I have a region on a planet with identical parameters to Earth but different landmasses that is rather similar to the southern ocean on Earth.

There is a single piece of land around the size of the Pacific Northwest that sticks down into the 50 S latitudes. To the west of it but beneath the 60 S parallel, there is a continent twice the size of Greenland generally extending south and fully glaciated. There is no other land south of the 45th parallel.

I'd like this ocean to generate cyclonic storms stronger than the ones in our own Southern Ocean. Will it already do that or are there any other changes to the distribution of land and water and other things that aren't like orbital distance and mass that I can do to increase the strength of low pressure systems forming in this ocean that will impact the land?

this is a map of Southern Winter temperatures with isotherms for reference

This is a map of southern winter average temperatures for reference.

Given the parameters that you've given, it is very likely that the storms generated in the southern hemisphere would be quite stronger than what exists in our world, and also likely that the South Pole, in the absence of any landmass, might end up being covered by a permanent storm system.

I draw a parallel with the recent discovery on Jupiter's pole, showing a massive storm orbited by smaller storms. While Jupiter isn't Earth-like, the physical laws governing the movement of a fluid, like an atmosphere, are the same no matter what your atmosphere is made of.

Thus, I believe that in your setting, the South Pole would be covered by a giant permanent storm system, fueled and maintained by sea currents, jet streams and the rotation of the planet, that would generate side storm that would wreak havoc on your Greenland and the south shores of the other landmass.

Given how 'thin', so to speak, the two landmasses you described are, this leaves a lot of open seas for storm systems to develop and acquire energy before they make landfall.

  • What you mention about Jupiter's storms is very true, I'm just worried that because cyclones rely on temperature/pressure gradients to strengthen, and if you look at the area near my southern ocean and land, the isotherms aren't all that compact, so I don't know which factor will win out in terms of strength. – Antarctica07 Sep 14 at 13:53
  • I guess that your isotherms are for air temperature, not ocean temperature? You could easily add some temperature to fuel the storms by having a warm oceanic current find it's way to the southern regions. It would carry warm water that would evaporate in contact with the cold air and all this warm moisture would fuel the permanent storm in the South Pole and it's children storms all around. – Sava Sep 14 at 22:58
  • Like the Gulf Stream in NE and Europe? My other concern then would be that the layout of continents would cause a cold current by the SW of my southern continent, inhibiting cyclonogensis. Another problem is storm tracks; if they are funneled to the SE by the Easterlies, then it may be hard for the cyclones that form to hit that coastline. The cyclones that do form would seem to be concentrated below the 60th parallel and with a lower intensity than ours due to the lack of a global polar ice sheet, but that is just my conjecture. – Antarctica07 Sep 15 at 2:13
  • If tehre's a cold current along your southern continent, it would probably be going away from the pole, along the SW coast, thus keeping the continent fully glaciated as it bring cold water and cools the air along the coast. My own conjecture would be that the absence of polar ice sheet would increase the intensity of the storms, and, with a jet stream basically circling the south pole as in our world, the secondary storms would probably be able to strike everything around randomly, with nothing to really guide them towards a particular place. – Sava Sep 15 at 20:33

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