that through that year, the temperatures were high compared to rainfall but slightly high. Whenever rainfall was high, the temperatures dropped while evaporation took a higher sport than temperature but lower than rainfall. Regarding the year 2011, whereby the evaporation bar was low while the rainfall bar was highest and these led to low evaporation rate. In short, it can be put down that the lower the rainfall, the higher the temperature and the higher the temperature, the higher the rate of evaporation. Annually it's observed the temperature was evenly distributed and created a friendly environment in the province hence creating a balance of the weather conditions all through.

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Decile Index

In terms of the decile index regarding temperature rainfall and evaporation in their relationship, it shows that each year experienced different variations to the relationship recorded. Throughout, the temperatures recorded shows that when the temperature was moderate, and the level of rainfall was very high while the evaporation rate remained moderate. Due to this variation, it shows that the level of the decile index was below 30. This indicates that the rainfall took the greatest part of the index hence lowering the decile index. Through this, it shows that even though the province recorded high rainfall, there was an aspect of drought, and that is what made the decile index record the lowest throughout the years.

Studying through the standardized precipitation index, it clearly shows that the temperature into relation with the rainfall changed with the degree of dryness when the values fluctuated until zero. The SPI was very low because when the temperature recorded high, the level of evaporation became intense even though the rainfall recorded at the highest rate. In the argument, it seems that the rainfall however high it was unable to balance the rate at which the temperatures controlled the province hence creating a chance for a relatively high evaporation rate of water into the atmosphere. This aspect lowers the fact the rainfall was high, bringing it down to the average result of rainfall in the region. This clearly shows that the higher the rate of evaporation, the higher the temperature and the lower the amount of water in the ground.

Looking at the three analyses of data into comparing the temperature rainfall and evaporation it clearly shows that for one to take place, there must be a competitive aspect and dependency in an example it clearly shows that when the temperature rises the chances of evaporation will be high even if the rate of the rainfall is high. This shows the dependency on each aspect of the climate.

Meteorological Weather Patterns

On comparing the temperature rainfall and evaporation under the per cent of the normal index for Kamphaeng Phet. Concerning temperature, the SPI relation shows that through that year, the temperatures were high compared to rainfall but slightly high. At the moment rainfall was high the temperatures dropped while evaporation took a higher sport than temperature but lower than rainfall. This can be given through an example in figure 37, regarding the year 2011, where the evaporation bar was low while the rainfall bar was highest, and these led to a low evaporation rate. In short, it can be put down that the lower the rainfall, the higher the temperature and the higher the temperature, the higher the rate of evaporation. Yearly it is observed the temperature was evenly distributed and created a friendly environment in the province hence creating a balance of the weather conditions all through.

In decile index regarding temperature rainfall and evaporation in the relationship, it shows that each year experienced different variations to the relationship recorded. All through the temperatures recorded shows that when the temperature was moderate, and the level of rainfall was very high while the evaporation rate remained moderate. Due to this variation, it shows that the level of the decile index was below 30. This indicates that the rainfall took the greatest part of the index hence lowering the decile index. Through this, it shows that even though the province recorded high rainfall, there was an aspect of drought, and that is what made the decile index record the lowest throughout the years.

Also taking a study on the standardized precipitation index, it clearly shows that the temperature into relation with the rainfall changed with the degree of dryness when the values fluctuated until zero. The SPI was very low since when the temperature recorded high, the level of evaporation became intense even though the rainfall recorded at the highest rate. In the argument, it seems that the rainfall however high it was unable to balance the rate at which the temperatures controlled the province hence creating a chance for a relatively high evaporation rate of water into the atmosphere. This aspect lowers the fact the rainfall was high, bringing it down to the average result of rainfall in the region. This clearly shows that the higher the rate of evaporation, the higher the temperature and the lower the amount of water in the ground.

Conclusion

In all the three analyses of data into comparing the temperature rainfall and evaporation, it clearly shows that for one to take place, there must be a competitive aspect and dependency in an example it clearly shows that when the temperature rises the chances of evaporation will be high even if the rate of the rainfall is high. This shows the dependency on each aspect of the climate as related to the description and modulation.