Heat's effect on the wind cycle is most easily observed near the sea. During the day, the ocean absorbs heat from the surface, keeping the air above it cooler than above the land. When the warm air rises from the shore, the cooler air from the ocean blows in to take its place. At night, the land cools quickly, while the ocean radiates the heat it absorbed, keeping the air above warm. This reverses the effect, causing the air offshore to rise and creating a breeze from the land. Uneven heating can also occur due geographical features. A mountainside exposed to the sun will warm more than a shadowed valley below it, creating a wind that blows uphill during the day and downhill at night.
The same principle is responsible for global wind patterns. The polar regions receive less solar radiation than areas near the equator, resulting in a global shift in temperature according to latitude. This, along with differences in temperature and density in various layers of the atmosphere, creates global wind patterns like the jet stream that help drive weather systems.
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Answer:
Caulobacter crescentus is a specie of gram negative aquatic bacteria. There is gene called as Ccrm gene in them that is responsible for the the synthesis of Ccrm enzyme that is crucial for the proper cell division of cells. When, there is a mutation in this gene, the bacteria won't be able to synthesize Ccrm enzyme anymore. This causes accumulation of two conserved FtsZ and MipZ proteins in cells and result in severe defects and irregulations during cell division.
Answer: apical dominace
Explanation:
is when the main stem grows more strongly than branches. It is an occurrence where the the central stem is dominant as compared to the other stems. It is a common phenomenon in a plant's stems and aerial parts. It happens when the the apex prevents the lateral buds' growth so plant grows vertically in such case.
Answer:
first option for the first question and second option for the second question.
Explanation: