Higher temperatures often result in greater precipitation primarily because higher temperatures simulate evaporation.
When temperatures rise, the rate of evaporation from bodies of water, such as oceans, lakes, and rivers, increases. This leads to more moisture being introduced into the atmosphere. As the air can hold more moisture at higher temperatures, this increased humidity can result in more precipitation when the moisture condenses and falls as rain or snow.
In summary, the correct statement is: High temperatures simulate evaporation.