In most cases, the water temperature only affects land temperatures when the land is in relatively close proximity to the water. The winds will flow accross the warmer water and carry the radiated heat over the land closest to the shoreline. As the wind blows further inland, the affects of the water are slowly dropped off. In contrast, the air temperatures can SLOWLY affect the water temperatures. Over time, cooler/warmer air temps will cool/warm the waters if the temps are fairily consistent for a period of time. The larger the body of water, the longer it takes for the air to affect it.
Plants take in sunlight and Carbon Dioxide, and as a by product, produce water and oxygen. when it is humid the air is wet and damp like bathing with hot water. so the plant takes in the water to make photosynthesis.
The relationship between water temperature and air temperature is that they can influence each other. Water temperature changes more slowly than air temperature because water has a higher specific heat capacity. This means that bodies of water can help moderate nearby air temperatures, and vice versa. Warmer water can lead to warmer air temperatures, while cooler water can lead to cooler air temperatures.
No, hydrogen is just water in extreme temperatures.
Less.
Water temperature can affect air temperature near the water by influencing the rate of heat exchange between the water and the air. Warmer water can lead to warmer air temperatures, while cooler water can result in cooler air temperatures. This is because water has a higher specific heat capacity than air, meaning it can absorb and retain more heat energy. As a result, warmer water can transfer heat to the surrounding air, raising the air temperature, and vice versa.
Warmer temperatures hold more water.
Cool temperatures cause condensation of water vapor, turning it into liquid water. This process occurs when the air temperature reaches the dew point, causing the water vapor in the air to change state from a gas to a liquid.
Warmer air is able to hold more water vapour than cooler air. As warm humid air cools, the water vapour condenses out as water droplets.
Higher temperatures increase the amount of water vapor that air can hold. When the temperature decreases, the air becomes saturated and condensation occurs, leading to the formation of water droplets or clouds. Warmer temperatures can also accelerate the evaporation of water into vapor.
Water in the air doesn't heat the air up. Water in the air moderates temperatures. It tends to make daytime temperatures cooler and nighttime temperatures warmer than they would be in drier air.
At higher temperatures, air can hold more water vapor because warm air molecules have more energy and can accommodate more water molecules. This means that warmer air has a higher capacity for holding water vapor compared to cooler air, which can lead to increased humidity levels.
Stellar temperature can be measured by analysing the spectrum of light that stars emit; shorter wavelengths correspond to higher temperatures.