If you double the air temperature, the chirp rate of crickets typically increases. Research has shown that the chirp rate of crickets is temperature-dependent, often following a general rule where a rise in temperature leads to an increase in chirping frequency. Specifically, for many species, increasing the temperature by about 10 degrees Celsius can result in a significant increase in the number of chirps per minute. Therefore, doubling the temperature would likely lead to a substantial increase in chirp rate.
If you increase the air temperature, the chirp rate of certain insects, such as crickets, will generally increase. Warmer temperatures typically enhance metabolic processes, leading to more frequent chirping. This relationship is often used as a rough indicator of temperature in ecological studies, where a higher chirp rate corresponds to higher temperatures.
In the evening, most bugs are less active than during the day. This is because their food sources, such as nectar, are not available and they have limited energy reserves. Additionally, the air temperature can get too cold for many bugs to survive. Some bugs, such as crickets, will chirp in the evening, but most bugs are not active enough to chirp. The following are the main reasons why most bugs don't chirp in the evening: Food sources are not available. Energy reserves are limited. Air temperature can get too cold.Therefore, although some bugs might still be active in the evening, most of them won't chirp due to the lack of food and energy sources as well as the colder air temperature.
Lapse rate is the rate at which air temperature decreases with existing altitude
That is not a standard quantity. It depends on temperature, surface area and air movement.
dependent - the rate at which the grass grows independent - the temperature of the air
Crickets have been known to accurately indicate the temperature. By counting the number of chirps a cricket makes in 15 seconds and then adding 37 to that number you can gain a good estimate of the temperature in Fahrenheit.
As elevation increases, the temperature typically decreases. This is because air pressure decreases with altitude, causing the air to expand and cool. The rate of temperature decrease with elevation is called the lapse rate.
When air temperature decreases, the rate of evaporation also decreases because cold air holds less moisture than warm air, reducing the ability of water molecules to evaporate from a liquid state into a vapor.
Air is already in evaporated state(gas) . however the rate of evaporation decreases in the sense its volume decreases(less space is occupied by the molecules)
When air is cooled, the rate of evaporation decreases. Cool air has less capacity to hold moisture, which results in a slower evaporation rate. As the temperature decreases, the relative humidity of the air increases and the rate of evaporation slows down.
The increase in temperature with an increase in altitude is referred to as a "temperature inversion." In this scenario, the normal lapse rate is reversed, leading to warmer air above cooler air. This phenomenon can lead to various atmospheric conditions, including smog and air quality issues.
As air temperature decreases, the rate of evaporation also decreases. This is because lower temperatures result in less energy available to convert liquid water into vapor.