The presence of enormous floating glacial ice plates that are connected to the ice sheet and nourished by snow accumulation is a significant glacial feature of Antarctica. They are known as ice shelves.
An ice shelf is a sizable ice platform that develops as an ice sheet or glacier flows down to a coastline and onto the water's surface. Antarctica, Greenland, Northern Canada, and the Russian Arctic are the only places where ice shelves exist. The grounding line is the line separating the floating ice shelf from the anchor ice that feeds it and is resting on bedrock. Ice shelves can have a thickness of 100 to 1,000 meters. Around the Antarctic continent, it can also be found in the Southern Ocean.
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under neutral enso conditions, where over the equatorial pacific ocean would you expect to find relatively higher atmospheric pressure (subsidence)?
Under neutral ENSO conditions, in the eastern equatorial Pacific Ocean, off the coast of South America, we expect to find relatively higher atmospheric pressure (subsidence).
An El Niño circumstance takes place whilst floor water inside the equatorial Pacific becomes hotter than average and east winds blow weaker than every day. The other situation is referred to as La Niña. In the course of this section of ENSO, the water is cooler than normal and the east winds are more potent. El Niños generally arise every 3 to five years.
In the impartial kingdom (neither El Niño nor la Niña) trade winds blow east to west across the floor of the tropical Pacific Ocean, bringing heat moist air, and hotter floor waters towards the western Pacific and preserving the important Pacific Ocean noticeably cool.
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