No, this isn't "ground wave" when using a low dipole.
The answer has to do with how radio waves are reflected (or refracted) by the ionosphere.
At any moment there is a factor called the "critical frequency": below that frequency
signals will reflect straight back down to Earth, allow Near Vertical Incident Skywave ("NVIS")
propagation within a few hundred miles. Above that frequency the ionosphere doesn't
reflect the waves straight back down, so you can't cover shorter distances, but it may reflect
them at an angle allowing coverage of longer distances.
The "common wisdom" is to use 40m during the day and 80m at night, but here at 45 degrees
North we are using 80m during the day and 160m at night, even during the summer, because
those are the only bands that support local contacts well in the current ionospheric conditions.
For example, here is a current map of the Critical Frequency from
this website.You can see it varies with latitude, season, time of day, etc.

At the moment, the Critical Frequency is between 5 and 6 MHz for most of the continental US,
so 80m (or perhaps 60m) would be the most likely band for local contacts. But looking at the
red area of the chart (and visualizing it rotation around the world) there are even going to be
times at the higher latitudes when 160m may not be open.
One of my other favorite charts from that site is the
Local Area Mobile Prediction (LAMP), which
shows the best bands to use for distances out to about 600 miles from your location for each
hour of of the day. It looks like this:

Under current conditions, for distances less than 200 miles from my location, I need to
use 80m during the day and 160m at night, except that even 160m might not make the
path between 0300Z and 0600Z.
There are some conditions where the higher HF bands might get though, depending on
the size of your ARES districts, but those aren't as likely when using low dipoles that
are relying on a high angle of radiation.