The Earth's atmosphere varies in temperature with altitude. Generally, air at ground level is warmer. As altitude increases, the air temperature falls. When the Sun is shining it warms the ground. The warm ground warms the air immediately above it. This produces a bubble of warm air that begins to rise. Warm air rises because warm air is less dense than cold air. In theory, a bubble of air at ground level will cool as it rises and expands.
When the atmosphere is at low pressure, the rising air bubble is always warmer than the surrounding air. Under conditions of low pressure, the heated air will continue to rise. As it rises it cools; but it does not cool as quickly as the surrounding air. As it is always warmer than the surrounding air, it continues rising.
Low pressure leads to unstable air conditions. When the ground is heated, the air will rise and keep rising. Eventually, the rising air will cool enough to produce condensation (cloud and rain).
When the atmosphere is at high pressure, the rising air bubble is always cooler than the surrounding air. Under conditions of high pressure, the heated air will not continue to rise. As it rises it cools; it cools more quickly than the surrounding air. Being cooler than the surrounding air, it will not rise.
High pressure leads to stable air conditions. When the ground is heated, the air will not rise. If air does not rise, rain cannot condense.
Stratocumulus clouds are most commonly seen in the spring and summer seasons. They are low-lying clouds that often form in stable atmospheric conditions when there is enough moisture present for cloud formation.
Because it evaporate the water in summer season
The average relative humidity during hurricane season can vary depending on the region, but typically ranges from around 75% to 85%. This high humidity can contribute to the formation and intensification of hurricanes by providing the necessary moisture for storm development.
Cold weather front have low pressure air and rain/snow/hail/tornadoes and even hurricanes depending on location. Cold fronts bring huge, towering, billowing clouds [Cumulonimbus] that bring thunderstorms. Warm weather fronts bring gentle precipitation and high pressure air. Warm weather fronts also bring sheetlike clouds [Stratus] and wispy clouds [Cirrus] On the other hand, when there is no front, puffy white clouds [Cumulus] come on fair sunny days.
In the summer, the air near the Earth's surface becomes warmer and expands, causing it to rise. As warm air rises, it creates lower pressure at the surface, leading to a decrease in atmospheric pressure. This change in pressure is also influenced by the movement and distribution of air masses in the atmosphere during the summer season.
Clouds are actually the water that is evaporated from our water sources in hot season,these are the cause of rain
Stratocumulus clouds are most commonly seen in the spring and summer seasons. They are low-lying clouds that often form in stable atmospheric conditions when there is enough moisture present for cloud formation.
Cumulonimbus clouds cann occur at any time of year, but are most common in the summer.
Because it evaporate the water in summer season
The only difference between dark clouds and light clouds are they're thickness. A dark cloud is thikcer than a light cloud so it doesn't let as much light through. SO to answer your question, clouds are black in the rainy season because they are "holding" more water than they hold during the dry season
Theres clouds in every season
when it is summer season the water evaporates ant clouds become heavy
The burst of monsoon is typically associated with two key weather conditions: a sudden increase in humidity and a drop in atmospheric pressure. As warm, moist air rises, it leads to the formation of cumulonimbus clouds, resulting in heavy rainfall. This transition often marks the onset of the monsoon season in tropical regions, bringing significant changes in weather patterns.
winter
Winter
The average relative humidity during hurricane season can vary depending on the region, but typically ranges from around 75% to 85%. This high humidity can contribute to the formation and intensification of hurricanes by providing the necessary moisture for storm development.
Cold weather front have low pressure air and rain/snow/hail/tornadoes and even hurricanes depending on location. Cold fronts bring huge, towering, billowing clouds [Cumulonimbus] that bring thunderstorms. Warm weather fronts bring gentle precipitation and high pressure air. Warm weather fronts also bring sheetlike clouds [Stratus] and wispy clouds [Cirrus] On the other hand, when there is no front, puffy white clouds [Cumulus] come on fair sunny days.