Because if there are no plants the animals move , adapt, or die and if there are a lot of plants there tends to be a large ecosystem
Because it does not directly affect the landform thus why it's considered as a passive agent. Those that do directly affect landforms are tectonic activities, winds, and water flow. Weather only onsets the formations.
Answer:
Consequently, during neutral conditions, rainfall is greatest in the western tropical Pacific where SST are: highest.
Explanation:
SST is the abbreviation for Sea Surface Temperature. This temperature is measured using satellite data and is essential to understand the occurrence of precipitation in the tropical pacific, as shown in the question above. This is because the higher the surface temperature of the sea, that is, the higher the SST, the higher the rate of evaporation of sea water. According to the water cycle, when sea water evaporates, it is released into the atmosphere as water vapor. This vapor is captured by the clouds, which condense it, transforming it into water again. When the clouds become very heavy with this condensed water, precipitation will occur, which is the release of clouds from water that was previously evaporated from the sea, due to the high temperature of the sea surface. Therefore, we can conclude that when precipitation in the Western Tropical Pacific is higher, it means that SST is higher.
Thunderstorms are the rain bearing cloud produces lightning. It is a violent weather disturbance associated with heavy rain or hail, lightning ,strong winds, thunder etc. Every thunderstorm produces lightning. The basic factors affects the thunderstorms are moisture, unstable air, and lift.
<h3>What are thunderstorms?</h3>
Thunderstorms are ferocious, brief meteorological disturbances that are nearly always accompanied by lightning, thunder, thick clouds, significant amounts of rain or hail, and powerful gusts of wind. Layers of warm, moist air rise in a strong updraft to colder areas of the atmosphere, whereupon thunderstorms form. At that location, the updraft's moisture condenses to create imposing cumulonimbus clouds and, eventually, precipitation. Cooled air columns then descend to the ground and are met by powerful downdrafts and horizontal winds. In parallel, electrical charges build up on cloud particles (water droplets and ice).
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