Like any object moving through a fluid, a high-speed train distorts the air as it moves through it.
Broadly speaking, there are three main regions of flow structure around a high-speed train: the upstream distortion, boundary layer and wake. These can be collectively referred to as the slipstream. The effects of the slipstream on a static observer (e.g. a person on a platform) vary depending what part of the train is passing:
1. Head/Nose Passage
From the observer's perspective, air accelerates immediately before the nose passes, followed by a sudden deceleration (i.e. a pressure pulse, or gust).
2. Body Passage
After the initial gust, slipstream velocity begins to increase again as a boundary layer grows on the side wall of the train/carriages. This is going to be a relatively steady build-up but carriages, undercarriage etc. will impact this.
3. Tail Passage
Immediately after the tail passes the wake is already being generated. There is another big velocity spike here as the wake meets the observer. In addition, the exact structure of the wake depends on (train) geometry, but it may have:
- a separation bubble / recirculation region where the flow detaches from the train body.
- shedding vortices
Generally a wake is going to be lower-than-ambient pressure, but in the case of vortices, they can actually result in air being accelerated down behind the tail, creating a low pressure region and sucking air in.
"back draft"
It's not a very descriptive term IMHO but anyway:
- it's possible a push-pull type of effect may occur in the situation where the is indeed a low pressure region behind the train actually sucking air in (the gust hits, then the suction).
- additionally, the closer you get to the train body the higher the slipstream velocity. Although this will produce a force in the direction of motion, if the slipstream sweeps an object up it may effectively get sucked in and behind
It's very much not about volume of air displaced, but rather how it's displaced.
Reference