Water has a high specific heat capacity, which means it absorbs a lot of energy in order to increase in temperature (thus releases a lot of energy when it decreases in temperature). This means water can absorb a great deal of the energy on hot days, keeping the surrounding air cooler, and release a lot of energy to the air on cool days, keeping the air warmer
A large drop in air temperature around the cylinder would likely cause the flame of the camping stove to diminish or even extinguish. This is because lower temperatures can reduce the efficiency of combustion by causing a decrease in the vaporization of the fuel and its mixing with air. Additionally, cooler air can lead to a decrease in the flame's temperature, affecting its stability and intensity.
A daily change in weather is primarily caused by the movement of air masses, which are large bodies of air with uniform temperature and humidity. These air masses interact with one another and with the Earth's surface, leading to variations in temperature, precipitation, and wind patterns. Additionally, factors such as the Earth's rotation and topography can influence these weather changes. Overall, the dynamic nature of the atmosphere drives daily weather fluctuations.
The name of the effect is called the Coriolis effect. It causes winds to curve rather than moving in a straight line due to the rotation of the Earth.
The daily temperature in the city of Mumbai is 34 degrees. But in summer it rises to 40 degrees.Daily mean temperature is calculated by The average of a series of temperatures taken over a period of time, such as a day or a month. It is the average temperature in each 24 hour period. It is measured in degrees Celsius.
The temperature of sand can affect the local climate by influencing air temperature through heat absorption and reflection. Warmer sand can lead to warmer air above it, while cooler sand can have the opposite effect. Water temperature, especially in large bodies of water like oceans, can affect local climate by moderating temperatures of nearby land areas through oceanic currents and winds. Warmer water can lead to warmer and more humid conditions, while cooler water can have a cooling effect on the surrounding area.
On a warm day, water absorbs from its warmer environment, lowering the air tempurature. On a cool night, heat is transferred from the water to its cooler environment, raising the air tempurature.
It denatures it.
You would expect the daily temperature range to be higher in a continental climate compared to a maritime climate. Continental climates tend to have larger temperature variations between day and night due to the absence of moderating effects from large bodies of water.
Continentality can be defined as large landmass. It results to severe temperature in Europe.
A large drop in air temperature around the cylinder would likely cause the flame of the camping stove to diminish or even extinguish. This is because lower temperatures can reduce the efficiency of combustion by causing a decrease in the vaporization of the fuel and its mixing with air. Additionally, cooler air can lead to a decrease in the flame's temperature, affecting its stability and intensity.
Being windward of a large body of water typically results in milder temperatures due to the moderating influence of the water. This effect, known as maritime influence, can lead to cooler summers and milder winters compared to inland areas. The water helps regulate temperature by absorbing and releasing heat more slowly than land.
Water has a high specific heat, meaning it takes large energy transfers for it to change temperature. Additionally, water from deep down, where surface temperatures have little effect, can mix with surface water, reducing or lessening temperature changes. As a result, the ocean warms less in the summer and cools less in the winter than land does, resulting in fewer extremes of temperature.
Latitude, elevation, proximity to the ocean, and the temperature of any ocean currents effect the temperature of a location. Temperature, in combination with landforms and distance from large bodies of water, effects humidity and precipitation. Temperature, humidity, and precipitation are the main aspects of climate, along with wind direction and seasons, which are effected by latitude and the other above factors.
Latitude, elevation, proximity to the ocean, and the temperature of any ocean currents effect the temperature of a location. Temperature, in combination with landforms and distance from large bodies of water, effects humidity and precipitation. Temperature, humidity, and precipitation are the main aspects of climate, along with wind direction and seasons, which are effected by latitude and the other above factors.
Europe is a large continent and on any given day there is a wide range of temperatures, from very cold to very hot, so it is impossible to give a single answer.
Yes, due to the of the lack of humidity and cloud cover the difference between day and night temperatures in the desert can be quite extreme.
Water generally moderates the temperature and keeps it more constant, so it'll rarely get very hot or very cold at the seaside, relative to the average temperature.