Gene: im not sure i follow your first point, i think the dryline does require the trough. If the discontinuity is "gradual", then it's not really a dryline, no?
Searching for the official dryline definition leads to many answers and just as many opinions. Like this one for recognizing a dryline on a synoptic map.
Dryline definition: dew point contrasts of 15 degrees or more in 100 miles and a recognizable non-frontal surface wind confluence zone. This is closer to what I was characterizing in my first definition. The link follows......
http://www.mmm.ucar.edu/pdas/Relocation/dryline.html
Given that opinion, look at this source which summaries numerous different definitions and links to supporting articles.
http://en.mimi.hu/meteorology/dry_line.html
One paper I found with Google Search studying the cross sectional area of drylines states that the discontinuity can very greatly along the boundary. In this particular instance a convergent low pressure trof separates the two air masses. In some of the definitions the word "sharp" is used to further define the boundary, others not. Looking up sources from the OU school of meteorology they stress a
strong moist-dry difference across the boundary. This is a definition of a good dryline for severe weather, but not necessarily all drylines. In the early summer months over the high plains we get mix out drylines that are much less a part of a large synoptic scale. They certainly don't fit the strict definition I see for OU students, but given conditional instability, subtle convergence and strong afternoon heating a (surprise) severe storm will form.
We chasers tend to look at meteorological features in terms of severe weather. In that context
sharp drylines in a well defined trof are best suited to what we study and chase. That said, in the wider meteorological view of changing air masses the term must be less restrictive. If for instance Dodge City has a 57Td at 2 PM with a south wind and two hours later they report a 35 Td with a west wind then they most likely had a dryline passage, albeit gradual over a longer time period. The same thing can be said for frontal systems where the change to a totally different air mass may come gradually.
The original dryline paper, at least the oldest one I remember studied the so called "Marifa Dryline" and it keyed more on the mix out process forming and moving the dryline. Today we look for more dynamic features such as large scale subsidence on the models. It can be argued how a dryline actually moves, by mix out, or by strong westerlies mixing down associated with an upper level system, all linked to the larger synoptic scale. I think where we differ is that I'm not looking at dryline in the strictest terms for synoptic scale severe weather, but more with regard to changing and moving air masses. This view also allows us to more accurately predict when things don't go right. Like veering winds and decreasing dewpoints in advance of the dryline-trof.
This subject get damm deep
Gene Moore