Climate change!!!!!!!!!!!!
Answer:
The social impacts that South Indian high pressure cell have on climate of south Africa during summer is that the anticyclonic circulation brings about dry climate.
How is climate of south Africa affected by Indian high pressure cell?
South Atlantic High usually bring about warm weather which comes from the direction of east coast of South America and moves to Africa in summer .
Therefore, the impacts that South Indian high pressure cell brings is dry climate.
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Answer:
Orange Groves are affected by the climate of the region. In the US, states such as Florida and Georgia are the biggest orange producers because of their climate. Also, oranges need good soil to grow, so dry soils are not suitable for growing oranges.
Nurseries are more "human controlled" than orange groves. A big human factor that plays a role in growing the food properly is temperature. If the temperature is too hot or cold, the plants may not grow properly and might even die. Also, many nurseries can control the humidity inside the nursery. Some plants require specific humidities to grow- and are vulnerable to a change in humidity.
Coffee plants require moist soil to be grown well. Thus, if the soil is too dry, the coffee plant may die. In other words, a coffee plant would grow much better in a farm, than a desert. Also, Coffee Plants require a high temperature, and that is why most of the world's coffee is grown in places like Africa and South America as they have hotter temperatures.
<h2>Answer:</h2>
By digging tube wells
<h2>Explanation:</h2>
Water can be obtained from the land by digging a hole in the earth surface. The process is called boring. A tube well is a type of water well in which a long, 100–200 millimeters-wide, stainless steel tube or pipe is bored into an underground aquifer. In this way people who supply their own water to other areas or people generally obtain it by using tube wells where they attach a motor to it for speedy suction and then transfer the water to destination by using pipes.
The heat that remains inside the Earth from its creation and radioactive decay are its main heat sources.
The deep earth receives heat from three main sources: (1) heat left over from the planet's formation and accretion, (2) frictional heating brought on by denser core material sinking to the planet's centre, and (3) heat from radioactive element decay.
The energy produced when unstable atoms decay is known as radioactivity, and it is a substantial contributor to the Earth's heat. The main source are the radioactive isotopes of uranium-235 (235U), uranium-238 (238U), potassium-40 (40K), and thorium-232 (232Th) in the Earth's mantle.
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