when the sun heat the ocean,sea,and the water vapour rises and condenses with cool air and form cumulus clouds then the rain fall down.
Relief rainfall occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools and condenses to form clouds and eventually rain. The diagram would show warm, moist air approaching the mountain, rising, cooling, condensing, and then raining on the windward side of the mountain. The leeward side of the mountain would be in a rain shadow, receiving significantly less rainfall.
Convective rainfall occurs when warm, moist air rises rapidly, cools, and condenses to form clouds and eventually rain. This type of rainfall is common in tropical regions where daily heating of the ground leads to the formation of thunderstorms and heavy downpours. Convective rainfall tends to be intense and localized.
First the sun warms the ocean water causing it to turn into a gas which is known as evaporation. Clouds are formed from the gas (condensation). Then the cloud takes in lots of the gas until it cant hold anymore then it rains or if its cold hails or snows(participation) .
Laterite soils are formed in tropical and subtropical regions with high rainfall. The prolonged leaching process due to heavy rainfall removes soluble nutrients, leaving behind iron and aluminum oxides. The warm and humid climate accelerates the weathering of parent rock material, contributing to the formation of laterite soil.
temperate cyclones causes rainfall. westerlies are strong winds..............
rainfall
rainfall
Diagram of Sperm Formation :)))
their formation
Cloud formation is primarily influenced by temperature and air pressure. As warm air rises and cools, it reaches its dew point, causing condensation to form clouds. Rainfall can also be a result of this condensation process within clouds.
comes from rainfall.
Relief rainfall occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools and condenses to form clouds and eventually rain. The diagram would show warm, moist air approaching the mountain, rising, cooling, condensing, and then raining on the windward side of the mountain. The leeward side of the mountain would be in a rain shadow, receiving significantly less rainfall.
they can't act as air barriers because they have large air space between them
Yes, humans can contribute to rainfall formation through activities that influence local and regional climates, such as land use changes, urbanization, and greenhouse gas emissions. Urban areas can create "heat islands" that enhance convection and lead to increased precipitation. Additionally, large-scale deforestation and agriculture can alter local weather patterns, potentially affecting rainfall distribution. However, the overall impact of human activities on global rainfall patterns is complex and multifaceted.
Convective rainfall occurs when warm, moist air rises rapidly, cools, and condenses to form clouds and eventually rain. This type of rainfall is common in tropical regions where daily heating of the ground leads to the formation of thunderstorms and heavy downpours. Convective rainfall tends to be intense and localized.
First the sun warms the ocean water causing it to turn into a gas which is known as evaporation. Clouds are formed from the gas (condensation). Then the cloud takes in lots of the gas until it cant hold anymore then it rains or if its cold hails or snows(participation) .
1) The nonequilibrium martensite does not appear on the diagram; and 2) The diagram provides no indication as to the time-temperature relationships for the formation of pearlite, bainite, and spheroidite, all of which are composed of the equilibrium ferrite and cementite phases.