Answer:
B) Above average rainfall
Explanation:
The Southern Oscillation, also known as El Nino, brings in significant changes of the weather on all areas that are affected by it. Texas is also affected by El Nino, and that is manifested in milder temperatures and increased precipitation.
La Nina and El Nino have the total opposite effect on the weather conditions of Texas. While La Nina brings in warmer and drier weather conditions, El Nino actually brings in milder weather and much more rainfall.
Texas in general is semi arid. The temperatures are mild in winter and high in summer, with the rainfall mostly being absent for most of the year, and the majority of it falling intensively and seasonally. When El Nino is active though, Texas receives much more rainfall, making its temperatures lower in the process as well.
This is actually welcomed by the Texans, as the increased rainfall is good for the agriculture. The people are happy as well that they have lower temperatures for some time, so they are experiencing extremely high and unbearable temperatures.
Answer:
groundwater is water that occupies the zone of saturation within the ground. the water table is the upper limit of the groundwater.
Answer:
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Answer:
c. A dam can significantly reduce or shut off the supply of sediment to a delta.
Explanation:
- The rivers that drain into the ocean have deltas and they form the mouth of the river and the soil rich land is a called as the delta. The dam can significantly stop or shut the supply of the sediments to the deltas.
The convection currents are the ones that create the force that breaks up and moves the crustal plates on the surface of the planet. By moving the crustal plates, the convection currents contribute to the formation of different types of plate boundaries, including the divergent plate boundaries.
The divergent plate boundaries are the boundaries where two plates are moving away from one another because the convection currents are dictating that kind of movement from bellow them. As they move away from each other, they leave a gap between them, and the convection currents push up a lot of magma towards the surface. The magma cools of very quickly in the water, thus forming rocks constantly, rocks that little by little start to make a big mas, that eventually turns into an underwater mountain, or rather a mid-ocean ridge.
