Answer: When the amount of sediments that are added to a coast and the amount of sediments removed from the coast are in equilibrium, then this equilibrium state is known as the sediment budget.
These sediments in the coastal areas are added by the ocean currents frequently striking at the base of a cliff, and also by the longshore current,and rivers that deposits the materials at the shore.
whereas, the materials are removed from the beach by the erosional processes, in which the longshore currents trnsports the sediments from the beach to the offshore.
The factor that would have the net effect of making a place warmer during summer would be that it is in the middle of a landmass.
The reason why a warmer summer would be present at the middle of a landmass is because landmass:
1. Has a lower specific heat capacity, and therefore can be heated up quickly, through receiving insolation from the sun.
2. Land is opaque, therefore insolation only concentrate in shallow areas, making the surface temperature increase.
3. There is no mixing of warm and cold layers, along with the lack of presence of evaporation, there would be less cooling
In sum, the above effects can be called continental climate, and thus the middle of a land mass is cooler.
For your reference, here's why the other options are not correct:
At a high elevation near an ocean - near the ocean would mean it has a maritime effect and therefore a cooler summer.
At a high latitude - with the less dense air, heat will be absorbed faster resulting in faster heat loss hence a cooler summer.
Hope it helps!
The force caused bu the wind pushing on a building is called pressure
Mount Aso, Sakurajima.
Yellowstone- last caldera forming eruption was 640,000 yrs ago
<span>Raton- hotspot located in northeastern new Mexico. no recorded activity in modern times. </span>
Answer:
Arithmetic Density
Explanation:
it is the total number of people divided by the total land area and this is just talking about population density not the amount of arable land (physiological density) or comparing the number of farmers to the area of arable land (agricultural density)
