Tim Vasquez
EF5
- Joined
- Dec 4, 2003
- Messages
- 3,411
I suppose one thing every enterprising forecaster should see at least once is a sounding from the South Pole. Here is the sounding from last night.
Some tidbits for beginners:
* The elevation of the station is 9300 ft MSL. That's why the sounding doesn't extend to the bottom of the diagram. It's amazing to think how much snow it took to create those two miles of ice.
* Note the radiational inversion from 670 to 640 mb. That's a depth of about 900 ft. It's a layer of cold air close to the ground where radiational cooling is strongest.
* The surface temperature (-54C or -65F) has the potential to be much colder, but the surface winds, when they blow, tend to mix up the air with warmer air just above the surface. However the layer of air near the surface (the boundary layer) still remains strongly decoupled from the free atmosphere.
* The tropopause is not very sharp here but is being reported as 240 mb, or 22,000 ft. That's only 13,000 ft above the ground.
* How does it compare with model data? (see next image) The 500 mb GFS analysis suggests winds blowing from the north-northwest. This agrees fairly well with the sounding. Note that at the poles, directions are always referenced to the prime meridian.
* The low-level winds at the South Pole blow from the north or northeast whenever cold air from the vast interior is draining into the Ross Ice Shelf area (one of the two large "gulfs" in Antarctica) near McMurdo Bay. This is the most common kind of pattern and is what is occurring here.
Tim
Some tidbits for beginners:
* The elevation of the station is 9300 ft MSL. That's why the sounding doesn't extend to the bottom of the diagram. It's amazing to think how much snow it took to create those two miles of ice.
* Note the radiational inversion from 670 to 640 mb. That's a depth of about 900 ft. It's a layer of cold air close to the ground where radiational cooling is strongest.
* The surface temperature (-54C or -65F) has the potential to be much colder, but the surface winds, when they blow, tend to mix up the air with warmer air just above the surface. However the layer of air near the surface (the boundary layer) still remains strongly decoupled from the free atmosphere.
* The tropopause is not very sharp here but is being reported as 240 mb, or 22,000 ft. That's only 13,000 ft above the ground.
* How does it compare with model data? (see next image) The 500 mb GFS analysis suggests winds blowing from the north-northwest. This agrees fairly well with the sounding. Note that at the poles, directions are always referenced to the prime meridian.
* The low-level winds at the South Pole blow from the north or northeast whenever cold air from the vast interior is draining into the Ross Ice Shelf area (one of the two large "gulfs" in Antarctica) near McMurdo Bay. This is the most common kind of pattern and is what is occurring here.
Tim

