One of the characteristics of being a good student is to ask questions and then dig in a bit, instead of depending on a TV show for answers.
The answer about wake vortex associated with HSR is as expected not simple. It depends on the ambient conditions and wind flows in the ambient relative to the train. Without further comments take a look at:
An example of what happens under cross wind conditions:
http://iawe.org/Proceedings/CWE2006/TB3-02.pdf
And how under certain conditions there can be negative pressure generated in the wake:
http://www.ara.com/Projects/SVO/Papers_white/train_aero.pdf
A personal anecdote which has some relevance to this discussion.....
In my graduate school days at Stony Brook I had the incredible fortune of attending a lecture given by the great Nobel Laureate Physicist Richard Feynman. Had the incredible humbling experience of talking to the great man whose Masters Thesis was what turned out to be the beginning of an entire area of Physics called Quantum Electrodynamics! Allegedly he also entertained himself while involved with Project Manhattan at Los Alamos by picking locks of cabinets holding highly confidential documents and leaving pithy notes like "Guess Who?" in them, sending the security folks into a tizzy.
In the conversation he pointed out that there is no question that is inherently stupid. The issue is whether one wants to dig in and see the nuances associated with the question or not, i.e. are we good students or have we come to the position of Mr. Know It All already
![Wink ;) ;)](data:image/gif;base64,R0lGODlhAQABAIAAAAAAAP///yH5BAEAAAAALAAAAAABAAEAAAIBRAA7)
You know that you have become a true good student when you are at peace with the realization that the more you know, the more you know what you are yet to learn and know. That is the nature of the beast and what makes life fascinating.
Anyway, there are several other papers on this subject of wake vortices that I have access to through my professional memberships, but they cost mucho dinero, so I won't giver references to here.