The number 1 on the map identifies the Atlas Mountains. It is the mountainous region just south of the Mediterranean in Northwest Africa.
The Atlas mountains pass through the northern cost of West Africa, including Tunisia, Algeria, and Morocco. This impressive mountain range provided both advantages and challenges to civilizations in the region, and is host to a number of unique species.
Other Branches of Earth Science[edit]Geology<span>, </span>oceanography<span>, and </span>meteorology represent a large part of Earth science, while astronomy<span> represents science beyond Earth.</span>
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The earths surface is heated by the Sun's rays which are directed at the equator 0° latitude. If there were sea currents the closer you got to the equator the hotter it will get and the further away you go from the equator the colder it will get. Thus ocean currents distribute the heat at the equator around the earths oceans to even out the difference in the heat zones, so that the equator is not a desert and the rest of the earth is an ice age.
Evapotranspiration (ET): The combination of two separate tactics wherein water is misplaced. the only hand from the soil surface by evaporation and however from the crop via. transpiration is known as evapotranspiration.
Evapotranspiration is the system of evaporating water from leaves through plant transpiration at some stage in photosynthesis. It varies due to a multitude of things like wind, temperature, humidity, and water availability.
Evapotranspiration (ET) is the loss of water to the ecosystem thru evaporation and transpiration through plant life. due to the fact it's miles a widespread issue of the water finances in many ecosystems, estimating or measuring evapotranspiration is regularly important in making sure powerful water and groundwater control.
In a warming climate, improved evapotranspiration can also shift the fraction of precipitation that runs off as floor water or infiltrates the subsurface as recharge. long-term shifts in recharge patterns can alternate groundwater levels and finally groundwater floor water interactions and soil moisture.
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