Answer:
Panthalassic Ocean
Explanation:
During the time at which the last super-continent Pangaea existed, there was an enormous ocean as well. This ocean was stretching from one side of Pangaea to the other side of it, circling the rest of the planet that was not covered with land. The name that was given to this ocean is the Panthalassic Ocean. It has to be mentioned though that it was not the only ocean during this time though, as there were two other much smaller oceans, the Paleo Tethys Ocean and the Tethys Ocean, both being located between the land masses that later gave birth to Eurasia and Australia. Because of the size of the Panthalassic Ocean it was capable of producing much stronger storms and waves that the human kind had ever witnessed, and it is certain that those storms and waves were doing enormous damage along the coastline of Pangaea.
Answer:
i think a but im not sure about it
Air masses that form over <u>water</u> carry much more moisture due to evaporation.
<h3>Which air mass has the most moisture?</h3>
- Maritime air masses, also known as ocean air masses, are more humid than continental air masses, which are air masses that originate over land.
- The air mass's temperature, which varies depending on the latitude at where it formed, is indicated by the second component of the name.
<h3>Why do you suppose the air masses that develop over water are moist?</h3>
- High air pressure is present in polar or cold air masses.
- Unsurprisingly, whether an air mass arises over land or water affects its humidity.
- Due to water evaporation across oceans, maritime air masses frequently have a humid climate.
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Answer:
Insufficient dissolved oxygen in the water can cause: death of adults and young reduced growth failed eggs and larvae changes that occur in the species in various water bodies.
<u>Answer:</u>
<u>An atmospheric cycle </u>is not a major biogeochemical cycle.
<u>Explanation:</u>
The flow of air from the high-pressure area to the low-pressure area is called the atmosphere cycle. Low-pressure areas are created by the upliftment of the heated air. Higher and colder atmosphere will fall eventually by creating a high-pressure area.
Monsoon patterns are the result of these atmosphere cycles. The weather in high-pressure areas is stable with clear skies compared to low-pressure areas where weather is highly unstable with clouds (formed from vapour due to the higher temperature).
